CN110685600B - A Bit Adjustment Prediction Method for Geosteering - Google Patents
A Bit Adjustment Prediction Method for Geosteering Download PDFInfo
- Publication number
- CN110685600B CN110685600B CN201810635374.9A CN201810635374A CN110685600B CN 110685600 B CN110685600 B CN 110685600B CN 201810635374 A CN201810635374 A CN 201810635374A CN 110685600 B CN110685600 B CN 110685600B
- Authority
- CN
- China
- Prior art keywords
- formation
- stratum
- distance
- drilling
- drill bit
- Prior art date
- Legal status (The legal status is an assumption and is not a legal conclusion. Google has not performed a legal analysis and makes no representation as to the accuracy of the status listed.)
- Active
Links
- 238000000034 method Methods 0.000 title claims abstract description 85
- 230000015572 biosynthetic process Effects 0.000 claims abstract description 277
- 238000005553 drilling Methods 0.000 claims abstract description 114
- 230000004044 response Effects 0.000 claims abstract description 48
- 238000012937 correction Methods 0.000 claims abstract description 30
- 230000010287 polarization Effects 0.000 claims abstract description 21
- 238000005259 measurement Methods 0.000 claims description 52
- 238000003384 imaging method Methods 0.000 claims description 51
- 230000008859 change Effects 0.000 claims description 21
- 238000001514 detection method Methods 0.000 claims description 20
- 238000004364 calculation method Methods 0.000 claims description 16
- 238000004088 simulation Methods 0.000 claims description 15
- 238000012545 processing Methods 0.000 claims description 12
- 238000004422 calculation algorithm Methods 0.000 claims description 9
- 238000011478 gradient descent method Methods 0.000 claims description 8
- 238000007781 pre-processing Methods 0.000 claims description 6
- 230000000149 penetrating effect Effects 0.000 claims 1
- 238000005755 formation reaction Methods 0.000 description 244
- 239000010410 layer Substances 0.000 description 69
- 230000014509 gene expression Effects 0.000 description 21
- 230000008569 process Effects 0.000 description 19
- 238000010586 diagram Methods 0.000 description 12
- 238000005516 engineering process Methods 0.000 description 10
- 238000005070 sampling Methods 0.000 description 7
- 238000010276 construction Methods 0.000 description 6
- 230000005684 electric field Effects 0.000 description 5
- 230000009545 invasion Effects 0.000 description 5
- 238000011161 development Methods 0.000 description 4
- 239000011159 matrix material Substances 0.000 description 4
- 230000035699 permeability Effects 0.000 description 4
- 238000004458 analytical method Methods 0.000 description 3
- 238000011157 data evaluation Methods 0.000 description 2
- 238000013461 design Methods 0.000 description 2
- 238000007598 dipping method Methods 0.000 description 2
- 230000000694 effects Effects 0.000 description 2
- 230000008030 elimination Effects 0.000 description 2
- 238000003379 elimination reaction Methods 0.000 description 2
- 238000011156 evaluation Methods 0.000 description 2
- 239000008398 formation water Substances 0.000 description 2
- 238000009499 grossing Methods 0.000 description 2
- 239000003208 petroleum Substances 0.000 description 2
- 238000005316 response function Methods 0.000 description 2
- 238000012502 risk assessment Methods 0.000 description 2
- 238000010845 search algorithm Methods 0.000 description 2
- 230000009466 transformation Effects 0.000 description 2
- XLYOFNOQVPJJNP-UHFFFAOYSA-N water Substances O XLYOFNOQVPJJNP-UHFFFAOYSA-N 0.000 description 2
- 238000012952 Resampling Methods 0.000 description 1
- 238000010521 absorption reaction Methods 0.000 description 1
- 230000009286 beneficial effect Effects 0.000 description 1
- 230000000295 complement effect Effects 0.000 description 1
- 239000004020 conductor Substances 0.000 description 1
- 238000013480 data collection Methods 0.000 description 1
- 230000003247 decreasing effect Effects 0.000 description 1
- 238000012217 deletion Methods 0.000 description 1
- 230000037430 deletion Effects 0.000 description 1
- 238000006073 displacement reaction Methods 0.000 description 1
- 230000005672 electromagnetic field Effects 0.000 description 1
- 230000007613 environmental effect Effects 0.000 description 1
- 230000006698 induction Effects 0.000 description 1
- 238000004573 interface analysis Methods 0.000 description 1
- 239000011229 interlayer Substances 0.000 description 1
- 238000004519 manufacturing process Methods 0.000 description 1
- 238000010606 normalization Methods 0.000 description 1
- 239000000047 product Substances 0.000 description 1
- 238000011084 recovery Methods 0.000 description 1
- 238000012827 research and development Methods 0.000 description 1
- 238000012552 review Methods 0.000 description 1
- 239000011435 rock Substances 0.000 description 1
- 239000002356 single layer Substances 0.000 description 1
- 238000000638 solvent extraction Methods 0.000 description 1
- 238000006467 substitution reaction Methods 0.000 description 1
- 239000013589 supplement Substances 0.000 description 1
- 230000009469 supplementation Effects 0.000 description 1
- 238000003786 synthesis reaction Methods 0.000 description 1
- 238000012360 testing method Methods 0.000 description 1
- 230000017105 transposition Effects 0.000 description 1
Images
Classifications
-
- E—FIXED CONSTRUCTIONS
- E21—EARTH OR ROCK DRILLING; MINING
- E21B—EARTH OR ROCK DRILLING; OBTAINING OIL, GAS, WATER, SOLUBLE OR MELTABLE MATERIALS OR A SLURRY OF MINERALS FROM WELLS
- E21B7/00—Special methods or apparatus for drilling
- E21B7/04—Directional drilling
-
- E—FIXED CONSTRUCTIONS
- E21—EARTH OR ROCK DRILLING; MINING
- E21B—EARTH OR ROCK DRILLING; OBTAINING OIL, GAS, WATER, SOLUBLE OR MELTABLE MATERIALS OR A SLURRY OF MINERALS FROM WELLS
- E21B47/00—Survey of boreholes or wells
-
- E—FIXED CONSTRUCTIONS
- E21—EARTH OR ROCK DRILLING; MINING
- E21B—EARTH OR ROCK DRILLING; OBTAINING OIL, GAS, WATER, SOLUBLE OR MELTABLE MATERIALS OR A SLURRY OF MINERALS FROM WELLS
- E21B49/00—Testing the nature of borehole walls; Formation testing; Methods or apparatus for obtaining samples of soil or well fluids, specially adapted to earth drilling or wells
Landscapes
- Life Sciences & Earth Sciences (AREA)
- Engineering & Computer Science (AREA)
- Geology (AREA)
- Mining & Mineral Resources (AREA)
- Physics & Mathematics (AREA)
- Environmental & Geological Engineering (AREA)
- Fluid Mechanics (AREA)
- General Life Sciences & Earth Sciences (AREA)
- Geochemistry & Mineralogy (AREA)
- Geophysics (AREA)
- Geophysics And Detection Of Objects (AREA)
Abstract
本发明公开了一种用于地质导向的钻头调整预测方法,包括:利用历史邻井和/或导眼井测井数据,构建地质导向模型;利用实时获取到的随钻方位伽马和电磁波电阻率测井曲线求取井眼地层相对倾角、地层方位角和边界距指示极化值,对地质导向模型进行修正,建立随钻地层初始模型;基于随钻地层初始模型的响应结果,对该模型进行修正,根据预设的地质模型反演数据库,通过快速查库法,得到地层真实参数;根据地层真实参数,预测层界面在沿待钻水平井井轴方向上的变化,计算钻头在目标层内调整的安全距离。本发明能够通过常规的随钻测井数据,预测地层走向和钻头到层边界距离,提高测井数据利用效率,指导工程师的地质导向作业。
The invention discloses a drill bit adjustment and prediction method for geosteering, comprising: constructing a geosteering model by using historical offset well and/or pilot hole logging data; The relative dip angle of the wellbore formation, the formation azimuth angle and the boundary distance indicated polarization values were obtained from the rate logging curve, and the geosteering model was revised to establish the initial formation model while drilling; based on the response results of the initial formation model while drilling, the model was Make corrections, invert the database according to the preset geological model, and obtain the real parameters of the formation through the fast database search method; Adjustable safety distance within. The invention can predict the stratum trend and the distance from the drill bit to the layer boundary through the conventional logging data while drilling, improve the utilization efficiency of the logging data, and guide the geosteering operation of the engineer.
Description
技术领域technical field
本发明涉及油田开发技术领域,具体地说,是涉及一种基于随钻方位伽马成像和常规随钻电磁波电阻率的用于地质导向的钻头调整预测方法。The invention relates to the technical field of oilfield development, in particular to a drill bit adjustment and prediction method for geosteering based on azimuthal gamma imaging while drilling and conventional electromagnetic wave resistivity while drilling.
背景技术Background technique
电缆测井总是在随钻测井完工之后,用电缆将仪器下放入井中进行测量,然而,在某些情况下,如:(1)井斜超过70度的大斜度井甚至水平井,电缆测井难以进行数据测量;(2)井壁状况不好发生坍塌或堵塞也难取得测井资料;(3)一般情况下井钻完后再测井,由于钻井液的侵入,地层的各种参数与原始地层参数存在一定的差异。伴随着石油的大量开采,整装油气藏逐渐减少,复杂、难动油气藏逐渐增加,20世纪末期,为适应石油工业的发展需要,尤其是为了提高钻井效率和提高油藏采收率,水平井钻井及地质导向技术逐渐发展起来。80年代初期,随着定向井技术的成熟和新的井下工具、仪器的应用,水平井钻井进入了一个蓬勃发展时期。随钻测井己经成为水平井井油藏评价的重要手段,也是完成水平井钻井设计,实时井场数据采集、解释和现场决策以及指导地质导向钻井的关键技术。Wireline logging is always done after logging while drilling, and the tool is put into the well with a wireline for measurement, however, in some cases, such as: (1) Highly deviated wells or even horizontal wells with a well deviation of more than 70 degrees , it is difficult to measure data with wireline logging; (2) it is difficult to obtain logging data if the well wall is not in good condition, and it is difficult to obtain logging data; (3) under normal circumstances, logging is performed after the well is drilled. There are some differences between these parameters and the original formation parameters. With the massive exploitation of oil, the number of integrated oil and gas reservoirs gradually decreased, and the complex and difficult-to-break oil and gas reservoirs gradually increased. At the end of the 20th century, in order to meet the development needs of the petroleum industry, especially to improve drilling efficiency and oil reservoir recovery, water Horizontal well drilling and geosteering technology have gradually developed. In the early 1980s, with the maturity of directional well technology and the application of new downhole tools and instruments, horizontal well drilling entered a period of vigorous development. Logging while drilling has become an important means of reservoir evaluation for horizontal wells, and it is also a key technology to complete horizontal well drilling design, real-time well site data acquisition, interpretation and field decision-making, and to guide geosteering drilling.
由于随钻测井的地层钻开时间短,测井曲线除了能够实时反映钻遇地层变化外,还能够提供多种探测深度曲线,随钻测井数据信息量大,测井曲线丰富。因此广泛应用在水平井地质导向、钻后解释评价方面。同时,随钻测井工具日益丰富,当前国际上LWD能够测量30多种参数(电阻率、伽马、密度、声波、地震、核磁等),基本上所有电缆测井项目均有随钻测量与之对应,仪器外径为44.5~216.0mm,基本上满足各种定向井的需要。在LWD时效性、高利润的驱使下,世界上主要的石油技术服务公司近年加强了随钻技术的研发力度。Due to the short formation drilling time of LWD, the logging curve can not only reflect the real-time stratum change, but also provide a variety of detection depth curves. The LWD data is rich in information and rich in logging curves. Therefore, it is widely used in horizontal well geosteering, post-drilling interpretation and evaluation. At the same time, logging while drilling tools are increasingly abundant. Currently, LWD can measure more than 30 parameters (resistivity, gamma, density, acoustic wave, seismic, nuclear magnetic, etc.) Correspondingly, the outer diameter of the tool is 44.5-216.0mm, which basically meets the needs of various directional wells. Driven by the timeliness and high profits of LWD, the world's major petroleum technology service companies have strengthened the research and development of drilling-while-drilling technology in recent years.
在现有技术中,通常根据实时采集到的测井数据进行地层模型的建立,从而构建出井眼轨迹-地层位置关系,并将其作为地质导向技术的数据基础。在实际随钻测井过程中,由于实测数据的采集量和处理量非常庞大,因此这种需要对地层模型进行实时构建的方法会使得测井数据的处理效率较低,从而影响地质导向作业的准确性和及时性。另外,针对具体的钻头导向调整的计算方法少有涉及。In the prior art, the formation model is usually established according to the logging data collected in real time, so as to construct the relationship between the wellbore trajectory and the formation position, and use it as the data basis of the geosteering technology. In the actual logging while drilling process, due to the huge amount of measured data collection and processing, this method that requires real-time construction of the formation model will make the processing efficiency of logging data low, thus affecting the performance of geosteering operations. Accuracy and timeliness. In addition, the calculation method for the specific drill steering adjustment is rarely involved.
发明内容SUMMARY OF THE INVENTION
为了解决上述技术问题,本发明提供了一种用于地质导向的钻头调整预测方法,该方法包括如下步骤:步骤一,将经过标准化的邻井和/或导眼井测井数据进行快速反演处理,并根据反演结果划分地层层位,构建地质导向模型;步骤二,利用随钻测井作业中实时获取的随钻方位伽马成像测井曲线和随钻电磁波电阻率测井曲线的实测数据,得到相应的包括井眼地层相对倾角、地层方位角和边界距指示极化值的随钻测量参数;步骤三,结合所述随钻测量参数,将所述地质导向模型进行实时修正,建立随钻地层初始模型;步骤四,基于所述随钻地层初始模型的响应结果,根据预设的地质模型反演数据库,通过快速查库法,进一步修正所述随钻地层初始模型,得到地层真实参数,所述地层真实参数包括所述井眼地层相对倾角、测量点到地层边界距离以及地层层厚;步骤五,根据所述地层真实参数,对未钻遇地层进行等倾角顺延,并预测层界面在沿待钻水平井井轴方向上的变化以及钻头调整的安全距离,以指导地质导向作业。In order to solve the above technical problems, the present invention provides a method for predicting the adjustment of a drill bit for geosteering. The method includes the following steps:
优选地,所述步骤五进一步包括:获取钻头井斜角,并计算地层视倾角;根据所述地层视倾角以及所述地层真实参数,预测探测范围外的地层电阻率和地层层厚在沿井轴方向上的变化,绘制地层二维剖面图;根据所述地层二维剖面图、钻头距测量点的距离以及钻头方向,对未钻遇地层进行等倾角顺延的层界面位置预测,进一步确定钻头钻出目标层的距离。Preferably, the
优选地,所述步骤四进一步包括:对比所述随钻地层初始模型的响应结果与所述实测数据,利用梯度下降法,得到初步修正后的随钻地层初始模型对应的模型修正量;利用所述模型修正量,从所述地质模型反演数据库中查找所述初步修正后的随钻地层初始模型的测井响应,对比查库得到的测井响应与所述实测数据,得到二次修正后的随钻地层初始模型,进一步将所述二次修正后的随钻地层模型作为反演结果,得到相应的所述真实地层参数。Preferably, the
优选地,在所述步骤四中,根据随钻测井作业中待钻水平井所在区域的地层特性参数以及随钻测量仪器参数,建立分类正演地质仿真模型库;基于麦克斯韦方程,利用解析解数值模拟算法,对分类正演地质仿真模型库中各类别参数进行数值正演仿真计算,得到地层模型-电磁波电阻率曲线-边界距的关系,形成所述地质模型反演数据库。Preferably, in the fourth step, according to the formation characteristic parameters of the area where the horizontal well to be drilled in the logging-while-drilling operation and the parameters of the measurement-while-drilling instrument, a classified forward modeling geological simulation model library is established; The numerical simulation algorithm performs numerical forward simulation calculation on each type of parameters in the classified forward modeling geological simulation model database, obtains the relationship between the formation model-electromagnetic wave resistivity curve-boundary distance, and forms the geological model inversion database.
优选地,所述步骤一进一步包括如下步骤:获取快速反演处理后得到的地层电阻率和地层结构参数,利用拐点法将反演结果进行地层层位划分,确定地层层界面以及展示地层层位横向与深度对应关系的层位划分结果;将经过标准化预处理的邻井和/或导眼井的测井数据作为初始参数,结合所述层位划分结果,得到所述地质导向模型。Preferably, the first step further includes the following steps: acquiring the formation resistivity and formation structure parameters obtained after the fast inversion processing, using the inversion method to divide the inversion results into formation horizons, determining the formation boundary and displaying the formation horizons The horizon division result of the horizontal and depth correspondence; the geosteering model is obtained by taking the log data of the offset wells and/or pilot wells that have undergone standardized preprocessing as initial parameters and combining the horizon division results.
优选地,在利用拐点法将反演结果进行地层层位划分,确定地层层界面以及展示地层层位横向与深度对应关系的层位划分结果步骤中,还包括:若具备多口邻井,则需要对每口邻井进行分层,得到待钻水平井与各邻井井位坐标对应的地层层位划分情况;根据邻井井位坐标分布信息,将各个邻井层位的分层结果进行对比和链接,获得展示待钻水平井的整个地层层位横向与深度对应关系的所述层位划分结果。Preferably, in the step of dividing the inversion results into stratigraphic horizons by using the inflection point method, determining the stratigraphic horizons, and displaying the horizon dividing results of the horizontal and depth correspondence of the stratigraphic horizons, it also includes: if there are multiple offset wells, then It is necessary to stratify each adjacent well to obtain the stratum layer division corresponding to the horizontal well to be drilled and the well position coordinates of each adjacent well; By comparing and linking, the layer division result showing the horizontal and depth correspondence of the entire formation horizon of the horizontal well to be drilled is obtained.
优选地,在所述步骤二中,通过如下步骤获取所述井眼地层相对倾角:利用拐点法根据实时获取到的所述随钻方位伽马成像测井曲线,确定方位伽马成像数据穿越层界面位置深度;根据所述方位伽马成像数据穿越层界面位置深度,计算方位伽马成像数据高程差;基于获取到的当前导眼井井径曲线和方位伽马成像仪器探测深度,根据所述方位伽马成像数据高程差,从所述随钻方位伽马成像测井曲线中提取所述井眼地层相对倾角。Preferably, in the second step, the relative dip angle of the wellbore formation is obtained by the following steps: using the inflection point method to determine the azimuth gamma imaging data crossing layer according to the azimuth gamma imaging logging curve acquired in real time interface position depth; according to the position depth of the azimuth gamma imaging data crossing the layer interface, calculate the elevation difference of the azimuth gamma imaging data; The elevation difference of the azimuthal gamma imaging data is used to extract the relative dip angle of the wellbore formation from the azimuthal gamma imaging logging curve while drilling.
优选地,所述步骤三进一步包括:根据所述地质导向模型的响应数据和所述层位划分结果,确定地层层数、每层电阻率以及层厚在横向上的变化;利用从所述随钻方位伽马成像测井曲线中提取的所述井眼地层相对倾角,将所述地质导向模型中得到的所述井眼地层相对倾角进行修正;根据通过所述随钻电磁波电阻率测井曲线得到的边界距指示极化值,计算测量点到地层边界面的距离,进一步将完成井眼地层相对倾角修正的所述地质导向模型中的地层层位横向与深度对应关系进行深度校正,建立所述随钻地层初始模型。Preferably, the third step further includes: determining the number of formation layers, the resistivity of each layer and the lateral change of layer thickness according to the response data of the geosteering model and the layer division result; The relative dip angle of the wellbore formation extracted from the drilling azimuth gamma imaging logging curve is corrected, and the relative dip angle of the wellbore formation obtained in the geosteering model is corrected; The obtained boundary distance indicates the polarization value, calculate the distance from the measurement point to the formation boundary surface, and further perform depth correction on the corresponding relationship between the horizontal and depth of the formation horizon in the geosteering model that has completed the correction of the relative dip angle of the wellbore and formation, and establish the The initial model of the formation while drilling is described.
优选地,在根据所述地层二维剖面图、钻头距测量点的距离以及钻头方向,对未钻遇地层进行等倾角顺延的层界面位置预测,进一步确定钻头钻出目标层的距离步骤中,当所述钻头井斜角小于90度时,进一步包括:利用包括所述井眼地层相对倾角以及测量点到地层边界距离的所述地层真实参数,计算钻头与地层上界面距离,从而得到钻头与地层下界面距离,用以确定钻头在目标层内的位置;根据所述钻头与地层下界面距离,预测钻头钻出地层下界面的距离,并将其作为所述钻头调整的安全距离。Preferably, in the step of further determining the distance at which the drill bit drills out of the target layer, according to the two-dimensional cross-sectional view of the stratum, the distance from the drill bit to the measurement point, and the direction of the drill bit, predicting the position of the layer boundary of the stratum that has not been drilled at an equal dip angle, and further determining the distance from the drill bit to the target layer, When the inclination angle of the drill bit is less than 90 degrees, the method further includes: calculating the distance between the drill bit and the upper boundary of the formation by using the real formation parameters including the relative inclination angle of the wellbore formation and the distance from the measurement point to the formation boundary, so as to obtain the distance between the drill bit and the formation boundary. The distance from the lower boundary of the formation is used to determine the position of the drill bit in the target layer; according to the distance between the drill bit and the lower boundary of the formation, predict the distance that the bit drills out of the lower boundary of the formation, and use it as the safety distance for the adjustment of the drill bit.
优选地,在根据所述地层二维剖面图、钻头距测量点的距离以及钻头方向,对未钻遇地层进行等倾角顺延的层界面位置预测,进一步确定钻头钻出目标层的距离步骤中,当所述钻头井斜角大于90度时,进一步包括:利用包括所述井眼地层相对倾角以及测量点到地层边界距离的所述地层真实参数,计算钻头与地层下界面距离,从而得到钻头与地层上界面距离,用以确定钻头在目标层内的位置;根据所述钻头与地层上界面距离,预测钻头钻出地层上界面的距离,并将其作为所述钻头调整的安全距离。Preferably, in the step of further determining the distance at which the drill bit drills out of the target layer, according to the two-dimensional cross-sectional view of the stratum, the distance from the drill bit to the measurement point, and the direction of the drill bit, predicting the position of the layer boundary of the stratum that has not been drilled at an equal dip angle, and further determining the distance from the drill bit to the target layer, When the inclination angle of the drill bit is greater than 90 degrees, the method further includes: calculating the distance between the drill bit and the lower boundary of the formation by using the real formation parameters including the relative inclination angle of the wellbore formation and the distance from the measurement point to the formation boundary, so as to obtain the distance between the drill bit and the formation boundary. The distance from the upper boundary of the formation is used to determine the position of the drill bit in the target layer; according to the distance between the drill bit and the upper boundary of the formation, the distance that the drill bit drills out of the upper boundary of the formation is predicted and used as the safety distance for the adjustment of the drill bit.
与现有技术相比,上述方案中的一个或多个实施例可以具有如下优点或有益效果:Compared with the prior art, one or more embodiments of the above solutions may have the following advantages or beneficial effects:
本发明能够通过方位伽马成像与常规电磁波电阻率随钻测井数据,预测地层走向和钻头到地层边界的距离,是地质导向过程中迫切需要的数据处理技术,这种方法充分发挥各类测井数据的探测优势,综合利用,提高了测井数据利用效率,指导导向工程师在地质导向过程中调整钻头角度,从而指导地质导向。The present invention can predict the stratum trend and the distance from the drill bit to the stratum boundary through azimuthal gamma imaging and conventional electromagnetic wave resistivity logging while drilling data, which is an urgently needed data processing technology in the process of geosteering. The advantages of well data detection and comprehensive utilization improve the utilization efficiency of logging data, and guide the steering engineer to adjust the angle of the drill bit in the process of geosteering, thereby guiding the geosteering.
本发明的其他优点、目标,和特征在某种程度上将在随后的说明书中进行阐述,并且在某种程度上,基于对下文的考察研究对本领域技术人员而言将是显而易见的,或者可以从本发明的实践中得到指导。本发明的目标和其他优点可以通过下面的说明书,权利要求书,以及附图中所特别指出的结构来实现和获得。Other advantages, objects, and features of the present invention will be set forth in the specification to the extent that follows, and will be apparent to those skilled in the art based on a review of the following, or may be Guidance is gained from the practice of the present invention. The objectives and other advantages of the invention may be realized and attained by the structure particularly pointed out in the description and claims hereof as well as the appended drawings.
附图说明Description of drawings
附图用来提供对本发明的进一步理解,并且构成说明书的一部分,与本发明的实施例共同用于解释本发明,并不构成对本发明的限制。在附图中:The accompanying drawings are used to provide a further understanding of the present invention, and constitute a part of the specification, and together with the embodiments of the present invention, are used to explain the present invention, and do not constitute a limitation to the present invention. In the attached image:
图1是本发明实施例的用于地质导向的钻头调整预测方法的步骤图。FIG. 1 is a step diagram of a method for predicting drill bit adjustment for geosteering according to an embodiment of the present invention.
图2a是本发明实施例的用于地质导向的钻头调整预测方法的电阻率井眼校正图版。Fig. 2a is a resistivity wellbore correction chart of the method for predicting the adjustment of bit adjustment for geosteering according to an embodiment of the present invention.
图2b是本发明实施例的用于地质导向的钻头调整预测方法的电阻率介电校正图版。FIG. 2b is a resistivity and dielectric correction chart of the method for predicting the adjustment of a drill bit for geosteering according to an embodiment of the present invention.
图3是本发明实施例的用于地质导向的钻头调整预测方法的邻井反演结果示例图。FIG. 3 is an example diagram of an offset well inversion result of the drill bit adjustment prediction method for geosteering according to an embodiment of the present invention.
图4是本发明实施例的用于地质导向的钻头调整预测方法的地质导向模型示意图。FIG. 4 is a schematic diagram of a geosteering model of the drill bit adjustment prediction method for geosteering according to an embodiment of the present invention.
图5是本发明实施例的用于地质导向的钻头调整预测方法的随钻电磁波电阻率曲线合成指示层边界距信号(Peak值信号)响应示意图。FIG. 5 is a schematic diagram of the response of the electromagnetic wave resistivity curve synthesis while drilling indicating layer boundary distance signal (Peak value signal) of the drill bit adjustment prediction method for geosteering according to an embodiment of the present invention.
图6a是本发明实施例的用于地质导向的钻头调整预测方法的中当钻头井斜角度小于90°情况下,地质导向中钻头位置确定及钻头距地层界面距离的情景示意图。6a is a schematic diagram of the location of the bit and the distance between the bit and the formation interface in geosteering when the inclination angle of the bit is less than 90° in the method for predicting bit adjustment for geosteering according to an embodiment of the present invention.
图6b是本发明实施例的用于地质导向的钻头调整预测方法的中当钻头井斜角度大于90°情况下,地质导向中钻头位置确定及钻头距地层界面距离的情景示意图。6b is a schematic diagram of the location of the bit and the distance between the bit and the formation interface in geosteering when the inclination angle of the bit is greater than 90° in the method for predicting bit adjustment for geosteering according to an embodiment of the present invention.
图7是本发明实施例的用于地质导向的钻头调整预测方法的地质导向实时反演剖面图。7 is a cross-sectional view of a real-time inversion of geosteering for a method for predicting drill bit adjustment for geosteering according to an embodiment of the present invention.
具体实施方式Detailed ways
以下将结合附图及实施例来详细说明本发明的实施方式,借此对本发明如何应用技术手段来解决技术问题,并达成技术效果的实现过程能充分理解并据以实施。需要说明的是,只要不构成冲突,本发明中的各个实施例以及各实施例中的各个特征可以相互结合,所形成的技术方案均在本发明的保护范围之内。The embodiments of the present invention will be described in detail below with reference to the accompanying drawings and examples, so as to fully understand and implement the implementation process of how the present invention applies technical means to solve technical problems and achieve technical effects. It should be noted that, as long as there is no conflict, each embodiment of the present invention and each feature of each embodiment can be combined with each other, and the formed technical solutions all fall within the protection scope of the present invention.
本发明实施例旨在形成一种应用解析解仿真算法建立可供查询的地质模型反演数据库,利用邻井和导眼井测井数据通过反演方法,获得地层参数并划分地层层位,建立导向模型,进一步应用随钻方位伽马成像和常规电磁波电阻率,建立地质导向模型修正量,校正导向模型为地层反演初始模型。而后,以初始模型为出发点,利用梯度下降法计算模型修正量,通过开发快速查库算法,比较修正模型模拟响应与实测数据测井响应残差,根据残差情况循环迭代使用梯度下降法修改模型,直至模型响应与测井响应残差足够小,从而输出反演得到的井眼地层相对倾角、边界距离等信息,基于此,再根据测量点到钻头距离、井眼轨迹预测钻头距离层边界距离指导地质导向。The embodiment of the present invention aims to form a geological model inversion database that can be queried by applying an analytical solution simulation algorithm, and uses the logging data of offset wells and pilot wells to obtain the formation parameters and divide the formation horizons through the inversion method. Steering model, further use azimuth gamma imaging while drilling and conventional electromagnetic wave resistivity to establish the correction value of the geosteering model, and correct the steering model as the initial model of formation inversion. Then, taking the initial model as the starting point, the gradient descent method is used to calculate the model correction amount, and by developing a fast database search algorithm, the simulated response of the corrected model and the log response residual of the measured data are compared, and the gradient descent method is used to modify the model according to the residual conditions. , until the residuals between the model response and the logging response are small enough to output the inversion information such as the relative dip angle and boundary distance of the wellbore formation. Guiding geosteering.
图1是本发明实施例的用于地质导向的钻头调整预测方法的步骤图。如图1所示,在步骤S110(步骤一)中,将经过标准化的邻井和/或导眼井测井数据进行快速反演处理,并根据反演结果划分地层层位,构建地质导向模型。FIG. 1 is a step diagram of a method for predicting drill bit adjustment for geosteering according to an embodiment of the present invention. As shown in Fig. 1, in step S110 (step 1), the standardized logging data of offset wells and/or pilot wells are subjected to rapid inversion processing, and the formation layers are divided according to the inversion results to construct a geosteering model .
在步骤S110(步骤一)中,基于经过标准化预处理的钻前采集到的邻井和/或导眼井的历史测井数据,对预处理结果进行地层测井参数的快速反演处理,获得地层电阻率参数和包括地层层位划分结果的地层结构参数,利用拐点法将反演结果进行地层层位划分,确定地层层界面以及展示地层层位横向与深度对应关系的层位划分结果,进一步,将经过标准化预处理的邻井和/或导眼井的历史测井数据作为初始参数,结合层位划分结果,得到构建地质导向模型。具体的,针对这一过程包括如下几个步骤:In step S110 (step 1), based on the historical logging data of the offset wells and/or pilot wells collected before the standardization and pre-drilling, the preprocessing results are subjected to rapid inversion processing of formation logging parameters to obtain The formation resistivity parameters and the formation structure parameters including the formation horizon division results are used to divide the inversion results into the formation horizons, determine the stratigraphic layer boundaries, and display the horizon division results of the horizontal and depth correspondence between the formation horizons, and further , taking the historical logging data of offset wells and/or pilot wells after standardized preprocessing as initial parameters, and combining the results of horizon division, a geosteering model is constructed. Specifically, this process includes the following steps:
首先,(步骤S1101)需要将钻前采集到的邻井和/或导眼井的历史测井数据依次进行包括错误数据剔除、缺失数据补充、非地层影响因素校正的标准化处理。First, (step S1101 ) the historical logging data of offset wells and/or pilot wells collected before drilling needs to be subjected to standardization processing including erroneous data elimination, missing data supplementation, and correction of non-strata influencing factors in sequence.
在错误数据剔除中,建立如下错误数据评判指标:In error data elimination, the following error data evaluation indicators are established:
其中,Erk为邻井和导眼井任一测井曲线上的第k个采样点的错误指标函数,Rak、Rai分别表示邻井和导眼井第k个、第i个测量点测井响应,m为错误数据评判指标窗长,当错误指标函数满足下面任何一个条件时,判断当前测井数据为错误数据:Among them, Er k is the error index function of the k-th sampling point on any logging curve of the offset and pilot wells, and Ra k and Ra i represent the k-th and i-th measurement points of the offset and pilot wells, respectively Logging response, m is the window length of the error data evaluation index, when the error index function satisfies any of the following conditions, the current logging data is judged as error data:
接下来,对错误数据进行删除,将错误数据对应位置的测井响应删除,并将该位置数据设置成缺失数据。Next, delete the erroneous data, delete the logging response of the position corresponding to the erroneous data, and set the position data as missing data.
进一步,将错误数据删除后形成的历史测井数据采用多点采样的线性平滑法进行缺失点数据补充,并用如下表达式表示上述方法:Further, the historical logging data formed after the deletion of the erroneous data adopts the linear smoothing method of multi-point sampling to supplement the missing point data, and the above method is expressed by the following expression:
其中,Ti表示第i个测量点测井值,Ti+k表示第i+k个测量点的测井值,i、k为记录测量值下标,m表示平滑窗长,Ai表示第i个点的权重因子,表示重采样后第i个采样点取值。Among them, T i represents the logging value of the i-th measurement point, T i+k represents the log value of the i+k-th measurement point, i and k are the subscripts of the recorded measurement values, m represents the length of the smoothing window, and A i represents the The weighting factor of the i-th point, Indicates the value of the i-th sampling point after resampling.
最后,将经过缺失数据补充的测井数据进行非地层因素校正。本例中,这一过程采用校正采样图版法,依次经过井眼校正、偏心校正和介电常数校正等针对非地层因素的校正过程。图2a是本发明实施例的用于地质导向的钻头调整预测方法的电阻率井眼校正图版。图2b是本发明实施例的用于地质导向的钻头调整预测方法的电阻率介电校正图版。如图2a、图2b所示,横坐标为电阻率测井响应,纵坐标为校正系数。在图版校正时,先通过横坐标找到当前测量值对应的图版横轴位置,在其上做一条直线与图版中曲线相交,交点对应的纵坐标值即为校正系数。测量值与校正系数的乘积即为非地层因素校正后的电阻率测井响应。这样,完成了对邻井和/或导眼井的测井数据的标准化处理,以得到原状地层电阻率参数。Finally, the log data supplemented by missing data is corrected for non-strata factors. In this example, the calibration sampling plate method is used in this process, and the calibration processes for non-strata factors such as borehole calibration, eccentricity calibration and dielectric constant calibration are successively performed. Fig. 2a is a resistivity wellbore correction chart of the method for predicting the adjustment of bit adjustment for geosteering according to an embodiment of the present invention. FIG. 2b is a resistivity and dielectric correction chart of the method for predicting the adjustment of a drill bit for geosteering according to an embodiment of the present invention. As shown in Fig. 2a and Fig. 2b, the abscissa is the resistivity logging response, and the ordinate is the correction coefficient. When the plate is calibrated, first find the horizontal axis position of the plate corresponding to the current measurement value through the abscissa, and make a straight line on it to intersect the curve in the plate, and the ordinate value corresponding to the intersection point is the correction coefficient. The product of the measured value and the correction factor is the resistivity log response corrected for non-formation factors. In this way, the normalization processing of the log data of the offset well and/or pilot hole is completed to obtain the undisturbed formation resistivity parameter.
然后,(步骤S1102)在完成标准化预处理后,对标准化处理后的数据进行全参数的反演,通过反演获得地层电性参数(包括侵入带电阻率、原状地层电阻率等),利用拐点法将反演结果进行地层层位划分,确定地层层界面以及展示地层层位横向与深度对应关系的层位划分结果,从而得到相应的地层结构参数(包括:侵入深度、地层层界面位置等)。Then (step S1102) after the standardization preprocessing is completed, perform full-parameter inversion on the standardized data, obtain the formation electrical parameters (including the resistivity of the invasion zone, the resistivity of the original formation, etc.) through the inversion, and use the inflection point The inversion results are divided into stratigraphic horizons using the method to determine stratigraphic horizons and horizon partitioning results showing the horizontal and depth correspondence between stratigraphic horizons, so as to obtain the corresponding stratigraphic structure parameters (including: invasion depth, stratigraphic horizon location, etc.) .
在本例中,利用拐点法对标准化处理后的历史测井数据进行地层层位划分工作,用差分代替微分,通过求解标准化处理后的测井曲线二阶差分,将原状地层电阻率相同的测井深度段划分为同一地层,并确定在电阻率变化剧烈位置(测井曲线二次导数为0)的地方为地层界面,即将拐点函数等于0处的拐点位置,判断为地层层界面。其中,用如下表达式表示测井曲线的二阶差分方程:In this example, the inflection point method is used to divide the normalized historical logging data, and the difference is used to replace the differential. The well depth section is divided into the same formation, and the place where the resistivity changes sharply (the second derivative of the logging curve is 0) is determined as the formation interface, that is, the inflection point position where the inflection point function is equal to 0 is determined as the formation boundary. Among them, the second-order difference equation of the logging curve is expressed by the following expression:
其中,x表示测井曲线的采样点位置,f1(x)表示采样点位置在x时的经过标准化预处理的邻井和/或导眼井的测井数据的反演响应结果,f1(x-h)、f1(x+h)则分别表示测井曲线在x-h和x+h处的经过标准化预处理的邻井和/或导眼井的测井数据的正演响应结果,h表示步长,g1(x)为反演响应结果的二阶差分值。当g1(x)=0时的x值即为界面位置。Among them, x represents the sampling point position of the logging curve, f 1 (x) represents the inversion response result of the normalized and preprocessed logging data of the offset well and/or pilot well when the sampling point location is x, f 1 (xh), f 1 (x+h) represent the forward modeling response results of the log data of the offset well and/or pilot well that have been standardized and preprocessed at xh and x+h, respectively, and h represents Step size, g 1 (x) is the second-order difference value of the inversion response result. The value of x when g 1 (x)=0 is the interface position.
将经过标准化预处理的邻井和/或导眼井测井数据中的电阻率值作为地层电阻率初值,结合拐点法层位划分结果(上述邻井和/或导眼井测井数据的地层层界面分析结果),建立邻井快速反演初始模型。The resistivity value in the log data of the offset and/or pilot wells that have undergone standardized preprocessing is used as the initial value of formation resistivity, combined with the horizon division results of the inflection point method (the above-mentioned offset and/or pilot well logging data Formation interface analysis results), to establish the initial model for the rapid inversion of offset wells.
图3是本发明实施例的用于地质导向的钻头调整预测方法的邻井反演结果示例图。如图3所示,邻井快速反演初始模型包括:反演结果绘制侵入剖面、测量点对应井深、侵入半径、反演结果、视电阻率、中子密度和孔隙度。FIG. 3 is an example diagram of an offset well inversion result of the drill bit adjustment prediction method for geosteering according to an embodiment of the present invention. As shown in Fig. 3, the initial model for rapid inversion of offset wells includes: plotting invasion profile from inversion results, well depth corresponding to measurement points, invasion radius, inversion results, apparent resistivity, neutron density and porosity.
接着,通过对比邻井快速反演初始模型的响应数据和邻井及导眼井的历史测井数据的残差平方和,建立目标函数:Next, the objective function is established by comparing the response data of the initial model for the rapid inversion of the offset wells and the residual sum of squares of the historical logging data of the offset wells and pilot wells:
其中,r表示邻井快速反演初始模型的反演结果;R表示自变量向量;m表示未知量个数;n表示正演响应曲线个数;x表示模型参数(包括:电阻率、层厚、边界距、侵入深度、井眼直径等);f(x)表示目标函数,T表示矩阵转置。Among them, r represents the inversion results of the initial model of the offset well rapid inversion; R represents the independent variable vector; m represents the number of unknowns; n represents the number of forward response curves; x represents the model parameters (including resistivity, layer thickness, etc.) , boundary distance, invasion depth, borehole diameter, etc.); f(x) represents the objective function, and T represents the matrix transposition.
通过梯度下降方法求解目标函数雅可比矩阵,形成雅可比线性方程组,求解方程组计算目标函数最速下降方向,并用下列表达式表示:The Jacobian matrix of the objective function is solved by the gradient descent method to form a system of Jacobian linear equations, and the steepest descent direction of the objective function is calculated by solving the equation system, which is expressed by the following expression:
按照以下公式来计算目标函数的梯度:Calculate the gradient of the objective function according to the following formula:
其中,x是模型参数,r(x)模型参数x对应的响应函数,Y(x)是r(x)的雅可比矩阵,g(x)是梯度函数,是微分算子,ri(x)是模型参数x对应的响应函数第i个分量。求解目标函数需要先在最速下降方向上确定步长h;进一步根据求得邻井快速反演初始模型改变方向和改变步长,确定该模型的改变量,改变模型,完成一次模型更新,进而,通过设置循环终止条件,循环调用模型更新过程,直至满足循环终止条件,从而构建地质导向模型,得到地层测井参数。where x is the model parameter, r(x) is the response function corresponding to the model parameter x, Y(x) is the Jacobian matrix of r(x), g(x) is the gradient function, is the differential operator, and ri (x) is the ith component of the response function corresponding to the model parameter x. To solve the objective function, it is necessary to first determine the step size h in the direction of the steepest descent; further, according to the obtained offset well rapid inversion initial model change direction and change step size, determine the change amount of the model, change the model, and complete a model update, and then, By setting the cycle termination conditions, the model update process is called cyclically until the cycle termination conditions are met, so as to build a geosteering model and obtain formation logging parameters.
需要说明的是,在地层层位划分过程中,若待钻水平井具有多口邻井,则需要对每口邻井按照相同的方法进行分层,得到待钻水平井与各邻井井位坐标对应的地层层位划分情况。再根据邻井井位坐标分布信息,将各邻井按照相同深度的层位划分情况进行对比和链接,获得展示待钻水平井的整个地层层位横向与深度对应关系的所述层位划分结果。进一步将井间界面通过线性差值方法,链接不同邻井中的同一层位界面,从而获得相应的地层剖面。It should be noted that, in the process of stratum level division, if the horizontal well to be drilled has multiple offset wells, each offset well needs to be layered according to the same method to obtain the well positions of the horizontal well to be drilled and each offset well. The division of the stratum corresponding to the coordinates. Then, according to the coordinate distribution information of the adjacent wells, compare and link each adjacent well according to the horizon division of the same depth, and obtain the horizon division result showing the horizontal and depth correspondence of the entire formation horizon of the horizontal well to be drilled. . Furthermore, the interface between wells is connected to the same horizon interface in different offset wells through the linear difference method, so as to obtain the corresponding stratigraphic profile.
最后,结合上述邻井和/或导眼井的测井数据的地层层界面分析结果,通过邻井层位对比或井眼地层相对倾角研究成果,构建三维导向模型,并应用到二维剖面中进行展示,完成地质导向模型的建立,能够从中得到包括地层层界面位置、目标层(待测井的井眼位置)和上下地层测井信息、井眼地层相对倾角等,从而得到整个地层层位横向与深度对应关系。图4是本发明实施例的用于地质导向的钻头调整预测方法的地质导向模型示意图。如图4所示,该模型展示出了地层层界面位置(图4左侧处,其中,水平平行线为已确定的地层层界面)、目标层和地层电阻率信息,曲线为水平井设计完成的井眼轨迹。Finally, a 3D steering model is constructed and applied to the 2D profile based on the analysis results of the stratigraphic interface of the logging data of the above-mentioned offset wells and/or pilot wells, and the results of the horizon comparison of the offset wells or the relative dip angle of the wellbore strata. Display and complete the establishment of the geosteering model, from which the position of the stratum boundary, the target layer (the position of the wellbore to be logged), the logging information of the upper and lower strata, the relative dip angle of the wellbore stratum, etc. can be obtained, so as to obtain the entire stratum horizon. Horizontal and depth correspondence. FIG. 4 is a schematic diagram of a geosteering model of the drill bit adjustment prediction method for geosteering according to an embodiment of the present invention. As shown in Figure 4, the model shows the position of the formation interface (at the left of Figure 4, where the horizontal parallel line is the determined formation boundary), the target layer and formation resistivity information, and the curve is the completion of the horizontal well design wellbore trajectory.
在步骤S110中,根据钻前收集到的邻井和/或导眼井的钻前测井历史数据、导眼井所在地区的固有地质参数(包括:地层电阻率、地层各向异性、层厚、边界距离、地层介电常数、地层水矿化度、岩石空隙度和密度、自然伽马等)等背景信息,先进行邻井快速反演初始模型,再利用邻井及导眼井的历史测井数据将邻井快速反演初始模型进行修正,从而完成地质导向模型的构建工作。这种方法具备方便可行,计算精度高的优势:一方面无需在随钻测井过程中重新构建导向初始模型,只利用历史测井数据预先完成模型构建的工作,提高随钻测井作业的工作效率;另一方面,考虑到随钻测井中环境背景的影响,使得模型构建的参数更加全面,提高了测井响应的准确度,更加符合实际地质导向作业应用环境,增加钻头调整的精确度。In step S110, according to the pre-drilling historical logging data of the offset well and/or the pilot hole collected before drilling, and the inherent geological parameters of the area where the pilot hole is located (including: formation resistivity, formation anisotropy, layer thickness , boundary distance, formation permittivity, formation water salinity, rock porosity and density, natural gamma, etc.), first perform a rapid inversion of the initial model for the adjacent well, and then use the history of the adjacent well and pilot well. The logging data corrects the initial model of the rapid inversion of the offset well, thereby completing the construction of the geosteering model. This method has the advantages of convenience, feasibility and high calculation accuracy: on the one hand, there is no need to rebuild the initial steering model during the logging while drilling process, and only the historical logging data is used to complete the model construction in advance, which improves the work of logging while drilling. On the other hand, considering the influence of the environmental background in LWD, the parameters of the model construction are more comprehensive, the accuracy of the logging response is improved, it is more in line with the actual application environment of geosteering operations, and the accuracy of bit adjustment is increased. .
在完成了上述地质导向模型的建立后,进入到步骤S120中。在步骤S120(步骤二)中,利用随钻测井作业中实时获取到的随钻方位伽马成像测井数据和随钻电磁波电阻率测井曲线的实测数据,得到相应的包括井眼地层相对倾角、地层方位角和边界距指示极化值的随钻测量参数,以确定待分析水平井所在的地层层位。具体地,将实时探测到的随钻方位伽马成像测井曲线,利用拐点法计算方位数据高程差,并提取方位角和基于所述方位数据高程差获得的井眼地层相对倾角;同时,根据实时探测到的随钻电阻率测井曲线,利用常规随钻电磁波电阻率极化效应合成边界指示极化值(Peak值)信号。After the establishment of the above-mentioned geosteering model is completed, step S120 is entered. In step S120 (step 2), using the azimuth-while-drilling gamma imaging logging data obtained in real time during the logging-while-drilling operation and the measured data of the electromagnetic wave resistivity logging curve while drilling, the corresponding data including the borehole formation relative Dip, formation azimuth and boundary distance indicate MWD parameters of polarization values to determine the formation horizon where the horizontal well to be analyzed is located. Specifically, using the azimuth gamma imaging logging curve detected in real time, the inflection point method is used to calculate the elevation difference of the azimuth data, and the azimuth angle and the relative dip angle of the borehole formation obtained based on the elevation difference of the azimuth data are extracted; The resistivity logging curve detected in real time is used to synthesize the boundary indicating polarization value (Peak value) signal by using the resistivity polarization effect of conventional electromagnetic wave while drilling.
下面针对步骤S120中包含的子步骤进行详细说明。The sub-steps included in step S120 will be described in detail below.
首先,(步骤S1201)根据实时获取探测到的随钻方位伽马成像测井曲线,以及方位伽马成像数据变化,利用拐点法计算方位伽马成像数据穿层界面位置深度。利用如下表达式定义随钻方位伽马成像测井曲线的拐点曲线为:First, (step S1201 ) according to the real-time acquisition of the detected azimuthal gamma imaging logging curve while drilling and the change of the azimuthal gamma imaging data, the inflection point method is used to calculate the depth of the azimuthal gamma imaging data through the layer interface. The inflection point curve of the azimuth-while-drilling gamma imaging logging curve is defined by the following expression:
其中,t表示测量点的深度值,G(t)表示随钻方位伽马成像测井曲线在t处的拐点函数值,f3(t)表示在测试点t位置处的随钻方位伽马成像测井曲线的测量值,为求导数符号。进一步,拐点曲线相应的离散公式为:Among them, t represents the depth value of the measurement point, G(t) represents the inflection point function value of the azimuth-while-drilling gamma imaging logging curve at t, and f 3 (t) represents the azimuth-while-drilling gamma at the test point t. Imaging log measurements, for the derivative symbol. Further, the corresponding discrete formula of the inflection point curve is:
其中,△表示采样间隔,f3(t+△)表示地质导向模型在t+Δ处的响应数据,f3(t-△)表示地质导向模型在t-Δ处的响应数据。从拐点的定义公式可以看出,令G(t)=0求得t即为界面位置,拐点实际上为随机信号f3(t)在的二次导数等于零的位置处,这样,可以很好地反映测井曲线的动态性质。因此,在此定义的拐点曲线下,当拐点曲线等于0时,就是地质导向模型的响应曲线变化最剧烈处,即岩性不同的地层分界面,从而确定了实测方位伽马成像数据穿层界面的位置,进一步确定其深度。Among them, △ represents the sampling interval, f 3 (t+△) represents the response data of the geosteering model at t+Δ, and f 3 (t-△) represents the response data of the geosteering model at t-Δ. From the definition formula of the inflection point, it can be seen that t is the interface position by setting G(t)=0, and the inflection point is actually the position where the second derivative of the random signal f 3 (t) is equal to zero. It reflects the dynamic nature of the well logging curve. Therefore, under the inflection point curve defined here, when the inflection point curve is equal to 0, it is the place where the response curve of the geosteering model changes most violently, that is, the stratum interface with different lithology, thus determining the interlayer interface of the measured azimuth gamma imaging data. position to further determine its depth.
然后,进入到步骤S1202中。从上述方位伽马成像数据穿层界面位置数据中获取相应的方位伽马成像数据穿层界面位置深度和方位信息,基于此计算方位伽马成像数据高程差。具体地,当仪器以一定倾角穿过层界面时,方位伽马测量曲线不同方位遇到边界面的时刻不同,对应的深度也不同。因此,随钻方位伽马成像测井曲线的360°方位展开曲线满足余弦分布,且周期为2π。此处,假设余弦函数方程为y=Acos(αx+θ)+b,将方位测量的测井响应(方位伽马成像数据穿层界面位置深度)和对应的方位带入公式,可求得余弦函数未知量(A、α、θ和b),特别是表示余弦曲线振幅的参数A,该参数等价于方位伽马成像数据高程差。进一步的说,由于余弦振幅等价于方位伽马成像数据高程差H,故令H=A。当H值大于0时,表示方位仪器低边先遇到地层层界面,仪器以与层界面法线相对夹角小于90度的姿态穿过层界面;当H小于0时,表示方位仪器高边先遇到层界面,仪器与界面法线夹角大于90度的姿态穿过层界面。Then, it proceeds to step S1202. The corresponding azimuth gamma imaging data cross-layer interface position depth and orientation information are obtained from the above-mentioned azimuth gamma imaging data cross-layer interface position data, and the azimuth gamma imaging data elevation difference is calculated based on this. Specifically, when the instrument passes through the layer interface at a certain inclination angle, the azimuth gamma measurement curve encounters the boundary surface at different times in different directions, and the corresponding depths are also different. Therefore, the 360° azimuth expansion curve of the azimuth-while-drilling gamma imaging logging curve satisfies the cosine distribution, and the period is 2π. Here, assuming that the cosine function equation is y=Acos(αx+θ)+b, the cosine can be obtained by bringing the logging response of the azimuth measurement (the depth of the azimuth gamma imaging data through the interface position) and the corresponding azimuth into the formula The functional unknowns (A, α, θ, and b), in particular the parameter A representing the amplitude of the cosine curve, which is equivalent to the azimuthal gamma imaging data elevation difference. Further, since the cosine amplitude is equivalent to the elevation difference H of the azimuth gamma imaging data, let H=A. When the H value is greater than 0, it means that the low side of the azimuth tool encounters the formation interface first, and the tool passes through the layer interface with an angle less than 90 degrees relative to the normal of the layer interface; when H is less than 0, it means the high side of the azimuth tool The layer interface is encountered first, and the gesture with the included angle between the instrument and the interface normal greater than 90 degrees passes through the layer interface.
接着,(步骤S1203)由于方位伽马成像在井眼地层相对倾角提取时,与曲线探测深度密切相关,因而要根据仪器的探测特性先进行相应的探测深度校正。具体地,基于获取到的当前导眼井井径曲线和方位伽马成像仪器探测深度,获得当前测量点方位伽马成像仪器探测深度,进一步结合上述方位伽马成像数据高程差,利用反正切函数,计算井眼地层界面法线间相对夹角(即井眼地层相对倾角),即从随钻方位伽马成像测井曲线中提取井眼地层相对倾角。其中,当前测量点方位伽马成像仪器探测深度用下列表达式:Next, (step S1203), since the azimuth gamma imaging is closely related to the curve detection depth when extracting the relative dip angle of the borehole formation, the corresponding detection depth correction should be performed first according to the detection characteristics of the instrument. Specifically, based on the obtained caliber curve of the current pilot hole and the detection depth of the azimuth gamma imaging instrument, the detection depth of the azimuth gamma imaging instrument at the current measurement point is obtained, and further combined with the above-mentioned elevation difference of the azimuth gamma imaging data, the arc tangent function is used. , calculate the relative angle between the normals of the borehole formation interface (that is, the relative dip angle of the borehole formation), that is, extract the relative dip angle of the borehole formation from the azimuth-while-drilling gamma imaging logging curve. Among them, the detection depth of the current measurement point azimuth gamma imaging instrument is expressed by the following expression:
Del=DH+2*DOIEFF (11) Del =DH+2*DOI EFF (11)
其中,Del表示探测直径,DH表示导眼井井径;DOIEFF表示仪器探测深度。电直径Del的数值与仪器自身性质相关,并且满足Del>DH的条件。通常情况下,探测深度DOIEFF与真实的井径无关,取决于介质背景值和地层吸收,高伽马地层可能比低伽马地层探测深度大。Among them, D el represents the detection diameter, DH represents the diameter of the pilot hole; DOI EFF represents the detection depth of the instrument. The value of the electrical diameter Del is related to the properties of the instrument itself, and satisfies the condition of Del >DH. Typically, the depth of detection DOI EFF is independent of the true borehole diameter, depending on the medium background value and formation absorption, high-gamma formations may be deeper than low-gamma formations.
最后,通过如下表达式表示从随钻方位伽马成像测井曲线中提取的井眼地层相对倾角的计算式:Finally, the calculation formula of the relative dip angle of the wellbore formation extracted from the azimuth-while-drilling gamma imaging logging curve is expressed by the following expression:
在式(12)中,DIP表示提取的井眼-地层相对倾角。In Equation (12), DIP represents the extracted wellbore-formation relative dip.
在计算地层方位角时,由于方位伽马成像360°测井展开平面满足余弦函数,且周期为2π,因此,根据这一性质利用解析法计算方位伽马成像测井数据的测量值(下列余弦曲线中的x)满足余弦函数初始相位,从而得到地层方位角。具体地,定义此处的余弦曲线的方程为:When calculating the formation azimuth, since the azimuth gamma imaging 360° logging development plane satisfies the cosine function, and the period is 2π, the measured value of the azimuth gamma imaging logging data is calculated by the analytical method according to this property (the following cosine x) in the curve satisfies the initial phase of the cosine function, thereby obtaining the formation azimuth. Specifically, the equation defining the cosine curve here is:
y=A0 cos(ωx-β)+y0 (13)y=A 0 cos(ωx-β)+y 0 (13)
其中,ω表示余弦曲线的周期即展开图的图像宽度,y0表示伽马值的纵坐标偏移量(伽马均值),(n=2或n=4),β为初始相位(地层方位角),yi表示方位伽马成像测井数据的测量值,n表示方位测量个数。至此余弦方程中只有A0与β未知,因此将高边、低边方位测井值带入余弦曲线方程,得:Among them, ω represents the period of the cosine curve, that is, the image width of the expanded graph, y 0 represents the ordinate offset of the gamma value (gamma mean value), (n=2 or n=4), β is the initial phase (formation azimuth), yi represents the measurement value of the azimuth gamma imaging logging data, and n represents the number of azimuth measurements. So far, only A 0 and β are unknown in the cosine equation, so the high-side and low-side azimuth logging values are put into the cosine curve equation, and we get:
求解上面方程组,得到:Solving the above system of equations, we get:
其中,将上述提取出的井眼地层相对倾角代入φ中,进而,求得地层方位角β。Among them, the relative dip angle of the wellbore formation extracted above is substituted into φ, and further, the formation azimuth angle β is obtained.
接下来,针对边界距指示极化值的计算过程进行说明。从实时传输的随钻电磁波电阻率测井曲线中,选择测井质量较高、具有不同探测深度的若干条曲线,借助解析法中的数值仿真算法,合成指示层边界距信号(Peak值信号)。图5是本发明实施例的用于地质导向的钻头调整预测方法的随钻电磁波电阻率曲线合成指示层边界距信号(Peak值信号)响应示意图。如图5所示,横轴表示测量点距层界面距离,纵轴表示边界距指示极化值信号(Peak值信号)的响应,不同的曲线代表不同电阻率对比度下的边界距指示极化值信号。Next, the calculation process of the boundary distance indicating polarization value will be described. From the electromagnetic wave resistivity logging curves transmitted in real time, select several curves with high logging quality and different detection depths, and use the numerical simulation algorithm in the analytical method to synthesize the indicator layer boundary distance signal (Peak value signal) . FIG. 5 is a schematic diagram showing the response of the electromagnetic wave resistivity curve while drilling synthetically indicating layer boundary distance signal (Peak value signal) of the drill bit adjustment prediction method for geosteering according to an embodiment of the present invention. As shown in Figure 5, the horizontal axis represents the distance between the measurement point and the layer interface, the vertical axis represents the response of the boundary distance indicating polarization value signal (Peak value signal), and different curves represent the boundary distance indicating polarization value under different resistivity contrasts Signal.
层边界距信号(Peak值信号)的计算,利用同一地层在直井和斜井两种测井环境下随钻电磁波电阻率测井曲线响应对比下定义极化值大小得到的。边界距指示极化值利用如下表达式计算:The calculation of layer boundary distance signal (peak value signal) is obtained by defining the polarization value by comparing the response of electromagnetic wave resistivity logging curves while drilling in the same formation in vertical well and inclined well logging environment. The boundary distance indicates the polarization value is calculated using the following expression:
其中,Peak表示边界距指示极化值的大小,Ra表示视电阻率,Dip表示上述井眼-地层界面法线相对夹角(DIP),θ表示井眼与地层界面法线相对夹角的某一角度值,Ra|Dip=θ表示井眼与地层界面法线夹角为θ时测量得到的视电阻率(即斜井测井环境下,随钻电磁波电阻率测井曲线响应值),Ra|Dip=0表示井眼与地层界面法线夹角为0时测量得到的视电阻率(即直井测井环境下,随钻电磁波电阻率测井曲线响应值)。Among them, Peak represents the magnitude of the polarization value indicated by the boundary distance, Ra represents the apparent resistivity, Dip represents the above-mentioned relative angle between the borehole and the formation interface normal (DIP), and θ represents a certain relative angle between the borehole and the formation interface normal. An angle value, Ra | Dip=θ represents the apparent resistivity measured when the normal angle between the borehole and the formation interface is θ (that is, the response value of the electromagnetic wave resistivity logging curve while drilling in the deviated well logging environment), Ra | Dip=0 means the apparent resistivity measured when the normal angle between the borehole and the formation interface is 0 (that is, the response value of the electromagnetic wave resistivity logging curve while drilling in the vertical well logging environment).
再次参考图5,可知测量点距离层边界越近,Peak值信号响应幅度越大,根据这一性质,可以求得指示边界距的极化值Peak,从而确定了水平井钻头所在的层位,进一步可以对边界距离进行计算,而后进入到步骤S130中。Referring to Figure 5 again, it can be seen that the closer the measurement point is to the layer boundary, the greater the response amplitude of the Peak value signal. According to this property, the polarization value Peak indicating the boundary distance can be obtained, thereby determining the layer where the horizontal well drill bit is located. Further, the boundary distance may be calculated, and then step S130 is entered.
在步骤S130中,基于上述地质导向模型中的反演结果,结合包括从实测方位伽马成像数据中提取的井眼地层相对倾角、地层方位角以及边界距指示极化值的随钻测量参数,进一步基于边界距指示极化值计算出的测量点到边界距离,结合上述随钻测量参数以及模型正演曲线与实测数据对比匹配情况,将地质导向模型进行实时修正,建立随钻地层初始模型。In step S130, based on the inversion results in the above-mentioned geosteering model, combined with the measurement-while-drilling parameters including the relative dip angle of the wellbore formation, the formation azimuth angle and the boundary distance indicated polarization value extracted from the measured azimuth gamma imaging data, Further, based on the distance from the measurement point to the boundary calculated by the boundary distance indicator polarization value, combined with the above measurement while drilling parameters and the comparison and matching of the model forward curve and the measured data, the geosteering model was corrected in real time, and the initial formation model while drilling was established.
具体地,先根据地质导向模型的反演结果(响应数据),通过邻井间层位对应关系和水平井钻头所在层位(待分析水平井所在的地层层位),进一步,确定建模地层层数、每层电阻率以及层厚在水平方向上的变化。Specifically, first, according to the inversion results (response data) of the geosteering model, through the horizon correspondence between adjacent wells and the horizon where the horizontal well bit is located (the horizon where the horizontal well to be analyzed is located), further, determine the modeling stratigraphy The number of layers, the resistivity of each layer, and the layer thickness change in the horizontal direction.
然后,利用根据实时探测到的随钻方位伽马成像测井曲线中提取的井眼地层相对倾角,将已得到的地质导向模型中的井眼地层相对倾角进行修正。Then, the relative inclination angle of the wellbore formation in the obtained geosteering model is corrected by using the relative inclination angle of the wellbore formation extracted from the real-time azimuth-while-drilling gamma imaging logging curve.
接着,利用实时探测到的随钻电磁波电阻率测井曲线,借助已建立的地质导向模型中的边界距指示极化值和数值模拟算法,定义并合成实测曲线中的边界距指示信号。进一步根据通过随钻电磁波电阻率测井曲线得到的边界距指示极化值(边界距指示信号的幅度大小),计算出测量点到地层边界的距离,基于此,将完成井眼地层相对倾角修正的地质导向模型中的地层层位横向与深度对应关系与当前测量点对应的地层层位进行深度校正,实时更新地质导向模型,从而完成随钻地层初始模型的建立。Then, using the electromagnetic wave resistivity logging curve detected in real time, with the aid of the boundary distance indicating polarization value and numerical simulation algorithm in the established geosteering model, the boundary distance indicating signal in the measured curve is defined and synthesized. Further, according to the boundary distance indicating polarization value (the magnitude of the boundary distance indicating signal) obtained through the electromagnetic wave resistivity logging curve while drilling, the distance from the measurement point to the formation boundary is calculated. Based on this, the relative dip angle correction of the wellbore formation will be completed. The horizontal and depth correspondence between the stratum horizons in the geosteering model and the stratigraphic horizons corresponding to the current measurement points are corrected in depth, and the geosteering model is updated in real time, thereby completing the establishment of the initial stratigraphic model while drilling.
接下来,对步骤S140进行说明。在该步骤中,基于上述随钻地层初始模型的响应结果,根据预设的地质模型反演数据库,通过预先创建的快速查库算法,进一步修正随钻地层初始模型,得到地层真实参数,其中,地层真实参数包括井眼地层相对倾角、测量点到地层边界距离以及地层层厚等。Next, step S140 will be described. In this step, based on the response results of the above-mentioned initial formation model while drilling, according to a preset geological model inversion database, and through a pre-created fast database search algorithm, the initial formation model while drilling is further revised to obtain the real formation parameters, wherein, The real formation parameters include the relative dip angle of the wellbore formation, the distance from the measurement point to the formation boundary, and the formation thickness.
首先,对地质模型反演数据库的构建过程进行详细说明。First, the construction process of the geological model inversion database is described in detail.
由于在随钻作业的水平井环境下,正演仿真计算量大、计算速度慢,制约了随钻电磁波正反演在地质导向中的应用,现有的导向技术仅仅是通过测量值和相关经验定性判断井眼在地层中的位置,钻头的调整依赖较浅探测随钻伽马测井数据,深探测电阻率测井数据仅仅起到了结论验证的功能,没有发挥随钻电磁波电阻率仪器的优势。Due to the large amount of calculation and slow calculation speed of forward modeling in the horizontal well environment while drilling, the application of electromagnetic wave forward and inversion while drilling in geosteering is restricted. The existing steering technology is only based on measured values and relevant experience Qualitatively determine the position of the wellbore in the formation, the adjustment of the drill bit depends on the shallow detection gamma logging while drilling data, and the deep detection resistivity logging data only plays the function of verifying the conclusion, and does not give full play to the advantages of the electromagnetic wave resistivity instrument while drilling .
本发明通过建立分类正演地质仿真模型,开发快速查库反演解决了计算量和计算速度的瓶颈问题,利用深探测功能的随钻电磁波电阻率的测井曲线进行地质导向,可提前预知地层界面的存在,通过反演方法,能够精确计算测量点到层边界距离,实现了地质导向从定性判断到定量计算,从储层导向到油藏导向的转变。The invention solves the bottleneck problem of calculation amount and calculation speed by establishing a classification and forward modeling geological simulation model, and develops rapid database inversion and inversion, and utilizes the logging curve of electromagnetic wave resistivity while drilling with deep detection function for geosteering, which can predict the formation in advance. The existence of the interface, through the inversion method, can accurately calculate the distance from the measurement point to the layer boundary, and realize the transformation of geosteering from qualitative judgment to quantitative calculation, and from reservoir steering to reservoir steering.
在构建地质模型反演数据库的过程中,需要先获取随钻测井作业中待钻水平井所在区域的地层特性参数以及随钻测量仪器参数,以其为背景数据,充分考虑下述随钻地层初始模型中包括井眼地层相对倾角、地层电阻率Rt、上下地层电阻率(RT1、RT2)、井眼-地层相对位置关系等响应结果,建立分类正演地质仿真模型库的索引,并对当前索引结果进行分类,最终形成分类正演地质仿真模型库。In the process of constructing the geological model inversion database, it is necessary to first obtain the formation characteristic parameters of the area where the horizontal well to be drilled in the logging while drilling operation and the parameters of the measurement while drilling instrument, which are used as the background data and fully consider the following formation while drilling. The initial model includes response results such as the relative dip angle of the wellbore formation, formation resistivity Rt, upper and lower formation resistivity (RT1, RT2), and the relative position relationship between the wellbore and formation. The index results are classified, and finally the classification and forward modeling geological simulation model library is formed.
具体地,结合针对性油田区块特征,确定地层模型的参数维度,将多维模型参数在不同维度上变化,设置变化步长,建立地质模型快速反演数据库的索引,其设置过程如下所示。Specifically, combined with the characteristics of the targeted oilfield blocks, the parameter dimensions of the formation model are determined, the multi-dimensional model parameters are changed in different dimensions, the change step is set, and the index of the geological model fast inversion database is established. The setting process is as follows.
针对分类正演地质仿真模型库所应用的区块,收集该区块地质参数,用区块地层参数指导设置分类正演地质仿真模型库。表1为某一区块地层参数的一个具体示例。For the block applied by the classification forward modeling geological simulation model library, collect the geological parameters of the block, and use the block stratigraphic parameters to guide the setting of the classification forward modeling geological simulation model library. Table 1 is a specific example of formation parameters of a certain block.
表1区块地层参数Table 1 Block formation parameters
其中,分类正演地质仿真模型库包含仪器参数如仪器半径7in、线圈半径6.75in、6发2收线圈结构,发射线圈距仪器中点距离分别15in、-15in、25in、-25in、45in、-45in,接收线圈间距6in;钻铤相对磁导率1,钻铤为良导体,仪器工作频率2MHz和500KHz;井眼尺寸6in~17in变化,步长间隔0.5in;泥浆电阻率0.02ohm.m~3ohm.m变化,步长间隔0.01ohm.m;包括地层参数电阻率0.1ohm.m~2000ohm.m变化,步长间隔0.1ohm.m;各向异性系数1~4,间隔0.2;层厚变化0.1m~20m,步长间隔0.2m;边界距变化0m~10m,步长间隔0.1m;相对介电常数变化1~300,步长间隔1。最后,将分类正演地质仿真模型库按照井径-泥浆-层厚-边界距-各向异性系数-介电常数-地层电阻率维度顺序排列,每一维度数据按增序排序。Among them, the classified forward modeling geological simulation model library includes instrument parameters such as instrument radius 7in, coil radius 6.75in, 6 transmitters and 2 receiver coils, and the distances between the transmitter coil and the midpoint of the instrument are 15in, -15in, 25in, -25in, 45in, - 45in, the spacing between the receiving coils is 6in; the relative permeability of the drill collar is 1, the drill collar is a good conductor, the instrument operating frequency is 2MHz and 500KHz; the hole size varies from 6in to 17in, and the step interval is 0.5in; the mud resistivity is 0.02ohm.m~ 3ohm.m change, step interval 0.01ohm.m; including formation parameter resistivity 0.1ohm.m~2000ohm.m change, step interval 0.1ohm.m;
为了准确、快捷构建以及调用地质模型库,需要构建地质模型库索引。构建索引时,按影响因素的先后影响因素进行分类,再在每一类中进行细分。例如,地层模型可以分为单层模型、、两层模型、三层模型等;比如在两层模型这一类中,我们又可以分出子类:各项异性地层为一类,各项同性地层为一类;在各项同性地层中,我们又可以分出子类:垂直井为一类、井斜30度为一类、井斜60度为一类、井斜90度为一类等。In order to construct and call the geological model library accurately and quickly, it is necessary to construct the index of the geological model library. When constructing the index, the factors are classified according to the influencing factors in sequence, and then subdivided in each category. For example, the formation model can be divided into single-layer model, two-layer model, three-layer model, etc.; for example, in the two-layer model, we can divide into sub-categories: anisotropic formation is one type, isotropic Strata is one type; in isotropic formations, we can divide into sub-categories: vertical well is one type, 30 degrees is one type, 60 degrees is one type, 90 degrees is one type, etc. .
接着,基于麦克斯韦方程,利用解析解方法的数值模拟算法(解析解数值模拟算法),对分类正演地质仿真模型库中各类别参数进行数值正演仿真计算,建立模型参数与测井响应对应关系,并且利用测井响应与边界距的关系(即边界距指示极化值与对应的边界距的关系),进一步按照上述分类顺序将计算结果进行保存,得到地层模型-电磁波电阻率曲线-边界距的关系,从而形成地质模型快速反演数据库。Next, based on Maxwell's equations, the numerical simulation algorithm of the analytical solution method (analytical solution numerical simulation algorithm) is used to carry out numerical forward simulation calculation for each type of parameters in the classified forward modeling geological simulation model library, and the corresponding relationship between the model parameters and the logging response is established. , and use the relationship between the logging response and the boundary distance (that is, the relationship between the boundary distance indicating polarization value and the corresponding boundary distance), and further save the calculation results according to the above classification sequence, and obtain the formation model-electromagnetic wave resistivity curve-boundary distance relationship to form a database for rapid inversion of geological models.
其中,解析解方法数值模拟算法包含以下步骤:在仪器发射线圈到接收线圈间距较大,线圈半径较小时,线圈可等价于一个点,因此可以用磁偶极子理论来替代感应线圈。设单位磁偶极子源随时间的变化关系为exp(iωt),其中ω为角频率,并假设在地层直角坐标系中(水平面为xy面)源点的位置坐标为rt=(xt,yt,zt),场点的位置坐标为r=(x,y,z),则方向单位磁偶极子在均匀各向异性介质中产生的Hertz势可用如下表达式表示:Among them, the numerical simulation algorithm of the analytical solution method includes the following steps: when the distance between the transmitter coil and the receiver coil of the instrument is large and the coil radius is small, the coil can be equivalent to a point, so the magnetic dipole theory can be used to replace the induction coil. Let the variation relationship of the unit magnetic dipole source with time be exp(iωt), where ω is the angular frequency, and it is assumed that the position coordinate of the source point in the formation Cartesian coordinate system (the horizontal plane is the xy plane) is r t = (x t , y t , z t ), the position coordinates of the field point are r=(x, y, z), then The Hertz potential generated by a directional unit magnetic dipole in a homogeneous anisotropic medium can be expressed by the following expression:
其中,μb表示均匀介质磁导率,σhb表示均匀各向异性介质的水平复电导率,i为虚数单位,ω为角频率。in, μ b is the magnetic permeability of the homogeneous medium, σ hb is the horizontal complex conductivity of the homogeneous anisotropic medium, i is the imaginary unit, and ω is the angular frequency.
经过转化处理,式(17)可以表示为如下Sommerfeld积分形式:After transformation, equation (17) can be expressed as the following Sommerfeld integral form:
其中,λ表示积分变量,Jv表示v阶Bessel函数,J0表示0阶Bessel函数。方向单位磁偶极子在均匀各向异性介质中产生的Hertz势可用如下表达式表示:where λ represents the integral variable, J v represents the v-order Bessel function, and J 0 represents the 0-order Bessel function. The Hertz potential generated by a directional unit magnetic dipole in a homogeneous anisotropic medium can be expressed by the following expression:
其中,表示各向异性系数,σvb表示垂直电导率、kv 2=-iωμbσvb。经推导式(19)、式(20)可以分别表示如下表达式Sommerfeld积分形式:in, represents anisotropy coefficient, σ vb represents vertical conductivity, k v 2 =-iωμ b σ vb . After deriving equations (19) and (20), the following expressions can be expressed as the Sommerfeld integral form:
其中, in,
由于电磁场与Hertz势之间的关系可用如下表达式表示:Since the relationship between the electromagnetic field and the Hertz potential can be expressed by the following expression:
其中,表示均匀各向异性介质的电导率张量,H表示Hertz势。将式(18)、式(21)、式(22)带入式(23),可以得到沿三个方向单位磁偶极子产生的电场和磁场各分量的解析式及Sommerfeld积分形式,其中电场和磁场z分量的Sommerfeld积分形式分别用如下表达式表示:in, represents the conductivity tensor of a homogeneous anisotropic medium, and H represents the Hertz potential. Substituting formula (18), formula (21), and formula (22) into formula (23), we can get along Analytical expressions and Sommerfeld integral forms of the electric and magnetic field components generated by unit magnetic dipoles in three directions, in which the Sommerfeld integral forms of the z-components of the electric field and magnetic field are expressed by the following expressions:
Ez (3)(r,rt)=0 (26)E z (3) (r, r t )=0 (26)
其中,Ez (1)、Ez (2)、Ez (3)分别表示沿三个方向单位磁偶极子在z方向上电场分量,Hz (1)、Hz (2)、Hz (3)分别表示沿三个方向单位磁偶极子在z方向上磁场分量,上述各分量均被表示成了波模积分的形式。例如:Among them, E z (1) , E z (2) , and E z (3) represent edge The electric field components of the unit magnetic dipole in the three directions in the z direction, Hz (1) , Hz (2) , Hz (3) represent the direction along the The magnetic field components of the unit magnetic dipoles in the three directions in the z-direction are expressed in the form of wave mode integrals. E.g:
其中,表示某一积分变量λ对应的波模,λ表示积分变量。in, represents the wave mode corresponding to an integral variable λ, and λ represents the integral variable.
根据Maxwell方程组,电场和磁场波模的切向分量与纵向分量之间的关系可利用如下表达式表示:According to Maxwell's equations, the relationship between the tangential and longitudinal components of the electric and magnetic modes can be expressed by the following expressions:
其中,分别表示磁场在x、y、z方向上的分量,分别表示电场在x、y、z方向上的分量,εh表示水平介电常数、μ表示磁导率,将式(24)~式(29)中对应的变量代入式(30)~式(31)即可分别计算得到电场和磁场x、y分量。而后,根据接收线圈处的电场强度或磁场强度计算得到接收线圈处的感应电动势,进而计算得到两个接收线圈之间的相位差和幅度比值,再经过电阻率转换即可得到相位差电阻率与幅度比电阻率,从而形成了地层模型-电磁波电阻率曲线数值-仪器类型关系库。进一步根据边界距指示极化值与对应的边界距的关系,按照上述分类顺序结果进行保存,便可得到地层模型-电磁波电阻率曲线-边界距的关系库,以完成地质模型快速反演数据库的构建。in, represent the components of the magnetic field in the x, y, and z directions, respectively, respectively represent the components of the electric field in the x, y, and z directions, ε h represents the horizontal permittivity, and μ represents the magnetic permeability. Substitute the corresponding variables in equations (24) to (29) into equations (30) to ( 31) The x and y components of the electric field and the magnetic field can be calculated separately. Then, the induced electromotive force at the receiving coil is calculated according to the electric field strength or magnetic field strength at the receiving coil, and then the phase difference and amplitude ratio between the two receiving coils are calculated, and then the phase difference resistivity and Amplitude specific resistivity, thus forming formation model-electromagnetic wave resistivity curve numerical-instrument type relation library. Further, according to the relationship between the polarization value and the corresponding boundary distance indicated by the boundary distance, and the results of the above classification sequence are stored, the relationship library of stratigraphic model-electromagnetic wave resistivity curve-boundary distance can be obtained to complete the rapid inversion database of geological model. Construct.
其中,地质模型反演数据库具备以模拟出不同测量仪器环境不同地层电阻率等环境下所对应的边界距参数及井眼地层相对倾角,在反演过程中,需要获得相应的真实的随钻作业环境的地层特性参数以及仪器参数,便可得到相应的电磁波电阻率曲线,从而得到包括井眼地层相对倾角、测量点到地层边界距离以及层厚等信息在内的真实的地层参数,进一步实现了快速的反演过程,解决了随钻导向作业中计算量大、计算速度慢的问题,达到了高速高效的目的。Among them, the geological model inversion database is equipped to simulate the boundary distance parameters and the relative dip angle of the wellbore formation under different environments such as different measuring instruments and different formation resistivities. During the inversion process, it is necessary to obtain the corresponding real operation while drilling. The corresponding electromagnetic wave resistivity curve can be obtained according to the formation characteristic parameters of the environment and the instrument parameters, so as to obtain the real formation parameters including the relative dip angle of the wellbore formation, the distance from the measurement point to the formation boundary and the layer thickness, etc. The fast inversion process solves the problems of large amount of calculation and slow calculation speed in the steerable while drilling operation, and achieves the purpose of high speed and high efficiency.
具体地,以随钻地层初始模型为初始值,利用梯度下降法,构建目标函数,对比随钻地层初始模型的测井响应结果与实测数据,计算该测井响应与实测数据的残差,确定下降方向及相应的下降步长,即可计算出初步修正后的随钻地层初始模型对应的模型修正量,即初步修正后的随钻地层初始模型。Specifically, taking the initial formation model while drilling as the initial value, the gradient descent method is used to construct the objective function, the logging response results of the initial formation while drilling model are compared with the measured data, and the residual between the logging response and the measured data is calculated to determine According to the descending direction and the corresponding descending step length, the model correction amount corresponding to the preliminary corrected initial stratum model while drilling can be calculated, that is, the preliminary corrected initial stratum while drilling model.
基于上述以构建完成的地质模型反演数据库,通过快速查库法,查找初步修正后的随钻地层初始模型的测井响应的数值,对比初步修正后的随钻地层初始模型的数值(测井响应)与实时测量的数据,以得到新的初始模型(二次修正后的随钻地层初始模型),进一步将新的初始模型(二次修正后的随钻地层初始模型)的构建结果作为本次反演结果,从而获取到深层的真实地层数据,用以进行深层地层导向作业的数据基础。Based on the above-mentioned geological model inversion database, the value of the logging response of the initial corrected formation while drilling model was found by the quick database search method, and the values of the initial corrected initial formation while drilling model were compared (logging response) and real-time measurement data to obtain a new initial model (initial stratum-while-drilling model after secondary correction), and further use the construction result of the new initial model (initial stratum-while-drilling model after secondary correction) as this The second inversion results are used to obtain the deep real formation data, which is used as the data basis for deep formation steering operations.
具体地,快速查库方法包含如下几个步骤:第一,根据随钻地层初始模型的初值模型参数值,按照正演仿真库索引次序进行查找,得到修正后的初始模型对应的测井响应;第二,根据测井响应与实测数据的测井响应对比,建立如下最小二乘目标函数;通过梯度下降方法求解目标函数雅可比矩阵,形成雅可比线性方程组,求解方程组计算目标函数最速下降方向;第三,求解目标函数,在最速下降方向上确定步长,进一步根据求得快速反演初始模型改变方向和改变步长,确定该模型的改变量,改变模型,完成一次模型更新;通过设置循环终止条件,循环调用模型更新过程,直至满足循环终止条件,从而构建新的初始模型,完成快速查库反演处理,得到相应的真实地层参数,进入步骤S150。其中,地层真实参数至少包括地层层位划分数据、地层电阻率、地层自然伽马等,地层层位划分数据包含:地层电阻率值、(仪器)测量点到层边界的距离以及地层层厚等。Specifically, the quick database search method includes the following steps: First, according to the initial value model parameter values of the initial model of the formation while drilling, search is performed according to the index order of the forward modeling simulation library, and the logging response corresponding to the corrected initial model is obtained. ; Second, according to the comparison between the logging response and the logging response of the measured data, the following least squares objective function is established; the Jacobian matrix of the objective function is solved by the gradient descent method, and the Jacobian linear equation system is formed, and the objective function is the fastest by solving the equation system. Descending direction; third, solve the objective function, determine the step size in the direction of the fastest descent, and further change the direction and step size according to the obtained fast inversion initial model, determine the change amount of the model, change the model, and complete a model update; By setting the loop termination condition, the model update process is called cyclically until the loop termination condition is met, so as to construct a new initial model, complete the fast database search and inversion processing, and obtain the corresponding real formation parameters, and go to step S150. Among them, the real parameters of the formation include at least formation horizon division data, formation resistivity, formation natural gamma, etc. The formation horizon division data includes: formation resistivity value, distance from (instrument) measurement point to layer boundary, and formation layer thickness, etc. .
在步骤S150中,根据通过快速查库法得到的包括井眼地层相对倾角、地层电阻率值、地层层界面位置及层厚在水平位移方向上变化的地层真实参数,对未钻遇地层进行层界面位置预测,进一步对未钻遇地层进行等倾角顺延,预测层界面在沿待钻水平井井轴方向上的变化,计算钻头在目标层内调整的安全距离,用以指导地质导向作业,尤其是钻头的调整。In step S150, according to the real stratum parameters obtained by the quick library search method, including the relative dip angle of the wellbore stratum, the stratum resistivity value, the position of the stratum layer interface and the change of the layer thickness in the horizontal displacement direction, the stratum is not encountered in the stratum. Interface position prediction, further carry out equal dip extension of the undrilled strata, predict the change of the layer interface along the well axis of the horizontal well to be drilled, and calculate the safety distance of the drill bit in the target layer to guide the geosteering operation, especially It is the adjustment of the drill bit.
钻头调整的具体实施过程包含如下步骤:The specific implementation process of drill bit adjustment includes the following steps:
第一(步骤S1501),根据反演得到的地层真实参数中的井眼地层相对倾角,以及实时获取的钻头井斜角测量值,计算地层视倾角,确定钻头方向,并利用如下表达式计算:First (step S1501), according to the relative inclination of the wellbore formation in the real formation parameters obtained by inversion, and the measured value of the inclination angle of the drill bit obtained in real time, calculate the apparent inclination of the formation, determine the direction of the drill bit, and use the following expression to calculate:
γ=φ-α (34)γ=φ-α (34)
其中:γ表示地层视倾角,φ表示反演后得到的井眼地层相对倾角,α表示井斜角。需要说明的是,当γ>0时,地层为下倾地层;当γ<0时,地层为上倾地层。当地层上倾时,为保证钻头在地层合适的位置穿行,需向上调整转头,同样,当地层下倾时,要向下调整钻头以保证钻头不从顶部出层,其中,最优调整角度需按照γ值确定。Among them: γ represents the apparent dip angle of the formation, φ represents the relative dip angle of the wellbore formation obtained after inversion, and α represents the well inclination angle. It should be noted that when γ>0, the stratum is a downdip stratum; when γ<0, the stratum is an updip stratum. When the formation is up-dipping, in order to ensure that the drill bit travels through the proper position of the formation, the rotor needs to be adjusted upward. Similarly, when the formation is down-dipping, the drill bit should be adjusted downward to ensure that the bit does not come out from the top of the formation. Among them, the optimal adjustment angle It needs to be determined according to the γ value.
第二(步骤S1502)根据地层视倾角以及反演出的包括地层电阻率值、地层真倾角γ、地层厚度H的地层真实参数,顺延地层,预测探测范围外的地层电阻率Rt、上下地层电阻率(RT1、RT2)以及地层层厚在水平方向(井轴方向)上的变化,绘制地层二维剖面图。Second (step S1502 ), according to the apparent dip angle of the formation and the inversion real formation parameters including formation resistivity value, formation true dip angle γ, and formation thickness H, follow the formation to predict formation resistivity Rt, upper and lower formation resistivity outside the detection range (RT 1 , RT 2 ) and the variation of the formation thickness in the horizontal direction (well axis direction), draw a two-dimensional cross-sectional view of the formation.
第三(步骤S1503),根据所述地层二维剖面图、钻头距测量点的距离以及钻头方向,对未钻遇地层进行等倾角顺延的层界面位置预测,进一步计算钻头钻出目标层的距离。Third (step S1503), according to the two-dimensional cross-sectional view of the stratum, the distance between the drill bit and the measurement point and the direction of the drill bit, predict the position of the layer interface with an iso-inclined extension on the stratum that has not been drilled, and further calculate the distance that the drill bit drills out of the target layer .
图6a是本发明实施例的用于地质导向的钻头调整预测方法的中当钻头井斜角度小于90°情况下,地质导向中钻头位置确定及钻头距地层界面距离的情景示意图。如图6a所示,这种情况下需要利用地层真实参数中的井眼地层相对倾角以及测量点到地层边界距离,计算钻头与地层上界面距离,从而得到钻头与地层下界面距离,用于确定钻头在目标层内的位置,然后,根据钻头与地层下界面距离,预测出钻头钻出地层下界面的距离,并将其作为钻头调整的安全距离。6a is a schematic diagram of the location of the bit and the distance between the bit and the formation interface in geosteering when the inclination angle of the bit is less than 90° in the method for predicting bit adjustment for geosteering according to an embodiment of the present invention. As shown in Figure 6a, in this case, it is necessary to use the relative dip angle of the wellbore formation in the real formation parameters and the distance from the measurement point to the formation boundary to calculate the distance between the drill bit and the upper boundary of the formation, so as to obtain the distance between the drill bit and the lower boundary of the formation, which is used to determine The position of the drill bit in the target layer, and then, according to the distance between the drill bit and the lower interface of the formation, predict the distance that the drill bit drills out of the lower interface of the formation, and use it as the safety distance for the drill bit to adjust.
首先,利用井眼地层相对倾角,仪器测量点距地层边界面距离(此处为上边界)、仪器测量点到钻头距离,可利用如下表达式计算钻头与地层上界面距离、钻头与地层下界面距离(如图6a所示):First, using the relative dip angle of the wellbore formation, the distance between the tool measurement point and the formation boundary (here is the upper boundary), and the distance between the tool measurement point and the bit, the following expressions can be used to calculate the distance between the bit and the upper boundary of the formation, and the distance between the bit and the lower boundary of the formation Distance (as shown in Figure 6a):
DTBBit-u=DTB+L*sinφ (35)DTB Bit-u = DTB+L*sinφ (35)
其中,DTBBit-u表示钻头与地层上界面距离,DTB表示测量点到地层边界距离,L表示钻头距仪器测量点的距离,φ表示井眼地层相对倾角。Among them, DTB Bit-u represents the distance between the drill bit and the upper boundary of the formation, DTB represents the distance from the measurement point to the formation boundary, L represents the distance between the drill bit and the measurement point of the tool, and φ represents the relative dip angle of the wellbore formation.
进一步的,利用如下表达式表示钻头与地层下界面距离:Further, the following expression is used to express the distance between the drill bit and the lower interface of the formation:
DTBBit-d=H-DTBBit-u (36)DTB Bit-d = H-DTB Bit-u (36)
其中,DTBBit-d表示钻头与地层下界面距离,H表示真实地层参数中的地层层厚。当DTBBit-d>0,则表示钻头尚在目标层中,当DTBBit-d小于0时则表示钻头已钻入下部地层。Among them, DTB Bit-d represents the distance between the drill bit and the lower interface of the formation, and H represents the thickness of the formation in the real formation parameters. When DTB Bit-d > 0, it means that the drill bit is still in the target layer, and when DTB Bit-d is less than 0, it means that the drill bit has drilled into the lower formation.
最后,依据上述得到的钻头距下界面距离,井眼地层相对倾角,可利用如下表达式预测钻头钻出地层下界面的距离:Finally, according to the obtained distance between the bit and the lower interface and the relative dip angle of the wellbore formation, the following expression can be used to predict the distance that the bit drills out of the lower interface of the formation:
S=DTBBit-d*tanφ (37)S=DTB Bit-d *tanφ(37)
式中,S表示钻头钻出地层下界面的距离。此时,钻井工程师应根据井眼地层相对倾角、钻头钻出地层下界面的距离等信息进行提前预警,并根据钻井参数进行风险评估,确保钻头不钻出目标层。In the formula, S represents the distance that the drill bit drills out of the lower boundary of the formation. At this time, the drilling engineer should give advance warning based on the relative dip angle of the wellbore formation and the distance the drill bit drills out of the lower boundary of the formation, and conduct risk assessment based on the drilling parameters to ensure that the drill bit does not drill out of the target layer.
图6b是本发明实施例的用于地质导向的钻头调整预测方法的中当钻头井斜角度大于90°情况下,地质导向中钻头位置确定及钻头距地层界面距离的情景示意图。如图6b所示,这种情况下需要利用地层真实参数中的井眼地层相对倾角以及测量点到地层边界距离,计算钻头与地层下界面距离,从而得到钻头与地层上界面距离,用于确定钻头在目标层内的位置。然后,根据钻头与地层上界面距离,预测出钻头钻出地层上界面的距离,将其作为钻头调整的安全距离。6b is a schematic diagram of the location of the bit and the distance between the bit and the formation interface in geosteering when the inclination angle of the bit is greater than 90° in the method for predicting bit adjustment for geosteering according to an embodiment of the present invention. As shown in Figure 6b, in this case, it is necessary to use the relative dip angle of the wellbore formation in the real formation parameters and the distance from the measurement point to the formation boundary to calculate the distance between the bit and the lower boundary of the formation, so as to obtain the distance between the bit and the upper boundary of the formation, which is used to determine The position of the drill bit within the target layer. Then, according to the distance between the drill bit and the upper interface of the formation, predict the distance that the bit drills out of the upper interface of the formation, and use it as the safety distance for the adjustment of the drill bit.
首先,利用井眼地层相对倾角,仪器测量点距地层界面距离(此处为下边界)、仪器测量点到钻头距离,可利用如下表达式计算钻头距下界面距离DTBBit-d、上界面距离DTBBit-u(如图6a所示):First, using the relative dip angle of the wellbore formation, the distance between the tool measurement point and the formation interface (here is the lower boundary), and the distance between the tool measurement point and the drill bit, the following expressions can be used to calculate the distance between the drill bit and the lower interface DTB Bit-d and the distance from the upper interface DTB Bit-u (as shown in Figure 6a):
DTBBit-d=DTB+L*sinφ (38)DTB Bit-d = DTB+L*sinφ (38)
其中,DTBBit-d表示钻头与地层下界面距离,DTB表示测量点到地层边界距离,L表示钻头距仪器测量点的距离,φ表示井眼地层相对倾角。Among them, DTB Bit-d represents the distance between the drill bit and the lower boundary of the formation, DTB represents the distance from the measurement point to the formation boundary, L represents the distance between the drill bit and the measurement point of the tool, and φ represents the relative dip angle of the wellbore formation.
进一步的,利用如下表达式表示钻头与地层上界面距离:Further, the following expression is used to express the distance between the drill bit and the upper interface of the formation:
DTBBit-u=H-DTBBit-d (39)DTB Bit-u = H-DTB Bit-d (39)
其中,DTBBit-u表示钻头与地层上界面距离,H表示真实地层参数中的地层层厚。当DTBBit-u>0,则表示钻头尚在目标层中,当DTBBit-u小于0时则表示钻头已钻入下部地层。Among them, DTB Bit-u represents the distance between the drill bit and the upper interface of the formation, and H represents the thickness of the formation in the real formation parameters. When DTB Bit-u >0, it means that the drill bit is still in the target layer, and when DTB Bit-u is less than 0, it means that the drill bit has drilled into the lower formation.
最后,依据上述得到的钻头距上界面距离,井眼地层相对倾角,可利用如下表达式预测钻头钻出地层上界面的距离:Finally, according to the distance between the bit and the upper interface obtained above and the relative dip angle of the wellbore formation, the following expression can be used to predict the distance that the bit drills out of the upper boundary of the formation:
S=DTBBit-u*tanφ (40)S=DTB Bit-u *tanφ (40)
式中,S表示钻头钻出地层上界面的距离。此时,钻井工程师应根据井眼地层相对倾角、钻头钻出地层上界面的距离等信息进行提前预警,并根据钻井参数进行风险评估,确保钻头不钻出目标层。In the formula, S represents the distance that the drill bit drills out of the upper boundary of the formation. At this time, the drilling engineer should give early warning based on the relative dip angle of the wellbore formation and the distance the drill bit drills out of the upper boundary of the formation, etc., and conduct risk assessment according to the drilling parameters to ensure that the drill bit does not drill out of the target layer.
图7是本发明实施例的用于地质导向的钻头调整预测方法的地质导向实时反演剖面图(地层二维剖面图)。如图7所示,图中自下向上第一道为地质模型二维剖面道;第二道为测量点的深度道;第三道为相位差电阻率道;第四道为幅度比电阻率道;第五道为地层边界指示信号道;第六道为方位伽马成像道。7 is a geosteering real-time inversion cross-sectional view (a two-dimensional cross-sectional view of the formation) of the drill bit adjustment prediction method for geosteering according to an embodiment of the present invention. As shown in Figure 7, the first track from bottom to top is the two-dimensional profile track of the geological model; the second track is the depth track of the measurement point; the third track is the phase difference resistivity track; the fourth track is the amplitude specific resistivity track The fifth track is the formation boundary indicator signal track; the sixth track is the azimuth gamma imaging track.
本发明联合水平井中随钻方位伽马成像测井数据和随钻电磁波电阻率测井数据进行地质导向,先通过对邻井和/或导眼井数据的反演,获得初始地层测井参数和地层层位,其次,利用方位伽马成像数据计算地层倾角,并且利用随钻电磁波电阻率曲线提取边界距指示信号计算地层边界距,实时更新地层初始模型。在更新后的地层模型上,利用解析法数值仿真算法建立快速反演库,结合梯度下降方法进行实测数据的快速反演,获得地层真实电阻率、相对倾角、边界距等参数。进一步,通过井眼轨迹数据,计算地层视倾角,预测钻头距边界距离,并计算钻头调整安全距离,指导地质导向钻头调整。本发明能从实测数据中获得地层倾角、层界面位置和仪器与层界面相对关系,继而能够计算地质导向中钻头调整安全距离,是生产中迫切需要的一种数据处理技术,同时本发明充分发挥各类测井数据的探测优势,优势互补,综合利用,提高测井数据利用效率,在不增加测井项目的情况下,能够从已有数据中挖掘更多、更丰富地层信息。The invention combines the azimuth-while-drilling gamma imaging logging data and the electromagnetic wave resistivity logging data while drilling to perform geosteering, and firstly obtains initial formation logging parameters and/or logging parameters by inverting the data of offset wells and/or pilot wells. Second, use the azimuth gamma imaging data to calculate the formation dip, and use the electromagnetic wave resistivity curve while drilling to extract the boundary distance indicator signal to calculate the formation boundary distance, and update the initial formation model in real time. On the updated stratigraphic model, a fast inversion library is established by using the analytical numerical simulation algorithm, and the measured data is quickly inverted with the gradient descent method to obtain parameters such as the real resistivity, relative dip angle, and boundary distance of the formation. Further, through the wellbore trajectory data, the apparent dip angle of the formation is calculated, the distance between the bit and the boundary is predicted, and the safety distance for bit adjustment is calculated to guide the adjustment of the geosteering bit. The invention can obtain the formation dip, the position of the layer interface and the relative relationship between the instrument and the layer interface from the measured data, and then can calculate the safety distance of the drill bit adjustment in the geosteering, which is a data processing technology urgently needed in production. The detection advantages of various logging data, complementary advantages, comprehensive utilization, improve the efficiency of logging data utilization, and can mine more and richer formation information from existing data without adding logging projects.
以上所述,仅为本发明较佳的具体实施方式,但本发明的保护范围并不局限于此,任何熟悉该技术的人员在本发明所揭露的技术范围内,可轻易想到的变化或替换,都应涵盖在本发明的保护范围之内。因此,本发明的保护范围应该以权利要求的保护范围为准。The above is only a preferred embodiment of the present invention, but the protection scope of the present invention is not limited to this. Any person familiar with the technology can easily think of changes or substitutions within the technical scope disclosed by the present invention. , all should be covered within the protection scope of the present invention. Therefore, the protection scope of the present invention should be subject to the protection scope of the claims.
Claims (10)
Priority Applications (1)
Application Number | Priority Date | Filing Date | Title |
---|---|---|---|
CN201810635374.9A CN110685600B (en) | 2018-06-20 | 2018-06-20 | A Bit Adjustment Prediction Method for Geosteering |
Applications Claiming Priority (1)
Application Number | Priority Date | Filing Date | Title |
---|---|---|---|
CN201810635374.9A CN110685600B (en) | 2018-06-20 | 2018-06-20 | A Bit Adjustment Prediction Method for Geosteering |
Publications (2)
Publication Number | Publication Date |
---|---|
CN110685600A CN110685600A (en) | 2020-01-14 |
CN110685600B true CN110685600B (en) | 2021-01-19 |
Family
ID=69106248
Family Applications (1)
Application Number | Title | Priority Date | Filing Date |
---|---|---|---|
CN201810635374.9A Active CN110685600B (en) | 2018-06-20 | 2018-06-20 | A Bit Adjustment Prediction Method for Geosteering |
Country Status (1)
Country | Link |
---|---|
CN (1) | CN110685600B (en) |
Families Citing this family (21)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
CN113803061B (en) * | 2020-06-01 | 2024-09-24 | 中国石油化工集团有限公司 | Encoding method and device for azimuth electromagnetic wave boundary detection signal while drilling |
CN111784832B (en) * | 2020-06-22 | 2024-01-09 | 长江大学 | Stratum dynamic correction method of geological model |
CN113882853B (en) * | 2020-07-03 | 2024-06-04 | 中国石油化工股份有限公司 | Method for transmitting near-bit logging while drilling data |
CN111985081B (en) * | 2020-07-15 | 2023-08-01 | 北京金阳普泰石油技术股份有限公司 | Logging curve construction method, system, equipment and readable storage medium |
CN113738345B (en) * | 2020-11-25 | 2024-05-28 | 中国石油天然气集团有限公司 | Method for judging drilling situation based on conventional while-drilling tool |
CN112502613B (en) * | 2020-11-27 | 2022-01-07 | 中国科学院地质与地球物理研究所 | A drilling method and device |
CN113130018B (en) * | 2021-04-20 | 2023-05-12 | 东北石油大学 | Lithology recognition method based on reservoir meta-target invariant feature description |
CN112983385B (en) * | 2021-05-12 | 2021-08-10 | 中煤科工集团西安研究院有限公司 | Broken soft low-permeability coal seam roof or bottom plate segmented fracturing horizontal well coal seam gas extraction method |
CN115898384B (en) * | 2021-08-11 | 2025-03-21 | 中国石油天然气股份有限公司 | Method for establishing logging while drilling model for horizontal wells in edge-bottom water reservoirs |
CN115929282A (en) * | 2021-09-22 | 2023-04-07 | 中国石油化工股份有限公司 | Logging system and method based on orientation while drilling gamma and ultrasonic imaging |
CN116136167A (en) * | 2021-11-17 | 2023-05-19 | 中国石油天然气集团有限公司 | Real-time Quantitative Method for Horizontal Well Geosteering Calculation Boundary Distance |
CN114526055A (en) * | 2022-02-21 | 2022-05-24 | 西安石油大学 | Attitude measurement system and test method based on virtual instrument |
CN114991762B (en) * | 2022-06-17 | 2025-03-11 | 中国石油大学(北京) | Autonomous boundary detection and guidance method and device for underground machine based on while drilling data |
CN115162958B (en) * | 2022-07-08 | 2023-08-08 | 安徽省皖北煤电集团有限责任公司 | Directional drilling control method and system |
CN115434688B (en) * | 2022-08-16 | 2024-01-30 | 成都捷科思石油天然气技术发展有限公司 | Drilling curve control method for logging while drilling of horizontal well |
CN115749724B (en) * | 2022-11-15 | 2024-09-10 | 核工业北京化工冶金研究院 | Drilling control method |
CN115576028B (en) * | 2022-12-01 | 2023-03-14 | 武汉盛华伟业科技股份有限公司 | Geological feature layer prediction method and system based on support vector machine |
CN116398126B (en) * | 2023-06-07 | 2023-08-25 | 山东万洋石油科技有限公司 | Data processing method of small diameter while drilling resistivity based on casing window horizontal well |
CN117094232B (en) * | 2023-10-19 | 2023-12-15 | 中国科学院地质与地球物理研究所 | Method and system for updating deep oil gas accurate navigation three-dimensional lithology model in real time |
CN118132897B (en) * | 2024-05-07 | 2024-07-16 | 中国石油大学(华东) | A fast calculation method for array resistivity logging response based on numerical geometry factor |
CN118361229B (en) * | 2024-05-20 | 2025-02-25 | 伟卓石油科技(北京)有限公司 | A dynamic monitoring method, device, system and storage medium for wellbore trajectory |
Citations (6)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
CN103573250A (en) * | 2013-07-22 | 2014-02-12 | 中国石油天然气股份有限公司 | Method for calculating distance from horizontal well hole to upper and lower interfaces of stratum |
CN105938503A (en) * | 2016-03-24 | 2016-09-14 | 杭州迅美科技有限公司 | Multi-layer interface recognition method of direction signals |
WO2017161230A1 (en) * | 2016-03-18 | 2017-09-21 | Baker Hughes Incorporated | Determining the robustness of discrete fracture network permeability estimates |
CN107861917A (en) * | 2017-11-29 | 2018-03-30 | 中国石油集团长城钻探工程有限公司 | Method of the multivariate data combined calculation well to stratigraphic boundary distance in horizontal well |
CN108073765A (en) * | 2017-12-11 | 2018-05-25 | 中海石油(中国)有限公司湛江分公司 | A kind of horizontal well routine well logging bed boundary identification is with border away from inversion method |
CN108240213A (en) * | 2016-12-24 | 2018-07-03 | 中石化石油工程技术服务有限公司 | The geosteering device and geosteering method of a kind of more investigation depths |
-
2018
- 2018-06-20 CN CN201810635374.9A patent/CN110685600B/en active Active
Patent Citations (6)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
CN103573250A (en) * | 2013-07-22 | 2014-02-12 | 中国石油天然气股份有限公司 | Method for calculating distance from horizontal well hole to upper and lower interfaces of stratum |
WO2017161230A1 (en) * | 2016-03-18 | 2017-09-21 | Baker Hughes Incorporated | Determining the robustness of discrete fracture network permeability estimates |
CN105938503A (en) * | 2016-03-24 | 2016-09-14 | 杭州迅美科技有限公司 | Multi-layer interface recognition method of direction signals |
CN108240213A (en) * | 2016-12-24 | 2018-07-03 | 中石化石油工程技术服务有限公司 | The geosteering device and geosteering method of a kind of more investigation depths |
CN107861917A (en) * | 2017-11-29 | 2018-03-30 | 中国石油集团长城钻探工程有限公司 | Method of the multivariate data combined calculation well to stratigraphic boundary distance in horizontal well |
CN108073765A (en) * | 2017-12-11 | 2018-05-25 | 中海石油(中国)有限公司湛江分公司 | A kind of horizontal well routine well logging bed boundary identification is with border away from inversion method |
Also Published As
Publication number | Publication date |
---|---|
CN110685600A (en) | 2020-01-14 |
Similar Documents
Publication | Publication Date | Title |
---|---|---|
CN110685600B (en) | A Bit Adjustment Prediction Method for Geosteering | |
US10451765B2 (en) | Post-well reservoir characterization using image-constrained inversion | |
CN106324689B (en) | Resistivity anisotropy recognition methods under a kind of horizontal well ground environment | |
US8364404B2 (en) | System and method for displaying data associated with subsurface reservoirs | |
CN103046868B (en) | Integrated geosteering method for horizontal well | |
CN108073765A (en) | A kind of horizontal well routine well logging bed boundary identification is with border away from inversion method | |
CN108875122B (en) | Artificial intelligence method and system for calculating geological parameters by using logging-while-drilling data | |
EP3410160A1 (en) | Method for real-time downhole processing and detection of bed boundary for geosteering application | |
US10295697B2 (en) | Determination of true formation resistivity | |
WO2018132705A1 (en) | Measuring petrophysical properties of an earth formation by regularized direct inversion of electromagnetic signals | |
NO338483B1 (en) | Method and system for geo-management during drilling in a foundation formation | |
NO320904B1 (en) | Method for Determining the Distance Between an Electromagnetic Source Logging Instrument and Multiple Formation Layer Limits in Inversion Processing of Painting Data | |
EA007587B1 (en) | Directional electromagnetic wave resistivity apparatus and method | |
US11727583B2 (en) | Core-level high resolution petrophysical characterization method | |
CN105938503B (en) | A kind of direction signal multilayer interface identification method | |
CN110073246B (en) | Improved method relating to quality control | |
RU2326414C1 (en) | Method of multi-component inductive logging device while performing drilling parameters control and while interpreting measurement results of specific electric resistance in horisontal boreholes | |
CN110513105A (en) | A kind of cubical array induction logging instrument data processing system and method | |
US12146403B2 (en) | Borehole localization relative to objects and subterranean formations | |
CN107944159A (en) | One kind is with brill electromagnetic wave forward modeling simulation data base high accuracy compression method | |
CN108019207A (en) | A kind of measuring method of SYMMETRIC ELECTROMAGNETIC ripple resistivity | |
CN112528106A (en) | Volcanic lithology identification method | |
US12091964B2 (en) | Borehole localization relative to objects and subterranrean formations | |
CN102635348B (en) | Method for correcting dual-frequency dielectric constants of EWR (electromagnetic wave resistivity) logging-while-drilling instrument | |
US6795774B2 (en) | Method for asymptotic dipping correction |
Legal Events
Date | Code | Title | Description |
---|---|---|---|
PB01 | Publication | ||
PB01 | Publication | ||
SE01 | Entry into force of request for substantive examination | ||
SE01 | Entry into force of request for substantive examination | ||
GR01 | Patent grant | ||
GR01 | Patent grant |