CN118407753B - Logging component extraction method of logging while drilling instrument and electric anisotropy identification application - Google Patents
Logging component extraction method of logging while drilling instrument and electric anisotropy identification application Download PDFInfo
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Abstract
Description
技术领域Technical Field
本发明涉及随钻测井技术领域,尤其涉及一种随钻测井仪器的测井分量提取方法和电各向异性识别应用。The invention relates to the technical field of logging while drilling, and in particular to a logging component extraction method and electrical anisotropy identification application of a logging while drilling instrument.
背景技术Background Art
根据统计,世界存在三成的油气存储与砂泥岩交互层中,这种储层可等效为宏观的单轴各向异性地层,因此,地层电阻率各向异性(以下统称为电各向异性)测量作为评价层状储层潜力的重要因素,探测与识别该类地层对与油气开发由重要的现实需要。According to statistics, 30% of the world's oil and gas storage is in alternating layers of sandstone and mudstone. This type of reservoir can be equivalent to a macroscopic uniaxial anisotropic formation. Therefore, the measurement of formation resistivity anisotropy (hereinafter referred to as electrical anisotropy) is an important factor in evaluating the potential of layered reservoirs. The detection and identification of this type of formation is of great practical need for oil and gas development.
随钻电磁波电阻率测井也经历了三个发展阶段:第一阶段,由于测井仪器采用轴向发射轴向接收天线系结构,仅能通过测量信号获取地层电阻率;第二阶段,仪器引入了横向或倾斜发射接收天线,通过构建和或分量组成的信号,能够在获取地层电阻率和临近界面信息在测量地层电阻率的同时,还可以探测临近的地层界面;正在发展中的第三阶段(现阶段),仪器采用多方向发射接收天线结构,在理论上可以获取、、、、、、、、全部3方向上的9个分量,即三维全息,在完成获取地层电阻率、界面信息的测井任务基础上,还能够获得含电阻率各向异性信息的各类交叉分量。而在井下工作中,仪器的传输带宽仍然极其有限(4-8bits) ,为了在随钻中实时主动指导钻头的导向,要求仪器通过最少的传输信号获得更全面的井下地层信息,因此测井分量的全部提取,与对应功能信号的构建成为了痛点问题。The electromagnetic wave resistivity logging while drilling has also gone through three stages of development: In the first stage, due to the axial transmission and axial receiving antenna structure of the logging instrument, it can only measure Signal acquisition of formation resistivity; in the second stage, the instrument introduced a horizontal or inclined transmitting and receiving antenna, and constructed and or The signal composed of components can obtain the formation resistivity and adjacent interface information. While measuring the formation resistivity, it can also detect the adjacent formation interface; the third stage (current stage) under development, the instrument adopts a multi-directional transmitting and receiving antenna structure, which can theoretically obtain , , , , , , , , The nine components in all three directions, namely the three-dimensional hologram, can not only complete the logging task of obtaining formation resistivity and interface information, but also obtain various cross components containing resistivity anisotropy information. In downhole work, the transmission bandwidth of the instrument is still extremely limited (4-8 bits). In order to actively guide the direction of the drill bit in real time while drilling, the instrument is required to obtain more comprehensive downhole formation information through the least transmission signal. Therefore, the extraction of all logging components and the construction of corresponding functional signals have become pain points.
多方向发射接收天线的测井仪器近年发展迅速,如斯伦贝谢公司的Periscope系列、哈里伯顿公司的ADR系列、中海油的DWPR等。基于以上测井仪器与Michael Zhdanov的方位电磁波理论基础,在对各向异性识别信号的研究中,Deng等在第二阶段的信号中,通过对称线圈进一步引入分量、、的磁场形式,改进并重新对地质信号进行构建,以反映并抵抗地层各向异性影响;Pardo等通过联合XZ面所有交叉分量构建的信号,表达了测井仪器的井下方位信息,且不受各向异性与井眼偏心的负面影响;中海油研究员马明学等,通过仪器的旋转测量,使用旋转分量比值构建的信号中含倾斜线圈特有的分量和,使信号对地层各向异性更加敏感,更易于获得仪器的方位信息。而上列仪器的测井分量提取多通过前两阶段的线圈计算方式,直接测量电压值得出分量,并由于仪器中仅包含仪器坐标系下XZ面发射接收天线结构(Co-planar),无法真正做到真正的三维全息,因而目前多以对方位信息与地质信号的研究为主,对各向异性更为系统的研究分析则较少,且上述信号多旨在抵消各向异性影响,均不能在实时导向中直接获取电阻率各向异性信息以供后续的评价工作。而全部9个分量的提取,与三维方向的天线结构密不可分,目前仍然缺少明确的分量提取方法以支撑现阶段仪器获取全分量的可行性,含全面信息的全分量更是构建仪器识别各向异性地层信号的基础。Well logging instruments with multi-directional transmitting and receiving antennas have developed rapidly in recent years, such as Schlumberger's Periscope series, Halliburton's ADR series, CNOOC's DWPR, etc. Based on the above well logging instruments and Michael Zhdanov's azimuthal electromagnetic wave theory, in the study of anisotropic identification signals, Deng et al. further introduced components in the second stage of the signal through symmetrical coils. , , The magnetic field form was used to improve and reconstruct the geological signal to reflect and resist the influence of formation anisotropy; Pardo et al. constructed a signal by combining all the cross components of the XZ plane to express the downhole position information of the logging instrument, which was not negatively affected by anisotropy and wellbore eccentricity; Ma Mingxue, a researcher at CNOOC, and others used the rotation measurement of the instrument to construct a signal containing a component unique to the tilt coil using the ratio of the rotation components. and , making the signal more sensitive to the anisotropy of the formation and making it easier to obtain the azimuth information of the instrument. The logging component extraction of the above instruments is mostly through the coil calculation method of the first two stages, directly measuring the voltage value to obtain the component, and because the instrument only contains the XZ plane transmitting and receiving antenna structure (Co-planar) in the instrument coordinate system, it is impossible to truly achieve true three-dimensional holography. Therefore, the current research is mainly focused on the research of azimuth information and geological signals, and there are fewer more systematic research and analysis on anisotropy. In addition, the above signals are mostly intended to offset the influence of anisotropy, and none of them can directly obtain resistivity anisotropy information in real-time guidance for subsequent evaluation work. The extraction of all 9 components is inseparable from the antenna structure in the three-dimensional direction. At present, there is still a lack of clear component extraction methods to support the feasibility of the current instrument to obtain full components. The full components containing comprehensive information are the basis for building instruments to identify anisotropic formation signals.
发明内容Summary of the invention
有鉴于此,本发明提供了一种随钻测井仪器的测井分量提取方法和电各向异性识别应用,用以实现在实时导向中直接获取电阻率各向异性信息,并且提高随钻测井仪器的电各向异性识别能力,有效地保证随钻测井仪器的工作。In view of this, the present invention provides a logging component extraction method and electrical anisotropy identification application for a logging while drilling instrument, so as to directly obtain resistivity anisotropy information in real-time guidance, improve the electrical anisotropy identification capability of the logging while drilling instrument, and effectively ensure the operation of the logging while drilling instrument.
第一方面,本发明提供了一种随钻测井仪器的测井分量提取方法,所述方法包括:In a first aspect, the present invention provides a method for extracting logging components of a logging while drilling instrument, the method comprising:
步骤S1、在随钻测井仪器坐标系下,设定三个方向单位磁矩发射-三个方向单位磁矩接收的仪器,所接收到的信号电压共有9个分量,并通过分量矩阵V表示,其表达式为:Step S1: In the coordinate system of the logging while drilling instrument Under the condition of setting the instrument of unit magnetic moment emission in three directions and unit magnetic moment reception in three directions, the received signal voltage has 9 components in total, which are expressed by the component matrix V , and its expression is:
; ;
其中,表示m方向单位磁矩发射时,n方向单位磁矩接收的电压信号;9个分量包含了三维轴向上所有的发射接收组合;in, It represents the voltage signal received by the unit magnetic moment in the n direction when the unit magnetic moment in the m direction is emitted; the 9 components include all the emission and reception combinations in the three-dimensional axis;
步骤S2、根据步骤S1,设定单方向发射单方向接收测量单元模型,通过三角坐标变换,得到任意方向上的发射-接收的响应通式,其表达式为:Step S2: According to step S1, a unidirectional transmitting and unidirectional receiving measurement unit model is set, and a general response formula of transmitting and receiving in any direction is obtained through triangular coordinate transformation, and its expression is:
; ;
其中,发射磁矩与仪器轴的夹角为,发射磁矩与仪器旋转轴的夹角为;接收磁矩与仪器轴的夹角为,接收磁矩与仪器旋转轴的夹角为;仪器旋转角为,规定为仪器高边角,为低边角,发射磁矩与接收磁矩强度均为1;Among them, the emission magnetic moment The angle with the instrument axis is , the emission magnetic moment The angle with the instrument rotation axis is ; Receive magnetic moment The angle with the instrument axis is , receiving magnetic moment The angle with the instrument rotation axis is ; The instrument rotation angle is ,Regulation is the high corner of the instrument, For low edge angles, the transmitting magnetic moment and the receiving magnetic moment strength are both 1;
步骤S3、将步骤S2引入共面Co-planar与异面Anti-planar两类天线对模式中,设定天线磁矩方向与仪器轴向之间的夹角分别为和,磁矩角度为倾斜发射-倾斜接收,即,,仪器旋转角为,当发射天线和接收天线的磁矩在同一平面,即,此天线模式即为仪器线圈系的共面模式;Step S3, introducing step S2 into two types of antenna pair modes: co-planar and anti-planar, setting the angles between the antenna magnetic moment direction and the instrument axis to be and , the magnetic moment angle is tilted emission-tilted reception, that is , , the instrument rotation angle is , when the magnetic moments of the transmitting antenna and the receiving antenna are in the same plane, that is , this antenna mode is the coplanar mode of the instrument coil system;
设定共面倾斜发射-倾斜接收模型,固定旋转角,获得响应,其表达式为:Set up a coplanar tilted transmit-tilted receive model, fix the rotation angle, and obtain the response , whose expression is:
; ;
将上述表达式中括号内的公式进行联立,获得参变量方程组:Combine the formulas in the brackets in the above expressions to obtain the parameter equation system:
; ;
随钻测井仪器使用多扇区方位测量,即将旋转周期划分为N个扇区,分别记录对应仪器旋转角下的响应,经过仪器的多扇区旋转测量,将响应进行简化,简化后的表达式为:The logging while drilling tool uses multi-sector azimuth measurement, that is, the rotation cycle Divided into N sectors, each recording the corresponding instrument rotation angle The response under the condition is measured by multi-sector rotation of the instrument. Simplify, the simplified expression for:
; ;
其中,i为扇区号,为第i扇区下接收天线的电压响应值,为第i扇区对应的仪器旋转角;Where i is the sector number, is the voltage response value of the receiving antenna in the i - th sector, is the instrument rotation angle corresponding to the i- th sector;
步骤S4、根据步骤S3中的对至进行求解,获得至;Step S4: according to step S3 right to Solve and obtain to ;
a、求解,对叠加求和,获得的求解式为:a. Solve ,right Add up and get The solution is:
; ;
b、求解,对进行变换后,再叠加求和,根据三角函数的正交性,获得的求解式为:b. Solve ,right conduct After transformation, we can add and sum them up, and according to the orthogonality of trigonometric functions, we can get The solution is:
; ;
c、求解,对进行变换后,再叠加求和,根据三角函数的正交性,获得的求解式为:c. Solve ,right conduct After transformation, we can add and sum them up, and according to the orthogonality of trigonometric functions, we can get The solution is:
; ;
d、求解与,对分别进行变换与变换,再分别进行求和,根据三角函数的正交性,获得和的求解式分别为:d. Solution and ,right Separately Transformation and Transform, and then sum them up respectively. According to the orthogonality of trigonometric functions, we get and The solutions are:
; ;
; ;
步骤S5、将已知量至、与代入步骤S3的参变量方程组中,获得所有共面天线系模型的分量,即获得、、、、、、、;Step S5: The known quantity to , and Substitute into the parameter equation group of step S3 to obtain the components of all coplanar antenna system models, that is, , , , , , , , ;
步骤S6、设定天线磁矩方向与仪器轴向之间的夹角分别为和,磁矩角度为,,仪器旋转角为,当发射天线和接收天线的磁矩分别位于互相正交的两个平面上,此天线模式即为仪器线圈系的异面模式;Step S6: Set the angles between the antenna magnetic moment direction and the instrument axis to be and , the magnetic moment angle is , , the instrument rotation angle is , when the magnetic moments of the transmitting antenna and the receiving antenna are located on two mutually orthogonal planes, this antenna mode is the out-of-plane mode of the instrument coil system;
设定仪器线圈系的异面模式,根据步骤2的响应通式,获得XZ面倾斜发射-YZ面倾斜接收模式下的响应,其表达式为:Set the out-of-plane mode of the instrument coil system and obtain the response in the XZ plane tilted transmission-YZ plane tilted reception mode according to the response formula in step 2 , whose expression is:
; ;
获得YZ面倾斜发射-XZ面倾斜接收模式下的响应,其表达式为:Get the response in the YZ tilt transmission-XZ tilt reception mode , whose expression is:
; ;
将上述响应和响应表达式中括号内的公式分别进行联立,获得参变量方程组:The above response and response The formulas in the brackets in the expression are combined to obtain the parameter equation system:
; ;
; ;
利用步骤S4中的方式对至、至分别求解,获得至、至;Using the method in step S4 to , to Solve separately and obtain to , to ;
步骤S7、将已知量至、至分别代入步骤S6的参变量方程组中,获得所有异面天线系模型的分量,即获得、、、、、、、;并结合步骤S5中所有共面天线系模型的分量,以获得步骤S1中的9个分量,即获得。Step S7: The known quantity to , to Substitute them into the parameter equation group of step S6 respectively to obtain the components of all the out-of-plane antenna system models, that is, , , , , , , , ; and combine the components of all coplanar antenna system models in step S5 to obtain the 9 components in step S1, that is, obtain .
第二方面,本发明提供了一种随钻测井仪器的电各向异性识别应用,所述随钻测井仪器的电各向异性识别应用基于随钻测井仪器的测井分量提取方法实现;In a second aspect, the present invention provides an electrical anisotropy identification application of a logging while drilling instrument, wherein the electrical anisotropy identification application of the logging while drilling instrument is implemented based on a logging component extraction method of the logging while drilling instrument;
步骤V1、以对称天线逆补偿和多源距聚焦的模式对电各向异性的分量进行提取,得到主分量、和交叉分量、、、、、;Step V1: Extract the electrical anisotropy component by using the symmetric antenna inverse compensation and multi-source focusing mode to obtain the main component , and cross components , , , , , ;
步骤V2、利用步骤V1中的主分量和交叉分量,通过随钻测井仪器同步计算幅度比信号与相位差信号,构建幅度比信号与相位差信号,其表达式分别为:Step V2: Using the principal component and cross component in step V1, the amplitude ratio signal and the phase difference signal are synchronously calculated by the logging while drilling instrument to construct the amplitude ratio signal Phase difference signal , whose expressions are:
; ;
; ;
其中,angle为取复数的角度;Wherein, angle is the angle of complex number;
步骤V3、根据步骤V2,设置三层均匀地层模型,随钻测井仪器工作频率取2MHz,井斜角=50°,设定模型的围岩层为各向同性地层,各向异性系数λ为1,此时水平电阻率和垂直电阻率相同,均为1;目的层分别设定各向同性地层中各向异性系数λ=1,水平电阻率和垂直电阻率均为4;各向异性地层中各向异性系数λ=2,水平电阻率为4,垂直电阻率为16;上围岩地层边界位置的垂直深度TVD为5m,下围岩地层边界位置的垂直深度TVD为10,中间目的层厚度为5m,通过广义反射系数解析法计算的电各向异性信号响应正演模拟,获取其对应的模拟结果;Step V3: According to step V2, a three-layer uniform formation model is set, the operating frequency of the logging while drilling instrument is 2 MHz, and the well inclination angle is =50°, the surrounding rock layer of the model is set to be isotropic, and the anisotropy coefficient λ is 1. At this time, the horizontal resistivity and vertical resistivity Same, both are 1 ; The target layer is set to have anisotropy coefficient λ=1 in the isotropic formation and horizontal resistivity and vertical resistivity All 4 ; In anisotropic formations, the anisotropy coefficient λ=2, and the horizontal resistivity For 4 , vertical resistivity For 16 ; The vertical depth TVD of the upper surrounding rock stratum boundary is 5m, the vertical depth TVD of the lower surrounding rock stratum boundary is 10, the thickness of the intermediate target layer is 5m, and the corresponding simulation results are obtained by forward modeling the electrical anisotropy signal response calculated by the generalized reflection coefficient analytical method;
步骤V4、设置三层均匀地层模型,井斜角=50°,上围岩地层边界位置的垂直深度TVD为5m,下围岩地层边界位置的垂直深度TVD为10m,设定模型的围岩层为各向同性层,目的层设定各向异性系数由1至5逐渐增加,选取随钻测井仪器工作频率为2MHz和400KHz的条件下进行正演模拟,获取其对应的模拟结果;Step V4: Set up a three-layer uniform formation model and well inclination angle =50°, the vertical depth TVD of the upper surrounding rock formation boundary is 5m, the vertical depth TVD of the lower surrounding rock formation boundary is 10m, the surrounding rock layer of the model is set as an isotropic layer, the anisotropy coefficient of the target layer is set to gradually increase from 1 to 5, and the forward simulation is carried out under the conditions of 2MHz and 400KHz working frequencies of the logging while drilling instrument to obtain the corresponding simulation results;
步骤V5、设置三层均匀地层模型,上围岩地层边界位置的垂直深度TVD为TVD=5m;下围岩地层边界位置的垂直深度TVD为10m;模型的围岩层为各向同性层,其各向异性系数λ为1,水平电阻率和垂直电阻率均为1 ;中间目的层的各向异性系数λ固定为5,水平电阻率为4,垂直电阻率为100,改变井斜角,将其由0°逐渐增至90°,选取随钻测井仪器工作频率为2MHz和400KHz的条件下进行正演模拟,获取其对应的模拟结果;Step V5: Set a three-layer uniform stratum model. The vertical depth TVD of the upper surrounding rock stratum boundary is TVD=5m; the vertical depth TVD of the lower surrounding rock stratum boundary is 10m; the surrounding rock layer of the model is an isotropic layer, its anisotropy coefficient λ is 1, and the horizontal resistivity and vertical resistivity are all 1; the anisotropy coefficient λ of the intermediate target layer is fixed at 5, and the horizontal resistivity is 4, vertical resistivity To 100, change the well inclination , gradually increase it from 0° to 90°, select the working frequency of the logging while drilling instrument as 2MHz and 400KHz to perform forward simulation, and obtain the corresponding simulation results;
步骤V6、通过步骤V5对相位差信号进行筛选,以模拟电各向异性识别的方位成像。Step V6: Screen the phase difference signal through step V5 to simulate the azimuth imaging of electrical anisotropy recognition.
本发明提供的技术方案中,该方法包括获取信号电压9个分量的分量矩阵;设定单方向发射单方向接收测量单元模型,通过三角坐标变换,得到任意方向上的发射-接收的响应通式;设定共面倾斜发射-倾斜接收模型,固定旋转角,获得响应;根据响应对至进行求解,获得至;根据至、与,获得所有共面天线系模型的分量;设定仪器线圈系的异面模式,获得XZ面倾斜发射-YZ面倾斜接收模式下的响应,并获得至、至;根据获得至、至获得所有异面天线系模型的分量,并结合所有共面天线系模型的分量,以获得9个分量,该方法实现了在实时导向中直接获取电阻率各向异性信息,并且提高了随钻测井仪器的电各向异性识别能力,有效地保证了随钻测井仪器的工作。In the technical solution provided by the present invention, the method includes obtaining a component matrix of 9 components of the signal voltage; setting a unidirectional transmitting and unidirectional receiving measurement unit model, and obtaining a general response formula of transmitting and receiving in any direction through triangular coordinate transformation; setting a coplanar tilted transmitting and tilted receiving model, fixing the rotation angle, and obtaining a response ; According to the response right to Solve and obtain to ;according to to , and , obtain the components of all coplanar antenna system models; set the out-of-plane mode of the instrument coil system to obtain the response in the XZ plane tilted transmission-YZ plane tilted reception mode , and obtain to , to According to the obtained to , to The components of all out-of-plane antenna system models are obtained, and combined with the components of all coplanar antenna system models to obtain 9 components. This method realizes the direct acquisition of resistivity anisotropy information in real-time guidance, improves the electrical anisotropy recognition capability of the logging while drilling instrument, and effectively ensures the operation of the logging while drilling instrument.
附图说明BRIEF DESCRIPTION OF THE DRAWINGS
为了更清楚地说明本发明实施例的技术方案,下面将对实施例中所需要使用的附图作简单地介绍,显而易见地,下面描述中的附图仅仅是本发明的一些实施例,对于本领域普通技术人员来讲,在不付出创造性劳动的前提下,还可以根据这些附图获得其它的附图。In order to more clearly illustrate the technical solutions of the embodiments of the present invention, the drawings required for use in the embodiments will be briefly introduced below. Obviously, the drawings described below are only some embodiments of the present invention. For ordinary technicians in this field, other drawings can be obtained based on these drawings without paying creative work.
图1为本发明实施例提供的测井分量提取方法的流程图;FIG1 is a flow chart of a method for extracting well logging components provided by an embodiment of the present invention;
图2为本发明实施例提供的随钻测井仪器坐标系的示意图;FIG2 is a schematic diagram of a coordinate system of a logging while drilling instrument provided in an embodiment of the present invention;
图3为本发明实施例提供的单方向发射单方向接收测量单元模型的示意图;FIG3 is a schematic diagram of a unidirectional transmitting and unidirectional receiving measurement unit model provided by an embodiment of the present invention;
图4为本发明实施例提供的共面倾斜发射-倾斜接收模型的示意图;FIG4 is a schematic diagram of a coplanar tilted transmission-tilted reception model provided by an embodiment of the present invention;
图5为本发明实施例提供的共面天线系模型的示意图,其中,(a)为共轴天线系模型的示意图;(b)为X轴向发射-Z轴向接收天线系模型的示意图;(c)为Z轴向发射-X轴向接收天线系模型的示意图;(d)为X轴向发射-X轴向接收天线系模型的示意图;(e)为Z轴向发射-XZ面倾斜接收天线系模型的示意图;(f)为XZ面倾斜发射-Z轴向接收天线系模型的示意图;(g)为X轴向发射-XZ面倾斜接收天线系模型的示意图;(h)为XZ面倾斜发射-X轴向接收天线系模型的示意图;Fig. 5 is a schematic diagram of a coplanar antenna system model provided by an embodiment of the present invention, wherein (a) is a schematic diagram of a coaxial antenna system model; (b) is a schematic diagram of an X-axis transmitting-Z-axis receiving antenna system model; (c) is a schematic diagram of a Z-axis transmitting-X-axis receiving antenna system model; (d) is a schematic diagram of an X-axis transmitting-X-axis receiving antenna system model; (e) is a schematic diagram of a Z-axis transmitting-XZ plane tilted receiving antenna system model; (f) is a schematic diagram of an XZ plane tilted transmitting-Z-axis receiving antenna system model; (g) is a schematic diagram of an X-axis transmitting-XZ plane tilted receiving antenna system model; (h) is a schematic diagram of an XZ plane tilted transmitting-X-axis receiving antenna system model;
图6a为本发明实施例提供的XZ面倾斜发射-YZ面倾斜接收模型的示意图;FIG6a is a schematic diagram of an XZ plane tilted emission-YZ plane tilted reception model provided by an embodiment of the present invention;
图6b为本发明实施例提供的YZ面倾斜发射-XZ面倾斜接收模型的示意图;FIG6 b is a schematic diagram of a YZ plane tilted emission-XZ plane tilted reception model provided by an embodiment of the present invention;
图7为本发明实施例提供的异面天线系模型的示意图,其中,(a)为X轴向发射-Y轴向接收天线系模型的示意图;(b)为X轴向发射-YZ面斜收天线系模型的示意图;(c)为XZ面倾斜发射-Y轴向接收天线系模型的示意图;(d)为Y轴向发射-X轴向接收天线系模型的示意图;(e)为Y轴向发射-XZ面倾斜接收天线系模型的示意图;(f)为YZ面倾斜发射-X轴接收天线系模型的示意图;FIG7 is a schematic diagram of an out-of-plane antenna system model provided by an embodiment of the present invention, wherein (a) is a schematic diagram of an X-axis transmitting-Y-axis receiving antenna system model; (b) is a schematic diagram of an X-axis transmitting-YZ-plane tilted receiving antenna system model; (c) is a schematic diagram of an XZ-plane tilted transmitting-Y-axis receiving antenna system model; (d) is a schematic diagram of a Y-axis transmitting-X-axis receiving antenna system model; (e) is a schematic diagram of a Y-axis transmitting-XZ-plane tilted receiving antenna system model; and (f) is a schematic diagram of a YZ-plane tilted transmitting-X-axis receiving antenna system model.
图8为本发明实施例提供的随钻测井仪器的局部结构示意图;FIG8 is a schematic diagram of a partial structure of a logging while drilling instrument provided in an embodiment of the present invention;
图9a为本发明实施例提供的幅度比信号的曲线图;FIG9a is a curve diagram of an amplitude ratio signal provided by an embodiment of the present invention;
图9b为本发明实施例提供的相位差信号的曲线图;FIG9b is a graph of a phase difference signal provided by an embodiment of the present invention;
图10a为本发明实施例提供的2MHz下的幅度比信号的模拟图;FIG10a is a simulation diagram of an amplitude ratio signal at 2 MHz provided by an embodiment of the present invention;
图10b为本发明实施例提供的2MHz下的相位差信号的模拟图;FIG10b is a simulation diagram of a phase difference signal at 2 MHz provided by an embodiment of the present invention;
图10c为本发明实施例提供的400KHz下的幅度比信号的模拟图;FIG10c is a simulation diagram of an amplitude ratio signal at 400 KHz provided by an embodiment of the present invention;
图10d为本发明实施例提供的400KHz下的相位差信号的模拟图;FIG10d is a simulation diagram of a phase difference signal at 400 KHz provided by an embodiment of the present invention;
图11a为本发明实施例提供的2MHz下的幅度比信号的模拟图;FIG11a is a simulation diagram of an amplitude ratio signal at 2 MHz provided by an embodiment of the present invention;
图11b为本发明实施例提供的2MHz下的相位差信号的模拟图;FIG11b is a simulation diagram of a phase difference signal at 2 MHz provided by an embodiment of the present invention;
图11c为本发明实施例提供的400KHz下的幅度比信号的模拟图;FIG. 11c is a simulation diagram of an amplitude ratio signal at 400 KHz provided by an embodiment of the present invention;
图11d为本发明实施例提供的400KHz下的相位差信号的模拟图;FIG11d is a simulation diagram of a phase difference signal at 400 KHz provided by an embodiment of the present invention;
图12为本发明实施例提供的各向异性信号成像的示意图。FIG. 12 is a schematic diagram of anisotropic signal imaging provided by an embodiment of the present invention.
具体实施方式DETAILED DESCRIPTION
为使本发明实施例的目的、技术方案和优点更加清楚,下面将结合本发明实施例中的附图,对本发明实施例中的技术方案进行清楚、完整地描述,显然,所描述的实施例是本发明一部分实施例,而不是全部的实施例。基于本发明中的实施例,本领域普通技术人员在没有做出创造性劳动前提下所获得的所有其他实施例,都属于本发明保护的范围。In order to make the purpose, technical solution and advantages of the embodiments of the present invention clearer, the technical solution in the embodiments of the present invention will be clearly and completely described below in conjunction with the drawings in the embodiments of the present invention. Obviously, the described embodiments are part of the embodiments of the present invention, not all of the embodiments. Based on the embodiments of the present invention, all other embodiments obtained by ordinary technicians in this field without creative work are within the scope of protection of the present invention.
应当明确,所描述的实施例仅仅是本发明一部分实施例,而不是全部的实施例。基于本发明中的实施例,本领域普通技术人员在没有做出创造性劳动前提下所获得的所有其它实施例,都属于本发明保护的范围。It should be clear that the described embodiments are only some embodiments of the present invention, not all embodiments. Based on the embodiments of the present invention, all other embodiments obtained by ordinary technicians in this field without creative work are within the scope of protection of the present invention.
在本发明实施例中使用的术语是仅仅出于描述特定实施例的目的,而非旨在限制本发明。在本发明实施例中所使用的单数形式的“一种”、“所述”和“该”也旨在包括多数形式,除非上下文清楚地表示其他含义。The terms used in the embodiments of the present invention are only for the purpose of describing specific embodiments, and are not intended to limit the present invention. The singular forms "a", "said" and "the" used in the embodiments of the present invention are also intended to include plural forms, unless the context clearly indicates other meanings.
应当理解,本文中使用的术语“和/或”仅仅是一种描述关联对象的关联关系,表示可以存在三种关系,例如,甲和/或乙,可以表示:单独存在甲,同时存在甲和乙,单独存在乙这三种情况。另外,本文中字符“/”,一般表示前后关联对象是一种“或”的关系。It should be understood that the term "and/or" used in this article is only a description of the association relationship of associated objects, indicating that there can be three relationships. For example, A and/or B can represent: A exists alone, A and B exist at the same time, and B exists alone. In addition, the character "/" in this article generally indicates that the associated objects before and after are in an "or" relationship.
取决于语境,如在此所使用的词语“如果”可以被解释成为“在……时”或“当……时”或“响应于确定”或“响应于检测”。类似地,取决于语境,短语“如果确定”或“如果检测(陈述的条件或事件)”可以被解释成为“当确定时”或“响应于确定”或“当检测(陈述的条件或事件)时”或“响应于检测(陈述的条件或事件)”。The word "if" as used herein may be interpreted as "at the time of" or "when" or "in response to determining" or "in response to detecting", depending on the context. Similarly, the phrases "if it is determined" or "if (stated condition or event) is detected" may be interpreted as "when it is determined" or "in response to determining" or "when detecting (stated condition or event)" or "in response to detecting (stated condition or event)", depending on the context.
本发明从假想的三方向电磁波仪器出发,结合测井线圈系基本测量原理为理论前提,推导得出共面天线对与异面天线对两大类天线结构的发射-接收响应式,对全部9个测井分量进行求解提取,形成在实际测井工程可直接计算使用的电磁测井分量提取方法。以该方法作为理论,构建使随钻测井仪器具备各向异性地层识别能力的信号,应用至自主研发的三维全息随钻电磁波电阻率仪器中,并对信号进行响应特性分析,进一步比较与筛选信号,保证在井下工作使用尽可能少的传输资源,后以典型砂泥岩互层模型进行方位成像,完成随钻测井仪器电各向异性识别功能的应用。The present invention starts from an imaginary three-directional electromagnetic wave instrument, combines the basic measurement principle of the logging coil system as a theoretical premise, derives the transmission-receiving response formula of two types of antenna structures, namely, coplanar antenna pairs and skew antenna pairs, and solves and extracts all 9 logging components, forming an electromagnetic logging component extraction method that can be directly calculated and used in actual logging projects. Using this method as a theory, a signal that enables the logging while drilling instrument to have the ability to identify anisotropic formations is constructed, applied to the independently developed three-dimensional holographic electromagnetic wave resistivity instrument while drilling, and the response characteristics of the signal are analyzed, and the signal is further compared and screened to ensure that as few transmission resources as possible are used in underground work, and then azimuth imaging is performed with a typical sandstone-mudstone interlayer model to complete the application of the electrical anisotropy identification function of the logging while drilling instrument.
图1为本发明实施例提供的测井分量提取方法的流程图,如图1所示,该方法包括:FIG1 is a flow chart of a method for extracting well logging components provided by an embodiment of the present invention. As shown in FIG1 , the method includes:
步骤S1、在随钻测井仪器坐标系下,设定三个方向单位磁矩发射-三个方向单位磁矩接收的仪器,所接收到的信号电压共有9个分量,并通过分量矩阵V表示,其表达式为:Step S1: In the coordinate system of the logging while drilling instrument Under the condition of setting the instrument of unit magnetic moment emission in three directions and unit magnetic moment reception in three directions, the received signal voltage has 9 components in total, which are expressed by the component matrix V , and its expression is:
; ;
其中,表示m方向单位磁矩发射时,n方向单位磁矩接收的电压信号;9个分量包含了三维轴向上所有的发射接收组合。in, It represents the voltage signal received by the unit magnetic moment in the n direction when the unit magnetic moment in the m direction is emitted. The 9 components include all the emission and reception combinations in the three-dimensional axis.
本发明实施例中,如图2所示,在坐标系中标记了发射端和接收端;由于9个分量包含了三维轴向上所有的发射接收组合,因而具备全方向上的地层信息,可以作为随钻测井仪器功能信号的基础分量。In the embodiment of the present invention, as shown in FIG2, in the coordinate system The transmitting end and the receiving end are marked in the figure; since the nine components include all the transmitting and receiving combinations in the three-dimensional axis, they have omnidirectional formation information and can be used as the basic components of the functional signal of the while drilling logging tool.
步骤S2、根据步骤S1,设定单方向发射单方向接收测量单元模型,通过三角坐标变换,得到任意方向上的发射-接收的响应通式,其表达式为:Step S2: According to step S1, a unidirectional transmitting and unidirectional receiving measurement unit model is set, and a general response formula of transmitting and receiving in any direction is obtained through triangular coordinate transformation, and its expression is:
; ;
其中,如图3所示,发射磁矩与仪器轴的夹角为,发射磁矩与仪器旋转轴的夹角为;接收磁矩与仪器轴的夹角为,接收磁矩与仪器旋转轴的夹角为;仪器旋转角为,规定为仪器高边角,为低边角,发射磁矩与接收磁矩强度均为1。Among them, as shown in Figure 3, the emission magnetic moment The angle with the instrument axis is , the emission magnetic moment The angle with the instrument rotation axis is ; Receive magnetic moment The angle with the instrument axis is , receiving magnetic moment The angle with the instrument rotation axis is ; The instrument rotation angle is ,Regulation is the high corner of the instrument, It is a low angle, and the intensity of the transmitting magnetic moment and the receiving magnetic moment are both 1.
本发明实施例中,如图3所示,标记①处的圆形与箭头代表发射线圈模型及其磁矩方向,标记②处的圆形与箭头代表接收线圈模型及其磁矩方向。In the embodiment of the present invention, as shown in FIG. 3 , the circle and arrow at mark ① represent the transmitting coil model and its magnetic moment direction, and the circle and arrow at mark ② represent the receiving coil model and its magnetic moment direction.
步骤S3、将步骤S2引入共面Co-planar与异面Anti-planar两类天线对模式中,设定天线磁矩方向与仪器轴向之间的夹角分别为和,磁矩角度为倾斜发射-倾斜接收,即,,仪器旋转角为,当发射天线和接收天线的磁矩在同一平面,即,此天线模式即为仪器线圈系的共面模式。Step S3, introducing step S2 into two types of antenna pair modes: co-planar and anti-planar, setting the angles between the antenna magnetic moment direction and the instrument axis to be and , the magnetic moment angle is tilted emission-tilted reception, that is , , the instrument rotation angle is , when the magnetic moments of the transmitting antenna and the receiving antenna are in the same plane, that is , this antenna mode is the coplanar mode of the instrument coil system.
设定共面倾斜发射-倾斜接收模型,固定旋转角,获得响应,其表达式为:Set up a coplanar tilted transmit-tilted receive model, fix the rotation angle, and obtain the response , whose expression is:
; ;
响应为9个分量、接收与发射天线的磁矩角度与、随钻测井仪器旋转角的加权函数,而全分量的提取,需要对响应进行解析计算;将上述表达式中括号内的公式进行联立,获得参变量方程组:response is the 9 components, the magnetic moment angle of the receiving and transmitting antennas and , the weighted function of the rotation angle of the logging while drilling tool, and the extraction of the full component requires the response Perform analytical calculations; combine the formulas in brackets in the above expressions to obtain the parameter equation group:
; ;
本发明实施例中,如图4所示,标记③处的箭头代表发射天线磁矩方向,标记④处的箭头代表与发射天线磁矩所在的面共面的接收天线磁矩方向。In the embodiment of the present invention, as shown in FIG. 4 , the arrow at mark ③ represents the direction of the magnetic moment of the transmitting antenna, and the arrow at mark ④ represents the direction of the magnetic moment of the receiving antenna coplanar with the plane where the magnetic moment of the transmitting antenna is located.
为了获得仪器旋转方位信息,将旋转方位角与该状态下的测井响应相对应以便于计算,随钻测井仪器使用多扇区方位测量,即将旋转周期划分为N个扇区,分别记录对应仪器旋转角下的响应,经过仪器的多扇区旋转测量,将响应进行简化,简化后的表达式为:In order to obtain the rotation azimuth information of the tool, the rotation azimuth angle is corresponded to the logging response in this state for calculation. The logging while drilling tool uses multi-sector azimuth measurement, that is, the rotation period is Divided into N sectors, each recording the corresponding instrument rotation angle The response under the condition is measured by multi-sector rotation of the instrument. Simplify, the simplified expression for:
; ;
其中,i为扇区号,为第i扇区下接收天线的电压响应值,为第i扇区对应的仪器旋转角。Where i is the sector number, is the voltage response value of the receiving antenna in the i - th sector, is the instrument rotation angle corresponding to the i- th sector.
步骤S4、根据步骤S3中的对至进行求解,获得至;Step S4: according to step S3 right to Solve and obtain to ;
a、求解,对叠加求和,获得的求解式为:a. Solve ,right Add up and get The solution is:
; ;
b、求解,对进行变换后,再叠加求和,根据三角函数的正交性,获得的求解式为:b. Solve ,right conduct After transformation, we can add and sum them up, and according to the orthogonality of trigonometric functions, we can get The solution is:
; ;
c、求解,对进行变换后,再叠加求和,根据三角函数的正交性,获得的求解式为:c. Solve ,right conduct After transformation, we can add and sum them up, and according to the orthogonality of trigonometric functions, we can get The solution is:
; ;
d、求解与,对分别进行变换与变换,再分别进行求和,根据三角函数的正交性,获得和的求解式分别为:d. Solution and ,right Separately Transformation and Transform, and then sum them up respectively. According to the orthogonality of trigonometric functions, we get and The solutions are:
; ;
; ;
由此完成了~共5个参变量的求解。This completes ~ A total of 5 parameters are solved.
步骤S5、将已知量至、与代入步骤S3的参变量方程组中,获得所有共面天线系模型的分量,即获得、、、、、、、。Step S5: The known quantity to , and Substitute into the parameter equation group of step S3 to obtain the components of all coplanar antenna system models, that is, , , , , , , , .
此时在上述参变量方程组中,~、与是确定的已知量,需要求解9个分量,而由于上述参变量方程组中仅有5项独立方程,即使经过了旋转方位测量,也仍然无法对全部分量进行解析,因此需要讨论共面的特殊天线布置模式下的信号响应,对响应式进一步简化,具体的共面天线模式分类如图5所示,即图5中的(a)至图5中的(h)。采取上述计算方法,如表1所示,可得到各类共面天线系模型的分量和解析提取的情况与结果。At this time, in the above parameter equations, ~ , and is a known quantity, and 9 components need to be solved. However, since there are only 5 independent equations in the above parameter variable equation group, even after the rotation azimuth measurement, it is still impossible to analyze all the components. Therefore, it is necessary to discuss the signal response under the special coplanar antenna arrangement mode and further simplify the response formula. The specific classification of coplanar antenna modes is shown in Figure 5, that is, (a) to (h) in Figure 5. Using the above calculation method, as shown in Table 1, the components and analytical extraction conditions and results of various coplanar antenna system models can be obtained.
表1Table 1
。 .
图5中的(a)为共轴天线系模型的示意图;图5中的(b)为X轴向发射-Z轴向接收天线系模型的示意图;图5中的(c)为Z轴向发射-X轴向接收天线系模型的示意图;图5中的(d)为X轴向发射-X轴向接收天线系模型的示意图;图5中的(e)为Z轴向发射-XZ面倾斜接收天线系模型的示意图;图5中的(f)为XZ面倾斜发射-Z轴向接收天线系模型的示意图;图5中的(g)为X轴向发射-XZ面倾斜接收天线系模型的示意图;图5中的(h)为XZ面倾斜发射-X轴向接收天线系模型的示意图;上述表1中,以图5中的(a)为例,其天线系名称为共轴天线系,根据共轴天线系可以解得1个分量和1个独立方程,其中可解分量为,独立方程式为=,即可解分量由解析提取式表示,又例如,图5中的(d)中=。(a) in Figure 5 is a schematic diagram of the coaxial antenna system model; (b) in Figure 5 is a schematic diagram of the X-axis transmission-Z-axis reception antenna system model; (c) in Figure 5 is a schematic diagram of the Z-axis transmission-X-axis reception antenna system model; (d) in Figure 5 is a schematic diagram of the X-axis transmission-X-axis reception antenna system model; (e) in Figure 5 is a schematic diagram of the Z-axis transmission-XZ plane tilted reception antenna system model; (f) in Figure 5 is a schematic diagram of the XZ plane tilted transmission-Z-axis reception antenna system model; (g) in Figure 5 is a schematic diagram of the X-axis transmission-XZ plane tilted reception antenna system model; (h) in Figure 5 is a schematic diagram of the XZ plane tilted transmission-X-axis reception antenna system model; In the above Table 1, taking (a) in Figure 5 as an example, the name of the antenna system is the coaxial antenna system. According to the coaxial antenna system, one component and one independent equation can be solved, where the solvable component is , the independent equation is = , that is, the solvable components are expressed by analytical extraction formulas. For example, in (d) of Figure 5 = .
本发明实施例中,如表1所示,在图5中的(d)、图5中的(g)和图5中的(h)情况下,由于分量数与独立方程数不对等,将分量视为一个分量,方程组才可被求解,出现了这两个分量无法被独立解析,无法做到三维全息的问题,为此,需要使用异面天线模式的线圈系进行解决。In the embodiment of the present invention, as shown in Table 1, in the cases of (d), (g) and (h) in FIG. 5, since the number of components is not equal to the number of independent equations, the components The system of equations can only be solved if they are regarded as one component. However, the two components cannot be analyzed independently and three-dimensional holography cannot be achieved. Therefore, a coil system with an out-of-plane antenna mode is needed to solve the problem.
步骤S6、设定天线磁矩方向与仪器轴向之间的夹角分别为和,磁矩角度为,,仪器旋转角为,当发射天线和接收天线的磁矩分别位于互相正交的两个平面上,此天线模式即为仪器线圈系的异面模式。Step S6: Set the angles between the antenna magnetic moment direction and the instrument axis to be and , the magnetic moment angle is , , the instrument rotation angle is When the magnetic moments of the transmitting antenna and the receiving antenna are located on two mutually orthogonal planes, this antenna mode is the out-of-plane mode of the instrument coil system.
设定仪器线圈系的异面模式,根据步骤2的响应通式,获得XZ面倾斜发射-YZ面倾斜接收模式下的响应,其表达式为:Set the out-of-plane mode of the instrument coil system and obtain the response in the XZ plane tilted transmission-YZ plane tilted reception mode according to the response formula in step 2 , whose expression is:
; ;
获得YZ面倾斜发射-XZ面倾斜接收模式下的响应,其表达式为:Get the response in the YZ tilt transmission-XZ tilt reception mode , whose expression is:
; ;
将上述响应和响应表达式中括号内的公式分别进行联立,获得参变量方程组:The above response and response The formulas in the brackets in the expression are combined to obtain the parameter equation system:
; ;
; ;
利用步骤S4中的方式对至、至分别求解,获得至、至。Using the method in step S4 to , to Solve separately and obtain to , to .
本发明实施例中,如图6a和图6b分别代表异面模式下的XZ面倾斜发射-YZ面倾斜接收(,)和YZ面倾斜发射-XZ面倾斜接收(,)两种,图6a和图6b中标记⑤处的箭头代表发射天线磁矩方向,标记⑥处的箭头代表与发射天线磁矩所在面正交上的接收天线磁矩方向。In the embodiment of the present invention, FIG. 6a and FIG. 6b respectively represent the XZ plane tilted transmission and the YZ plane tilted reception in the out-of-plane mode. , ) and YZ tilted emission-XZ tilted reception ( , ) There are two types. The arrow marked at ⑤ in Figure 6a and Figure 6b represents the direction of the magnetic moment of the transmitting antenna, and the arrow marked at ⑥ represents the direction of the magnetic moment of the receiving antenna that is orthogonal to the plane where the magnetic moment of the transmitting antenna is located.
步骤S7、将已知量至、至分别代入步骤S6的参变量方程组中,获得所有异面天线系模型的分量,即获得、、、、、、、;并结合步骤S5中所有共面天线系模型的分量,以获得步骤S1中的9个分量,即获得。Step S7: The known quantity to , to Substitute them into the parameter equation group of step S6 respectively to obtain the components of all the out-of-plane antenna system models, that is, , , , , , , , ; and combine the components of all coplanar antenna system models in step S5 to obtain the 9 components in step S1, that is, obtain .
本发明实施例中,由于参变量方程组至、至中仅有5项独立方程,即使经过了旋转方位测量,也无法对全部分量进行解析,因此需要讨论更特殊的异面天线布置模式下的信号响应。具体的异面天线模式如图7所示,即图7中的(a)至图7中的(f)所示。采取相同的计算方法,如表2所示,可得到各类异面天线系模型的分量和解析提取的情况与结果。In the embodiment of the present invention, since the parameter equation group to , to There are only five independent equations in the equation. Even after the rotation azimuth measurement, it is impossible to analyze all the components. Therefore, it is necessary to discuss the signal response under a more special out-of-plane antenna arrangement mode. The specific out-of-plane antenna mode is shown in Figure 7, that is, as shown in Figure 7 (a) to Figure 7 (f). Using the same calculation method, as shown in Table 2, the components and analytical extraction conditions and results of various out-of-plane antenna system models can be obtained.
表2Table 2
。 .
图7中的(a)为X轴向发射-Y轴向接收天线系模型的示意图;图7中的(b)为X轴向发射-YZ面斜收天线系模型的示意图;图7中的(c)为XZ面倾斜发射-Y轴向接收天线系模型的示意图;图7中的(d)为Y轴向发射-X轴向接收天线系模型的示意图;图7中的(e)为Y轴向发射-XZ面倾斜接收天线系模型的示意图;图7中的(f)为YZ面倾斜发射-X轴接收天线系模型的示意图;上述表2中,以图7中的(a)为例,其天线系名称为X轴向发射-Y轴向接收天线系,根据X轴向发射-Y轴向接收天线系可以解得4个分量和3个独立方程,由于分量数与独立方程数不对等,将分量视为一个分量,方程组才可被求解,其中,=;=;=。(a) in Figure 7 is a schematic diagram of the X-axis transmission-Y-axis reception antenna system model; (b) in Figure 7 is a schematic diagram of the X-axis transmission-YZ plane tilt reception antenna system model; (c) in Figure 7 is a schematic diagram of the XZ plane tilt transmission-Y-axis reception antenna system model; (d) in Figure 7 is a schematic diagram of the Y-axis transmission-X-axis reception antenna system model; (e) in Figure 7 is a schematic diagram of the Y-axis transmission-XZ plane tilt reception antenna system model; (f) in Figure 7 is a schematic diagram of the YZ plane tilt transmission-X-axis reception antenna system model. In the above Table 2, taking (a) in Figure 7 as an example, the antenna system name is the X-axis transmission-Y-axis reception antenna system. According to the X-axis transmission-Y-axis reception antenna system, 4 components and 3 independent equations can be solved. Since the number of components is not equal to the number of independent equations, the components Considered as a component, the system of equations can be solved, where = ; = ; = .
本发明实施例中,分量与无法被独立解析,结合共面线圈系模式下可解析的分量,全部9个分量均可被独立提取,达成了真正的三维全息。In the embodiment of the present invention, the component and It cannot be analyzed independently. Combined with the components that can be analyzed in the coplanar coil system mode, all 9 components can be extracted independently, achieving true three-dimensional holography.
至此可得,在随钻测井仪器中,对于以上任意一种单向发射单向接收天线对,均可通过方法中的分量解析提取式,直接计算得出单个分量的测井响应,并在实际测井工程中结合仪器具体的天线模式,直接计算使用选定分量,参与目标信号构建。且可证明,自主研发的三维全息随钻方位电阻率测井仪器可以利用该分量提取方法,使用9个含有全方向信息的全息分量,作为随钻测井各向异性识别功能的基础信号分量的可行性。So far, it can be concluded that in the logging while drilling instrument, for any of the above unidirectional transmitting and unidirectional receiving antenna pairs, the component analytical extraction formula in the method can be used to directly calculate the logging response of a single component, and in the actual logging project, combined with the specific antenna mode of the instrument, the selected component can be directly calculated and used to participate in the target signal construction. It can also be proved that the independently developed three-dimensional holographic azimuthal resistivity logging while drilling instrument can use this component extraction method and use 9 holographic components containing omnidirectional information as the basic signal components of the anisotropy identification function of the logging while drilling.
电各向异性是测井工作中极为重要的地层参数,其与地层平均电阻率以及层界面联合分析可直接获取井下的地质构成,获得各向异性信息更是后续如反演等测井工作的前提。各向异性信号用于指示地层的电各向异性系数变化,当仪器靠近或经过各向异性目的层时,其响应特征必须通过特定的方式,明确指示出地层各向异性系数的相对性,且反应出地层界面区分度,表达出仪器在地层中的方位性。电各向异性的识别,即通过各向异性信号在仪器中的应用,使测量获得的信息可清晰的表达地层电各向异性,以发挥出充分的识别能力。Electrical anisotropy is an extremely important formation parameter in logging work. Its joint analysis with the average resistivity of the formation and the layer interface can directly obtain the geological composition of the well. Obtaining anisotropy information is the prerequisite for subsequent logging work such as inversion. The anisotropy signal is used to indicate the change of the electrical anisotropy coefficient of the formation. When the instrument approaches or passes through the anisotropic target layer, its response characteristics must clearly indicate the relativity of the formation anisotropy coefficient in a specific way, and reflect the differentiation of the formation interface, and express the orientation of the instrument in the formation. The identification of electrical anisotropy, that is, through the application of anisotropy signals in the instrument, the information obtained by the measurement can clearly express the electrical anisotropy of the formation, so as to give full play to the recognition ability.
本发明实施例中,如图8所示,随钻测井仪器为三维全息随钻电磁波电阻率仪器,采用六发射六接收的全对称天线系结构;其中,仪器的发射天线包括第一发射天线T1、第二发射天线T2、第三发射天线T3、第四发射天线T4、第五发射天线T5、第六发射天线T6;接收天线包括第一接收天线R1、第二接收天线R2、第三接收天线R3、第四接收天线R4、第五接收天线R5、第六接收天线R6。In an embodiment of the present invention, as shown in Figure 8, the logging while drilling instrument is a three-dimensional holographic logging while drilling electromagnetic wave resistivity instrument, which adopts a fully symmetrical antenna system structure with six transmitters and six receivers; wherein the transmitting antenna of the instrument includes a first transmitting antenna T1, a second transmitting antenna T2, a third transmitting antenna T3, a fourth transmitting antenna T4, a fifth transmitting antenna T5, and a sixth transmitting antenna T6; the receiving antenna includes a first receiving antenna R1, a second receiving antenna R2, a third receiving antenna R3, a fourth receiving antenna R4, a fifth receiving antenna R5, and a sixth receiving antenna R6.
第一发射天线T1、第二发射天线T2、第三发射天线T3、第四发射天线T4为Z方向发射天线;第五发射天线T5、第六发射天线T6为X方向发射天线;第一接收天线R1、第二接收天线R2为轴向接收天线;第五接收天线R5、第六接收天线R6为XZ面倾斜接收天线;第三接收天线R3、第四接收天线R4为YZ面倾斜接收天线;所有倾斜天线与仪器轴向夹角为45°;其中,轴向为Z向。The first transmitting antenna T1, the second transmitting antenna T2, the third transmitting antenna T3, and the fourth transmitting antenna T4 are Z-direction transmitting antennas; the fifth transmitting antenna T5 and the sixth transmitting antenna T6 are X-direction transmitting antennas; the first receiving antenna R1 and the second receiving antenna R2 are axial receiving antennas; the fifth receiving antenna R5 and the sixth receiving antenna R6 are XZ-plane inclined receiving antennas; the third receiving antenna R3 and the fourth receiving antenna R4 are YZ-plane inclined receiving antennas; the angle between all inclined antennas and the instrument axis is 45°; wherein the axis is the Z direction.
本发明实施例中,随钻测井仪器采取3种测量工作频率:2MHz、400KHz与100KHz,并随着随钻测井仪器旋转,按16扇区记录仪器工具面角及各接收天线信号,经井下数字信号处理技术DSP和现场可编程逻辑门阵列FPGA控制运算结构的数据快速处理,得以实现常规电阻率测量、方位电阻率成像测量、地质成像测量和各向异性测量等多类测井需求。随钻测井仪器含有共5类发射-接收天线系模式:共轴天线系、X轴向发射-Z轴向接收、Z轴向发射-XZ面倾斜接收天线系,X轴向发射-XZ面倾斜接收天线系与X轴向发射-YZ面倾斜接收;可见,以上天线系模式均能够采用前述测井分量提取方法,直接计算并综合提取3个方向中的全部9个分量,同时这也是“三维全息”的概念;因此,该随钻测井仪器在测井工程任务中,具备着不可替代的“三维全息”的全息分量优势。全息分量的使用,是后续构建的方位各向异性信号得以最大化地包含地层电阻率各向异性信息的前提。In the embodiment of the present invention, the logging while drilling instrument adopts three measurement working frequencies: 2MHz, 400KHz and 100KHz, and records the tool face angle of the instrument and the signals of each receiving antenna according to 16 sectors as the logging while drilling instrument rotates. After the data of the downhole digital signal processing technology DSP and the field programmable logic gate array FPGA control operation structure is quickly processed, conventional resistivity measurement, azimuthal resistivity imaging measurement, geological imaging measurement and anisotropy measurement and other logging requirements can be realized. The logging while drilling instrument contains a total of 5 types of transmitting-receiving antenna system modes: coaxial antenna system, X-axis transmitting-Z-axis receiving, Z-axis transmitting-XZ plane tilt receiving antenna system, X-axis transmitting-XZ plane tilt receiving antenna system and X-axis transmitting-YZ plane tilt receiving; it can be seen that the above antenna system modes can adopt the above logging component extraction method to directly calculate and comprehensively extract all 9 components in 3 directions, which is also the concept of "three-dimensional holography"; therefore, the logging while drilling instrument has an irreplaceable advantage of "three-dimensional holography" holographic components in logging engineering tasks. The use of holographic components is a prerequisite for the subsequent construction of azimuthal anisotropy signals to maximize the inclusion of formation resistivity anisotropy information.
本发明实施例中,随钻测井仪器的电各向异性识别应用基于随钻测井仪器的测井分量提取方法实现;In the embodiment of the present invention, the electrical anisotropy identification application of the logging while drilling instrument is implemented based on the logging component extraction method of the logging while drilling instrument;
步骤V1、以对称天线逆补偿和多源距聚焦的模式对电各向异性的分量进行提取,得到主分量、和交叉分量、、、、、。Step V1: Extract the electrical anisotropy component by using the symmetric antenna inverse compensation and multi-source focusing mode to obtain the main component , and cross components , , , , , .
根据在先前的研究中,已规定随钻测井仪器的各向异性测量主要可选取2MHz与400KHz的工作频率进行。源距越大,定向信号越强,能预测的层界面的距离越大,而源距越小,定向信号则对地层的电磁场敏感性越强,能获得的地质信息更为丰富。基于以上概念,使随钻测井仪器更大程度地停留在储层内,提高储层评价质量,选择以下列天线系为基础进行信号构建。选择随钻测井仪器中X轴向发射-XZ面倾斜接收天线系:T5-R5、T6-R6对称天线系,在多扇区下计算提取出分量与;选择X轴向发射-YZ面倾斜接收天线系:T5-R3、T6-R4对称天线系,在多扇区下计算提取分量与;Z轴向发射-XZ面倾斜接收天线系:T3-R5、T4-R6与T1-R5、T2-R6两组对称天线系,形成“多源距聚焦”的构建模式,并在多扇区下计算提取含更丰富测井信息量的多源距分量与;选择仪器中X轴向发射-XZ面倾斜接收天线系:T5-R5、T6-R6与X轴向发射-YZ面倾斜接收天线系:T5-R3、T6-R4两组对称天线系,在多扇区下计算提取多源距分量与。其中所涉及的全部份量均采用对称天线逆补偿以放大地层各向异性响应,并以对应垂直轴向分量的加和比值形式进行信号构建。According to previous studies, it has been stipulated that the anisotropy measurement of the logging while drilling instrument can be mainly carried out at the operating frequencies of 2MHz and 400KHz. The greater the source distance, the stronger the directional signal, and the greater the distance of the layer interface that can be predicted. The smaller the source distance, the stronger the sensitivity of the directional signal to the electromagnetic field of the formation, and the richer the geological information that can be obtained. Based on the above concepts, in order to make the logging while drilling instrument stay in the reservoir to a greater extent and improve the quality of reservoir evaluation, the following antenna system is selected as the basis for signal construction. Select the X-axis transmitting-XZ plane tilted receiving antenna system in the logging while drilling instrument: T5-R5, T6-R6 symmetrical antenna system, and calculate and extract the components under multiple sectors. and ; Select the X-axis transmitting-YZ plane tilt receiving antenna system: T5-R3, T6-R4 symmetrical antenna system, calculate and extract components under multi-sector and ; Z-axis transmitting-XZ plane tilted receiving antenna system: two sets of symmetrical antenna systems T3-R5, T4-R6 and T1-R5, T2-R6, forming a "multi-source distance focusing" construction mode, and calculating and extracting multi-source distance components with richer logging information in multiple sectors. and ; Select the two symmetrical antenna systems of X-axis transmitting-XZ plane tilt receiving antenna system: T5-R5, T6-R6 and X-axis transmitting-YZ plane tilt receiving antenna system: T5-R3, T6-R4 in the instrument, and calculate and extract multi-source distance components under multi-sectors and All the components involved are inversely compensated by symmetrical antennas to amplify the anisotropic response of the formation, and the signal is constructed in the form of the sum ratio of the corresponding vertical axial components.
步骤V2、利用步骤V1中的主分量和交叉分量,通过随钻测井仪器同步计算幅度比信号与相位差信号,构建幅度比信号与相位差信号,其表达式分别为:Step V2: Using the principal component and cross component in step V1, the amplitude ratio signal and the phase difference signal are synchronously calculated by the logging while drilling instrument to construct the amplitude ratio signal Phase difference signal , whose expressions are:
; ;
; ;
其中,angle为取复数的角度。Here, angle is the complex angle.
本发明实施例中,将幅度比信号与相位差信号作为电各向异性识别信号,用于完成目标应用。以上幅度比信号与相位差信号作为各向异性信号的本质与主流随钻测井仪器相同,即不同分量的组合形式,信号包含了主分量、与交叉分量、、、、、;其中,两个主分量主要用来探测来自地层界面的电阻率变化信息,指示仪器的地层方位,来自三向的交叉分量能够在全三维方向上,最大程度测量地层电阻率各向异性信息,多类信息的交错综合可以使仪器对各向异性信息评价的完备性尽可能最大化。以上信号在三维全息随钻电磁波电阻率仪器中,联合不同频率、源距、间距、天线组合的应用,可解决电各向异性识别能力欠佳的问题。In the embodiment of the present invention, the amplitude ratio signal Phase difference signal As an electrical anisotropy identification signal, it is used to complete the target application. Phase difference signal The essence of anisotropic signals is the same as that of mainstream logging while drilling tools, that is, the combination of different components. The signal contains the main component , With cross component , , , , , Among them, the two main components are mainly used to detect resistivity change information from the formation interface and indicate the formation orientation of the instrument. The cross components from three directions can measure the anisotropy information of the formation resistivity to the greatest extent in all three-dimensional directions. The interlaced integration of multiple types of information can maximize the completeness of the instrument's evaluation of anisotropy information. The above signals in the three-dimensional holographic electromagnetic wave resistivity instrument, combined with the application of different frequencies, source distances, spacings, and antenna combinations, can solve the problem of poor electrical anisotropy recognition ability.
为了证明应用具备充足的电各向异性识别能力,对其进行一系列效果验证,且为了解决随钻测井仪器的井下传输带宽有限,需要最少的传输信号表达更全面电各向异性的问题, 通过识别效果的分析,对可用信号进行进一步筛选。In order to prove that the application has sufficient electrical anisotropy recognition capability, a series of effect verifications were carried out. In order to solve the problem that the downhole transmission bandwidth of the logging while drilling instrument is limited and the minimum transmission signal is needed to express a more comprehensive electrical anisotropy, the available signals were further screened through the analysis of the recognition effect.
步骤V3、根据步骤V2,设置三层均匀地层模型,随钻测井仪器工作频率取2MHz,井斜角=50°,设定模型的围岩层为各向同性地层,各向异性系数λ为1,此时水平电阻率和垂直电阻率相同,均为1;目的层分别设定各向同性地层中各向异性系数λ=1,水平电阻率和垂直电阻率均为4;各向异性地层中各向异性系数λ=2,水平电阻率为4,垂直电阻率为16;上围岩地层边界位置的垂直深度TVD为5m,下围岩地层边界位置的垂直深度TVD为10,中间目的层厚度为5m,通过广义反射系数解析法计算的电各向异性信号响应正演模拟,获取其对应的模拟结果。Step V3: According to step V2, a three-layer uniform formation model is set, the operating frequency of the logging while drilling instrument is 2 MHz, and the well inclination angle is =50°, the surrounding rock layer of the model is set to be isotropic, and the anisotropy coefficient λ is 1. At this time, the horizontal resistivity and vertical resistivity Same, both are 1 ; The target layer is set to have anisotropy coefficient λ=1 in the isotropic formation and horizontal resistivity and vertical resistivity All 4 ; In anisotropic formations, the anisotropy coefficient λ=2, and the horizontal resistivity For 4 , vertical resistivity For 16 The vertical depth TVD of the upper surrounding rock stratum boundary is 5m, the vertical depth TVD of the lower surrounding rock stratum boundary is 10, the thickness of the middle target layer is 5m, and the corresponding simulation results are obtained by forward modeling of the electrical anisotropy signal response calculated by the generalized reflection coefficient analytical method.
本发明实施例中,如图9a和图9b所示,其中,图9a中横坐标为井眼垂直深度TVD,纵坐标为各向异性幅度比信号;图9b中横坐标为井眼垂直深度TVD,纵坐标为各向异性相位差信号;当随钻测井仪器处于围岩各向同性层时,幅度比信号与相位差信号维持在恒定0值;当随钻测井仪器由围岩层接近目的层时,幅度比信号与相位差信号的响应出现下降,随后响应明显上升直至最大值。在进入目的层时,两信号响应自最大值开始明显下降,最后在极小值处产生一次波动并达到稳定值,若目的层为各向同性层,该稳定值仍恒定为0,若目的层为各向异性层,该恒定值将明显高于围岩层的恒定0值响应,幅度比信号与相位差信号的有效动态范围分别为17dB与82°。由于随钻测井仪器采用高频测量,探测波长较短,信号在临近各向异性层界面时的反射响应较大,因此相位差信号的响应在最大值尖峰后的下降趋势中,额外产生了一次上下波动,而非单调下降。当随钻测井仪器离开各向异性层,再次进入围岩各向同性层,两信号产生与进入目的层时互为对称的响应,并在围岩层中重新恒定为0值。In the embodiment of the present invention, as shown in FIG9a and FIG9b, the horizontal axis in FIG9a is the vertical depth TVD of the wellbore, and the vertical axis is the anisotropy amplitude ratio signal ; In Figure 9b, the horizontal axis is the vertical depth TVD of the wellbore, and the vertical axis is the anisotropic phase difference signal ; When the logging while drilling tool is in the isotropic layer of the surrounding rock, the amplitude ratio signal Phase difference signal Maintain a constant value of 0; when the logging while drilling tool approaches the target layer from the surrounding rock layer, the amplitude ratio signal Phase difference signal The response of the two signals decreases, and then the response increases significantly until it reaches the maximum value. When entering the target layer, the response of the two signals decreases significantly from the maximum value, and finally produces a fluctuation at the minimum value and reaches a stable value. If the target layer is an isotropic layer, the stable value is still constant at 0. If the target layer is an anisotropic layer, the constant value will be significantly higher than the constant 0 value response of the surrounding rock layer, and the amplitude is higher than the signal. Phase difference signal The effective dynamic ranges are 17dB and 82° respectively. Since the logging while drilling instrument uses high frequency measurement and the detection wavelength is short, the reflection response of the signal near the anisotropic layer interface is large, so the phase difference signal The response of the logging tool produces an additional up-and-down fluctuation in the downward trend after the maximum peak, rather than a monotonous decline. When the logging tool leaves the anisotropic layer and enters the isotropic layer of the surrounding rock again, the two signals produce responses that are symmetrical to each other when entering the target layer, and they are stabilized to 0 in the surrounding rock layer.
幅度比信号与相位差信号因各向异性系数差异,响应产生不同的恒定值,表现出了各向异性地层优秀的识别能力,且在地层界面处产生了清晰的尖峰响应,对称的界面响应同时表现出了仪器的方位性,满足了三维全息随钻电阻率仪器对各向异性信号的要求。Amplitude ratio signal Phase difference signal Due to the difference in anisotropy coefficients, the response produces different constant values, demonstrating the excellent recognition ability of anisotropic formations, and a clear peak response is produced at the formation interface. The symmetrical interface response also demonstrates the orientation of the instrument, meeting the requirements of the three-dimensional holographic resistivity downhole instrument for anisotropic signals.
虽然幅度比信号与相位差信号都具备了各项异性地层的识别性能,但在实际随钻测井中,井下传输带宽资源的紧张,要求仪器使用最有限的信号,表达更充分的测井资料处理和解释评价方法的信息,针对这一问题,需要对幅度比信号与相位差信号进行进一步筛选,因此需要对随钻电磁波电阻率测井的响应特性联合其他井下条件,展开进一步分析。Although the amplitude is larger than the signal Phase difference signal Both have the ability to identify various anisotropic formations, but in actual LWD, the tight downhole transmission bandwidth resources require the instrument to use the most limited signal to express more complete information on logging data processing and interpretation and evaluation methods. To address this issue, it is necessary to further screen the amplitude ratio signal and the phase difference signal. Therefore, it is necessary to further analyze the response characteristics of LWD electromagnetic wave resistivity logging in combination with other downhole conditions.
步骤V4、设置三层均匀地层模型,井斜角=50°,上围岩地层边界位置的垂直深度TVD为5m,下围岩地层边界位置的垂直深度TVD为10m,设定模型的围岩层为各向同性层,目的层设定各向异性系数由1至5逐渐增加,选取随钻测井仪器工作频率为2MHz和400KHz的条件下进行正演模拟,获取其对应的模拟结果。Step V4: Set up a three-layer uniform formation model and well inclination angle =50°, the vertical depth TVD of the upper surrounding rock stratum boundary is 5m, the vertical depth TVD of the lower surrounding rock stratum boundary is 10m, the surrounding rock layer of the model is set as an isotropic layer, the anisotropy coefficient of the target layer is set to gradually increase from 1 to 5, and the forward simulation is carried out under the conditions of 2MHz and 400KHz working frequencies of the logging while drilling instrument to obtain the corresponding simulation results.
本发明实施例中,如图10a至图10d所示,当随钻测井仪器位于不同各项异性系数的地层时,响应存在明显差异并且有规律性变化,各向异性越强,幅度比信号与相位差信号响应的尖峰与在目的层中的恒定值数值越大,λ增至3之前,响应的有效动态范围增加更为明显,大于3后有效动态范围增加更为缓慢。由图10a、图10b与图10c、图10d比较可得,相位差各向异性地层数值分布更分散,且响应区分度大,因此相位差信号的各向异性识别效果优于幅度比信号。由图10a、图10b与图10c、图10d比较可得,400KHz的信号响应值相对于2MHz更小,各向异性的区分性能更弱,而400KHz信号相较2MHz,可在地层界面处提前约0.6m对其产生超过国际标准测量精度(0.02dB/0.2°)的响应,可更明显的表达仪器的方位特性。In the embodiment of the present invention, as shown in FIG. 10a to FIG. 10d, when the logging while drilling instrument is located in formations with different anisotropy coefficients, the responses are obviously different and change regularly. The stronger the anisotropy, the greater the amplitude ratio signal. Phase difference signal The larger the peak value of the response and the constant value in the target layer, the more obvious the increase of the effective dynamic range of the response is before λ increases to 3, and the more slowly the effective dynamic range increases after it is greater than 3. By comparing Figures 10a and 10b with Figures 10c and 10d, it can be seen that the phase difference The distribution of anisotropic formation values is more dispersed, and the response differentiation is large, so the phase difference signal The anisotropy recognition effect is better than the amplitude ratio signal Comparing Figures 10a and 10b with Figures 10c and 10d, it can be seen that the signal response value of 400KHz is smaller than that of 2MHz, and the anisotropy discrimination performance is weaker. However, compared with 2MHz, the 400KHz signal can produce a response exceeding the international standard measurement accuracy (0.02dB/0.2°) at the formation interface about 0.6m in advance, which can more clearly express the azimuth characteristics of the instrument.
步骤V5、设置三层均匀地层模型,上围岩地层边界位置的垂直深度TVD为TVD=5m;下围岩地层边界位置的垂直深度TVD为10m;模型的围岩层为各向同性层,其各向异性系数λ为1,水平电阻率和垂直电阻率均为1 ;中间目的层的各向异性系数λ固定为5,水平电阻率为4,垂直电阻率为100,改变井斜角,将其由0°逐渐增至90°,选取随钻测井仪器工作频率为2MHz和400KHz的条件下进行正演模拟,获取其对应的模拟结果。Step V5: Set a three-layer uniform stratum model. The vertical depth TVD of the upper surrounding rock stratum boundary is TVD=5m; the vertical depth TVD of the lower surrounding rock stratum boundary is 10m; the surrounding rock layer of the model is an isotropic layer, its anisotropy coefficient λ is 1, and the horizontal resistivity and vertical resistivity are all 1; the anisotropy coefficient λ of the intermediate target layer is fixed at 5, and the horizontal resistivity is 4, vertical resistivity To 100, change the well inclination , gradually increase it from 0° to 90°, select the working frequency of the logging while drilling instrument as 2MHz and 400KHz to carry out forward simulation and obtain the corresponding simulation results.
本发明实施例中,如图11a至图11d所示,幅度比信号与相位差信号的尖峰与稳定值的幅值在=0°到=55°左右逐渐上升,并达到最大值,在=55°之后开始下降。幅度比信号的响应在靠近界面处的下降部分,随井斜角的增加,不再单调,而是逐渐变为先上升后下降,一定程度上收到了井斜角的影响;相位差信号的响应位置不会受到井斜角变化的影响,信号对各向异性地层表现出的响应特性,仅在有效动态范围上受到了井斜角变化的影响,对各项异性的探测能力不减弱。In the embodiment of the present invention, as shown in FIG. 11a to FIG. 11d, the amplitude ratio signal Phase difference signal The peak and stable value of =0° to =55° and gradually rises to a maximum value. =55° and then starts to decrease. The response of the descending part near the interface changes with the well inclination. The increase is no longer monotonous, but gradually rises first and then falls, which is affected by the well inclination to a certain extent; the phase difference signal The response position will not be affected by the change of well inclination angle. The response characteristics of the signal to anisotropic formations are only affected by the change of well inclination angle in the effective dynamic range, and the detection capability of various anisotropies is not weakened.
以上分析表明幅度比信号与相位差信号在不同地层下都具有充足的识别能力,然而相位差信号对地层电阻率各向异性的识别能力优于幅度比信号,且在2MHz与400KHz的工作频率下均具有测量优势,可选择该信号完成井下电各向异性识别任务。The above analysis shows that both the amplitude ratio signal and the phase difference signal have sufficient recognition capabilities in different formations. However, the phase difference signal has better recognition ability for formation resistivity anisotropy than the amplitude ratio signal, and has measurement advantages at both 2MHz and 400KHz operating frequencies. This signal can be selected to complete the task of identifying downhole electrical anisotropy.
步骤V6、通过步骤V5对相位差信号进行筛选,以模拟电各向异性识别的方位成像。Step V6: Screen the phase difference signal through step V5 to simulate the azimuth imaging of electrical anisotropy recognition.
本发明实施例中,如图12所示,模拟真实的典型砂泥岩互层模型进行仪器响应成像。该模型由5层地层组成,第1层为各向同性地层,满足==1;第2层为各向异性地层,满足=4,=12;第3层为各项同性地层,满足==1;第4层为各项同性地层,满足==3;第5层为各向异性地层,满足=8,=40。图12中由上到下,第一道为地层模型与井眼轨迹,其中,TVD表示井眼垂直深度,THD表示井眼的水平距离;第二道为相位差信号响应曲线;第三道为该信号下联合工具面角的各向异性成像。In the embodiment of the present invention, as shown in FIG12 , a typical sandstone-mudstone interbed model is simulated to perform instrument response imaging. The model consists of five layers, the first layer is an isotropic layer, and satisfies = =1 ; The second layer is an anisotropic stratum, satisfying =4 , =12 ; The third layer is an isotropic layer, satisfying = =1 ; The fourth layer is an isotropic layer, satisfying = =3 ; The fifth layer is an anisotropic stratum, satisfying =8 , =40 From top to bottom in Figure 12, the first track is the formation model and wellbore trajectory, where TVD represents the vertical depth of the wellbore and THD represents the horizontal distance of the wellbore; the second track is the phase difference signal Response curve; the third track is the anisotropic imaging of the joint tool face angle under this signal.
模拟仪器在该模型中以大井斜角(=60°)由第1层穿入第5层,并在第5层中转动钻进至对称角度后穿回第1层。相位差信号响应曲线由两种频率下的响应组合表达而成,界面处的尖峰响应由两种频率加和组合表达,稳定值的响应由2MHz的信号响应表达,以在获得更直观的各向异性信息下,更优的表达仪器的方位特性。通过该响应曲线,通过引入仪器旋转角的方式,使用方位成像法,形成仪器的各向异性成像。The simulation tool is used in this model with a large well inclination ( =60°) from the 1st layer to the 5th layer, and then rotate and drill to a symmetrical angle in the 5th layer and then go back to the 1st layer. Phase difference signal The response curve is expressed by the combination of responses at two frequencies. The peak response at the interface is expressed by the sum of the two frequencies. The response of the stable value is expressed by the signal response of 2MHz. This is to better express the azimuth characteristics of the instrument while obtaining more intuitive anisotropic information. In this way, azimuthal imaging is used to form anisotropic imaging of the instrument.
本发明实施例中,如图12所示,当井眼轨迹通过地层界面时,信号成像显示出明显的正余弦特征,并通过设置门槛值,对响应产生的尖峰进行识别判断,使用亮暗斑交错的形式表征仪器的进入或离开地层界面的方位特性。In an embodiment of the present invention, as shown in FIG12 , when the borehole trajectory passes through the formation interface, the signal imaging shows obvious sine and cosine characteristics, and by setting a threshold value, the peaks generated by the response are identified and judged, and the azimuth characteristics of the instrument entering or leaving the formation interface are characterized in the form of alternating bright and dark spots.
在TVD值下降阶段,首先,在井眼轨迹位于各向同性层1时,由于信号响应值为0,成像无特征;在井眼轨迹由层1入层各向异性层2时,成像通过信号的尖峰,呈现出亮斑,表征进入新的地层,并在之后对各向异性层特性,显示为对称的条带;在由层2穿入层3时,成像通过信号的下降尖峰呈现出暗斑,表征进入新的地层,且由于层3为各向同性地层,此时成像无明显特征;在由层3穿入层4时,成像再次呈现出亮斑,虽然层4电阻率与层3电阻率不相同,然而其仍为各向同性层,成像无明显特征,这也良好的证明了信号不受电阻率对比度的干扰影响;在由层4穿入层5时,成像交错呈现暗斑,在各项异性层5中,成像仍显示为对称的条带,然而该阶段井斜角为变化值,对称的条带按照THD增长的方向由亮逐渐变暗,表现出了不同的特性,可以通过条带颜色的变化的现象,直接指导仪器的井斜方位,便于仪器在各向异性地层中进行方位调整。在TVD上升阶段,井眼轨迹由层5穿回层4时,信号响应与穿入时上下对称,本应交错显示的亮斑因为响应幅值小于0而变为暗斑,以本现象表征仪器再次穿过了同一地层界面;在之后的轨迹中,成像继续遵循规律,依照层界面,产生交错的亮暗斑,并在各向异性地层处呈现对称的条带。In the TVD value decreasing stage, first, when the borehole trajectory is located in the isotropic layer 1, the imaging has no features because the signal response value is 0; when the borehole trajectory enters the anisotropic layer 2 from layer 1, the imaging passes through the peak of the signal and presents a bright spot, indicating that it has entered a new formation, and then the anisotropic layer characteristics are displayed as symmetrical strips; when penetrating from layer 2 to layer 3, the imaging passes through the descending peak of the signal and presents a dark spot, indicating that it has entered a new formation, and since layer 3 is an isotropic formation, the imaging has no obvious features at this time; when penetrating from layer 3 to layer 4, the imaging again presents a bright spot, although Although the resistivity of layer 4 is different from that of layer 3, it is still an isotropic layer and the imaging has no obvious features. This also proves that the signal is not affected by the interference of resistivity contrast. When penetrating from layer 4 to layer 5, the imaging is staggered and dark spots appear. In the anisotropic layer 5, the imaging still appears as symmetrical strips. However, the well inclination angle is a variable value at this stage. The symmetrical strips gradually change from bright to dark in the direction of THD growth, showing different characteristics. The well inclination azimuth of the instrument can be directly guided by the phenomenon of strip color change, which is convenient for the instrument to adjust the azimuth in anisotropic formations. In the TVD rising stage, when the borehole trajectory passes from layer 5 back to layer 4, the signal response is symmetrical up and down with the penetration. The bright spots that should be staggered become dark spots because the response amplitude is less than 0. This phenomenon indicates that the instrument has passed through the same formation interface again. In the subsequent trajectory, the imaging continues to follow the rules, generating staggered bright and dark spots according to the layer interface, and presenting symmetrical strips in the anisotropic formation.
综上,信号在方位成像中,通过对称条带的方式表达地层的电阻率各向异性信息,通过亮暗斑的形式表达仪器的方位信息,有效地综合识别电各向异性,足以证明,自主研发的三维全息随钻电阻率仪器可以借助该信号,获得充足的电各向异性识别能力,可清晰的识别各向异性地层,且可以获得仪器在不同地层界面处的方位信息,得以为仪器在各向异性地层中的随钻导向工作,以及后续电阻率各向异性的反演评价工作降低难度。In summary, in azimuth imaging, the signal expresses the resistivity anisotropy information of the formation in the form of symmetrical strips, and expresses the azimuth information of the instrument in the form of bright and dark spots, effectively and comprehensively identifying the electrical anisotropy. This is sufficient to prove that the independently developed three-dimensional holographic downhole resistivity instrument can use this signal to obtain sufficient electrical anisotropy recognition capability, can clearly identify anisotropic formations, and can obtain the azimuth information of the instrument at different formation interfaces, which can reduce the difficulty of the downhole guidance work of the instrument in anisotropic formations and the subsequent inversion evaluation of resistivity anisotropy.
本发明实施例,实现了测井全分量的提取计算。对应求解参变量方程~(共面)、~(异面)、~(异面),通过考虑仪器方位的旋转测量,对共面与异面中代数方程构成的参变量方程组分别求解,可获得、、、、、、、、全部3方向上的9个分量在对应天线对中固定的提取式。对于任意的单向发射单向接收天线对,均可使用以上方法的分量提取式,直接计算具体选定分量的测井响应,在实际工程中结合仪器天线模式,直接计算使用选定分量,支撑目标功能信号构建,获取全面的电各向异性信息。The embodiment of the present invention realizes the extraction and calculation of all components of well logging. ~ (coplanar), ~ (different surface), ~ By considering the rotation measurement of the instrument orientation, the parametric equations consisting of the algebraic equations in the coplanar and skew planes are solved separately, and the following equations can be obtained: , , , , , , , , The 9 components in all 3 directions are fixed in the corresponding antenna pair. For any unidirectional transmitting and unidirectional receiving antenna pair, the component extraction formula of the above method can be used to directly calculate the logging response of the specific selected component. In actual engineering, combined with the instrument antenna mode, the selected component is directly calculated and used to support the construction of the target functional signal and obtain comprehensive electrical anisotropy information.
通过以上方法,应用于自主研发的三维全息随钻方位电磁波电阻率仪器中,使用全三维交叉分量构建新型各向异性信号:幅度比信号与相位差信号,使仪器能通过该应用,获得充足的地层电各向异性信息识别能力。Through the above method, it is applied to the independently developed three-dimensional holographic drilling azimuth electromagnetic wave resistivity instrument, and a new type of anisotropic signal is constructed using the full three-dimensional cross component: the amplitude ratio signal Phase difference signal , so that the instrument can obtain sufficient formation electrical anisotropy information identification capabilities through this application.
考虑到测井仪器普遍面对的传输带宽资源限制问题,由于相位差信号相比于幅度比信号,对电各项异性敏感性更高,识别更加精准,进一步选择相位差信号作为仪器的各向异性信号,使仪器仅占用1组信号的传输带宽下,表达全面的电各向异性信息。Considering the transmission bandwidth resource limitation commonly faced by logging instruments, due to the phase difference signal Compared to the amplitude ratio signal , which is more sensitive to electrical anisotropy, more accurate in identification, and further selects phase difference signals As the anisotropy signal of the instrument, the instrument only occupies the transmission bandwidth of one set of signals and expresses comprehensive electrical anisotropy information.
本发明提供的技术方案中,该方法包括获取信号电压9个分量的分量矩阵;设定单方向发射单方向接收测量单元模型,通过三角坐标变换,得到任意方向上的发射-接收的响应通式;设定共面倾斜发射-倾斜接收模型,固定旋转角,获得响应;根据响应对至进行求解,获得至;根据至、与,获得所有共面天线系模型的分量;设定仪器线圈系的异面模式,获得XZ面倾斜发射-YZ面倾斜接收模式下的响应,并获得至、至;根据获得至、至获得所有异面天线系模型的分量,并结合所有共面天线系模型的分量,以获得9个分量,该方法实现了在实时导向中直接获取电阻率各向异性信息,并且提高了随钻测井仪器的电各向异性识别能力,有效地保证了随钻测井仪器的工作。In the technical solution provided by the present invention, the method includes obtaining a component matrix of 9 components of the signal voltage; setting a unidirectional transmitting and unidirectional receiving measurement unit model, and obtaining a general response formula of transmitting and receiving in any direction through triangular coordinate transformation; setting a coplanar tilted transmitting and tilted receiving model, fixing the rotation angle, and obtaining a response ; According to the response right to Solve and obtain to ;according to to , and , obtain the components of all coplanar antenna system models; set the out-of-plane mode of the instrument coil system to obtain the response in the XZ plane tilted transmission-YZ plane tilted reception mode , and obtain to , to According to the obtained to , to The components of all out-of-plane antenna system models are obtained, and combined with the components of all coplanar antenna system models to obtain 9 components. This method realizes the direct acquisition of resistivity anisotropy information in real-time guidance, improves the electrical anisotropy recognition capability of the logging while drilling instrument, and effectively ensures the operation of the logging while drilling instrument.
所属领域的技术人员可以清楚地了解到,为描述的方便和简洁,上述描述的系统,装置和单元的具体工作过程,可以参考前述方法实施例中的对应过程,在此不再赘述。Those skilled in the art can clearly understand that, for the convenience and brevity of description, the specific working processes of the systems, devices and units described above can refer to the corresponding processes in the aforementioned method embodiments and will not be repeated here.
以上所述仅为本发明的较佳实施例而已,并不用以限制本发明,凡在本发明的精神和原则之内,所做的任何修改、等同替换、改进等,均应包含在本发明保护的范围之内。The above description is only a preferred embodiment of the present invention and is not intended to limit the present invention. Any modifications, equivalent substitutions, improvements, etc. made within the spirit and principles of the present invention should be included in the scope of protection of the present invention.
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Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
US6765385B2 (en) * | 2001-11-13 | 2004-07-20 | Weatherford/Lamb, Inc. | Method, apparatus and system for compensating the effects of borehole variations |
CN100592441C (en) * | 2008-03-14 | 2010-02-24 | 国网电力科学研究院 | Electronic current transformer for UHV transmission line and its corona loss measuring device |
US9354347B2 (en) * | 2012-12-13 | 2016-05-31 | Baker Hughes Incorporated | Method and apparatus for deep transient resistivity measurement while drilling |
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WO2016108909A1 (en) * | 2014-12-31 | 2016-07-07 | Halliburton Energy Serives, Inc. | Formation logging using multicomponent signal-based measurement of anisotropic permittivity and resistivity |
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Non-Patent Citations (3)
Title |
---|
The configuration and detection characteristics of a 3D holographic LWD instrument antenna system based on multi-component EM induction theory;Yixian Yu et al.;《Journal of Applied Geophysics》;20240503;第1-9页 * |
三维全息随钻方位电磁波电阻率仪器设计;房立奇等;《三维全息随钻方位电磁波电阻率仪器设计》;20240215;第1卷(第2期);第1-31页 * |
房立奇等.三维全息随钻方位电磁波电阻率仪器设计.《三维全息随钻方位电磁波电阻率仪器设计》.2024,第1卷(第2期),第1-31页. * |
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