CN111537544B - Improve nuclear magnetic resonance T 2 Conversion method for spectral characterization of pore size distribution precision of tight reservoir - Google Patents
Improve nuclear magnetic resonance T 2 Conversion method for spectral characterization of pore size distribution precision of tight reservoir Download PDFInfo
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Abstract
Description
技术领域technical field
本发明涉及储层预测技术,尤其涉及致密储层孔隙结构的核磁共振表征方法,属于石油勘探开发领域。The invention relates to reservoir prediction technology, in particular to a nuclear magnetic resonance characterization method for the pore structure of tight reservoirs, and belongs to the field of petroleum exploration and development.
背景技术Background technique
致密储层相比较与常规储层,主要的特点之一就是孔喉空间较小,这使得流体在其中的运移难度很大。因此,准确评估致密储层的孔隙结构是评价致密油气资源潜力、可采性和产能的前提条件之一,核磁共振是一个比较常用的测试手段,该方法需要将饱和水状态下的T2转换为孔隙半径。这样的优点在于(1)结合离心或者烘干手段,可以明确束缚流体的孔径分布;(2)结合饱锰样的驰豫谱,可以明确油相占据的孔径分布;(3)结合恒速压汞实验,可以明确喉道对束缚流体或者残余油的控制。Compared with conventional reservoirs, one of the main characteristics of tight reservoirs is the small pore throat space, which makes it very difficult for fluids to migrate in them. Therefore, accurate evaluation of the pore structure of tight reservoirs is one of the prerequisites for evaluating the potential, recoverability and production capacity of tight oil and gas resources. Nuclear magnetic resonance is a commonly used testing method. is the pore radius. The advantage of this is that (1) combined with centrifugation or drying means, the pore size distribution of the bound fluid can be clarified; (2) combined with the relaxation spectrum of the manganese-saturated sample, the pore size distribution occupied by the oil phase can be clarified; (3) combined with the constant velocity pressure Mercury experiments can clarify throat control of bound fluid or residual oil.
通常将T2转换为孔径分布是结合汞注入的实验手段。常规的转换方法是通过公式推导得到了:T2=Crt,其中,C为转换系数,rt为汞注入得到的孔径大小。上述方法在CN104634718A、CN106249306A等现有技术中有相关记载。但是该方法存在的问题是,T2和rt的线性关系并不能很好的对二者进行拟合。可能是由于复杂的孔喉结构和较小的孔径分布,这在致密储层中表现的更加明显。为此,也有部分研究学者在常规方法的基础上得到了经验公式:其中,n为常数。但该式不能通过数学推导得到,同时缺少物理意义。并且,通常的转化方法是基于实测的压汞孔径分布数据,如果实测数据在某一进汞饱和度段内分布密集,则转换公式会更多的考虑这部分权重,使得实测数据稀疏段的拟合程度较差现,导致利用T2转换为孔径分布的效果较差。Often the conversion of T2 to a pore size distribution is an experimental approach in conjunction with mercury injection. The conventional conversion method is derived through the formula: T 2 =Cr t , wherein, C is the conversion coefficient, and rt is the pore size obtained by mercury injection. The above method has related records in CN104634718A, CN106249306A and other prior art. However, the problem with this method is that the linear relationship between T 2 and r t cannot fit them well. It may be due to the complex pore throat structure and smaller pore size distribution, which is more obvious in tight reservoirs. For this reason, some researchers have obtained empirical formulas based on conventional methods: Among them, n is a constant. But this formula cannot be obtained through mathematical derivation, and lacks physical meaning at the same time. Moreover, the usual conversion method is based on the measured mercury injection pore size distribution data. If the measured data is densely distributed in a certain mercury saturation range, the conversion formula will take this part of the weight into consideration, so that the simulated data for the sparse segment of the measured data The degree of integration is poor, resulting in poor conversion of T2 to pore size distribution.
因此,本发明提出了利用T2转换孔径分布的新方法,在常用推导的基础上,还充分考虑了圆柱形孔隙模型。一方面说明了线性关系并不能很好的对横向弛豫时间T2进行孔径分布转换,另一方面提出的模型更符合物理意义。此外,通过本发明对压汞孔径大小分布数据的处理,能够有助于提高通过核磁共振实验得到孔径分布的准确性,相对准确的评价致密油气资源潜力。Therefore, the present invention proposes a new method of transforming the pore size distribution by using T2 , and on the basis of the usual derivation, the cylindrical pore model is also fully considered. On the one hand, it shows that the linear relationship is not good for transversal relaxation time T 2 to convert the pore size distribution, on the other hand, the proposed model is more in line with the physical meaning. In addition, the processing of the mercury injection pore size distribution data by the present invention can help improve the accuracy of the pore size distribution obtained through the nuclear magnetic resonance experiment, and relatively accurately evaluate the potential of tight oil and gas resources.
发明内容Contents of the invention
本发明的目的是提供一种具有一定物理意义,同时有助于提高核磁共振T2谱表征致密储层孔径分布精度的转换方法,相对准确的评价致密油气资源潜力。The purpose of the present invention is to provide a conversion method that has certain physical significance and helps to improve the accuracy of characterization of tight reservoir pore size distribution by nuclear magnetic resonance T2 spectrum, so as to evaluate the potential of tight oil and gas resources relatively accurately.
为实现上述目的,本发明实施例提供如下技术方案:一种提高核磁共振T2谱表征致密储层孔径分布精度的转换方法,包括如下步骤:In order to achieve the above object, the embodiment of the present invention provides the following technical solution: a conversion method for improving the precision of pore size distribution of tight reservoirs characterized by nuclear magnetic resonance T2 spectrum, comprising the following steps:
步骤一:对饱和地层水的致密储层样品进行核磁共振测试,获得核磁共振T2谱;Step 1: Carry out nuclear magnetic resonance test on the tight reservoir sample saturated with formation water, and obtain the nuclear magnetic resonance T2 spectrum;
步骤二:对干燥致密储层样品进行恒速压汞实验,获得压汞孔径大小分布数据;Step 2: Carry out a constant-speed mercury intrusion experiment on dry tight reservoir samples to obtain mercury intrusion pore size distribution data;
步骤三:对压汞孔径大小分布数据进行分段处理;Step 3: Perform segmentation processing on the mercury injection pore size distribution data;
步骤四:使用圆柱形孔隙模型获得T2与孔径大小之间转换关系;Step 4: Use the cylindrical pore model to obtain the conversion relationship between T2 and the pore size;
步骤五:将步骤三中的各段数据分别使用步骤四中的转换关系得到各段的T2与孔径大小之间的转换方法,从而获得完整的T2谱表征致密储层孔径分布的转换方法。Step 5: Use the conversion relationship in step 4 to obtain the conversion method between T 2 and pore size of each segment of the data in step 3, so as to obtain a complete T 2 spectrum to characterize the conversion method of tight reservoir pore size distribution .
进一步地,步骤三中的分段处理方法为:按照从小孔径到大孔径的顺序,对不同测试点的孔径大小数据进行差值计算,选取孔径差值在一个数量级范围内的孔径大小数据作为一个数据段。Further, the subsection processing method in step 3 is: in the order of small aperture to large aperture, calculate the difference between the aperture size data of different test points, and select the aperture size data whose aperture difference is within an order of magnitude range as a data segment.
进一步地,步骤四的转换关系为:Further, the conversion relationship in step 4 is:
使用KST模型表示的T2与孔隙体积、孔隙流体体积之间的关系:The relationship between T2 , pore volume and pore fluid volume expressed by KST model:
圆柱形孔隙模型中薄层流体的体积为:The volume of a thin layer of fluid in a cylindrical pore model is:
圆柱形孔隙的表面积为:The surface area of a cylindrical pore is:
St=2πrt·l (3)S t =2πr t ·l (3)
将式(2)、式(3)带入式(1)得到Put formula (2) and formula (3) into formula (1) to get
令make
其中,T2表示横向弛豫时间,T2s表示颗粒表面驰豫,Vs表示孔隙流体体积,V表示孔隙体积,Vs t表示圆柱形孔隙模型中薄层流体体积,h表示薄层流体厚度,rt表示孔隙半径,l表示圆柱形高度,St表示为圆柱形孔隙的表面积,ρ2为弛豫率;S/V是孔隙比表面;Fs为形状因子,无量纲,对球状孔隙,Fs=3;对柱状管道,Fs=2。弛豫率ρ2、孔隙形状因子Fs均可近似看作是常数,因此C为定值;Among them, T 2 represents the transverse relaxation time, T 2s represents the particle surface relaxation, V s represents the pore fluid volume, V represents the pore volume, V s t represents the volume of the thin layer fluid in the cylindrical pore model, h represents the thickness of the thin layer fluid , r t represents the pore radius, l represents the cylindrical height, S t represents the surface area of cylindrical pores, ρ 2 is the relaxation rate; S/V is the pore specific surface; F s is the shape factor, dimensionless, for spherical pores , F s =3; for columnar pipes, F s =2. The relaxation rate ρ 2 and the pore shape factor F s can be approximately regarded as constants, so C is a constant value;
将(5)、(6)和(7)带入(4),可以得到T2与孔径大小之间的转换关系:Bringing (5), (6) and (7) into (4), the conversion relationship between T2 and aperture size can be obtained:
进一步地,将各段数据通过最小二乘原理,可以得到各段的C和h值,从而获得各段的T2与孔径大小之间的转换方法;Further, the C and h values of each section can be obtained by the least squares principle by each section of data, thereby obtaining the conversion method between T2 and aperture size of each section;
进一步地,获得完整的T2谱表征致密储层孔径分布的转换方法。Further, a conversion method to obtain the complete T2 spectrum to characterize the pore size distribution of tight reservoirs.
与现有技术相比,本发明具有以下特点和优点:Compared with the prior art, the present invention has the following characteristics and advantages:
1、本发明充分考虑了岩石本身的孔隙结构模型,将核磁中共振常用的平面物理模型改变为与压汞实验一致的圆柱形孔隙模型,提高了核磁共振数据T2和压汞数据获得的孔隙半径之间对应关系的准确性。1. The present invention fully considers the pore structure model of the rock itself, changes the plane physical model commonly used by NMR into a cylindrical pore model consistent with the mercury injection experiment, and improves the pore obtained by the NMR data T2 and the mercury injection data The accuracy of the correspondence between radii.
2、本发明充分考虑了压汞数据分布的特点,使用分段拟合,减少了因为数据本身原因带来的拟合误差。2. The present invention fully considers the characteristics of the mercury intrusion data distribution, uses segmental fitting, and reduces the fitting error caused by the data itself.
附图说明Description of drawings
图1为压汞孔径大小分布数据的分段处理Figure 1 shows the segmentation processing of mercury injection pore size distribution data
图2为平面物理模型到圆柱形孔隙模型的转换过程Figure 2 shows the conversion process from the plane physical model to the cylindrical pore model
图3为本发明的转换方法获得的T2与孔隙半径的拟合关系Fig. 3 is the fitting relation of T obtained by conversion method of the present invention and pore radius
图4为利用本发明的转换方法计算得到的孔径分布与压汞孔径分布对比结果Fig. 4 is the comparison result of the pore size distribution calculated by the conversion method of the present invention and the mercury injection pore size distribution
图5为经验方法获得的T2与孔隙半径的拟合关系Figure 5 is the fitting relationship between T2 and pore radius obtained by empirical method
图6为利用经验方法获计算得到的孔径分布与压汞孔径分布对比结果Figure 6 is the comparison result of the pore size distribution calculated by using the empirical method and the mercury injection pore size distribution
图7为常规方法获得的T2与孔隙半径的拟合关系Figure 7 is the fitting relationship between T and pore radius obtained by conventional methods
图8为利用常规方法获计算得到的孔径分布与压汞孔径分布对比结果Fig. 8 is the comparison result of the pore size distribution calculated by the conventional method and the mercury injection pore size distribution
具体实施方式Detailed ways
结合附图和本发明具体实施方式的描述,能够更加清楚地了解本发明的细节。但是,在此描述的本发明的具体实施方式,仅用于解释本发明的目的,而不能以任何方式理解成是对本发明的限制。在本发明的教导下,技术人员可以构想基于本发明的任意可能的变形,这些都应被视为属于本发明的范围。The details of the present invention can be understood more clearly with reference to the accompanying drawings and the description of specific embodiments of the present invention. However, the specific embodiments of the present invention described here are only for the purpose of explaining the present invention, and should not be construed as limiting the present invention in any way. Under the teaching of the present invention, the skilled person can conceive any possible modification based on the present invention, and these should be regarded as belonging to the scope of the present invention.
实施例1Example 1
以四块来自于中国鄂尔多斯盆地伊陕斜坡的西部的致密砂岩样品为例;核磁共振和恒速压汞实验在中国科学院流体力学研究所完成。Taking four tight sandstone samples from the west of the Yishan slope in the Ordos Basin, China as an example; the nuclear magnetic resonance and constant-speed mercury injection experiments were completed at the Institute of Fluid Mechanics, Chinese Academy of Sciences.
核磁共振实验采用了RecCore2500型低场核磁共振仪器,共振频率2.38MHz,回波个数2048,扫描次数128,等待时间5000ms,回波间隔0.6ms,增益50。将岩样120℃抽真空至少24小时,称重后浸泡在模拟地层水(总矿化度25000mg/L)中至少24小时,用微湿滤纸去除岩样表面水,对岩样进行称重以及第一次核磁共振测量,得到T2谱图。RecCore2500 low-field nuclear magnetic resonance instrument was used in the nuclear magnetic resonance experiment. The resonance frequency is 2.38MHz, the number of echoes is 2048, the number of scans is 128, the waiting time is 5000ms, the echo interval is 0.6ms, and the gain is 50. Vacuumize the rock sample at 120°C for at least 24 hours, weigh it and soak it in simulated formation water (total salinity 25000mg/L) for at least 24 hours, remove the surface water of the rock sample with slightly wet filter paper, weigh the rock sample and The first NMR measurement yielded a T2 spectrum.
恒速压汞实验采用了Coretest公司生产的ASPE-730型恒速压汞实验装置,接触角140°,表面张力485dyne/cm。将岩样制备成直径1cm长度1cm的圆柱体岩心,120℃抽真空至少24小时,浸泡在汞溶液中,以恒定的0.00005ml/min的速度向岩心中进汞,压力达到6.2055MPa时实验结束。The constant-speed mercury intrusion experiment adopts the ASPE-730 constant-speed mercury intrusion experiment device produced by Coretest Company, with a contact angle of 140° and a surface tension of 485dyne/cm. The rock sample is prepared into a cylindrical core with a diameter of 1 cm and a length of 1 cm, vacuumed at 120°C for at least 24 hours, soaked in a mercury solution, and mercury is injected into the core at a constant speed of 0.00005ml/min, and the experiment ends when the pressure reaches 6.2055MPa .
进一步地,考虑数据点分布情况将影响到拟合精度,这是因为数据越集中的地方往往拟合效果更好,而数据点比较少或分布比较分散的地方拟合效果往往差强人意。Furthermore, considering the distribution of data points will affect the fitting accuracy, this is because the place where the data is more concentrated tends to have a better fitting effect, while the place where the data points are less or the distribution is more scattered is often not satisfactory.
而对于致密砂岩,大孔径相对较少,小孔径相对较少,同时,压汞测试的压力点集中分布在小孔径对应的高压区,所以反映在压汞数据上,表现为小孔径的数据点较多,分布较集中,而大孔径的数据点较少,分布较分散。For tight sandstone, there are relatively few large pores and relatively few small pores. At the same time, the pressure points of the mercury injection test are concentrated in the high-pressure area corresponding to the small pores, so reflected in the mercury injection data, it appears as data points with small pores. More, the distribution is more concentrated, while the data points of large apertures are less, the distribution is more scattered.
本发明按照从小孔径到大孔径的顺序,对不同测试点的压汞数据孔径大小进行了差值计算,结果表明:孔径差值依次增大,这表明了孔径越大,单位孔径范围的数据点越少(如图1所示,以样品J-1为例)。因此,以最小孔径差值为起始,选取孔径差值在一个数量级范围内的对应的孔径范围作为一个数据段。对孔径进行分段转化,可以在一定程度上避免数据在拟合过程中较少的考虑了分布稀疏的大孔径数据这一问题。According to the sequence from small aperture to large aperture, the present invention calculates the difference in the aperture size of the mercury intrusion data at different test points, and the results show that the aperture difference increases sequentially, which indicates that the larger the aperture, the larger the data points in the unit aperture range. The less (as shown in Figure 1, taking sample J-1 as an example). Therefore, starting from the minimum aperture difference value, a corresponding aperture range within an order of magnitude range is selected as a data segment. The segmental conversion of the aperture can avoid the problem that the large aperture data with sparse distribution is less considered in the data fitting process to a certain extent.
下一步,使用圆柱形孔隙模型获得T2与孔径大小的转换关系。具体过程为:In the next step, the conversion relationship between T2 and pore size is obtained using the cylindrical pore model. The specific process is:
使用KST模型表示的T2与孔隙体积、孔隙流体体积之间的关系:The relationship between T2 , pore volume and pore fluid volume expressed by KST model:
将常规方法或经验方法中的平面物理模型(薄层流体体积为Vs)替换为圆柱形孔隙模型(如图2所示),该圆柱形孔隙中薄层流体的体积为:Replace the plane physical model (thin-layer fluid volume V s ) in the conventional or empirical method with a cylindrical pore model (as shown in Fig. 2), the volume of the thin-layer fluid in the cylindrical pore is:
圆柱形孔隙的表面积为:The surface area of a cylindrical pore is:
St=2πrt·l (3)S t =2πr t ·l (3)
将式(2)、式(3)带入式(1)得到Put formula (2) and formula (3) into formula (1) to get
令make
将(5)、(6)和(7)带入(4),可以得到T2与孔隙半径之间的转换关系;Bringing (5), (6) and (7) into (4), the conversion relationship between T2 and pore radius can be obtained;
下一步,利用线性最小二乘原理,求取C和h值。求取C和h值得过程,参照发明人在先研究《Effects of pore-throat structure on gas permeability in the tightsandstonereservoirs of the Upper Triassic Yanchang formation in the WesternOrdos Basin,China》中披露的岩心T2谱横向驰豫时间换算孔隙半径分布方法。In the next step, use the principle of linear least squares to obtain the values of C and h. For the process of obtaining C and h values, refer to the T2 spectrum lateral relaxation of the rock core disclosed in the inventor's previous study "Effects of pore-throat structure on gas permeability in the tights and stone reservoirs of the Upper Triassic Yanchang formation in the Western Ordos Basin, China" Time conversion pore radius distribution method.
最后,对其他段数据采取同样方法获得不同段的C和h值,从而获得完整的岩心T2谱图表征孔径分布的转换方法。计算结果如表1所示:Finally, use the same method to obtain the C and h values of different segments in the same way for the data of other segments, so as to obtain the conversion method of the complete core T2 spectrum to characterize the pore size distribution. The calculation results are shown in Table 1:
以上述方法获得的T2与孔隙半径的拟合关系如图3所示(以样品T-6为例):The fitting relationship between T2 and pore radius obtained by the above method is shown in Figure 3 (taking sample T-6 as an example):
以上述方法计算得到的孔隙半径分布与压汞孔隙半径分布的对比结果如图4所示(以样品T-6为例)The comparison results of the pore radius distribution calculated by the above method and the mercury injection pore radius distribution are shown in Figure 4 (taking sample T-6 as an example)
对比例1Comparative example 1
以经验方法为例,即:两侧取对数,采用最小二乘原理得到C和n值。Take the empirical method as an example, namely: Take the logarithm on both sides, and use the principle of least squares to get the values of C and n.
计算结果如表2所示:The calculation results are shown in Table 2:
以经验方法获得的T2与孔隙半径的拟合关系如图5所示(以样品T-6为例):The fitting relationship between T2 and pore radius obtained by empirical method is shown in Fig. 5 (taking sample T-6 as an example):
以经验方法计算得到的孔隙半径分布与压汞孔隙半径分布的对比结果如图6所示(以样品T-6为例):The comparison results of the pore radius distribution calculated by the empirical method and the mercury injection pore radius distribution are shown in Figure 6 (taking sample T-6 as an example):
对比例2Comparative example 2
以常规方法为例,即n取1,T2=Crt,采用最小二乘原理得到C值。Taking the conventional method as an example, that is, n takes 1, T 2 =Cr t , and the value of C is obtained by using the least square principle.
计算结果如表3所示:The calculation results are shown in Table 3:
以常规方法获得的T2与孔隙半径的拟合关系如图7所示(以样品T-6为例):The fitting relationship between T2 and pore radius obtained by conventional methods is shown in Figure 7 (taking sample T-6 as an example):
以常规方法计算得到的孔隙半径分布与压汞孔隙半径分布的对比结果如图8所示(以样品T-6为例):The comparison results of the pore radius distribution calculated by the conventional method and the mercury injection pore radius distribution are shown in Fig. 8 (taking sample T-6 as an example):
对比表1、表2和表3,同时,对比图3、图5和图7,结果表明,利用本发明得到的转换方法,T2值与孔径拟合系数均在0.99以上,直观上拟合效果更好,明显优于常规法和经验法,表明利用本发明获得转换关系可以更好的预测孔隙半径,在一定程度上更精确的反映核磁信号的孔径分布。Contrast Table 1, Table 2 and Table 3, meanwhile, contrast Fig. 3, Fig. 5 and Fig. 7, the result shows, utilizes the conversion method that the present invention obtains, T Value and aperture fitting coefficient are all more than 0.99, visually fitting The effect is better, obviously superior to the conventional method and the empirical method, indicating that the conversion relationship obtained by the present invention can better predict the pore radius, and reflect the pore size distribution of the nuclear magnetic signal more accurately to a certain extent.
进一步,对比图4、图6和图8,结果表明,利用本发明得到的转换方法得到的核磁共振T2谱换算的孔径与恒速压汞孔喉半径相比,两者之间的对应关系更好。利用常规方法得到的核磁共振T2谱换算的孔径与恒速压汞孔喉半径相比,常规公式法预测结果整体差异较大。而利用经验方法得到的核磁共振T2谱换算的孔径与恒速压汞孔喉半径相比,经验公式法预测结果中小孔径部分虽然对应关系很好,但是大孔径部分的对应关系较差,表明经验公式法对于大孔径预测的精度不高,侧面说明了本发明将压汞数据分段处理,提高了预测的精度,特别是对于大孔径段的预测。Further, compare Fig. 4, Fig. 6 and Fig. 8, the result shows, utilize the conversion method that the present invention obtains to obtain the nuclear magnetic resonance T The pore diameter converted from the spectrum is compared with the constant-speed mercury injection pore-throat radius, the corresponding relationship between the two better. Compared with the pore diameter converted from the NMR T 2 spectrum obtained by the conventional method and the pore throat radius of the constant-speed mercury injection, there is a large difference in the prediction results of the conventional formula method. However, compared with the pore diameter converted from the NMR T2 spectrum obtained by the empirical method and the pore-throat radius of the constant-velocity mercury injection, although the small pore diameter part of the prediction result of the empirical formula method has a good corresponding relationship, the corresponding relationship of the large pore diameter part is poor, indicating that The accuracy of the empirical formula method for large aperture prediction is not high, which shows that the present invention processes the mercury injection data in segments, which improves the prediction accuracy, especially for the prediction of large aperture segments.
因此,本发明将T2谱与孔径转换关系使用圆柱模型,同时将压汞数据进行分段处理,获得了一种精度更高的核磁共振T2谱表征致密储层孔径分布的转换方法。Therefore, the present invention uses a cylinder model for the conversion relationship between T2 spectrum and pore size, and at the same time processes the mercury injection data in segments to obtain a conversion method with higher precision for NMR T2 spectrum to characterize the pore size distribution of tight reservoirs.
针对上述各实施方式的详细解释,其目的仅在于对本发明进行解释,以便于能够更好地理解本发明,但是,这些描述不能以任何理由解释成是对本发明的限制,特别是,在不同的实施方式中描述的各个特征也可以相互任意组合,从而组成其他实施方式,除了有明确相反的描述,这些特征应被理解为能够应用于任何一个实施方式中,而并不仅局限于所描述的实施方式。The purpose of the detailed explanations for the above-mentioned embodiments is only to explain the present invention so as to better understand the present invention. However, these descriptions cannot be construed as limiting the present invention for any reason, especially, in different The various features described in the embodiments can also be combined arbitrarily with each other to form other embodiments. Unless there is an explicit description to the contrary, these features should be understood as being applicable to any embodiment and not limited to the described embodiment. Way.
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