CN110671100B - Method for manufacturing chessboard-like simulator in device for simulating rock heterogeneity - Google Patents
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- 239000011435 rock Substances 0.000 title claims abstract description 27
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Abstract
一种利用棋盘状仿真体模拟岩石非均质性的装置及制造方法。主要目的在于可在实验室内实现精准模拟岩石平面非均质性。其特征在于:装置由ISCO恒压泵,电子压力表,五通阀,导管,2×2×10cm的不同渗透率单元,浇筑非均质仿真体以及量筒组成。该装置的制造依赖于实际岩石的渗透率分布情况,首先收集待模拟区域所有井井点的各层渗透率数据,然后通过变差函数将这些渗透率数据进行离散,从而得到平面上任一点的渗透率值,这样可以把岩石的平面非均质性在仿真体中得到充分的体现,使得实验室模拟岩石平面非均质性成为可能,从而可以更加方便的研究平面非均质性对油藏开发的影响。A device and a manufacturing method for simulating rock heterogeneity using a chessboard-shaped simulation body. The main purpose is to accurately simulate rock plane heterogeneity in the laboratory. It is characterized in that: the device consists of an ISCO constant pressure pump, an electronic pressure gauge, a five-way valve, a conduit, a 2×2×10cm unit of different permeability, a casting heterogeneous simulation body and a graduated cylinder. The manufacture of the device depends on the permeability distribution of the actual rock. First, the permeability data of each layer of all well points in the area to be simulated are collected, and then these permeability data are discretized by the variogram to obtain the permeability of any point on the plane. In this way, the plane heterogeneity of the rock can be fully reflected in the simulation body, making it possible to simulate the plane heterogeneity of the rock in the laboratory, so that it can be more convenient to study the effect of plane heterogeneity on reservoir development. Impact.
Description
技术领域:Technical field:
本发明涉及一种用于驱油实验中模拟岩石非均质性的仿真体装置。The invention relates to a simulation body device for simulating rock heterogeneity in oil displacement experiments.
技术背景:technical background:
我国的油田主要就是以陆相碎屑岩储层为主,地质条件复杂性较高,非均质性强,原油的性质相差比较大,所以开采效率比较低。因此对非均质进行全面的研究是十分有必要的。由于储层在形成过程中受沉积作用、成岩作用和构造作用的影响,使其在空间分布及其内部各种属性都存在变化,目前研究储层的非均质性主要是实验方法,但是该方法仅仅是通过不同渗透率岩心的简单并联来模拟储层的非均质性。由于实验条件受限,并联的岩心个数不能太多,同时,每个岩心的渗透率数值都是使用某一研究区块的渗透率的平均值制成的,这样与实际储层的非均质性差距较大,不能很好的对储层进行模拟,从而导致实验室驱油实验的结果有时候不能很好的指导现场开发。my country's oilfields are mainly dominated by continental clastic rock reservoirs, with high complexity of geological conditions, strong heterogeneity, and relatively large differences in the properties of crude oil, so the extraction efficiency is relatively low. Therefore, it is necessary to conduct a comprehensive study of heterogeneity. Due to the influence of sedimentation, diagenesis and tectonic action in the formation process of the reservoir, its spatial distribution and various properties within it vary. At present, the research on the heterogeneity of the reservoir is mainly an experimental method. The method simply simulates the heterogeneity of the reservoir by a simple parallel connection of cores of different permeability. Due to the limited experimental conditions, the number of cores connected in parallel should not be too many. At the same time, the permeability value of each core is made by using the average value of the permeability of a certain research block, which is not uniform with the actual reservoir. The quality gap is large, and the reservoir cannot be simulated well, so that the results of the laboratory oil flooding experiment sometimes cannot guide the field development very well.
发明内容:Invention content:
为了解决技术背景中所提到的技术问题,本发明提供了一种利用棋盘状仿真体模拟岩石非均质性的装置。非均质性研究是油藏描述的重要内容,其参数的空间分布不仅具有随机性,而且具有结构性。本发明以研究区域所有井的渗透率数据为基础,从地质统计学关于变差函数的基本理论出发,根据一些已知的渗透率分布数据,通过变差函数将这些已知的渗透率数据进行离散,这样可以得到平面上任一点的渗透率值,从而形成棋盘状仿真体模型,来反映岩石的平面非均质特征。该模型以实际的渗透率分布为基础,通过变差函数对其进行离散,并用2×2×10cm的渗透率单元将其模拟出来,从而将岩石中渗透率的分布规律可以在棋盘状仿真体中得以充分的体现。同时,在对岩石渗透率分布进行了精细描述的棋盘状仿真体上布置单一的五点法井组,使得实验室中模拟岩石非均质性驱油实验更加接近实际情况,这样能够为现场开发提供更好的实验依据。In order to solve the technical problems mentioned in the technical background, the present invention provides a device for simulating rock heterogeneity by using a chessboard-shaped simulation body. Heterogeneity research is an important part of reservoir description, and the spatial distribution of its parameters is not only random but also structural. The present invention is based on the permeability data of all wells in the research area, starting from the basic theory of geostatistics about the variogram, and according to some known permeability distribution data, the known permeability data are processed by the variogram function. In this way, the permeability value of any point on the plane can be obtained, thus forming a checkerboard simulation model to reflect the plane heterogeneity of the rock. The model is based on the actual permeability distribution, which is discretized by the variogram, and simulated with a 2×2×10cm permeability unit, so that the distribution law of permeability in the rock can be displayed in a checkerboard simulation body. fully reflected in. At the same time, a single five-point method well group is arranged on a checkerboard-shaped simulation body that has a fine description of the rock permeability distribution, so that the simulated rock heterogeneous oil displacement experiment in the laboratory is closer to the actual situation, which can be used for field development. Provide a better experimental basis.
本发明的技术方案是:一种利用浇筑非均质仿真体模拟岩石非均质性的装置,包括ISCO恒压泵、导管、电子压力表、五通阀、第一螺纹接头、流量调节器、第二螺纹接头以及量筒,其独特之处在于:The technical scheme of the present invention is: a device for simulating rock heterogeneity by using a casting heterogeneous simulation body, comprising an ISCO constant pressure pump, a conduit, an electronic pressure gauge, a five-way valve, a first threaded joint, a flow regulator, The second threaded joint and the measuring cylinder are unique in that:
所述装置还包括浇筑非均质仿真体;所述浇筑非均质仿真体由长、宽、高分别为2厘米、2厘米和10厘米的若干个渗透率不同的单元体组成,所述若干个渗透率不同的单元体形成一个方形体;所述单元体的不同渗透率通过对实际地层渗透率的数值通过离散后模拟得出。The device also includes a casting heterogeneous simulation body; the casting heterogeneous simulation body is composed of several units with different permeability, each of which is 2 cm, 2 cm and 10 cm in length, width and height. Each unit body with different permeability forms a square body; the different permeability of the unit body is obtained by the numerical simulation of the actual formation permeability after discretization.
在所述浇筑非均质仿真体的外层浇筑环氧树脂浇筑层,且穿过所述环氧树脂浇筑层在浇筑非均质仿真体上布置有单一五点法井组,所述单一五点法井组采用中央一口井,位于四个对角四口井的模式。An epoxy resin casting layer is cast on the outer layer of the casting heterogeneous simulation body, and a single five-point method well group is arranged on the casting heterogeneous simulation body through the epoxy resin casting layer. The one-five-point well group adopts the pattern of one well in the center and four wells in four diagonal corners.
所述第二螺纹接头两端同时设置有螺纹,第二螺纹接头的下端与浇筑非均质仿真体上的单一五点法井组的螺纹通孔通过旋拧连接,第二螺纹接头的上端与流量调节器的螺纹通孔通过旋拧连接。Both ends of the second threaded joint are provided with threads at the same time, the lower end of the second threaded joint is connected with the threaded through hole of the single five-point method well group on the casting heterogeneous simulation body by screwing, and the upper end of the second threaded joint is connected by screwing. Connect with the threaded through hole of the flow regulator by screwing.
所述第一螺纹接头仅在一端设置有螺纹,其中第一螺纹接头有螺纹的一端与流量调节器的螺纹通孔通过旋拧连接,无螺纹的另一端与第二导管连接。The first threaded joint is provided with threads only at one end, wherein the threaded end of the first threaded joint is connected with the threaded through hole of the flow regulator by screwing, and the unthreaded other end is connected with the second conduit.
所述流量调节器具有两个螺纹通孔和一个旋钮,两个螺纹通孔分别与第一螺纹接头和第二螺纹接头相连接,旋钮用来控制模拟实际注入井和采出井的注入速度和采出速度。The flow regulator has two threaded through holes and a knob, the two threaded through holes are respectively connected with the first threaded joint and the second threaded joint, and the knob is used to control the injection speed and production rate of the simulated actual injection well and production well. out speed.
电子压力表通过第一导管连接在ISCO恒压泵和五通阀的液流输入口之间;五通阀的四个液流输出口分别通过第二导管与接入四个对角井的第一螺纹接头的无螺纹一端相连接;接入一个中央井的第一螺纹接头的无螺纹一端通过第二导管与量筒的入口连接。The electronic pressure gauge is connected between the ISCO constant pressure pump and the liquid flow input port of the five-way valve through the first conduit; The unthreaded end of the threaded joint is connected; the unthreaded end of the first threaded joint connected to a central well is connected with the inlet of the measuring cylinder through the second conduit.
用于制作所述模拟非均质岩石的棋盘状仿真体的方法有两种,第一种方法包括如下步骤:There are two methods for making the chessboard simulation body for simulating heterogeneous rocks, the first method includes the following steps:
第一步,限定渗透率不同的单元体(11)所模拟的平面尺寸为50×50m,待模拟区域的长为L,宽为D,按照公式(1)计算出每一层不同渗透率单元的数量为N;In the first step, the plane size simulated by the unit body (11) with different permeability is defined as 50×50m, the length of the area to be simulated is L, and the width is D. According to formula (1), calculate the unit with different permeability for each layer The number is N;
第二步,收集待模拟区域所有井井点的各层渗透率数据,建立已知渗透率数据库,其中井的数量为Q,层的数量为P,各井在XOY平面上的坐标为(i,j),则各井在第z层的渗透率值为Kz(i,j);The second step is to collect the permeability data of each layer of all wells in the area to be simulated, and establish a known permeability database, in which the number of wells is Q, the number of layers is P, and the coordinates of each well on the XOY plane are (i , j), then the permeability value of each well in the z-th layer is K z (i, j);
第三步,通过对第二步所获得的第一层渗透率数据进行离散,可以得到第一层平面上任一点的渗透率值,即可以知道第一层上渗透率的分布情况,其具体按照如下过程进行计算:In the third step, by discretizing the permeability data of the first layer obtained in the second step, the permeability value of any point on the plane of the first layer can be obtained, that is, the distribution of the permeability on the first layer can be known. The calculation is performed as follows:
首先,根据各井在第一层上第m行的渗透率值,利用公式(2)求得相距为h的两口井之间的渗透率的变差函数为Kz(h);First, according to the permeability value of each well in the mth row on the first layer, the variogram of the permeability between two wells with a distance of h is obtained by using formula (2) as K z (h);
其中,公式(2)为:Among them, formula (2) is:
式中:where:
N(h)——距离为h的两口井的对数。N(h) - the logarithm of two wells with distance h.
为了使得计算过程的表达更加方便引入中间替换变量x1、x2和y以及b0,b1和b2。基于公式(2)的结果,利用公式(3)、公式(4)和公式(5)可以求得一系列的x1、x2和y;In order to make the expression of the calculation process more convenient, intermediate substitution variables x 1 , x 2 and y and b 0 , b 1 and b 2 are introduced. Based on the result of formula (2), a series of x 1 , x 2 and y can be obtained by using formula (3), formula (4) and formula (5);
其中,公式(3)、公式(4)和公式(5)分别为:Among them, formula (3), formula (4) and formula (5) are respectively:
x1=h (3)x 1 = h (3)
x2=-h3 (4)x 2 = -h 3 (4)
y=Kz(h) (5)y=K z (h) (5)
然后,将求得的x1、x2和y代入带公式(6)中,使用线性规划的方法进行数据的拟合,可以求得b0,b1,b2;Then, substitute the obtained x 1 , x 2 and y into the belt formula (6), and use the linear programming method to fit the data to obtain b 0 , b 1 , b 2 ;
其中,公式(6)为:Among them, formula (6) is:
y=b0+b1x1+b2x2 (6)y=b 0 +b 1 x 1 +b 2 x 2 (6)
通过对比公式(6)和公式(7)可得公式(8)、公式(9)和公式(10)分别为:By comparing formula (6) and formula (7), formula (8), formula (9) and formula (10) can be obtained as:
C0=b0 (9)C 0 =b 0 (9)
最后可以确定第一层上第m行的渗透率的变差函数方程式,如公式(11)所示,即得到第一层第m行上任意两点的渗透率方差之半,从而可以求出第一层第m行上离散后的渗透率值,即可以得到第一层第m行上渗透率的分布情况;Finally, the variogram equation of the permeability of the m-th row on the first layer can be determined, as shown in formula (11), that is, half of the permeability variance of any two points on the m-th row of the first layer can be obtained. The discrete permeability value on the mth row of the first layer, that is, the distribution of the permeability on the mth row of the first layer can be obtained;
其中,公式(11)为:Among them, formula (11) is:
式中:where:
a——变程,在该范围内渗透率间具有相关性,而在变程外渗透率间不具有相关性;a - variable range, there is a correlation between the permeability within this range, but there is no correlation between the permeability outside the variable range;
C0——块金值,反映渗透率变差函数的变化幅度;C 0 — nugget value, reflecting the variation range of the permeability variation function;
C1——基台值,由于诸多因素影响导致渗透率在短距离内发生大变异;C 1 ——The value of the abutment, due to the influence of many factors, the permeability has a large variation in a short distance;
h——两点之间的距离;h - the distance between two points;
运用同样的方法求得第一层上已知部分渗透率的任意一行的变差函数方程式,从而可以求出该行上离散后的渗透率值,即可以得到该行上渗透率的分布情况;然后基于横向上每一行的渗透率值,在纵向上求出任意一列的变差函数方程式,这样就可以知道第一层上每一点的渗透率值,从而可以得到第一层的渗透率分布情况;Using the same method to obtain the variogram equation of any row of the known partial permeability on the first layer, the discrete permeability value of the row can be obtained, that is, the permeability distribution of the row can be obtained; Then, based on the permeability value of each row in the horizontal direction, the variogram equation of any column in the vertical direction is obtained, so that the permeability value of each point on the first layer can be known, and the permeability distribution of the first layer can be obtained. ;
第四步,重复第三步可以求得第二层上每一点的渗透率值,即可以得到第二层的渗透率分布情况,直到求出第P层上每一点的渗透率值为止,即可以获得所有层的渗透率值和渗透率分布情况;The fourth step, repeating the third step can obtain the permeability value of each point on the second layer, that is, the permeability distribution of the second layer can be obtained, until the permeability value of each point on the P-th layer is obtained, that is, The permeability value and permeability distribution of all layers can be obtained;
第五步,为了减少渗透率单元的制作数量,简化仿真体的制作步骤,同时又在实验误差允许的范围内,划分不同的渗透率区间进行统计分析;对第三步和第四步中所得到的每层渗透率数据进行统计分析,确定其分布到不同渗透率区间的数量,这样就可以确定分布到不同渗透率区间的单元数量;The fifth step, in order to reduce the number of permeability units, simplify the manufacturing steps of the simulation body, and at the same time, within the allowable range of experimental errors, divide different permeability intervals for statistical analysis; The obtained permeability data of each layer is statistically analyzed to determine the number of units distributed to different permeability ranges, so that the number of units distributed to different permeability ranges can be determined;
第六步,根据第五步所得到的分布在不同渗透率区间的渗透率单元数量,由不同粒度的石英砂和环氧树脂胶结形成分布在不同渗透率区间的渗透率单元,然后将每一层的N个具有不同渗透率的单元根据第三步和第四步计算得到的渗透率的分布情况进行排列,依次排列P层,使其所模拟的岩石更加符合实际情况。In the sixth step, according to the number of permeability units distributed in different permeability intervals obtained in the fifth step, the permeability units distributed in different permeability intervals are formed by cementing quartz sand and epoxy resin with different particle sizes. The N units with different permeability in the layer are arranged according to the distribution of permeability calculated in the third and fourth steps, and the P layers are arranged in sequence to make the simulated rocks more in line with the actual situation.
制作所述模拟非均质岩石的棋盘状仿真体的第二种方法包括如下步骤:The second method of making the chessboard simulation body for simulating heterogeneous rocks includes the following steps:
第一步,限定渗透率不同的单元体(11)所模拟的平面尺寸为50×50m,待模拟区域的长为L,宽为D,按照公式(1)计算出每一层不同渗透率单元的数量为N。In the first step, the plane size simulated by the unit body (11) with different permeability is defined as 50×50m, the length of the area to be simulated is L, and the width is D. According to formula (1), calculate the unit with different permeability for each layer The number is N.
第二步,收集待模拟区域所有井井点的各层渗透率数据,建立已知渗透率数据库,其中井的数量为Q,层的数量为P,各井在XOY平面上的坐标为(i,j),则各井在第z层的渗透率值为Kz(i,j)。The second step is to collect the permeability data of each layer of all wells in the area to be simulated, and establish a known permeability database, in which the number of wells is Q, the number of layers is P, and the coordinates of each well on the XOY plane are (i , j), then the permeability value of each well in the z-th layer is K z (i, j).
第三步,通过对第二步所获得的第一层渗透率数据进行离散,可以得到第一层平面上任一点的渗透率值,即可以知道第一层上渗透率的分布情况,其具体按照如下过程进行计算。In the third step, by discretizing the permeability data of the first layer obtained in the second step, the permeability value of any point on the plane of the first layer can be obtained, that is, the distribution of the permeability on the first layer can be known. The calculation is performed as follows.
首先,根据各井在第一层上第m行的渗透率值,利用公式(2)求得相距为h的两口井之间的渗透率的变差函数为Kz(h)。First, according to the permeability values of the m-th row of each well on the first layer, the variogram of the permeability between two wells separated by h is obtained by using formula (2) as K z (h).
其中,公式(2)为:Among them, formula (2) is:
式中:where:
N(h)——距离为h的两口井的对数。N(h) - the logarithm of two wells with distance h.
为了使得计算过程的表达更加方便引入中间替换变量x1、x2和y以及b0,b1和b2。基于公式(2)的结果,利用公式(3)、公式(4)和公式(5)可以求得一系列的x1、x2和y。In order to make the expression of the calculation process more convenient, intermediate substitution variables x 1 , x 2 and y and b 0 , b 1 and b 2 are introduced. Based on the result of formula (2), a series of x 1 , x 2 and y can be obtained using formula (3), formula (4) and formula (5).
其中,公式(3)、公式(4)和公式(5)分别为:Among them, formula (3), formula (4) and formula (5) are respectively:
x1=h (3)x 1 = h (3)
x2=-h3 (4)x 2 = -h 3 (4)
y=Kz(h) (5)y=K z (h) (5)
然后,将求得的x1、x2和y代入带公式(6)中,使用线性规划的方法进行数据的拟合,可以求得b0,b1,b2。Then, the obtained x 1 , x 2 and y are substituted into the belt formula (6), and the linear programming method is used to fit the data to obtain b 0 , b 1 , and b 2 .
其中,公式(6)为:Among them, formula (6) is:
y=b0+b1x1+b2x2 (6)y=b 0 +b 1 x 1 +b 2 x 2 (6)
通过对比公式(6)和公式(7)可得公式(8)、公式(9)和公式(10)分别为:By comparing formula (6) and formula (7), formula (8), formula (9) and formula (10) can be obtained as:
C0=b0 (9)C 0 =b 0 (9)
最后可以确定第一层上第m行的渗透率的变差函数方程式,如公式(11)所示,即得到第一层第m行上任意两点的渗透率方差之半,从而可以求出第一层第m行上离散后的渗透率值,即可以得到第一层第m行上渗透率的分布情况。Finally, the variogram equation of the permeability of the m-th row on the first layer can be determined, as shown in formula (11), that is, half of the permeability variance of any two points on the m-th row of the first layer can be obtained. The discrete permeability value on the mth row of the first layer can obtain the permeability distribution on the mth row of the first layer.
其中,公式(11)为:Among them, formula (11) is:
式中:where:
a——变程,在该范围内渗透率间具有相关性,而在变程外渗透率间不具有相关性;a - variable range, there is a correlation between the permeability within this range, but there is no correlation between the permeability outside the variable range;
C0——块金值,反映渗透率变差函数的变化幅度;C 0 — nugget value, reflecting the variation range of the permeability variation function;
C1——基台值,由于诸多因素影响导致渗透率在短距离内发生大变异;C 1 ——The value of the abutment, due to the influence of many factors, the permeability has a large variation in a short distance;
h——两点之间的距离。h - the distance between two points.
运用同样的方法求得第一层上已知部分渗透率的任意一行的变差函数方程式,从而可以求出该行上离散后的渗透率值,即可以得到该行上渗透率的分布情况。然后基于横向上每一行的渗透率值,在纵向上求出任意一列的变差函数方程式,这样就可以知道第一层上每一点的渗透率值,从而可以得到第一层的渗透率分布情况。Using the same method to obtain the variogram equation of any line of known partial permeability on the first layer, the discrete permeability value on the line can be obtained, that is, the permeability distribution on the line can be obtained. Then, based on the permeability value of each row in the horizontal direction, the variogram equation of any column in the vertical direction is obtained, so that the permeability value of each point on the first layer can be known, and the permeability distribution of the first layer can be obtained. .
第四步,重复第三步可以求得第二层上每一点的渗透率值,即可以得到第二层的渗透率分布情况,直到求出第P层上每一点的渗透率值为止,即可以获得所有层的渗透率值和渗透率分布情况。The fourth step, repeating the third step can obtain the permeability value of each point on the second layer, that is, the permeability distribution of the second layer can be obtained, until the permeability value of each point on the P-th layer is obtained, that is, Permeability values and permeability distributions for all layers can be obtained.
第五步,根据第三步和第四步中得到的所有层上的每一点渗透率值以及渗透率的分布情况,由不同粒度的石英砂和环氧树脂胶结形成M个不同渗透率单元,其中M由公式(12)计算得到。In the fifth step, according to the permeability value of each point on all the layers obtained in the third and fourth steps and the distribution of permeability, M units of different permeability are formed by cementing quartz sand and epoxy resin with different particle sizes, where M is calculated by formula (12).
其中,公式(12)为:Among them, formula (12) is:
M=NP (12)M=NP (12)
然后将每一层的N个具有不同渗透率的单元根据第三步和第四步计算得到的渗透率的分布情况进行排列,依次排列P层,使其所模拟的岩石更加符合实际情况。Then, the N units with different permeability in each layer are arranged according to the distribution of permeability calculated in the third and fourth steps, and the P layers are arranged in sequence to make the simulated rocks more in line with the actual situation.
本发明具有以下有益效果:本发明以所待模拟区域所有井井点的各层渗透率数据为基础,从地质统计学关于变差函数的基本理论出发,根据一些已知的渗透率分布数据,通过变差函数将这些已知的渗透率数据进行离散,这样可以得到平面上任一点的渗透率数据,和目前实验中并联几个仅代表某一研究区块平均渗透率的岩心相比,更加符合储层的非均质性,为现场开发提供更加可靠实验依据。The present invention has the following beneficial effects: the present invention is based on the permeability data of each layer of all well points in the area to be simulated, starting from the basic theory of geostatistics about variogram, and according to some known permeability distribution data, These known permeability data are discretized by the variogram, so that the permeability data of any point on the plane can be obtained, which is more in line with the current experiments in parallel with several cores that only represent the average permeability of a certain research block. The heterogeneity of the reservoir provides a more reliable experimental basis for field development.
附图说明:Description of drawings:
图1是利用棋盘状仿真体模拟岩石非均质性的综合装置示意图。Figure 1 is a schematic diagram of a comprehensive device for simulating rock heterogeneity using a checkerboard-shaped simulation body.
图2是棋盘状仿真体示意图。FIG. 2 is a schematic diagram of a checkerboard-shaped simulation body.
图3是棋盘状仿真体的横向剖面图。FIG. 3 is a transverse cross-sectional view of a checkerboard-shaped simulation body.
图4是棋盘状仿真体的纵向剖面图。FIG. 4 is a longitudinal cross-sectional view of a checkerboard-shaped simulation body.
图5是导管、第一螺纹接头和第二螺纹接头以及流量调节器零件示意图。Figure 5 is a schematic diagram of the conduit, the first and second threaded joints, and the flow regulator parts.
图6是第一螺纹接头与流量调节器连接剖面图。FIG. 6 is a sectional view of the connection between the first threaded joint and the flow regulator.
图7是第二螺纹接头与流量调节器连接剖面图。FIG. 7 is a sectional view of the connection between the second threaded joint and the flow regulator.
图8是ISCO恒压泵示意图。Figure 8 is a schematic diagram of an ISCO constant pressure pump.
图9是电子压力表示意图。Figure 9 is a schematic diagram of an electronic pressure gauge.
图10是五通阀示意图。Figure 10 is a schematic diagram of a five-way valve.
图11是待模拟正方形区域井位图。Figure 11 is a well map of the square area to be simulated.
图中1-ISCO恒压泵,2-导管,3-电子压力表,4-五通阀,5-第一螺纹接头,6-流量调节器,7-第二螺纹接头,8-浇筑非均质棋盘状仿真体,9-量筒,10-环氧树脂,11-2×2×10cm的不同渗透率单元,12-旋钮。In the picture 1-ISCO constant pressure pump, 2-duct, 3-electronic pressure gauge, 4-five-way valve, 5-first threaded joint, 6-flow regulator, 7-second threaded joint, 8-pouring non-uniform Quality checkerboard simulation body, 9-grading cylinder, 10-epoxy resin, 11-2×2×10cm units of different permeability, 12-knob.
具体实施方式:Detailed ways:
下面结合附图对本发明作进一步说明:The present invention will be further described below in conjunction with the accompanying drawings:
由图1到图10所示,本种利用浇筑非均质仿真体模拟岩石非均质性的装置,包括ISCO恒压泵1、导管2、电子压力表3、五通阀4、第一螺纹接头5、流量调节器6、第二螺纹接头7以及量筒9,其独特之处在于:As shown in Figure 1 to Figure 10, this device for simulating rock heterogeneity by using a casting heterogeneous simulation body includes an ISCO
所述装置还包括浇筑非均质仿真体8。The device also includes a casting
所述浇筑非均质仿真体8由长、宽、高分别为2厘米、2厘米和10厘米的若干个渗透率不同的单元体11组成,所述若干个渗透率不同的单元体11形成一个方形体;所述单元体11的不同渗透率通过对实际地层渗透率的数值通过离散后模拟得出。The casting
在所述浇筑非均质仿真体8的外层浇筑环氧树脂浇筑层10,且穿过所述环氧树脂浇筑层在浇筑非均质仿真体8上布置有单一五点法井组,所述单一五点法井组采用中央一口井,位于四个对角四口井的模式。An epoxy
所述第二螺纹接头7两端同时设置有螺纹,第二螺纹接头7的下端与浇筑非均质仿真体8上的单一五点法井组的螺纹通孔通过旋拧连接,第二螺纹接头7的上端与流量调节器6的螺纹通孔通过旋拧连接。Both ends of the second threaded joint 7 are provided with threads at the same time. The upper end of the joint 7 is connected with the threaded through hole of the
所述第一螺纹接头5仅在一端设置有螺纹,其中第一螺纹接头5有螺纹的一端与流量调节器6的螺纹通孔通过旋拧连接,无螺纹的另一端与第二导管连接。The first threaded joint 5 is provided with threads only at one end, wherein the threaded end of the first threaded joint 5 is connected with the threaded through hole of the
所述流量调节器6具有两个螺纹通孔和一个旋钮12,两个螺纹通孔分别与第一螺纹接头5和第二螺纹接头7相连接,旋钮12用来控制模拟实际注入井和采出井的注入速度和采出速度。The
电子压力表3通过第一导管2连接在ISCO恒压泵1和五通阀4的液流输入口之间;五通阀4的四个液流输出口分别通过第二导管与接入四个对角井的第一螺纹接头5的无螺纹一端相连接;接入一个中央井的第一螺纹接头5的无螺纹一端通过第二导管与量筒9的入口连接。The
下面给出制作所述模拟非均质岩石的棋盘状仿真体的第一种方法的一个具体实施例:包括如下步骤:A specific embodiment of the first method for making the chessboard-shaped simulation body for simulating heterogeneous rocks is given below: including the following steps:
第一步,限定渗透率单元所模拟的平面尺寸为50×50m,待模拟区域的长L为1500m,宽D为1470m,按照公式(1)计算出每一层不同渗透率单元的数量N为900。In the first step, the plane size simulated by the permeability unit is 50×50m, the length L of the area to be simulated is 1500m, and the width D is 1470m. According to formula (1), the number N of different permeability units in each layer is calculated as 900.
第二步,待模拟区域中井的数量Q为37,层的数量P为3,由于各个井都为垂直井,故每口井在各个层平面的坐标都是一样的,待模拟正方形区域的井位如图11所示,其每口井对应的平面坐标如表1所示。收集该区域所有井井点的各层渗透率数据,建立已知渗透率数据库,如表2所示。In the second step, the number of wells Q in the area to be simulated is 37, and the number of layers P is 3. Since each well is a vertical well, the coordinates of each well in each layer plane are the same, and the wells in the square area to be simulated are The positions are shown in Figure 11, and the plane coordinates corresponding to each well are shown in Table 1. Collect the permeability data of each layer of all wells in this area, and establish a database of known permeability, as shown in Table 2.
表1每口井平面坐标统计表Table 1 Statistical table of plane coordinates of each well
表2已知渗透率数据库Table 2 Known permeability database
第三步,通过对第二步所获得的第一层渗透率数据进行离散,可以得到第一层平面上任一点的渗透率值,即可以知道第一层上渗透率的分布情况,求取第一层上第26行的渗透率值和渗透率分布情况具体按照如下过程进行计算。In the third step, by discretizing the permeability data of the first layer obtained in the second step, the permeability value of any point on the plane of the first layer can be obtained, that is, the distribution of the permeability on the first layer can be known, and the first The permeability value and permeability distribution of the 26th row on the first layer are calculated according to the following process.
首先,根据各井在第一层上第26行的渗透率值,利用公式(2)求得相距为h的两口井之间的渗透率的变差函数为K1(h),设相邻的两个渗透率单元之间的距离为1,其计算结果如表3所示。First, according to the permeability value of each well on the 26th row of the first layer, the variogram of the permeability between two wells with a distance of h is obtained by using formula (2) as K 1 (h). The distance between the two permeability units is 1, and the calculation results are shown in Table 3.
其中,公式(2)为:Among them, formula (2) is:
表3变差函数计算结果Table 3 Variation function calculation results
为了使得计算过程的表达更加方便引入中间替换变量x1、x2和y以及b0,b1和b2。基于表3的计算结果,利用公式(3)、公式(4)和公式(5)可以求得一系列的x1、x2和y,其计算结果如表4所示。In order to make the expression of the calculation process more convenient, intermediate substitution variables x 1 , x 2 and y and b 0 , b 1 and b 2 are introduced. Based on the calculation results in Table 3, a series of x 1 , x 2 and y can be obtained by using formula (3), formula (4) and formula (5). The calculation results are shown in Table 4.
其中,公式(3)、公式(4)和公式(5)分别为:Among them, formula (3), formula (4) and formula (5) are respectively:
x1=h (3)x 1 = h (3)
x2=-h3 (4)x 2 = -h 3 (4)
y=K1(h) (5)y=K 1 (h) (5)
表4x1、x2及y的计算结果Table 4 Calculation results of x 1 , x 2 and y
然后,将求得的x1、x2和y代入带公式(6)中,使用线性规划的方法进行数据的拟合,可以求得b0=204,b1=44.66,b2=0.16,则最终得到拟合公式为:Then, substituting the obtained x 1 , x 2 and y into the belt formula (6), and using the linear programming method to fit the data, we can obtain b 0 =204, b 1 =44.66, b 2 =0.16, The final fitting formula is:
y=204+44.66x1+0.16x2 (6)y=204+44.66x 1 +0.16x 2 (6)
将b0=204,b1=44.66,b2=0.16带入到公式(8)、公式(9)和公式(10)中可以得到C0=204、C1=287.19以及a=9.65。Substituting b 0 =204, b 1 =44.66, b 2 =0.16 into formula (8), formula (9) and formula (10), one can obtain C 0 =204, C 1 =287.19 and a=9.65.
其中,公式(8)、公式(9)和公式(10)分别为:Among them, formula (8), formula (9) and formula (10) are respectively:
C0=b0=204 (9)C 0 =b 0 =204 (9)
最后可以确定第一层上第26行的渗透率的变差函数方程式为:Finally, it can be determined that the variogram equation of the permeability on the 26th line on the first layer is:
即已知第一层上第26行任意两点的渗透率方差之半,从而可以求出第一层上第26行离散后的渗透率值,即得到第一层上第26行的渗透率分布情况,如表1第26行所示(从下往上数)。运用同样的方法求得第一层上第6行、第11行、第16行和第21行上所有渗透率单元的渗透率值和渗透率分布情况。然后基于第6行、第11行、第16行、第21行和第26行上已经求得的渗透率值,在纵向上求出任意一列的变差函数方程式,这样就可以知道第一层上每一渗透率单元的渗透率值和渗透率分布情况,如表5所示。That is, half of the permeability variance of any two points on the 26th line on the first layer is known, so that the discrete permeability value of the 26th line on the first layer can be obtained, that is, the permeability of the 26th line on the first layer can be obtained. The distribution is shown in row 26 of Table 1 (counting from bottom to top). Use the same method to obtain the permeability values and permeability distributions of all permeability cells on the first layer on the 6th row, 11th row, 16th row and 21st row. Then, based on the permeability values that have been obtained on the 6th, 11th, 16th, 21st and 26th lines, the variogram equation of any column is obtained in the longitudinal direction, so that the first layer can be known. The permeability value and permeability distribution of each permeability unit are shown in Table 5.
表5第一层平面上渗透率分布表Table 5 Permeability distribution table on the first layer plane
第四步,重复第三步可以求得第二层上每一点的渗透率值,即可以得到第二层的渗透率分布情况,依次求出第三层上每一点的渗透率值,即可以获得所有层的渗透率值和渗透率分布情况,第二层和第三层上每一渗透率单元的渗透率值和渗透率分布情况如表6和表7所示。The fourth step, repeating the third step, the permeability value of each point on the second layer can be obtained, that is, the permeability distribution of the second layer can be obtained, and the permeability value of each point on the third layer can be obtained in turn, that is, The permeability values and permeability distributions of all layers are obtained. The permeability values and permeability distributions of each permeability unit on the second and third layers are shown in Tables 6 and 7.
表6第二层平面上渗透率分布表Table 6 Permeability distribution table on the second layer plane
表7第三层平面上渗透率分布表Table 7 Permeability distribution on the third layer plane
第五步,为了减少渗透率单元的制作数量,简化仿真体的制作步骤,同时又在实验误差允许的范围内,划分不同的渗透率区间进行统计分析。对第三步和第四步中所得到的每层渗透率数据进行统计分析,确定其分布到不同渗透率区间的数量,这样就可以确定分布到不同渗透率区间的单元数量,每一层不同渗透率区间统计情况如表8至表10所示。In the fifth step, in order to reduce the number of permeability units and simplify the manufacturing steps of the simulation body, at the same time, within the allowable range of experimental errors, different permeability intervals are divided for statistical analysis. Statistical analysis is performed on the permeability data of each layer obtained in the third and fourth steps to determine the number of them distributed to different permeability intervals, so that the number of units distributed to different permeability intervals can be determined, and each layer is different. The statistics of permeability interval are shown in Table 8 to Table 10.
表8第一层不同渗透率区间统计表Table 8 Statistical table of different permeability intervals of the first layer
表9第二层不同渗透率区间统计表Table 9 Statistical table of different permeability intervals of the second layer
表10第三层不同渗透率区间统计表Table 10 Statistical table of different permeability intervals of the third layer
第六步,根据第五步所得到的分布在不同渗透率区间的渗透率单元数量,采用不同粒径和数目的石英砂按照不同的排列方式进行填充,并运用不同的胶结方式进行胶结,这样可以制得分布在不同渗透率区间的渗透率单元。In the sixth step, according to the number of permeability units distributed in different permeability intervals obtained in the fifth step, use quartz sand with different particle sizes and numbers to fill in different arrangements, and use different cementation methods for cementation, so that Permeability cells distributed in different permeability intervals can be prepared.
由表8的统计结果可知,在第一层中分布在41-45mD渗透率区间的渗透率单元的数量为31,选择一定粒径和数目的石英砂按照一定的排列方式和胶结方式制作渗透率分布在41-45mD之间的大小为12×12×10cm的仿真体,然后通过切割得到31个2×2×10cm的渗透率单元,即完成了分布在41-45mD渗透率区间的渗透率单元的制作,依次完成第一层所有渗透率区间的渗透率单元的制作。根据表9和表10的统计结果完成第二层和第三层的不同渗透率区间的渗透率单元的制作。From the statistical results in Table 8, it can be seen that the number of permeability units distributed in the 41-45mD permeability range in the first layer is 31. Select a certain particle size and number of quartz sand to make permeability according to a certain arrangement and cementation method. The simulation volume with a size of 12×12×10cm distributed between 41-45mD, and then 31 permeability units of 2×2×10cm are obtained by cutting, that is, the permeability units distributed in the 41-45mD permeability range are completed. The production of permeability units in all permeability ranges of the first layer is completed in turn. According to the statistical results in Table 9 and Table 10, the fabrication of permeability units in different permeability intervals of the second layer and the third layer is completed.
根据直角坐标系定义表5、表6和表7左下角的网格坐标为(1,1),右上角的网格坐标为(30,30)。由表5可以看出,在第一层中坐标为(1,1)网格的渗透率为123mD,其对应表8的渗透率区间为121-125mD,从该渗透率区间选取已经制作好的渗透率单元,排列在该网格原来的位置上,即该渗透率单元的坐标为(1,1)。在第一层中坐标为(1,2)网格的渗透率为103mD,其对应表8的渗透率区间为101-105mD,从该渗透率区间选取已经制作好的渗透率单元,排列在该网格原来的位置上,即该渗透率单元的坐标为(1,2),这样依次完成第一层中所有渗透率单元的排列。根据表6和表7,并且与表9和表10相结合,就可以完成第二层和第三层中所有渗透率单元的排列。这样每层900个渗透率单元根据第三步和第四步计算得到的渗透率的分布情况进行排列,依次排列3层,使其所模拟的岩石更加符合实际情况。According to the Cartesian coordinate system, the grid coordinates of the lower left corner of Table 5, Table 6 and Table 7 are defined as (1,1), and the grid coordinates of the upper right corner are (30,30). It can be seen from Table 5 that the permeability of the grid with coordinates (1, 1) in the first layer is 123mD, which corresponds to the permeability range of Table 8 of 121-125mD. The permeability unit is arranged at the original position of the grid, that is, the coordinate of the permeability unit is (1,1). In the first layer, the permeability of the grid with coordinates (1,2) is 103mD, and the permeability range corresponding to Table 8 is 101-105mD. Select the prepared permeability units from this permeability range and arrange them in the In the original position of the grid, that is, the coordinates of the permeability unit are (1, 2), so that the arrangement of all permeability units in the first layer is completed in turn. According to Tables 6 and 7, and in combination with Tables 9 and 10, the arrangement of all permeability cells in the second and third layers can be completed. In this way, 900 permeability units in each layer are arranged according to the distribution of permeability calculated in the third and fourth steps, and 3 layers are arranged in sequence, so that the simulated rocks are more in line with the actual situation.
之后将形成的仿真体,外层由环氧树脂胶结,并在其上布置单一五点法井组和安装第一螺纹接头、流量调节器、第二螺纹接头等装置,最后形成利用棋盘状仿真体模拟岩石非均质性的装置。The outer layer of the simulation body to be formed is glued with epoxy resin, and a single five-point method well group is arranged on it, and the first threaded joint, flow regulator, second threaded joint and other devices are installed on it, and finally a checkerboard shape is formed. A device for simulating rock heterogeneity.
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