CN105386753A - Method for constructing pseudo capillary pressure curves by using NMR (nuclear magnetic resonance) logging - Google Patents
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Abstract
本发明公开了一种利用核磁共振测井构造伪毛管压力曲线方法。所述方法根据实际测量的核磁共振测井资料和有限的毛管压力资料,设定7个不同的弛豫时间,将核磁共振T2谱分为8个部分,计算8个部分的孔隙度组分百分含量,建立不同进汞压力下的进汞饱和度与核磁共振孔隙度组分百分含量之间的转换模型,依据所得转换模型,计算不同进汞压力下的进汞饱和度,根据计算的进汞饱和度和与之对应的进汞压力,构造伪毛管压力曲线,并依据伪毛管压力曲线,获取孔喉半径分布,计算储集层孔隙结构评价参数,实现利用核磁共振测井资料准确构造伪毛管压力曲线及连续定量评价储集层孔隙结构的目的。
The invention discloses a method for constructing a pseudo-capillary pressure curve by using nuclear magnetic resonance logging. According to the actually measured nuclear magnetic resonance logging data and limited capillary pressure data, the method sets 7 different relaxation times, divides the nuclear magnetic resonance T2 spectrum into 8 parts, and calculates the porosity components of the 8 parts percentage content, establish a conversion model between the mercury saturation at different mercury injection pressures and the percentage content of NMR porosity components, and calculate the mercury saturation at different mercury injection pressures according to the obtained conversion model. Based on the mercury saturation and the corresponding mercury injection pressure, the pseudo capillary pressure curve is constructed, and the pore throat radius distribution is obtained according to the pseudo capillary pressure curve, and the evaluation parameters of the reservoir pore structure are calculated to realize the accurate utilization of nuclear magnetic resonance logging data. The purpose of constructing pseudo capillary pressure curve and continuous quantitative evaluation of reservoir pore structure.
Description
技术领域technical field
本发明属于储集层评价领域,特别涉及一种利用核磁共振测井构造伪毛管压力曲线方法。The invention belongs to the field of reservoir evaluation, in particular to a method for constructing a pseudo-capillary pressure curve using nuclear magnetic resonance logging.
背景技术Background technique
随着国家对能源需求的不断增加,大量常规储集层已经被开发,其产量日益降低。加大对低孔低渗-致密储集层的勘探开发,已成为国家解决油气供应短缺,确保能源安全的重要途径。低孔低渗-致密储集层往往具有储集层致密、电阻率对比度低、孔隙结构复杂以及非均质性强等特点,导致常规的储集层评价方法对其应用效果不好,大量潜在的储集层被误判为水层或非储集层,储集层产能预测困难。为了提高针对复杂储集层的勘探效率,降低开发风险,对储集层孔隙结构进行定量评价是行之有效的方法。As the country's demand for energy continues to increase, a large number of conventional reservoirs have been developed, and their production is decreasing day by day. Increasing the exploration and development of low-porosity, low-permeability-tight reservoirs has become an important way for the country to solve the shortage of oil and gas supply and ensure energy security. Low-porosity and low-permeability-tight reservoirs often have the characteristics of tight reservoirs, low resistivity contrast, complex pore structure, and strong heterogeneity, which lead to poor application of conventional reservoir evaluation methods and a large number of potential reservoirs. reservoirs are misjudged as water layers or non-reservoirs, and it is difficult to predict reservoir productivity. In order to improve the exploration efficiency of complex reservoirs and reduce development risks, quantitative evaluation of reservoir pore structure is an effective method.
目前,毛管压力曲线是用以评价储集层孔隙结构,划分储集层类型最有效的资料。然而,受实验客观条件限制,通过岩心实验获取的毛管压力资料非常有限,无法利用其连续定量评价储集层孔隙结构。为了实现连续定量评价储集层孔隙结构的目的,目前最常用的方法就是利用核磁共振测井资料连续构造出伪毛管压力曲线,并利用其代替岩心毛管压力曲线来连续定量评价实际储集层的孔隙结构。At present, capillary pressure curve is the most effective data to evaluate reservoir pore structure and classify reservoir types. However, limited by the objective conditions of the experiment, the capillary pressure data obtained through the core experiment are very limited, which cannot be used to continuously and quantitatively evaluate the reservoir pore structure. In order to achieve the purpose of continuously and quantitatively evaluating the pore structure of reservoirs, the most commonly used method is to continuously construct pseudo-capillary pressure curves using nuclear magnetic resonance logging data, and use them instead of core capillary pressure curves to continuously and quantitatively evaluate the actual reservoir pore structure. Pore Structure.
目前已发表的文献中有关利用核磁共振测井资料构造伪毛管压力曲线的方法有以下几种:There are several methods for constructing pseudo-capillary pressure curves using nuclear magnetic resonance logging data in the published literature:
1、基于Swanson参数的伪毛管压力曲线构造方法。参见2008年6月《AppliedGeophysics》杂志中,XiaoLiang等人著作的《ANewMethodtoConstructReservoirCapillaryPressureCurvesUsingNMRLoggingDataandItsApplication》的文章,记载了基于Swanson参数的伪毛管压力曲线构造方法。该方法的基本步骤包括:首先,根据实验测量的毛管压力曲线数据,建立基于Swanson参数的储集层渗透率解释模型,利用其从核磁共振测井资料中计算储集层的渗透率;然后,根据毛管压力曲线的形态特征,建立不同进汞压力下的进汞饱和度与核磁孔隙度以及渗透率之间的相关关系,以利用岩石的孔隙度和渗透率参数计算出进汞饱和度,最后,结合计算的进汞饱和度与进汞压力,实现伪毛管压力曲线重构的目的。1. The pseudo-capillary pressure curve construction method based on Swanson parameters. See the article "ANewMethodtoConstructReservoirCapillaryPressureCurvesUsingNMRLoggingDataandItsApplication" written by XiaoLiang et al. in the journal "AppliedGeophysics" in June 2008, which records the method of constructing pseudo-capillary pressure curves based on Swanson parameters. The basic steps of this method include: firstly, according to the capillary pressure curve data measured experimentally, establish a reservoir permeability interpretation model based on Swanson parameters, and use it to calculate the reservoir permeability from nuclear magnetic resonance logging data; then, According to the morphological characteristics of the capillary pressure curve, the correlation between the mercury saturation and NMR porosity and permeability under different mercury injection pressures is established, so as to calculate the mercury saturation by using the rock porosity and permeability parameters, and finally , combined with the calculated mercury injection saturation and mercury injection pressure, to achieve the purpose of reconstructing the pseudo capillary pressure curve.
2、二维等面积刻度转换系数法。参见2009年2月《测井技术》杂志中,邵维志等人著作的《核磁共振测井在储集层孔隙结构评价中的应用》的文章,记载了采用二维等面积刻度转换系数法构造核磁伪毛管压力曲线的方法。该方法的基本步骤包括:首先根据孔喉半径与毛管压力之间的关系,将测量的毛管压力曲线转化为孔喉半径分布,利用微分相似原理,确定每块样品的T2谱与对应的孔喉半径分布之间的横向转换系数;然后,利用分段等面积刻度方法,确定每块样品的T2谱与对应的孔喉半径分布之间的纵向转换系数;最后,建立横向转换系数和纵向转换系数与岩石孔隙度以及渗透率之间的关系,以实现利用核磁共振测井构造伪毛管压力曲线的目的。2. Two-dimensional equal-area scale conversion coefficient method. See the article "Application of Nuclear Magnetic Resonance Logging in Reservoir Pore Structure Evaluation" written by Shao Weizhi et al. in the journal "Logging Technology" in February 2009, which records the use of two-dimensional equal-area scale conversion coefficient method to construct NMR Method of Pseudocapillary Pressure Curves. The basic steps of the method include: firstly, according to the relationship between the pore throat radius and the capillary pressure, the measured capillary pressure curve is transformed into the pore throat radius distribution, and the T2 spectrum of each sample is determined to correspond to the corresponding pore throat radius distribution by using the differential similarity principle. The horizontal conversion coefficient between the throat radius distributions; then, using the segmented equal - area scale method, determine the vertical conversion coefficient between the T2 spectrum of each sample and the corresponding pore throat radius distribution; finally, establish the horizontal conversion coefficient and the vertical The relationship between the conversion coefficient and rock porosity and permeability, in order to realize the purpose of constructing pseudo-capillary pressure curve by using nuclear magnetic resonance logging.
3、分段非线性幂函数刻度方法。参见2010年1月匡立春等发明的专利《一种利用核磁共振测井资料连续定量评价储集层孔隙结构的方法》,记载了采用分段非线性幂函数刻度方法来从核磁共振测井资料中构造伪毛管压力曲线的方法。其基本原理是:首先根据岩石孔隙度和渗透率计算一个反映储集层差异的参数并利用该参数将储集层划分为四类,针对每一类型储集层,分别采用不同的分段幂函数来构造伪毛管压力曲线。对于第一类、第二类和第三类储集层,采用分段的方法,在大孔喉和小孔喉段,分别采用不同的幂函数,而对于第四类储集层,采用单一的幂函数将核磁共振T2谱转化为孔喉半径分布,再根据孔喉半径与毛管压力之间的关系,构造出伪毛管压力曲线。3. Scale method of piecewise nonlinear power function. See the patent "A Method for Continuous and Quantitative Evaluation of Reservoir Pore Structure Using Nuclear Magnetic Resonance Logging Data" invented by Kuang Lichun et al. in January 2010. A method for constructing pseudocapillary pressure curves in . The basic principle is: firstly calculate a parameter reflecting the difference of reservoirs according to rock porosity and permeability And use this parameter to divide the reservoirs into four types. For each type of reservoirs, different subsection power functions are used to construct pseudo-capillary pressure curves. For the first, second and third types of reservoirs, the segmented method is adopted, and different power functions are used in the large pore-throat and small pore-throat sections, while for the fourth type of reservoir, a single The power function of the NMR T 2 spectrum is transformed into the pore throat radius distribution, and then the pseudo capillary pressure curve is constructed according to the relationship between the pore throat radius and the capillary pressure.
现有方法在利用核磁共振测井资料构造伪毛管压力曲线的过程中,均用到了两个中间参数:岩石的孔隙度和渗透率。然而,在实际储集层评价中,这两个中间参数均难以准确获取,尤其是在致密储集层以及复杂岩性含气储集层中,孔隙度和渗透率参数更难以有效获得,给利用上述方法构造伪毛管压力曲线增加了难度。同时,渗透率参数并不能够从核磁共振T2谱中直接获取,需要采用特殊的计算方法,这些计算过程的引入,势必会带来人为误差,而这些误差最终会传递到伪毛管压力曲线构造模型的建立过程中,导致利用现有方法构造的伪毛管压力曲线误差较大,达不到利用核磁共振测井资料准确定量评价储集层孔隙结构的目的。In the process of constructing the pseudo-capillary pressure curve using nuclear magnetic resonance logging data, the existing methods all use two intermediate parameters: porosity and permeability of the rock. However, in actual reservoir evaluation, these two intermediate parameters are difficult to obtain accurately, especially in tight reservoirs and complex lithology gas-bearing reservoirs, the porosity and permeability parameters are more difficult to obtain effectively, giving Using the above method to construct pseudo-capillary pressure curves increases the difficulty. At the same time, the permeability parameters cannot be directly obtained from the NMR T2 spectrum, and special calculation methods are required. The introduction of these calculation processes will inevitably bring about human errors, and these errors will eventually be transmitted to the structure of the pseudo capillary pressure curve. During the establishment of the model, the error of the pseudo-capillary pressure curve constructed by the existing method is relatively large, which fails to achieve the purpose of accurately and quantitatively evaluating the reservoir pore structure by using the nuclear magnetic resonance logging data.
发明内容Contents of the invention
为了克服现有方法的不足,本发明提供一种利用核磁共振测井构造伪毛管压力曲线的方法,实现根据实际测量的核磁共振测井资料和有限的毛管压力资料,准确构造伪毛管压力曲线的目的。In order to overcome the deficiencies of the existing methods, the present invention provides a method for constructing pseudo-capillary pressure curves using nuclear magnetic resonance logging to realize accurate construction of pseudo-capillary pressure curves based on actually measured nuclear magnetic resonance logging data and limited capillary pressure data Purpose.
为解决上述问题,本发明采用如下技术方案:In order to solve the above problems, the present invention adopts the following technical solutions:
根据实际测量的核磁共振测井资料和有限的毛管压力资料,设定7个不同的弛豫时间,将核磁共振T2谱分为8个部分,计算8个部分的孔隙度组分百分含量,建立不同进汞压力下的进汞饱和度与核磁共振孔隙度组分百分含量之间的转换模型,依据所得转换模型,计算不同进汞压力下的进汞饱和度,根据计算的进汞饱和度和与之对应的进汞压力,构造伪毛管压力曲线,并依据伪毛管压力曲线,获取孔喉半径分布,计算储集层孔隙结构评价参数,实现利用核磁共振测井资料准确构造伪毛管压力曲线及连续定量评价储集层孔隙结构的目的。According to the actual measured nuclear magnetic resonance logging data and limited capillary pressure data, set 7 different relaxation times, divide the nuclear magnetic resonance T2 spectrum into 8 parts, and calculate the percentage of porosity components in the 8 parts , establish a conversion model between the mercury saturation at different mercury injection pressures and the percentage content of NMR porosity components, and calculate the mercury saturation at different mercury injection pressures according to the obtained conversion model. Saturation and corresponding mercury injection pressure, construct pseudo-capillary pressure curve, and obtain pore-throat radius distribution based on pseudo-capillary pressure curve, calculate reservoir pore structure evaluation parameters, and realize accurate construction of pseudo-capillary by using nuclear magnetic resonance logging data The purpose of pressure curve and continuous quantitative evaluation of reservoir pore structure.
本发明所述方法包括以下步骤:The method of the present invention comprises the following steps:
1)在分析岩心压汞实验特点及操作过程的基础上,确定M个进汞压力;1) On the basis of analyzing the characteristics of the core mercury injection experiment and the operation process, determine M mercury injection pressures;
2)利用核磁共振测井仪器,对目标储集层进行测量并反演得到实际测量的核磁共振测井T2谱; 2 ) Using nuclear magnetic resonance logging tools to measure the target reservoir and invert to obtain the actually measured nuclear magnetic resonance logging T2 spectrum;
3)给定7个不同的T2弛豫时间,将核磁共振T2谱划分为8个部分,然后计算出8个孔隙度组分百分含量; 3 ) Given 7 different T2 relaxation times, divide the NMR T2 spectrum into 8 parts, and then calculate the percentage of 8 porosity components;
4)建立M个不同进汞压力下的进汞饱和度与8个孔隙度组分百分含量之间的函数关系,并利用其从核磁共振测井资料中计算与M个进汞压力相对应的M个进汞饱和度值;4) Establish the functional relationship between the mercury saturation at M different mercury injection pressures and the percentage content of the eight porosity components, and use it to calculate the corresponding M mercury injection pressures from the nuclear magnetic resonance logging data M mercury saturation values of ;
5)根据计算的进汞饱和度和给定的进汞压力值,绘制构造的伪毛管压力曲线;5) Draw the constructed pseudo-capillary pressure curve according to the calculated mercury saturation and the given mercury pressure;
6)、利用构造的伪毛管压力曲线获取储集层孔喉半径分布,并计算平均孔喉半径、最大孔喉半径、中值半径、中值压力、排驱压力,均值系数,分选系数等储集层孔隙结构评价参数。6) Using the structural pseudo-capillary pressure curve to obtain the reservoir pore-throat radius distribution, and calculate the average pore-throat radius, maximum pore-throat radius, median radius, median pressure, displacement pressure, average coefficient, sorting coefficient, etc. Reservoir pore structure evaluation parameters.
所述步骤1)涉及的M个进汞压力按如下方式布点:The M mercury injection pressures involved in step 1) are distributed as follows:
Pc(i)=0.005×2i-1,i=1,2,......,MP c (i)=0.005×2 i-1 , i=1,2,...,M
式中:Pc(i)为第i个进汞压力,单位为MPa。In the formula: P c (i) is the i-th mercury injection pressure, the unit is MPa.
所述步骤3)给定的7个T2弛豫时间分别为T2(1)=1.0ms、T2(2)=3.0ms、T2(3)=10.0ms、T2(4)=33.0ms、T2(5)=100.0ms、T2(6)=300.0ms、T2(7)=1000.0ms。为描述方便,设定:最小T2弛豫时间记为T2(0),最大T2弛豫时间记为T2(8)。The seven T 2 relaxation times given in step 3) are respectively T 2 (1)=1.0ms, T 2 (2)=3.0ms, T 2 (3)=10.0ms, T 2 (4)= 33.0ms, T 2 (5) = 100.0ms, T 2 (6) = 300.0ms, T 2 (7) = 1000.0ms. For the convenience of description, it is assumed that the minimum T 2 relaxation time is recorded as T 2 (0), and the maximum T 2 relaxation time is recorded as T 2 (8).
所述步骤3)定义的最小T2弛豫时间T2(0)=0.3ms;最大T2弛豫时间T2(8)=3000.0ms。The minimum T 2 relaxation time T 2 (0)=0.3ms defined in the step 3); the maximum T 2 relaxation time T 2 (8)=3000.0ms.
所述步骤3)涉及的8个孔隙度组分百分含量分别为X1、X2、X3、X4、X5、X6、X7和X8,其计算方法是:The 8 porosity component percentages involved in the step 3) are respectively X1, X2, X3, X4, X5, X6, X7 and X8, and the calculation method is:
式中S(t)为与T2弛豫时间相关的孔隙度分布函数。where S(t ) is the porosity distribution function related to T2 relaxation time.
所述步骤4)涉及的进汞饱和度与孔隙度组分百分含量间的函数关系如下:The functional relationship between the mercury saturation involved in the step 4) and the porosity component percentage is as follows:
式中
所述步骤4)中在利用核磁共振测井资料计算进汞饱和度时,只计算进汞压力Pc(i)>0.08MPa那部分的进汞饱和度,对于进汞压力Pc(i)≤0.08MPa那部分的进汞饱和度设定等于0。In the step 4), when using NMR logging data to calculate the mercury saturation, only calculate the mercury saturation of the mercury injection pressure P c (i) > 0.08MPa, for the mercury injection pressure P c (i) The mercury saturation of the part ≤0.08MPa is set equal to 0.
所述步骤6)中利用伪毛管压力曲线获取储集层孔喉半径分布并计算储集层孔隙结构评价参数的方法按照杨胜来等著作的普通高等学校“十五”规划教材《油层物理学》中209-233页所述的方法进行。In the step 6), the method of using the pseudo-capillary pressure curve to obtain the reservoir pore throat radius distribution and calculate the reservoir pore structure evaluation parameters is in accordance with the "Tenth Five-Year Plan" planning textbook "Oil Reservoir Physics" for general colleges and universities written by Yang Shenglai and others. The method described on pages 209-233 was carried out.
本发明的有益效果是:利用核磁共振测井资料构造连续的伪毛管压力曲线,并利用伪毛管压力曲线获取储集层孔喉半径分布以及计算储集层孔隙结构评价参数,进而实现基于核磁共振测井资料连续定量评价储集层孔隙结构的目的。The beneficial effects of the present invention are: using nuclear magnetic resonance logging data to construct a continuous pseudo-capillary pressure curve, and using the pseudo-capillary pressure curve to obtain reservoir pore-throat radius distribution and calculate reservoir pore structure evaluation parameters, and then realize nuclear magnetic resonance-based The purpose of continuous and quantitative evaluation of reservoir pore structure from well logging data.
附图说明Description of drawings
下面结合附图和实施例对本发明作进一步说明。The present invention will be further described below in conjunction with drawings and embodiments.
图1是本发明提供的一种利用核磁共振测井资料构造伪毛管压力曲线方法流程图。Fig. 1 is a flowchart of a method for constructing a pseudo-capillary pressure curve using nuclear magnetic resonance logging data provided by the present invention.
图2是本发明实施例提供的国内西南地区某储集层四种不同孔隙结构岩心样品的压汞毛管压力曲线示意图。Fig. 2 is a schematic diagram of mercury injection capillary pressure curves of four core samples with different pore structures in a reservoir in Southwest China provided by an embodiment of the present invention.
图3是本发明实施例提供的国内西南地区某储集层四种不同孔隙结构岩心样品的核磁共振T2谱示意图。Fig. 3 is a schematic diagram of nuclear magnetic resonance T 2 spectra of four core samples with different pore structures in a reservoir in Southwest China provided by an embodiment of the present invention.
图4是本发明实施例提供的孔隙结构较好岩石的压汞毛管压力曲线与构造的伪毛管压力曲线形态对比示意图。Fig. 4 is a schematic diagram of the comparison between the mercury intrusion capillary pressure curve and the pseudo-capillary pressure curve of the structure provided by the embodiment of the present invention.
图5是本发明实施例提供的孔隙结构中等岩石的压汞毛管压力曲线与构造的伪毛管压力曲线形态对比示意图。Fig. 5 is a schematic diagram of the comparison between the mercury intrusion capillary pressure curve and the pseudo-capillary pressure curve of the structure provided by the embodiment of the present invention.
图6是本发明实施例提供的孔隙结构较差岩石的压汞毛管压力曲线与构造的伪毛管压力曲线形态对比示意图。Fig. 6 is a schematic diagram of the comparison between the mercury intrusion capillary pressure curve and the structural pseudo-capillary pressure curve of the rock with poor pore structure provided by the embodiment of the present invention.
图7是本发明实施例提供的利用本发明所述方法从实测的核磁共振测井资料中构造的伪毛管压力曲线以及利用伪毛管压力曲线计算的储集层孔隙结构评价参数与岩心实验结果对比效果图。Fig. 7 is a comparison between the pseudo capillary pressure curve constructed from the measured nuclear magnetic resonance logging data and the reservoir pore structure evaluation parameters calculated by using the pseudo capillary pressure curve and the core experiment results provided by the method of the present invention. renderings.
具体实施方式detailed description
理论分析theoretical analysis
下面以我国西南地区某储集层4块代表性岩心样品的压汞毛管压力曲线和核磁共振T2谱为例,来说明本发明的基本原理和思路。Below, the mercury intrusion capillary pressure curve and NMR T2 spectrum of 4 representative rock core samples of a certain reservoir in Southwest China are taken as examples to illustrate the basic principles and ideas of the present invention.
参见图2,所示为4块样品的压汞毛管压力实验结果,其中,X轴为进汞饱和度,单位为百分数%;Y轴为进汞压力,单位为MPa。4块样品的压汞毛管压力曲线的形态完全不同,其代表岩石的孔隙结构也存在明显差异。1号样品的毛管压力曲线位于图中的左下角,代表岩石的孔隙结构最好;2号样品的毛管压力曲线位于1号样品的毛管压力曲线之上,代表其孔隙结构较1号样品差;3号样品的毛管压力曲线位于1号和2号样品的毛管压力曲线之上,位于4号样品的毛管压力曲线之下,代表其孔隙结构较1号样品和2号样品差,而优于4号样品;4号样品的毛管压力曲线位于图中的最上方,代表其孔隙结构最差。Referring to Fig. 2, it shows the mercury injection capillary pressure test results of four samples, wherein, the X-axis is the mercury injection saturation, and the unit is percentage %; the Y-axis is the mercury injection pressure, and the unit is MPa. The shapes of the mercury injection capillary pressure curves of the four samples are completely different, and the pore structures of the rocks they represent are also significantly different. The capillary pressure curve of sample No. 1 is located in the lower left corner of the figure, indicating that the pore structure of the rock is the best; the capillary pressure curve of sample No. 2 is above the capillary pressure curve of sample No. 1, indicating that its pore structure is worse than that of sample No. 1; The capillary pressure curve of sample No. 3 is above the capillary pressure curves of samples No. 1 and No. 2, and below the capillary pressure curve of sample No. 4, which means that its pore structure is worse than that of samples No. 1 and No. 2, but better than that of No. 4 samples. Sample No. 4; the capillary pressure curve of sample No. 4 is at the top of the figure, representing the worst pore structure.
4块样品所对应的压汞毛管压力实验数据如表1所示。由表1可知,在进行压汞实验的过程中,对所有样品施加的进汞压力均相同,即图2中所有毛管压力曲线的Y轴坐标均相等。进汞压力的施加方式如下式所示:The experimental data of mercury injection capillary pressure corresponding to the four samples are shown in Table 1. It can be seen from Table 1 that during the mercury injection experiment, the mercury injection pressure applied to all samples is the same, that is, the Y-axis coordinates of all the capillary pressure curves in Figure 2 are equal. The method of applying the mercury injection pressure is shown in the following formula:
Pc(i)=0.005×2i-1,i=1,2,…,13P c (i)=0.005×2 i-1 , i=1,2,...,13
式中:Pc(i)为施加的第i个进汞压力,单位为MPa。In the formula: P c (i) is the i-th mercury injection pressure applied, and the unit is MPa.
由于所有的岩心样品在进行压汞实验时所施加的进汞压力均相同,因此,岩心样品的毛管压力曲线的形态主要受进汞饱和度的大小控制。在施加相同进汞压力的情况下,对于孔隙结构较好的岩石,压入岩石孔隙空间的进汞量较多,对应的进汞饱和度较高;反之,对于孔隙结构较差的岩石,压入岩石孔隙空间的进汞量较小,对应的进汞饱和度较低。Since all the core samples are subjected to the same mercury injection pressure during the mercury injection experiment, the shape of the capillary pressure curve of the core samples is mainly controlled by the saturation of mercury injection. Under the same mercury injection pressure, for rocks with better pore structure, the amount of mercury injected into the rock pore space is more, and the corresponding mercury injection saturation is higher; on the contrary, for rocks with poor pore structure, the pressure The amount of mercury injected into the rock pore space is small, and the corresponding mercury saturation is low.
由此可见,只需要计算出不同进汞压力下的进汞饱和度,结合固定施加的进汞压力,即可重构出毛管压力曲线。It can be seen that the capillary pressure curve can be reconstructed only by calculating the mercury saturation at different mercury injection pressures and combining the fixed mercury injection pressure.
表1四块代表性岩心样品压汞毛管压力实验数据表Table 1. Capillary pressure experiment data table of mercury injection for four representative core samples
对于岩心样品而言,当施加的进汞压力较小(小于0.08MPa)的情况下,几乎无非润湿相的汞被挤入到岩石的孔隙空间,即当进汞压力小于0.08MPa时,岩石的进汞饱和度较小,基本可以忽略,且这部分毛管压力曲线的形态对于评价岩石孔隙结构的贡献较小。因此,本发明提出只估算进汞压力大于0.08MPa部分的进汞饱和度来构造伪毛管压力曲线,对于进汞压力小于0.08MPa那部分,设定进汞饱和度等于0。For core samples, when the applied mercury injection pressure is small (less than 0.08MPa), almost no mercury in the non-wetting phase is squeezed into the pore space of the rock, that is, when the mercury injection pressure is less than 0.08MPa, the rock Mercury saturation is small and can be ignored basically, and the shape of capillary pressure curve in this part has little contribution to the evaluation of rock pore structure. Therefore, the present invention proposes only estimating the mercury injection saturation of the part where the mercury injection pressure is greater than 0.08MPa to construct a pseudo-capillary pressure curve, and setting the mercury injection saturation to be equal to 0 for the part where the mercury injection pressure is less than 0.08MPa.
参见图3,所示为4块样品的核磁共振T2谱的实验结果,其中X轴为T2弛豫时间,单位为ms;Y轴为相对幅度,单位为v/v。Referring to Fig. 3, it shows the experimental results of the NMR T 2 spectra of 4 samples, where the X-axis is the T 2 relaxation time in ms; the Y-axis is the relative amplitude in v/v.
对比图2和图3可以发现,孔隙结构较好的岩石,如图2中的1号样品,在图3中对应的岩石核磁共振T2谱主峰的位置靠右,且T2谱的分布较宽,主要分布在2~1600ms之间,以大孔隙分布为主,大孔隙组分在岩石总孔隙中所占的比重较大;对于孔隙结构稍差的2号样品,其核磁共振T2谱的分布范围较1号样品窄,且主峰的分布相对靠左,小孔隙组分在岩石总孔隙中所占的比重增大;对于孔隙结构更差的3号样品,T2谱的分布范围较1号和2号样品窄,主峰的位置进一步向左移动,且小孔隙组分在岩石总孔隙中所占的比重进一步增大,而大孔隙组分所占的比重相对减小;对于孔隙结构最差的4号样品,其T2谱主峰的位置位于图3中的最左边,岩石主要以小孔隙分布为主,大孔隙组分在岩石总孔隙中所占的比重最低。Comparing Figures 2 and 3, it can be found that for rocks with better pore structure, such as sample No. 1 in Figure 2 , the position of the main peak of the corresponding rock NMR T2 spectrum in Figure 3 is on the right, and the distribution of the T2 spectrum is relatively large. wide, mainly distributed between 2 and 1600 ms, with large pores as the main distribution, and the large pore components account for a large proportion in the total pores of the rock; for sample No. 2 with poor pore structure, its NMR T The distribution range of the T 2 spectrum is narrower than that of No. 1 sample, and the distribution of the main peak is relatively to the left, and the proportion of small pore components in the total rock pores increases; for No. 3 sample with worse pore structure, the distribution range of the T 2 spectrum is relatively Samples No. 1 and No. 2 are narrower, the position of the main peak moves further to the left, and the proportion of small pore components in the total pores of the rock further increases, while the proportion of large pore components decreases relatively; for the pore structure For the worst sample No. 4 , the position of the main peak of its T2 spectrum is at the far left in Fig. 3. The rock is mainly distributed with small pores, and the proportion of large pores in the total pores of the rock is the lowest.
综合上述分析可以发现,岩石中各孔隙组分在岩石总孔隙中所占的比重对岩石孔隙结构具有一定的指示作用。因此,其与岩石不同进汞压力下的进汞饱和度应具有较强的相关性。理论上,在相同进汞压力下,对于孔隙结构较好的岩石,进汞饱和度较高,大孔隙组分在总孔隙中所占的比重较大,小孔隙组分在总孔隙中所占的比重较小;反之,对于孔隙结构较差的岩石,进汞饱和度降低,大孔隙组分在总孔隙中所占的比重减小,而小孔隙组分在总孔隙中所占的比重增大。Based on the above analysis, it can be found that the proportion of each pore component in the total rock pore has a certain indicating effect on the rock pore structure. Therefore, it should have a strong correlation with the mercury saturation of rocks under different mercury injection pressures. Theoretically, under the same mercury injection pressure, for rocks with better pore structure, the mercury injection saturation is higher, the large pore components account for a larger proportion of the total pores, and the small pore components account for a larger proportion of the total pores. Conversely, for rocks with poor pore structure, the mercury saturation decreases, the proportion of large pore components in the total pores decreases, and the proportion of small pore components in the total pores increases. Big.
本发明在上述实验分析的基础上,提出用岩石各部分孔隙组分占岩石总孔隙组分的百分含量来计算不同进汞压力下的进汞饱和度,再结合计算的进汞饱和度和给定的进汞压力值来构造伪毛管压力曲线的方法。On the basis of the above-mentioned experimental analysis, the present invention proposes to use the percentage content of the pore components of each part of the rock in the total pore components of the rock to calculate the mercury saturation under different mercury injection pressures, and then combine the calculated mercury saturation and A method for constructing a pseudo-capillary pressure curve for a given mercury injection pressure value.
为了直观定量表征不同孔隙组分在岩石总孔隙中所占的比重,采用7个不同的T2弛豫时间T2(1)、T2(2)、T2(3)、T2(4)、T2(5)、T2(6)和T2(7),将岩石核磁共振T2谱划分为8个区间,然后分别根据8个区间内岩石孔隙度组分之和与总孔隙度的比值计算出8个孔隙度组分百分含量。具体的计算过程如下:In order to visually and quantitatively characterize the proportion of different pore components in the total rock pores, seven different T 2 relaxation times T 2 (1), T 2 (2), T 2 (3), T 2 (4 ), T 2 (5), T 2 (6) and T 2 (7), the rock NMR T 2 spectrum is divided into 8 intervals, and then according to the sum of the rock porosity components and the total porosity in the 8 intervals The percentages of 8 porosity components are calculated from the ratio of porosity. The specific calculation process is as follows:
式中S(t)为与T2弛豫时间相关的孔隙度分布函数。where S(t ) is the porosity distribution function related to T2 relaxation time.
在计算出上述8个孔隙度组分百分含量后,建立不同进汞压力下的进汞饱和度与上述8个孔隙度组分百分含量之间函数关系,实现利用核磁共振测井资料计算进汞饱和度,再结合固定的进汞压力值构造伪毛管压力曲线的目的。After calculating the percentages of the above eight porosity components, the functional relationship between the mercury saturation at different mercury injection pressures and the percentages of the above eight porosity components is established to realize the calculation using NMR logging data. The purpose of constructing the pseudo-capillary pressure curve is to combine the mercury injection saturation with the fixed mercury injection pressure value.
实施例1Example 1
参见图1,一种利用核磁共振测井构造伪毛管压力曲线方法,步骤如下:Referring to Fig. 1, a method for constructing a pseudo-capillary pressure curve using nuclear magnetic resonance logging, the steps are as follows:
1)、根据压汞实验的特点及操作过程,确定出13个进汞压力;1) According to the characteristics and operation process of the mercury injection experiment, 13 mercury injection pressures were determined;
2)、利用核磁共振测井仪器,对目标储集层进行测量并反演得到实际测量的核磁共振测井T2谱; 2 ) Using nuclear magnetic resonance logging tools to measure the target reservoir and invert to obtain the actually measured nuclear magnetic resonance logging T2 spectrum;
3)、给定7个不同的T2弛豫时间T2(1)、T2(2)、T2(3)、T2(4)、T2(5)、T2(6)和T2(7),将核磁共振T2谱划分为8个部分,然后计算出8个孔隙度组分百分含量;3), given 7 different T 2 relaxation times T 2 (1), T 2 (2), T 2 (3), T 2 (4), T 2 (5), T 2 (6) and T 2 (7), the nuclear magnetic resonance T 2 spectrum is divided into 8 parts, and then the percentage content of 8 porosity components is calculated;
4)、建立13个不同进汞压力下的进汞饱和度与8个孔隙度组分百分含量之间的函数关系,并利用其从核磁共振测井资料中计算13个进汞饱和度值;4) Establish the functional relationship between mercury saturation at 13 different mercury injection pressures and the percentage content of 8 porosity components, and use it to calculate 13 mercury saturation values from nuclear magnetic resonance logging data ;
5)、以计算的13个进汞饱和度值为横坐标,以给定的13个进汞压力值为纵坐标,建立平面直角坐标系,绘制伪毛管压力曲线;5), take the calculated 13 mercury injection saturation values as the abscissa, and take the given 13 mercury injection pressure values as the ordinate, establish a plane Cartesian coordinate system, and draw the pseudo-capillary pressure curve;
6)、根据孔喉半径与毛管压力之间的关系,获取储集层岩石孔喉半径分布,并计算平均孔喉半径、最大孔喉半径、中值半径、中值压力、排驱压力、均值系数和分选系数等储集层孔隙结构评价参数,以实现连续定量评价储集层孔隙结构的目的。6) According to the relationship between pore-throat radius and capillary pressure, the pore-throat radius distribution of reservoir rocks is obtained, and the average pore-throat radius, maximum pore-throat radius, median radius, median pressure, displacement pressure, and average value are calculated Reservoir pore structure evaluation parameters such as coefficient and sorting coefficient, in order to achieve the purpose of continuous and quantitative evaluation of reservoir pore structure.
所述步骤1)涉及的13个进汞压力值采用下式确定:The 13 mercury injection pressure values involved in said step 1) are determined by the following formula:
Pc(i)=0.005×2i-1,i=1,2,…13P c (i)=0.005×2 i-1 , i=1,2,...13
式中:Pc(i)为施加的第i个进汞压力,单位为MPa。In the formula: P c (i) is the i-th mercury injection pressure applied, and the unit is MPa.
所述步骤3)给定的7个T2弛豫时间分别为T2(1)=1.0ms、T2(2)=3.0ms、T2(3)=10.0ms、T2(4)=33.0ms、T2(5)=100.0ms、T2(6)=300.0ms和T2(7)=1000.0ms。The seven T 2 relaxation times given in step 3) are respectively T 2 (1)=1.0ms, T 2 (2)=3.0ms, T 2 (3)=10.0ms, T 2 (4)= 33.0 ms, T 2 (5) = 100.0 ms, T 2 (6) = 300.0 ms, and T 2 (7) = 1000.0 ms.
所述步骤3)定义的最小T2弛豫时间T2(0)=0.3ms;最大T2弛豫时间T2(8)=3000.0ms。The minimum T 2 relaxation time T 2 (0)=0.3ms defined in the step 3); the maximum T 2 relaxation time T 2 (8)=3000.0ms.
所述步骤3)涉及的8个孔隙度组分百分含量分别为X1、X2、X3、X4、X5、X6、X7和X8,其计算方法是:The 8 porosity component percentages involved in the step 3) are respectively X1, X2, X3, X4, X5, X6, X7 and X8, and the calculation method is:
式中S(t)为与T2弛豫时间相关的孔隙度分布函数。where S(t ) is the porosity distribution function related to T2 relaxation time.
所述步骤4)涉及的13个进汞饱和度采用如下公式计算:The 13 mercury saturation degrees involved in the step 4) are calculated using the following formula:
式中,
所述系数矩阵和常数矩阵的确定方法如下:The method for determining the coefficient matrix and the constant matrix is as follows:
钻取一部分代表性岩心样品,同时开展核磁共振和压汞实验,首先,根据7个给定的T2弛豫时间,将核磁共振T2谱划分为8个部分,并计算出8个岩石孔隙度组分百分含量作为自变量;然后,根据压汞毛管压力实验数据,确定出13个进汞饱和度值作为因变量;最后,采用多元线性统计回归的方法,分别确定出系数矩阵和常数矩阵的数值。Drill a part of representative core samples, carry out NMR and mercury injection experiments at the same time, first, divide the NMR T2 spectrum into 8 parts according to 7 given T2 relaxation times, and calculate the 8 rock pores The percent content of the mercury saturation component is used as the independent variable; then, according to the mercury injection capillary pressure experiment data, 13 mercury injection saturation values are determined as the dependent variable; finally, the coefficient matrix and the constant The numeric values of the matrix.
所述系数矩阵和常数矩阵的第一至第四行的数值均设为0,计算的进汞饱和度值也为0。The values in the first to fourth rows of the coefficient matrix and the constant matrix are all set to 0, and the calculated mercury saturation value is also 0.
实施例2Example 2
根据本发明所述的利用核磁共振测井构造伪毛管压力曲线方法,对国内西南地区某储集层钻取的20块岩心样品进行处理,标定进汞饱和度计算公式中系数矩阵和常数矩阵的数值,得到了连续构造毛管压力曲线的模型。利用标定的模型对实测的核磁共振测井资料进行处理,得到了连续的伪毛管压力曲线。为了评价毛管压力曲线构造模型的可靠性,读取了与20块岩心样品对应深度的伪毛管压力曲线,并将其与实验的压汞毛管压力曲线进行对比。According to the method of constructing pseudo-capillary pressure curve using nuclear magnetic resonance logging described in the present invention, 20 rock core samples drilled from a certain reservoir in Southwest China are processed, and the coefficient matrix and constant matrix in the mercury saturation calculation formula are calibrated Numerically, a model for the capillary pressure curve of the continuous construction was obtained. Using the calibrated model to process the measured NMR logging data, a continuous pseudo-capillary pressure curve is obtained. In order to evaluate the reliability of the capillary pressure curve structure model, the pseudo capillary pressure curves corresponding to the depths of 20 core samples were read and compared with the experimental mercury injection capillary pressure curves.
参见图4至图6,分别列举了孔隙结构较好、孔隙结构中等和孔隙结构较差的三类代表性岩心压汞毛管压力曲线与构造的伪毛管压力曲线对比图。从图中可以看到,对于各种不同类型的储集层岩石,利用本发明所述方法构造的伪毛管压力曲线与岩心实验得到的压汞毛管压力曲线均吻合较好。表2为20块岩心样品采用构造的伪毛管压力曲线计算的储集层孔隙结构评价参数与岩心压汞实验获取的储集层孔隙结构评价参数之间的误差统计表。从统计结果可以看到,利用本发明所述方法获取的伪毛管压力曲线计算的储集层孔隙结构评价参数与通过岩心压汞实验获取的结果之间的误差较小,其相对误差均小于10.0%,满足实际储集层孔隙结构定量评价的要求。Referring to Fig. 4 to Fig. 6, the comparison charts of mercury injection capillary pressure curves of three types of representative cores with good pore structure, medium pore structure and poor pore structure and pseudo-capillary pressure curves of structures are listed respectively. It can be seen from the figure that for various types of reservoir rocks, the pseudo capillary pressure curve constructed by the method of the present invention is in good agreement with the mercury injection capillary pressure curve obtained from the core experiment. Table 2 is a statistical table of errors between the evaluation parameters of reservoir pore structure calculated by using the constructed pseudo-capillary pressure curve of 20 core samples and the evaluation parameters of reservoir pore structure obtained from core mercury injection experiments. As can be seen from the statistical results, the error between the evaluation parameters of the reservoir pore structure calculated by the pseudo capillary pressure curve obtained by the method of the present invention and the result obtained by the core mercury injection experiment is small, and the relative errors are all less than 10.0 %, meeting the requirements for quantitative evaluation of actual reservoir pore structure.
表220块岩心样品不同方法计算的储集层孔隙结构评价参数误差统计表Table 220. Statistical table of error statistics of reservoir pore structure evaluation parameters calculated by different methods for 220 core samples
参见图7,为利用本发明所述方法构造的伪毛管压力曲线及计算的储集层孔隙结构评价参数与岩心压汞实验结果的对比图。图7所示的效果图共分为十二道,图中第一道包括自然伽马曲线(GR)和井径曲线(CAL),主要用于识别有效砂岩储集层;第二道为深度道,单位m;第三道为深侧向电阻率曲线(RT)和浅侧向电阻率曲线(RXO);第四道包括密度测井(DEN)曲线、中子测井(CNL)曲线和声波时差测井(AC)曲线,主要用于计算储集层的孔隙度;第五道包括实际测量的核磁共振测井T2谱T2_DIST;第六道包括根据本发明实施例提供的方法利用实际测量的核磁共振测井T2谱连续构造的伪毛管压力曲线与岩心压汞毛管压力曲线的对比,图中黑色曲线为利用核磁共振测井资料连续构造的伪毛管压力曲线,为了曲线显示的方便,本发明中将伪毛管压力曲线累加到最大进汞压力20.48MPa的状态,而离散曲线则为岩心压汞毛管压力曲线;第七道所示为利用本发明实施例所示方法构造的伪毛管压力曲线转换成的储集层孔喉半径分布与利用压汞毛管压力曲线获取的孔喉半径分布的对比图,图中离散的曲线即为根据岩心压汞毛管压力曲线获取的孔喉半径分布。从第六道和第七道显示的结果可以看出,利用本发明实施例所述的方法构造的伪毛管压力曲线及获取的孔喉半径分布与岩心压汞实验结果具有较好的一致性。第八道中RM为利用本发明实施例提供的方法连续构造的伪毛管压力曲线计算的平均孔喉半径,CRM为岩心压汞实验得到的平均孔喉半径;第九道中RC50为利用本发明实施例提供的方法连续构造的伪毛管压力曲线计算的中值半径,CR50为岩心压汞实验得到的中值半径;第十道中RMAX为利用本发明实施例提供的方法连续构造的伪毛管压力曲线计算的最大孔喉半径,CRMAX为岩心压汞实验得到的最大孔喉半径。第十一道中PD为利用本发明实施例提供的方法连续构造的伪毛管压力曲线计算的排驱压力,CPD为岩心压汞实验得到的排驱压力;第十二道中PC50为利用本发明实施例提供的方法连续构造的伪毛管压力曲线计算的中值压力,CP50为岩心压汞实验得到的中值压力。从图上可以看出,利用本发明所述方法连续构造的伪毛管压力曲线计算的储集层孔隙结构评价参数接近岩心压汞实验结果,这说明,利用本发明所述方法可以将核磁共振测井T2谱连续地转换成伪毛管压力曲线,以得到准确的储集层孔喉半径分布和储集层孔隙结构评价参数。Referring to Fig. 7, it is a comparison chart of the pseudo-capillary pressure curve constructed by the method of the present invention, the calculated reservoir pore structure evaluation parameters and the core mercury injection test results. The effect map shown in Fig. 7 is divided into twelve tracks. The first track in the figure includes the natural gamma ray curve (GR) and the caliper curve (CAL), which are mainly used to identify effective sandstone reservoirs; the second track is the depth Trace, unit m; the third trace is deep lateral resistivity curve (RT) and shallow lateral resistivity curve (RXO); the fourth trace includes density logging (DEN) curve, neutron logging (CNL) curve and Acoustic time-difference logging (AC) curves are mainly used to calculate the porosity of the reservoir; the fifth track includes the actually measured nuclear magnetic resonance logging T 2 spectrum T2_DIST; the sixth track includes the actual The comparison between the measured NMR logging T2 spectral continuous pseudo - capillary pressure curve and the core mercury injection capillary pressure curve. The black curve in the figure is the pseudo-capillary pressure curve continuously constructed using nuclear magnetic resonance logging data. For the convenience of curve display , in the present invention, the pseudo capillary pressure curve is added to the state of the maximum mercury injection pressure of 20.48MPa, while the discrete curve is the core mercury injection capillary pressure curve; the seventh track shows the pseudo capillary pressure constructed by the method shown in the embodiment of the present invention The comparison chart of the reservoir pore throat radius distribution converted from the pressure curve and the pore throat radius distribution obtained from the mercury injection capillary pressure curve. The discrete curve in the figure is the pore throat radius distribution obtained from the core mercury injection capillary pressure curve. From the results shown in the sixth and seventh tracks, it can be seen that the pseudo capillary pressure curve constructed by the method described in the embodiment of the present invention and the obtained pore throat radius distribution are in good agreement with the results of the core mercury injection experiment. In the eighth track, RM is the average pore-throat radius calculated from the pseudo-capillary pressure curve continuously constructed by the method provided by the embodiment of the present invention, and CRM is the average pore-throat radius obtained from the core mercury injection experiment; The median radius of the pseudo-capillary pressure curve calculated by the method provided by the example, CR50 is the median radius obtained by the core mercury injection experiment; RMAX in the tenth track is the calculation of the pseudo-capillary pressure curve of the continuous structure using the method provided by the embodiment of the present invention CRMAX is the maximum pore throat radius obtained from the core mercury injection experiment. In the eleventh track, PD is the displacement pressure calculated by using the pseudo-capillary pressure curve continuously constructed by the method provided by the embodiment of the present invention, and CPD is the displacement pressure obtained from the core mercury injection experiment; The median pressure calculated from the continuously constructed pseudo-capillary pressure curve provided by the method provided in the example, and CP50 is the median pressure obtained from the core mercury injection experiment. As can be seen from the figure, the reservoir pore structure evaluation parameters calculated by using the pseudo-capillary pressure curve continuously constructed by the method of the present invention are close to the results of the core mercury injection experiment. The well T2 spectrum is continuously converted into a pseudo-capillary pressure curve to obtain accurate reservoir pore throat radius distribution and reservoir pore structure evaluation parameters.
最后应说明的是:显然,上述实施例仅仅是为清楚地说明本发明所作的举例,而并非对实施方式的限定。对于所属领域的普通技术人员来说,在上述说明的基础上还可以做出其它不同形式的变化或变动。这里无需也无法对所有的实施方式予以穷举。而由此所引伸出的显而易见的变化或变动仍处于本发明的保护范围之中。Finally, it should be noted that: obviously, the above-mentioned embodiments are only examples for clearly illustrating the present invention, rather than limiting the implementation. For those of ordinary skill in the art, other changes or changes in different forms can be made on the basis of the above description. It is not necessary and impossible to exhaustively list all the implementation manners here. However, the obvious changes or changes derived therefrom still fall within the scope of protection of the present invention.
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