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CN108875140A - A kind of heavy crude reservoir asphaltene deposits absorption damage analogy method based on digital cores model - Google Patents

A kind of heavy crude reservoir asphaltene deposits absorption damage analogy method based on digital cores model Download PDF

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CN108875140A
CN108875140A CN201810508920.2A CN201810508920A CN108875140A CN 108875140 A CN108875140 A CN 108875140A CN 201810508920 A CN201810508920 A CN 201810508920A CN 108875140 A CN108875140 A CN 108875140A
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景成
何延龙
聂向荣
袁有金
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Xian Shiyou University
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Abstract

本发明公开了一种基于数字岩心模型的稠油油藏沥青质沉积吸附损害模拟方法,以原始含多种岩石矿物组分的数字岩心模型为参考,结合不同模拟条件下沥青质的沉积状况以及不同岩石矿物对沥青质的室内实验结果,通过基于模型离散点稳定性判别和沥青质沉积、吸附模拟等方法将室内研究结果与数字岩心紧密结合,实现了基于数字岩心技术对稠油油藏沥青质沉积损害的模拟,最后通过对储层伤害前后数字岩心模型微观结构及孔渗变化的分析,得到不同模拟条件下,稠油油藏中沥青质沉积、吸附造成的储层损害程度,该方法的提出进一步拓展了数字岩心技术在油气田开发领域的应用,也为稠油油藏沥青质的沉积吸附的伤害过程模拟与研究提供了新手段。

The invention discloses a method for simulating adsorption damage of asphaltene deposition in heavy oil reservoirs based on a digital core model, using the original digital core model containing various rock mineral components as a reference, combining asphaltene deposition conditions and The results of laboratory experiments on asphaltenes of different rock minerals are closely combined with digital cores through methods such as model-based discrete point stability discrimination, asphaltene deposition, and adsorption simulation. Finally, by analyzing the microstructure and pore-permeability changes of the digital core model before and after the reservoir damage, the degree of reservoir damage caused by asphaltene deposition and adsorption in heavy oil reservoirs under different simulation conditions is obtained. The proposal further expands the application of digital core technology in the field of oil and gas field development, and also provides a new method for the simulation and research of the damage process of asphaltene deposition and adsorption in heavy oil reservoirs.

Description

一种基于数字岩心模型的稠油油藏沥青质沉积吸附损害模拟 方法A simulation of asphaltene deposition adsorption damage in heavy oil reservoirs based on digital core model method

技术领域technical field

本发明属于油气田开发技术领域,涉及稠油油藏储层中沥青质造成的损害分析,特别涉及一种基于数字岩心模型的稠油油藏沥青质沉积吸附损害模拟方法,是一种针对不同模拟条件下,由于稠油油藏储层中沥青质的沉积以及在不同岩石矿物表面的吸附造成的储层伤害过程而开展的基于含多种岩石矿物组分的数字岩心模型的稠油油藏沥青质沉积损害模拟技术。The invention belongs to the technical field of oil and gas field development, and relates to the analysis of damage caused by asphaltenes in heavy oil reservoirs, in particular to a simulation method for asphaltene deposition adsorption damage in heavy oil reservoirs based on a digital core model, which is a method for different simulations Heavy oil reservoir bitumen based on a digital core model containing multiple rock mineral components due to the reservoir damage process caused by the deposition of asphaltenes in the heavy oil reservoir and the adsorption on the surface of different rock minerals Mass deposition damage simulation technology.

背景技术Background technique

稠油油藏在注蒸汽开发过程中,由于储层中温度、压力的变化,极易造成储层岩石及流体性质的变化,从而造成不同类型的储层伤害发生。超临界注汽锅炉可以实现300℃以上的高干度注入蒸汽,压力一般可达6~8MPa,稠油中的胶质、沥青质等重质组分在热采过程中,随着温度、压力场及原油组分性质的变化,原油中的大分子极性化合物不断聚集形成了复杂的沥青质聚集体,而组成沥青质的极性化合物中含有不同类型的大分子含氮、含硫和含氧化合物,其中含氧化合物包括酚类和多种有机酸,含硫化合物包括噻吩等,含氮化合物包括吡啶、咔唑等,不同类型的杂原子化合物在沥青质与岩石矿物的吸附过程中起到重要的作用,尤其是含氮和含氧化合物。含有表面活性基团的沥青质聚集体带有正电荷和较强的极性,同时黏土矿物是典型的硅铝酸盐,其表面具有四面体Si-OH和八面体Al-OH的基团,且晶片的表面为-OH,这些极性基团为沥青质在黏土矿物表面的吸附过程提供了较多的吸附位点,因此在极性、电荷、氢键等一系列作用下使得沥青质在岩石矿物表面发生了吸附。聚沉后的沥青质中含有较多的极性组分,极易在不同黏土矿物中发生吸附而加剧储层伤害。During steam injection development of heavy oil reservoirs, due to changes in temperature and pressure in the reservoir, it is very easy to cause changes in the properties of reservoir rocks and fluids, resulting in different types of reservoir damage. Supercritical steam injection boilers can inject steam with a high dryness above 300°C, and the pressure can generally reach 6-8MPa. During the thermal recovery process, the heavy components such as colloids and asphaltene in heavy oil will change with temperature and pressure. Due to changes in the field and the properties of crude oil components, the macromolecular polar compounds in crude oil continue to aggregate to form complex asphaltene aggregates, and the polar compounds that make up asphaltene contain different types of macromolecular nitrogen-containing, sulfur-containing and Oxygen compounds, where oxygen-containing compounds include phenols and various organic acids, sulfur-containing compounds include thiophene, etc., nitrogen-containing compounds include pyridine, carbazole, etc., and different types of heteroatom compounds play a role in the adsorption process of asphaltenes and rock minerals. play an important role, especially nitrogen-containing and oxygen-containing compounds. Asphaltene aggregates containing surface active groups have positive charges and strong polarity, and clay minerals are typical aluminosilicates, with tetrahedral Si-OH and octahedral Al-OH groups on the surface, And the surface of the wafer is -OH, and these polar groups provide more adsorption sites for the adsorption process of asphaltenes on the surface of clay minerals. Adsorption occurs on the surface of rock minerals. Coagulated asphaltenes contain more polar components, which are easily adsorbed in different clay minerals and aggravate reservoir damage.

随着计算机技术,仪器分析手段的不断发展,促进了数字岩心理论及相关技术的发展,而数字岩心重建技术作为一项发展较为迅速的微观尺度储层模拟分析手段而受到越来越多的关注,其应用也由最初的岩石基本物性研究扩展到了孔隙内流体的渗流、富集、岩石电性关系等多个方面。黏土矿物是储层岩石矿物的重要组成部分,其除遇水具有较强的可塑性外,多数还具有较强的吸附性和离子交换性等特点;是导致储层伤害的主控因素,而沥青质由于在储层温度、压力等变化条件下,极易造成沥青质的沉积,并吸附于不同类型的岩石矿物表面,因此本发明提出一种基于含多种岩石矿物组分数字岩心模型的稠油油藏沥青质沉积损害模拟方法,通过基于数值法构建的数字岩心模型,结合室内实验研究结果,模拟不同条件下稠油油藏沥青质沉积造成的储层伤害。With the continuous development of computer technology and instrumental analysis methods, the development of digital core theory and related technologies has been promoted, and digital core reconstruction technology has attracted more and more attention as a rapidly developing micro-scale reservoir simulation analysis method. , and its application has also been extended from the initial research on the basic physical properties of rocks to many aspects such as seepage, enrichment, and electrical properties of rocks in pores. Clay minerals are an important part of reservoir rock minerals. In addition to their strong plasticity when exposed to water, most of them also have strong adsorption and ion exchange properties; they are the main control factors that cause reservoir damage, while asphalt Asphaltene is easily deposited and adsorbed on the surface of different types of rock minerals under changing conditions such as reservoir temperature and pressure. Therefore, the present invention proposes a dense The simulation method of asphaltene deposition damage in oil reservoirs simulates the reservoir damage caused by asphaltene deposition in heavy oil reservoirs under different conditions through digital core models constructed based on numerical methods and combined with laboratory experimental research results.

发明内容Contents of the invention

为了克服上述现有技术的缺点,本发明的目的在于提供一种基于数字岩心模型的稠油油藏沥青质沉积吸附损害模拟方法,通过数字岩心技术将室内实验结果与现场资料相结合,为研究稠油油藏沥青质沉积、吸附造成的储层伤害过程提供手段。In order to overcome the above-mentioned shortcoming of prior art, the object of the present invention is to provide a kind of heavy oil reservoir asphaltene deposition adsorption damage simulation method based on digital rock core model, combine indoor experiment result with field data through digital rock core technology, for research It provides a means for the reservoir damage process caused by asphaltene deposition and adsorption in heavy oil reservoirs.

为了实现上述目的,本发明采用的技术方案是:In order to achieve the above object, the technical scheme adopted in the present invention is:

一种基于数字岩心模型的稠油油藏沥青质沉积吸附损害模拟方法,其特征在于,包括以下步骤:A method for simulating adsorption damage of asphaltene deposition in heavy oil reservoirs based on a digital core model, characterized in that it includes the following steps:

步骤1,基于真实储层二维信息,基于改进混合算法和聚类算法构建含多种岩石矿物的数字岩心模型;Step 1. Based on the two-dimensional information of the real reservoir, a digital core model containing various rock minerals is constructed based on the improved hybrid algorithm and clustering algorithm;

步骤2,通过室内实验得到不同模拟条件(不同温度,不同压力,不同原油类型,不同水类型,不同润湿环境)下,沥青质的沉积量以及沥青质在不同类型岩石矿物表面的吸附情况;Step 2. Under different simulation conditions (different temperatures, different pressures, different types of crude oil, different types of water, and different wetting environments), the deposition amount of asphaltene and the adsorption of asphaltene on the surface of different types of rock minerals are obtained through laboratory experiments;

步骤3,通过室内实验得到的不同原油在不同模拟条件下沥青质的沉积比例,在原始含多种岩石矿物数字岩心模型的基础上,将沉积沥青质按比例放置于孔隙空间占位,输出沉积沥青质后的数字岩心模型;Step 3. Based on the asphaltene deposition ratio of different crude oils under different simulation conditions obtained through laboratory experiments, on the basis of the original digital core model containing various rock minerals, the deposited asphaltene is placed in the pore space in proportion, and the deposition is output Digital core model after asphaltenes;

步骤4,基于不同模拟条件下沥青质在不同类型岩石矿物表面的吸附特征,将沉积在孔隙空间的沥青质按照室内实验得到的吸附特征放置于不同类型的岩石矿物表面,输出吸附沥青质后的数字岩心模型。Step 4: Based on the adsorption characteristics of asphaltene on the surface of different types of rock minerals under different simulation conditions, the asphaltene deposited in the pore space is placed on the surface of different types of rock minerals according to the adsorption characteristics obtained from laboratory experiments, and the asphaltene after adsorption is output. Digital core model.

所述步骤1中,真实储层二维信息包括铸体薄片、岩石粒度分布、黏土矿物分布、黏土矿物产状特征,具体的模型构建步骤包括:In the step 1, the two-dimensional information of the real reservoir includes cast thin sections, rock particle size distribution, clay mineral distribution, and clay mineral occurrence characteristics. The specific model construction steps include:

第一步,利用过程法构建基础数字岩心模型时,考虑黏土矿物的总含量,在沉积过程中,根据真实储层的粒度分布情况,随机选择沉积颗粒的半径,沉积颗粒的尺寸不但由原始的沉积颗粒粒度分布决定,同时额外考虑黏土矿物与储层砂岩颗粒之间的比例,在满足高能环境和重力势能梯度最大的下落模拟原则的基础上模拟沉积过程,并结合真实岩心孔隙度,选择压实因子控制数字岩心模型的孔隙度;In the first step, when using the process method to construct the basic digital core model, the total content of clay minerals is considered. During the deposition process, according to the particle size distribution of the real reservoir, the radius of the sedimentary particles is randomly selected. The size of the sedimentary particles is not only changed by the original The particle size distribution of sedimentary particles is determined, and the ratio between clay minerals and sandstone particles in the reservoir is additionally considered. The deposition process is simulated on the basis of satisfying the high-energy environment and the principle of falling simulation with the largest gravity potential energy gradient. Combined with the real core porosity, the selected pressure The real factor controls the porosity of the digital core model;

第二步,将单位体像素点的空间占位,即点、线和面占位三种类型,按其对邻域不稳定性的贡献程度赋予权值,其中面为5,边为3,点为2;在选取交换单位体像素点时,计算该体像素点与邻域占位点、线和面上的不稳定性贡献程度S,并基于模拟退火算法中能量值下降的过程,引入交换单位体像素点对其邻域不稳定性的贡献程度参数Sd,对交换点的可交换性进行判断,提高交换单位体像素点的有效性,其中Sd为与模拟过程中系统能量相关的无因次值:In the second step, the spatial occupancy of a unit pixel point, that is, the three types of point, line, and surface occupancy, is assigned a weight according to its contribution to the instability of the neighborhood, where the surface is 5, and the edge is 3. The point is 2; when selecting the exchange unit voxel point, calculate the instability contribution S of the voxel point and the adjacent occupancy point, line and surface, and based on the process of energy value decline in the simulated annealing algorithm, introduce The parameter S d of the contribution degree of the exchange unit voxel point to the instability of its neighborhood is used to judge the exchangeability of the exchange point and improve the effectiveness of the exchange unit voxel point, where S d is related to the system energy in the simulation process dimensionless value of :

Sd=N×β(E0-Ei/△Emax) (1)S d =N×β(E 0 -E i /△E max ) (1)

式中,N为单位体像素点影响的邻域接触点的个数,无量纲;β为单位体像素点对邻域不稳定性系数,无量纲;E0为系统的初始能量,无量纲;Ei为第i次降温后系统的能量,无量纲;ΔEmax为初始模型和基于储层岩石二维信息的参考模型系统的能量差值,无量纲,初始模型是指过程法构建的基础数字岩心模型;In the formula, N is the number of neighborhood contact points influenced by a unit voxel point, dimensionless; β is the instability coefficient of a unit voxel point to the neighborhood, dimensionless; E 0 is the initial energy of the system, dimensionless; E i is the energy of the system after the i-th cooling, dimensionless; ΔE max is the energy difference between the initial model and the reference model system based on the two-dimensional information of reservoir rocks, dimensionless, the initial model refers to the basic number constructed by the process method core model;

第三步,利用改进混合算法构建初始数字岩心模型的步骤为:The third step is to use the improved hybrid algorithm to construct the initial digital core model as follows:

①建立基于储层岩石二维信息的参考模型,将过程法构建的基础数字岩心模型作为改进混合算法的初始模型,设定初始温度,并计算初始系统的相关参数,包含自相关函数、线性路径函数、分形特征函数和能量值;① Establish a reference model based on two-dimensional information of reservoir rocks, use the basic digital core model constructed by the process method as the initial model of the improved hybrid algorithm, set the initial temperature, and calculate the relevant parameters of the initial system, including autocorrelation function and linear path functions, fractal characteristic functions and energy values;

②在保证模拟退火降温过程随机性的基础上,计算交换单位体像素点26个空间占位对邻域不稳定性的贡献程度S;当S>Sd时,认为该点的不稳定程度较高,可作为系统更新的交换点;当S<Sd时,则重复步骤②;② On the basis of ensuring the randomness of the simulated annealing cooling process, calculate the contribution S of the 26 spatial occupancy points of the exchange unit voxel to the instability of the neighborhood; when S>S d , it is considered that the point is less unstable High, it can be used as an exchange point for system update; when S<S d , repeat step ②;

③计算交换单位体像素点后系统的相关参数,包括单点概率函数、自相关函数、线性路径函数、分形函数和能量值,计算与未交换前系统的能量差值ΔE;当ΔE<0时,更新系统;当ΔE>0时,根据Metropolis准则来判断系统是否更新,即在一定的概率条件下接受系统更新;如果判断后不满足系统更新条件,则返回步骤②;③Calculate the relevant parameters of the system after exchanging unit voxels, including single-point probability function, autocorrelation function, linear path function, fractal function and energy value, and calculate the energy difference ΔE with the system before the exchange; when ΔE<0 , to update the system; when ΔE>0, judge whether the system is updated according to the Metropolis criterion, that is, accept the system update under a certain probability condition; if the system update condition is not satisfied after the judgment, return to step ②;

④判断内循环终止条件,即判断在同一温度条件下系统能量差值是否小于设定最小能量差值;同时为避免系统刚降温,系统能量上升而立刻导致内循环结束而产生的降温,通过设定系统更新的失败率ff来避免该现象的出现,其中:④ Judging the termination condition of the internal circulation, that is, judging whether the energy difference of the system is less than the set minimum energy difference under the same temperature condition; Set the failure rate f f of the system update to avoid this phenomenon, where:

式中,Nf为导致系统能量回升的更新失败的次数;N为系统更新的总次数;In the formula, N f is the number of update failures that lead to system energy recovery; N is the total number of system updates;

当ff大于一定值后,则进行降温处理,降温过程采取等比降温方案,并返回步骤②;When f f is greater than a certain value, the cooling process is carried out, and the cooling process adopts an equal-ratio cooling scheme, and returns to step ②;

⑤当模拟过程温度降低到最终设定温度时或与上次降温的系统能量差值ΔE小于设定值时,整个模拟过程终止;⑤ When the simulation process temperature drops to the final set temperature or the system energy difference ΔE from the previous cooling is less than the set value, the entire simulation process is terminated;

作为约束条件,模拟退火算法中使用的统计函数包括:单点概率函数P(r)、自相关函数、线性路径函数和分形函数,利用自相关函数和线性路径函数对初始系统进行退火模拟,当模型具备一定分形特征后,引入分形函数进一步约束重建模型;As constraints, the statistical functions used in the simulated annealing algorithm include: single-point probability function P(r), autocorrelation function, linear path function and fractal function, using the autocorrelation function and linear path function to perform annealing simulation on the initial system, when After the model has certain fractal characteristics, the fractal function is introduced to further constrain the reconstruction model;

第四步,将混合算法重建后初始数字岩心模型中的类球岩石颗粒,与过程法中构建的基础数字岩心模型的原始球形岩石颗粒相比较并取二者补集,将初始数字岩心模型初步划分为岩石骨架相、孔隙相和黏土矿物相三大类;The fourth step is to compare the spherical rock particles in the initial digital core model reconstructed by the hybrid algorithm with the original spherical rock particles in the basic digital core model constructed in the process method and take the complement of the two, and make the initial digital core model Divided into three categories: rock framework phase, pore phase and clay mineral phase;

第五步,通过Hoshen-Kopelman算法对初始数字岩心模型中的黏土矿物基团进行统计和划分,其中被M相占据的概率为c,被T相占据的概率为1-c,对于晶格中的每一个占位i,当其被M相占据时,则给该占位赋予一个基团标记其中α是基团标记的特征符号,t为基团标记的次数,某一离散点的标记由一系列自然数表示:The fifth step is to use the Hoshen-Kopelman algorithm to count and divide the clay mineral groups in the initial digital core model, in which the probability of being occupied by M phase is c, and the probability of being occupied by T phase is 1-c. For each occupancy i of , when it is occupied by the M phase, a group label is assigned to the occupancy Where α is the characteristic symbol of group labeling, t is the number of group labeling, and the labeling of a certain discrete point is represented by a series of natural numbers:

在这一系列自然数中只有一个自然数是基团α的准确标记,该标记为且该值是集合(3)中所有自然数的最小值,其它各基团标记之间的关系则由以下整数集给出:There is only one natural number in this series of natural numbers that is an accurate label for the group α, which is And this value is the minimum value of all natural numbers in the collection (3), and the relation between other each group mark is given by the following integer set:

其中,只有是正整数元素,该值为基团中M相的个数,当进行第t次标记时,若基团中M相个数少于上次标记过程基团α的M相个数,则将该差值表示为相应t次的基团α的T相个数,(4)中的其它元素皆为负整数,反映了与其它基团标记的关系,的关系用式(5)表示:Among them, only is a positive integer element, and this value is the number of M phases in the group. When marking the tth time, if the number of M phases in the group is less than the number of M phases in the group α in the previous marking process, then the The difference is expressed as the number of T phases of the group α corresponding to t times, and the other elements in (4) are all negative integers, reflecting label with other groups Relationship, and The relation of is expressed by formula (5):

检查被判断离散点是否有被扫描过的相邻离散点,若相邻离散点为T相,则将当前被判断离散点赋予新基团的标记;如果有一个相邻离散点已经赋予基团标记,则将当前网格与相邻离散点赋予相同的标记;如果有一个以上的相邻离散点已经赋予基团标记,且基团标记各不相同,则将基团中所有离散点赋予相同的标记,最后统计并划分模型中黏土矿物相基团的个数及尺寸;Check whether the judged discrete point has an adjacent discrete point that has been scanned. If the adjacent discrete point is T-phase, assign the current judged discrete point a new group mark; if there is an adjacent discrete point that has been assigned a group mark, assign the current grid and adjacent discrete points the same mark; if more than one adjacent discrete point has been assigned a group mark, and the group marks are different, assign the same mark to all the discrete points in the group Finally, count and divide the number and size of clay mineral phase groups in the model;

第六步,较大的连通基团为黏土相中基团尺寸大于相邻基质颗粒尺寸的黏土矿物基团,通过K-means算法对初始数字岩心模型中黏土矿物相基团尺寸较大的黏土矿物基团进行划分,具体步骤如下:In the sixth step, the larger connected group is the clay mineral group whose group size in the clay phase is larger than that of the adjacent matrix particle, and the clay mineral group with the larger size of the clay mineral phase group in the initial digital core model is analyzed by the K-means algorithm. Mineral groups are divided, the specific steps are as follows:

①读取数据样本的集合;① Read the collection of data samples;

②设定样本聚类的个数k,随机的选取k个数据样本作为初始的数据样本聚类中心;②Set the number k of sample clusters, and randomly select k data samples as the initial data sample cluster centers;

③计算欧氏距离,计算数据样本中每个数据到各聚类中心的欧式几何距离,然后根据最小误差平方和准则函数将数据按照远近距离划分到相应的不同聚类中心所对应的聚类当中;③ Calculate the Euclidean distance, calculate the Euclidean geometric distance from each data in the data sample to each cluster center, and then divide the data into the clusters corresponding to the corresponding different cluster centers according to the minimum error square sum criterion function ;

④更新聚类中心,将每个聚类中所有数据的均值作为各个聚类新的中心,并以最小误差平方和准则重新计算新的聚类中心的值;④ Update the cluster center, use the mean value of all data in each cluster as the new center of each cluster, and recalculate the value of the new cluster center with the minimum error square sum criterion;

⑤迭代判别,将步骤④中计算得到的数值与前一次计算得到的数值相比较,如果两者差值小于或等于预先设定的临界值,则停止迭代,否则重新进行步骤③进行迭代;⑤ Iterative discrimination, comparing the value calculated in step ④ with the value obtained in the previous calculation, if the difference between the two is less than or equal to the preset critical value, then stop the iteration, otherwise repeat step ③ to iterate;

⑥输出数据样本及聚类结果,包括每个聚类的聚类中心、大小;⑥ Output data samples and clustering results, including the cluster center and size of each cluster;

第七步,当黏土矿物基团边界的离散点为单个岩石颗粒时,则将该黏土矿物基团划分为交代形式,交代形式主要分布于岩石颗粒内,呈单个离散点的形式分布;当黏土矿物基团边界的相邻离散点为单个岩石骨架颗粒及孔隙时,则将该黏土矿物相基团划分为颗粒表面充填形式;In the seventh step, when the discrete point on the boundary of the clay mineral group is a single rock particle, the clay mineral group is divided into metasomatous forms, which are mainly distributed in the rock particles in the form of a single discrete point; when the clay mineral group When the adjacent discrete points on the boundary of the mineral group are single rock skeleton particles and pores, the clay mineral phase group is divided into the filling form of the particle surface;

当黏土矿物基团边界的相邻离散点为多个岩石骨架颗粒及孔隙时,则将该黏土矿物基团划分为粒间充填形式;When the adjacent discrete points on the boundary of a clay mineral group are multiple rock skeleton particles and pores, the clay mineral group is classified as an intergranular filling form;

将交代形式、颗粒表面充填形式和粒间充填形式的黏土矿物基团分别标记为A、B、C;最终得到不同结构黏土矿物基团分布和不同类型的黏土矿物基团分布;The clay mineral groups in the form of metasomatism, particle surface filling and intergranular filling are marked as A, B, and C, respectively; finally, the distribution of clay mineral groups with different structures and different types of clay mineral groups are obtained;

第八步,基于Hoshen-Kopelman算法和K-means算法得到初始数字岩心模型中黏土矿物基团大小及数量分布,以及按结构划分得到的黏土矿物基团类型及数量分布,结合真实储层黏土含量及分布以及主要的黏土矿物结构特点,按黏土矿物相基团大小和结构特点将模型中的黏土矿物赋予相应的黏土性质,得到含多组分岩石矿物分布的数字岩心模型。In the eighth step, based on the Hoshen-Kopelman algorithm and the K-means algorithm, the size and quantity distribution of clay mineral groups in the initial digital core model, and the type and quantity distribution of clay mineral groups obtained according to the structure are obtained, combined with the real reservoir clay content According to the size and structure characteristics of the clay mineral phase group, the clay minerals in the model are given corresponding clay properties, and a digital core model containing multi-component rock mineral distribution is obtained.

所述步骤2中,室内实验包括模拟原始储层及不同生产条件下,当储层温度、压力、层内流体和注入流体性质发生变化时,原油中的沥青质沉积量的变化;沥青质在岩石矿物表面的吸附规律及吸附特征,包括沥青质在不同类型岩石矿物表面的吸附量、吸附常数及最大吸附容量。In said step 2, the indoor experiment includes simulating the original reservoir and under different production conditions, when the reservoir temperature, pressure, intralayer fluid and injection fluid properties change, the change of asphaltene deposition in crude oil; asphaltene in The adsorption law and adsorption characteristics of rock mineral surfaces, including the adsorption amount, adsorption constant and maximum adsorption capacity of asphaltene on different types of rock mineral surfaces.

所述步骤3中得到输出沉积沥青质后的数字岩心模型是指模拟沥青质的沉积过程,步骤如下:Obtaining the digital core model after exporting deposited asphaltenes in said step 3 refers to simulating the deposition process of asphaltenes, and the steps are as follows:

第一步,由原始含多种岩石矿物的数字岩心模型得到数字岩心的孔隙体积;In the first step, the pore volume of the digital core is obtained from the original digital core model containing various rock minerals;

第二步,基于步骤2得到的原油中沥青质在不同模拟条件下(不同温度,不同压力,不同原油类型,不同水类型,不同润湿条件环境)的沉积比例以及步骤1得到的含多种岩石矿物组分数字岩心模型的孔隙体积,计算原始含多种岩石矿物数字岩心模型孔隙中的沥青质沉积量;The second step is based on the deposition ratio of asphaltenes in crude oil obtained in step 2 under different simulation conditions (different temperatures, different pressures, different crude oil types, different water types, and different wetting conditions) and the asphaltene content obtained in step 1. The pore volume of the digital core model of rock mineral composition, calculate the amount of asphaltene deposition in the pores of the original digital core model containing multiple rock minerals;

第三步,以步骤1得到的含多种岩石矿物组分数字岩心模型中最小的单位体像素点为基本沉积模拟单元,将需要沉积的沥青质以基本沉积模拟单元为最大模拟单位,随机放置在孔隙空间占位上,直到完成所有沥青质的沉积过程。The third step is to use the smallest unit voxel point in the digital core model containing multiple rock mineral components obtained in step 1 as the basic deposition simulation unit, and randomly place the asphaltenes to be deposited with the basic deposition simulation unit as the largest simulation unit On pore space occupation until all asphaltenes are deposited.

所述步骤4中得到输出吸附沥青质后的数字岩心模型是指模拟沥青质的吸附过程,步骤如下:Obtaining the digital core model after outputting the adsorbed asphaltenes in the step 4 refers to simulating the adsorption process of the asphaltenes, and the steps are as follows:

第一步,读取沥青质沉积后的含多种岩石矿物的数字岩心模型;The first step is to read the digital core model containing various rock minerals after asphaltene deposition;

第二步,基于步骤2得到的室内实验结果,输入不同类型岩石矿物在不同条件下的吸附平衡常数和最大吸附容量参数;In the second step, based on the laboratory experimental results obtained in step 2, input the adsorption equilibrium constant and maximum adsorption capacity parameters of different types of rock minerals under different conditions;

第三步,按所述的Hoshen-Kopelman基团划分与统计算法确定原始含多种岩石矿物组分数字岩心模型中不同类型岩石矿物的基团数量和大小,通过不同类型岩石矿物对沥青质的吸附特征关系确定不同类型岩石矿物表面沥青质的吸附量;The third step is to determine the group quantity and size of different types of rock minerals in the original digital core model containing multiple rock mineral components according to the Hoshen-Kopelman group division and statistical algorithm. Adsorption characteristic relationship to determine the adsorption amount of asphaltene on the surface of different types of rock minerals;

第四步,结合原始含多种岩石矿物组分数字岩心模型中各类岩石矿物基团大小以及实验中得到的不同模拟条件下不同类型岩石矿物表面沥青质的最大吸附容量,计算模型中岩石矿物基团总的吸附容量;The fourth step is to combine the size of various rock mineral groups in the original digital core model containing multiple rock mineral components and the maximum adsorption capacity of asphaltene on the surface of different types of rock minerals obtained in experiments under different simulation conditions to calculate the rock mineral content in the model. The total adsorption capacity of the group;

第五步,当岩石矿物基团的最大吸附容量大于沥青质的沉积质量时,岩石矿物表面的沥青质吸附比例按照模拟条件下吸附特征常数来确定,各类岩石矿物表面的沥青质总吸附量由沥青质的沉积量来控制;当岩石矿物基团的最大吸附容量小于等于沥青质的沉积质量时,岩石矿物表面的沥青质吸附比例按照模拟条件下各类岩石矿物的最大吸附容量来确定,各类岩石矿物表面的沥青质总的吸附量则由最大吸附容量来控制;In the fifth step, when the maximum adsorption capacity of the rock mineral group is greater than the asphaltene deposition mass, the asphaltene adsorption ratio on the rock mineral surface is determined according to the adsorption characteristic constant under the simulated conditions. The total adsorption amount of asphaltene on the surface of various rock minerals It is controlled by the amount of asphaltene deposition; when the maximum adsorption capacity of the rock mineral group is less than or equal to the deposition mass of asphaltene, the asphaltene adsorption ratio on the rock mineral surface is determined according to the maximum adsorption capacity of various rock minerals under the simulated conditions, The total adsorption amount of asphaltene on the surface of various rock minerals is controlled by the maximum adsorption capacity;

第六步,计算沥青质与黏土的“吸附距离”并排序,其中“吸附距离”与各黏土的吸附比例相关;The sixth step is to calculate and sort the "adsorption distance" between asphaltene and clay, where the "adsorption distance" is related to the adsorption ratio of each clay;

第七步,根据所述的空间占位的稳定性判别方法计算岩石矿物基团边界相邻孔隙占位的稳定性,将沥青质按“吸附距离”放置在优先等级较高的孔隙占位上,如果黏土达到最大吸附容量且已满足总吸附量时模拟过程结束,否则继续按上述过程进行模拟。The seventh step is to calculate the stability of the adjacent pore occupancy of the rock mineral group boundary according to the above-mentioned space occupancy stability discrimination method, and place the asphaltenes on the pore occupancy with higher priority according to the "adsorption distance" , if the clay reaches the maximum adsorption capacity and the total adsorption capacity is satisfied, the simulation process ends, otherwise continue to simulate according to the above process.

通过对比不同模拟条件下稠油油藏沥青质沉积损害前后数字岩心模型中沥青质在岩石矿物表面的吸附体积的变化、数字岩心模型的孔隙度和渗透率的变化,进一步研究稠油油藏沥青质损害前后对储层微观结构的影响。By comparing the changes of the adsorption volume of asphaltene on the surface of rock minerals in the digital core model before and after the asphaltene deposition damage in heavy oil reservoirs under different simulation conditions, and the changes of porosity and permeability in the digital core model, further research on asphalt in heavy oil reservoirs The effect on reservoir microstructure before and after qualitative damage.

与现有技术相比,本发明的一种基于数字岩心模型的稠油油藏沥青质沉积吸附损害模拟方法,通过将有限的矿场资料与室内实验结果相结合,提出了一种基于数字岩心技术的沥青质沉积、吸附造成的储层伤害模拟研究的新手段,该方法首先利用有限的矿场资料构建了包含多种岩石矿物类型与产状的数字岩心模型;其次,在不同模拟条件(温度、压力和流体性质等)下研究了原油中沥青质的沉积变化规律以及沥青质在岩石矿物表面的吸附规律,以此为基础,最后通过基于模型离散点稳定性判别和沥青质的沉积吸附模拟等方法将室内研究结果与数字岩心紧密结合,实现了基于数字岩心技术对稠油油藏沥青质沉积吸附损害过程的模拟,最后通过对储层伤害前后数字岩心模型微观结构及孔渗变化的分析,得到不同模拟条件下,稠油油藏沥青质沉积、吸附过程对储层伤害的程度,该方法的提出进一步拓展了数字岩心技术在油气田开发领域的应用,也为储层中沥青质的沉积吸附损害研究提供了新手段。Compared with the prior art, a simulation method of asphaltene deposition adsorption damage in heavy oil reservoirs based on a digital core model of the present invention proposes a method based on a digital core model by combining limited mine data with laboratory test results It is a new method for simulation research of reservoir damage caused by asphaltene deposition and adsorption. This method first uses limited mine data to construct a digital core model containing a variety of rock mineral types and occurrences; secondly, under different simulation conditions ( temperature, pressure, fluid properties, etc.) to study the asphaltene deposition change law in crude oil and the adsorption law of asphaltene on the surface of rock minerals. Simulation and other methods closely combine the laboratory research results with digital cores, and realize the simulation of the adsorption damage process of asphaltene deposition in heavy oil reservoirs based on digital core technology. According to the analysis, the degree of damage to the reservoir caused by asphaltene deposition and adsorption in heavy oil reservoirs under different simulation conditions is obtained. The study of sediment adsorption damage provides a new method.

附图说明Description of drawings

图1是含多种岩石矿物数字岩心模型重建流程图。Figure 1 is a flow chart of digital core model reconstruction with multiple rock minerals.

图2是沥青质吸附运算流程图。Fig. 2 is a flow chart of asphaltene adsorption operation.

图3是含多种岩石矿物数字岩心模型。Figure 3 is a digital core model containing various rock minerals.

图4是含多种岩石矿物数字岩心模型中黏土基团的分布。Figure 4 shows the distribution of clay groups in the digital core model containing various rock minerals.

图5是不同类型的黏土矿物模型及其分布。Figure 5 is a model of different types of clay minerals and their distribution.

图6是80℃模拟冷凝液模型中沥青质沉积后的二维模型。Fig. 6 is a two-dimensional model after asphaltene deposition in the simulated condensate model at 80 °C.

图7是不同模拟条件下的沥青质沉积模型。Fig. 7 is the asphaltene deposition model under different simulation conditions.

图8是180℃水湿条件下模拟冷凝液模型中沥青质吸附后的二维模型。Figure 8 is a two-dimensional model of asphaltene adsorption in the simulated condensate model under 180°C water-humidity conditions.

图9是不同模拟条件下的沥青质吸附模型。Fig. 9 is the asphaltene adsorption model under different simulation conditions.

具体实施方式Detailed ways

下面结合附图和实施例对本发明作详细说明,但本发明不限于下列的实施例。The present invention will be described in detail below in conjunction with the accompanying drawings and embodiments, but the present invention is not limited to the following embodiments.

本发明具体涉及到一种基于数字岩心模型的稠油油藏沥青质沉积吸附损害模拟方法,该实施例的稠油油藏沥青质沉积过程和吸附过程的模拟是通过以下步骤来实现的:The present invention specifically relates to a method for simulating adsorption damage of asphaltene deposition in heavy oil reservoirs based on a digital core model. The simulation of asphaltene deposition and adsorption processes in heavy oil reservoirs in this embodiment is achieved through the following steps:

实施例中所采用的是基于储层岩石二维信息的含多种岩石矿物的数字岩心重建技术,其中包含的储层岩石二维信息主要包括储层的粒度分布、铸体资料、孔隙度、岩石矿物含量及产状分布等。What is used in the embodiment is the digital core reconstruction technology containing multiple rock minerals based on the two-dimensional information of the reservoir rock. The two-dimensional information of the reservoir rock contained in it mainly includes the particle size distribution of the reservoir, casting data, porosity, Rock mineral content and occurrence distribution, etc.

(1)含多种岩石矿物原始数字岩心模型的构建(1) Construction of the original digital core model containing various rock minerals

含多种岩石矿物的数字岩心模型的构建按图1所示的过程进行构建,其中利用过程法构建基础数字岩心模型是在满足高能环境和重力势能梯度最大的下落模拟原则的基础上模拟沉积过程,并结合真实岩心孔隙度,选择压实因子控制数字岩心的孔隙度。为构建含多组分岩石矿物的数字岩心模型,在沉积过程中,根据真实粒度随机选择球体颗粒的半径时,考虑了其他类型岩石矿物所占体积,因此沉积颗粒的尺寸不但由原始的粒度分布决定,同时额外考虑了其他类型岩石矿物与储层砂岩颗粒之间的比例。在运用混合算法构建初始数字岩心模型时,将单位体像素点的空间占位(点、线和面)按其对邻域不稳定性的贡献程度赋予权值,其中面为5,边为3,点为2;在选取交换单位体像素点时,计算该体像素点与邻域占位点、线和面上的不稳定性贡献程度S,并基于模拟退火算法中能量值下降的过程,引入交换单位体像素点对其邻域不稳定性的贡献程度参数Sd,对交换单位体像素点的可交换性进行判断,提高交换单位体像素点的有效性,其中Sd为与模拟过程中系统能量相关的无因次值:The construction of the digital core model containing a variety of rock minerals is carried out according to the process shown in Figure 1, in which the process method is used to construct the basic digital core model to simulate the deposition process on the basis of satisfying the high-energy environment and the principle of falling simulation with the largest gravity potential energy gradient , combined with the porosity of the real core, the compaction factor is selected to control the porosity of the digital core. In order to construct a digital core model containing multi-component rock minerals, during the deposition process, when the radius of spherical particles is randomly selected according to the real particle size, the volume occupied by other types of rock minerals is considered, so the size of sedimentary particles is not only determined by the original particle size distribution decision, with additional consideration of the ratios between other types of rock minerals and reservoir sandstone grains. When using the hybrid algorithm to construct the initial digital core model, the spatial occupancy (point, line, and surface) of a unit pixel point is assigned a weight according to its contribution to the instability of the neighborhood, where the surface is 5 and the edge is 3. , the point is 2; when selecting the exchange unit voxel point, calculate the instability contribution S of the voxel point and the neighboring occupancy point, line and surface, and based on the process of energy value decline in the simulated annealing algorithm, Introduce the parameter S d of the contribution degree of the voxel point of the exchange unit to the instability of its neighborhood, judge the exchangeability of the voxel point of the exchange unit, and improve the effectiveness of the voxel point of the exchange unit, where S d is the same as the simulation process The dimensionless value of the energy dependence of the system in :

Sd=N×β(E0-Ei/△Emax) (1)S d =N×β(E 0 -E i /△E max ) (1)

式中,N为单位体像素点影响的邻域接触点的个数,无量纲;β为单位体像素点对邻域不稳定性系数,无量纲;E0为系统的初始能量,无量纲;Ei为第i次降温后系统的能量,无量纲;ΔEmax为初始模型和参考模型系统的能量差值,无量纲。In the formula, N is the number of neighborhood contact points influenced by a unit voxel point, dimensionless; β is the instability coefficient of a unit voxel point to the neighborhood, dimensionless; E 0 is the initial energy of the system, dimensionless; E i is the energy of the system after the i-th cooling, dimensionless; ΔE max is the energy difference between the initial model and the reference model system, dimensionless.

作为约束条件,模拟退火算法中常用的统计函数包括:单点概率函数、自相关函数、线性路径函数和分形函数等,利用自相关函数和线性路径函数对初始系统进行退火模拟,当模型具备一定分形特征后,引入分形函数进一步约束重建模型。As constraints, statistical functions commonly used in simulated annealing algorithms include: single-point probability functions, autocorrelation functions, linear path functions, and fractal functions, etc., using autocorrelation functions and linear path functions to anneal the initial system. When the model has a certain After the fractal features are introduced, the fractal function is introduced to further constrain the reconstruction model.

将混合算法重建后初始数字岩心模型中的类球岩石颗粒,与过程法中重建基础模型的原始球形岩石颗粒相比较,并将模型初步划分为岩石骨架相(R)、孔隙相(P)和黏土矿物相(C)三大类,其中C相在空间中以大小不同的不规则离散基团的形式分布,其中模型运算之前需要将三维重建模型划分为两相,孔隙相和岩石骨架相需合并为一相T,利用Hoshen-Kopelman算法得到模型中黏土基团的编号、尺寸和数量,由于统计划分的黏土矿物基团中存在部分尺寸较大的连通黏土基团,而在真实储层中不同种类的黏土矿物在岩石颗粒表面也存在连通、接触的情况;利用K-means聚类算法可以将对岩石颗粒(聚类中心)周围的黏土矿物按所属关系进行聚类。因此,本发明以岩石颗粒的球心和所有较大尺寸的黏土矿物基团作为K-means算法的数据样本对Hoshen-Kopelman算法划分后的黏土矿物基团进行有效划分。对于较大尺寸的连通黏土矿物基团可按照K-means算法划分为多个附着于岩石颗粒表面的有效黏土基团。The spherical rock particles in the initial digital core model reconstructed by the hybrid algorithm were compared with the original spherical rock particles in the basic model reconstructed by the process method, and the model was preliminarily divided into rock skeleton phase (R), pore phase (P) and There are three types of clay mineral phases (C), in which the C phases are distributed in the form of irregular discrete groups of different sizes in space, and the 3D reconstruction model needs to be divided into two phases before the model operation, the pore phase and the rock skeleton phase. Merge into one phase T, and use the Hoshen-Kopelman algorithm to obtain the number, size and quantity of the clay groups in the model. Since there are some connected clay groups with larger sizes in the statistically divided clay mineral groups, while in the real reservoir Different types of clay minerals also have connectivity and contact on the surface of rock particles; K-means clustering algorithm can be used to cluster the clay minerals around the rock particles (cluster center) according to their belonging relationship. Therefore, the present invention effectively divides the clay mineral groups divided by the Hoshen-Kopelman algorithm by taking the center of the rock particle and all larger-sized clay mineral groups as data samples of the K-means algorithm. For large-sized connected clay mineral groups, they can be divided into multiple effective clay groups attached to the surface of rock particles according to the K-means algorithm.

储层中常见的黏土矿物包括蒙脱石、伊利石、伊蒙混层、绿泥石、高岭石;常见的分布形式为粒间孔隙充填、颗粒包壳、交代和包壳衬边等,且不同黏土的分布特点也各不相同。重建模型中黏土矿物的填充形式主要为颗粒表面填充(单个黏土表面填充,多个黏土表面填充和层状黏土表面填充)、颗粒间填充(双颗粒间黏土填充、多颗粒间黏土填充)和颗粒内部填充,故在进行数字岩心模型的黏土矿物构建时,结合实际黏土的分布形式,按照单个黏土基团与岩石骨架颗粒的相邻关系将黏土矿物基团分布的主要形式划分为:粒间充填、颗粒表面充填和交代作用。Common clay minerals in reservoirs include montmorillonite, illite, illite-montmorillonite, chlorite, and kaolinite; the common distribution forms are intergranular pore filling, particle encrusting, metasomatism, and encrusting lining, etc., and The distribution characteristics of different clays are also different. The filling forms of clay minerals in the reconstruction model are mainly particle surface filling (single clay surface filling, multiple clay surface filling and layered clay surface filling), intergranular filling (clay filling between double grains, clay filling between multiple grains) and granular Therefore, when constructing the clay minerals of the digital core model, combined with the actual clay distribution form, the main form of clay mineral group distribution is divided into: intergranular filling according to the adjacent relationship between a single clay group and rock skeleton particles , Particle surface filling and replacement.

基于Hoshen-Kopelman算法得到模型中黏土矿物基团大小及数量分布,以及按结构划分得到的重建模型中黏土基团类型及数量分布,结合真实储层黏土含量及分布以及主要的黏土矿物结构特点,按黏土矿物基团大小和结构特点将模型中的黏土矿物赋予相应的黏土性质,得到含不同类型黏土矿物分布的三维重建多孔介质模型,如图3所示。Based on the Hoshen-Kopelman algorithm, the size and quantity distribution of clay mineral groups in the model are obtained, and the type and quantity distribution of clay mineral groups in the reconstructed model are obtained according to the structure division, combined with the real reservoir clay content and distribution and the main clay mineral structure characteristics, According to the size and structural characteristics of clay mineral groups, the clay minerals in the model are endowed with corresponding clay properties, and a three-dimensional reconstructed porous media model containing different types of clay mineral distribution is obtained, as shown in Figure 3.

(2)数字岩心模型岩石矿物分布特征(2) Distribution characteristics of rock minerals in digital core model

参考模型储层孔隙度为26.38%,渗透率0.614μm2,泥质含量12.36%;其中黏土含量分布为:蒙脱石40.8%,高岭石19.1%,绿泥石27.4%,伊利石6.3%。其中蒙脱石产状主要以颗粒包壳为主,存在部分粒间充填形式;高岭石以粒间孔隙充填,呈分散质点状集合体分布;绿泥石以包壳衬边,粒间充填和交代状分布;伊利石的分布形式包括粒间充填、交代和薄膜式分布。The porosity of the reference model reservoir is 26.38%, the permeability is 0.614μm 2 , and the shale content is 12.36%. The clay content distribution is as follows: montmorillonite 40.8%, kaolinite 19.1%, chlorite 27.4%, illite 6.3% . Among them, the occurrence of montmorillonite is mainly in the form of particle encrustation, and there are some forms of intergranular filling; kaolinite is filled with intergranular pores and distributed in the form of dispersed particle aggregates; chlorite is lined with encrustation and intergranular filling and replacement-like distribution; the distribution of illite includes intergranular filling, replacement and thin-film distribution.

①重建模型中的黏土基团分布① Distribution of clay groups in the reconstruction model

基于Hoshen-Kopelman算法得到的数字岩心模型中不同黏土矿物基团的分布情况如图4所示,其中最大的黏土矿物基团的尺寸为27953个体素,最小的黏土基团大小为1个体素(基团个数为9432)。基团大小小于11个体素的黏土基团仅占所有黏土基团的1.91%;而主要的黏土基团则分布在10000个体素到25000个体素之间,占总黏土体积的97.29%。整体的黏土基团分布呈现“大基团为主,小基团分散”的特点,这与实际储层中黏土矿物的分布形式相近似。The distribution of different clay mineral groups in the digital core model based on the Hoshen-Kopelman algorithm is shown in Fig. 4, where the largest clay mineral group has a size of 27953 voxels, and the smallest clay mineral group has a size of 1 voxel ( The number of groups is 9432). Clay groups with a group size of less than 11 voxels accounted for only 1.91% of all clay groups; while the main clay groups were distributed between 10000 voxels and 25000 voxels, accounting for 97.29% of the total clay volume. The overall distribution of clay groups presents the characteristics of "major groups dominated and small groups dispersed", which is similar to the distribution of clay minerals in actual reservoirs.

②结构划分后模型中黏土矿物的统计②Statistics of clay minerals in the model after structural division

通过黏土基团的结构判别,所有的黏土矿物基团按产状被划分为三种主要类型:表面充填,粒间充填和交代作用。其中以粒间充填形式分布的黏土矿物基团共有4685个基团,含量占黏土总体积的67.13%;表面充填产状的黏土矿物基团共有4530个,含量占黏土总体积的32.30%;而交代作用的黏土矿物则零星的分布于岩石颗粒当中,其含量仅占到黏土总体积的0.28%;模型中较大的黏土矿物基团主要为表面充填和粒间充填的形式。According to the structure discrimination of clay groups, all clay mineral groups are divided into three main types according to their occurrence: surface filling, intergranular filling and metasomatism. Among them, there are 4685 groups of clay mineral groups distributed in the form of intergranular filling, accounting for 67.13% of the total volume of clay; there are 4530 groups of clay mineral groups in the form of surface filling, accounting for 32.30% of the total volume of clay; and The metasomatized clay minerals are distributed sporadically in the rock particles, and their content only accounts for 0.28% of the total clay volume; the larger clay mineral groups in the model are mainly in the form of surface filling and intergranular filling.

通过对数字岩心模型中黏土矿物基团的划分和结构判别,每个黏土矿物基团都逐渐标记了不同的属性(包括基团大小、序号、产状等)。因此,结合真实储层的相关信息(包括黏土含量、黏土类型、黏土的产状等),模型中的黏土矿物按黏土含量和产状特征被划分为不同的黏土类型,蒙脱石是模型中含量最多的黏土矿物,含量占黏土矿物总体积的40.84%,绿泥石占27.43%,高岭石占19.11%,伊利石占6.28%。且对于不同尺寸的黏土矿物基团,各种黏土矿物基团的分布相对均匀。Through the division and structural discrimination of clay mineral groups in the digital core model, each clay mineral group is gradually marked with different attributes (including group size, serial number, occurrence, etc.). Therefore, combined with the relevant information of the real reservoir (including clay content, clay type, clay occurrence, etc.), the clay minerals in the model are divided into different clay types according to the clay content and occurrence characteristics, and montmorillonite is the The clay mineral with the most content accounts for 40.84% of the total volume of clay minerals, chlorite accounts for 27.43%, kaolinite accounts for 19.11%, and illite accounts for 6.28%. And for clay mineral groups of different sizes, the distribution of various clay mineral groups is relatively uniform.

③含多种岩石矿物数字岩心模型中黏土矿物的分布③Distribution of clay minerals in the digital core model containing multiple rock minerals

从各层中黏土矿物的分布情况来看,黏土矿物分布中包括部分基团大小小于5的黏土矿物颗粒,同时大基团黏土矿物的分布以粒间充填(双颗粒间和多粒间),颗粒表面充填(蚀变类黏土、包壳衬边、薄膜式)为主,存在少量交代式分布的黏土矿物。Judging from the distribution of clay minerals in each layer, the distribution of clay minerals includes some clay mineral particles with a group size of less than 5, while the distribution of large group clay minerals is filled between particles (double particles and multiple particles), The surface of the particles is mainly filled (altered clay, cladding lining, film type), and there are a small amount of clay minerals distributed in an alternate manner.

由图5a和图5e可以看出,,蒙脱石在模型中由于含量较高,主要成连片充填并附着于岩石基质表面,同时蒙脱石黏土基团主要以粒间充填和表面充填的形式分布于重建模型当中,基团数量分别为2117个和1935个;粒间充填类蒙脱石和表面充填类蒙脱石的含量占黏土矿物总体积的41.41%和58.39%;其中最大的粒间充填类蒙脱石基团大小为22716个体素,最大的表面充填类蒙脱石基团大小为21273个体素;由图5b和图5f可以看出,绿泥石以环状和部分连片的基团分布于模型当中,粒间充填类绿泥石共有900个基团,占黏土矿物总体积的62,53%;表面充填类绿泥石共有975个基团,占黏土矿物总体积的37.14%,最大的粒间充填类和表面充填类绿泥石基团大小分别为22767个体素和21193个体素;由图5c和图5g可以看出,高岭石一般以粒间充填的形式分布于储层岩石当中,而由模型中黏土矿物的分布可知,粒间充填是模型中高岭石的主要分布形式,占黏土总体积的98.58%,其中最大的粒间充填类黏土基团的大小为27953个体素;由图5d和图5h可以看出,伊利石在模型中的产状包括粒间充填,表面充填和交代形式,其中表面充填类和粒间充填类伊利石分别占41.32%和58.12%。交代作用在四种黏土矿物中均有分布,且主要以零星分布的形式分布于岩石颗粒当中,蒙脱石、绿泥石、高岭石和伊利石中交代状黏土基团的个数分别为504、619、61和244个,所构建的含黏土三维多孔介质模型与真实储层的黏土矿物分布、产状较为吻合。It can be seen from Figure 5a and Figure 5e that due to the high content of montmorillonite in the model, it is mainly filled in continuous sheets and attached to the surface of the rock matrix, while the clay group of montmorillonite is mainly filled between particles and on the surface. The forms are distributed in the reconstruction model, and the number of groups is 2117 and 1935 respectively; the content of intergranular filling montmorillonite and surface filling montmorillonite account for 41.41% and 58.39% of the total volume of clay minerals; the largest intergranular The size of the filled smectite-like group is 22716 voxels, and the size of the largest surface-filled smectite-like group is 21273 voxels; it can be seen from Figure 5b and Figure 5f that the chlorite is ring-shaped and partially connected The groups are distributed in the model. There are 900 groups in the intergranular filling chlorite, accounting for 62.53% of the total volume of clay minerals; there are 975 groups in the surface filling chlorite, accounting for 37.14% of the total volume of clay minerals. %, the largest intergranular filling and surface filling chlorite-like groups are 22,767 voxels and 21,193 voxels respectively; it can be seen from Figure 5c and Figure 5g that kaolinite is generally distributed in the form of intergranular filling in Among the reservoir rocks, the distribution of clay minerals in the model shows that intergranular filling is the main distribution form of kaolinite in the model, accounting for 98.58% of the total clay volume, and the largest intergranular filling clay-like group has a size of 27953 voxel; from Fig. 5d and Fig. 5h, it can be seen that the occurrence of illite in the model includes intergranular filling, surface filling and replacement forms, of which surface filling and intergranular filling illite account for 41.32% and 58.12% respectively . Metasomatism is distributed in all four clay minerals, and is mainly distributed among rock particles in the form of sporadic distribution. The number of metasomatous clay groups in montmorillonite, chlorite, kaolinite and illite is 504, respectively. , 619, 61 and 244, the clay-bearing three-dimensional porous media model constructed is in good agreement with the distribution and occurrence of clay minerals in real reservoirs.

(3)稠油油藏沥青质沉积后损害模型的构建(3) Construction of damage model after asphaltene deposition in heavy oil reservoirs

原油中的沥青质在不同的温度和压力条件下,其发生沉积的可能性和沉积量的大小各不相同;随着沥青质在孔隙中的不断沉积,部分悬浮在原油体系中的沥青质聚集体在氢键、金属键、酸碱作用等作用下吸附到岩石矿物的表面;在不同的水湿及温度条件下,沥青质在不同类型岩石矿物表面的吸附过程较好的满足Langmuir等温吸附方程和Freundlich等温吸附方程,可以得到不同类型岩石矿物的吸附性能参数(吸附平衡常数和最大吸附容量),如表1所示。Asphaltene in crude oil has different deposition possibilities and amounts under different temperature and pressure conditions; with the continuous deposition of asphaltene in pores, some asphaltene suspended in the crude oil system accumulates Asphaltenes are adsorbed to the surface of rock minerals under the action of hydrogen bonds, metal bonds, acid-base effects, etc.; under different water humidity and temperature conditions, the adsorption process of asphaltenes on the surface of different types of rock minerals satisfies the Langmuir isotherm adsorption equation better According to the Freundlich isothermal adsorption equation, the adsorption performance parameters (adsorption equilibrium constant and maximum adsorption capacity) of different types of rock minerals can be obtained, as shown in Table 1.

表1高温高pH模拟冷凝液条件下黏土矿物变化Table 1 Changes of clay minerals under high temperature and high pH simulated condensate conditions

沥青质的沉积量与储层的温度、压力及原油组成的变化等条件密切相关,由室内实验中不同模拟环境中沥青质的沉积变化规律可知,实施例的原油样品中沥青质的沉积量随着压力的升高呈先增大后减小的趋势,同时80℃和180℃条件下,其最大沉积量分别为3.27%和2.61%,按沥青质沉积模拟过程构建了原始储层模型中的沥青质沉积模型,其中图6a为原始含多种岩石矿物数字岩心模型的二维切片,图6b为沥青质发生沉积后的数字岩心模型的二维切片,沥青质沉积后从原油中析出形成较小的沥青质聚集体悬浮于储层孔隙中,同时在模拟沥青质沉积前后,储层模型的原始结构并没有发生变化;而由不同模拟条件下的沥青质沉积模型可以看出(图7a为80℃条件下沥青质沉积后的数字岩心模型,图7b为180℃条件下沥青质沉积后的数字岩心模型),低温条件下,沥青质在模型孔隙中的沉积现象更为明显。The amount of asphaltene deposition is closely related to the temperature, pressure, and changes in the composition of crude oil in the reservoir. From the law of asphaltene deposition in different simulated environments in laboratory experiments, it can be known that the amount of asphaltene deposition in the crude oil samples in the examples varies with The increase of the critical pressure showed a trend of first increasing and then decreasing. At the same time, the maximum deposition amount was 3.27% and 2.61% at 80°C and 180°C respectively. The asphaltene in the original reservoir model was constructed according to the asphaltene deposition simulation Sedimentary model, in which Fig. 6a is a two-dimensional slice of the original digital core model containing various rock minerals, and Fig. 6b is a two-dimensional slice of the digital core model after asphaltene deposition. Asphaltene aggregates are suspended in the reservoir pores, and the original structure of the reservoir model has not changed before and after simulating asphaltene deposition; however, it can be seen from the asphaltene deposition models under different simulation conditions (Figure 7a is 80°C Figure 7b is the digital core model after asphaltene deposition under the condition of 180 °C), and the deposition of asphaltene in the pores of the model is more obvious under low temperature conditions.

(4)稠油油藏沥青质吸附后损害模型的构建(4) Construction of damage model after asphaltene adsorption in heavy oil reservoirs

原油中沉积的沥青质以沥青质聚集体的形式悬浮于储层孔隙中,同时由于储层中的岩石矿物具有较强的吸附性能,其表面具有较多的吸附位点,为沥青质聚集体在岩石颗粒表面的吸附过程提供了必要的物质基础。而沥青质在岩石矿物表面的吸附过程不但受到不同类型岩石矿物性质的影响,同时温度及水湿条件等因素对于沥青质在岩石矿物表面的吸附过程有较大的影响。由室内实验得到模拟储层环境中不同类型岩石矿物在对沥青质的吸附规律,并利用Langmuir吸附模型和Freundlich吸附模型对不同吸附过程进行了拟合,得到了包括Langmuir吸附平衡常数KL、Freundlich吸附平衡常数、最大吸附容量Qmax、非线性因子n和平衡吸附量Qe等一系列参数如表1所示。由不同类型模型中黏土矿物的含量及不同黏土矿物的最大吸附容量可以得到不同条件下,沥青质在模型中的岩石矿物表面吸附的最大吸附量如表2所示。Asphaltene deposited in crude oil is suspended in the pores of the reservoir in the form of asphaltene aggregates. At the same time, because the rock minerals in the reservoir have strong adsorption properties, there are more adsorption sites on the surface, forming asphaltene aggregates. Adsorption processes on the surface of rock particles provide the necessary material basis. The adsorption process of asphaltene on the surface of rock minerals is not only affected by the properties of different types of rock minerals, but also factors such as temperature and water-humidity conditions have a greater impact on the adsorption process of asphaltene on the surface of rock minerals. The asphaltene adsorption law of different types of rock minerals in the simulated reservoir environment was obtained from laboratory experiments, and the Langmuir adsorption model and the Freundlich adsorption model were used to fit the different adsorption processes, including the Langmuir adsorption equilibrium constant K L , Freundlich A series of parameters such as adsorption equilibrium constant, maximum adsorption capacity Q max , nonlinear factor n and equilibrium adsorption capacity Q e are shown in Table 1. From the content of clay minerals in different types of models and the maximum adsorption capacity of different clay minerals, the maximum adsorption capacity of asphaltene on the surface of rock minerals in the model can be obtained under different conditions, as shown in Table 2.

表2不同模拟条件下沥青质在不同岩石矿物表面的最大吸附量Table 2 The maximum adsorption amount of asphaltenes on the surface of different rock minerals under different simulation conditions

模拟过程中黏土矿物的吸附参数按表1和表2设定,其中“其它”类型黏土矿物和石英砂的吸附参数选取60目石英砂的吸附参数。为模拟不同条件下沥青质沉积吸附造成的储层伤害过程,按图2所示的流程构建了沥青质沉积吸附过程造成的储层伤害模型,如图8、图9所示。During the simulation process, the adsorption parameters of clay minerals were set according to Table 1 and Table 2, and the adsorption parameters of "other" types of clay minerals and quartz sand were selected from the adsorption parameters of 60-mesh quartz sand. In order to simulate the reservoir damage process caused by asphaltene deposition and adsorption under different conditions, the reservoir damage model caused by asphaltene deposition and adsorption process was constructed according to the process shown in Fig. 2, as shown in Fig. 8 and Fig. 9.

图8a为原始含多种岩石矿物数字岩心模型的二维切片,图8b为沥青质吸附后的数字岩心模型的二维切片,悬浮在孔隙空间中的沥青质聚集体在不同类型岩石矿物的吸附作用下,按照不同的吸附能力吸附在岩石矿物表面,由于蒙脱石和绿泥石具有较强的吸附能力和较大的吸附容量,因此模拟过程结束后沥青质在这两类岩石矿物表面的吸附量较高,而在伊利石和石英砂表面的吸附量较小;同时满足Langmuir吸附模型的基本假设,沥青质聚集体基本以单层吸附的形式附着于各类岩石矿物的表面。由图9(图9a为80℃干燥条件下沥青质沉积吸附后的数字岩心模型,图9b为80℃水湿条件下沥青质沉积吸附后的数字岩心模型,图9c为180℃干燥条件下沥青质沉积吸附后的数字岩心模型,图9d为180℃水湿条件下沥青质沉积吸附后的数字岩心模型)可知,不同储层模拟条件下,沥青质的沉积吸附状况不同,其中干燥条件下沥青质沉积吸附造成的储层伤害更明显,大量的沥青质聚集体吸附于岩石矿物的表面;而水湿条件下,由于水膜一定程度上抑制了沥青质在岩石矿物表面的吸附,因此水湿条件下,沥青质的沉积吸附造成的储层伤害不明显。Figure 8a is a two-dimensional slice of the original digital core model containing various rock minerals, and Figure 8b is a two-dimensional slice of the digital core model after asphaltene adsorption, asphaltene aggregates suspended in the pore space are adsorbed on different types of rock minerals Under the influence of different adsorption capacities, it is adsorbed on the surface of rock minerals according to different adsorption capacities. Since montmorillonite and chlorite have strong adsorption capacity and large adsorption capacity, the adsorption of asphaltene on the surface of these two types of rock minerals after the simulation process is completed The adsorption amount on the surface of illite and quartz sand is relatively small; at the same time, the basic assumption of the Langmuir adsorption model is satisfied, and the asphaltene aggregates are basically attached to the surface of various rock minerals in the form of monolayer adsorption. Figure 9 (Figure 9a is the digital core model after asphaltene deposition and adsorption under dry conditions of 80°C, Figure 9b is the digital core model after asphaltene deposition and adsorption under 80°C wet conditions, and Figure 9c is the digital core model of asphaltene deposition under 180°C dry conditions Figure 9d is the digital core model after asphaltene deposition and adsorption under 180°C wet conditions) It can be seen that the asphaltene deposition and adsorption status is different under different reservoir simulation conditions, and the asphaltene deposition and adsorption status is different under dry conditions. Reservoir damage caused by sedimentation adsorption is more obvious, and a large number of asphaltene aggregates are adsorbed on the surface of rock minerals. Under the above conditions, the reservoir damage caused by the deposition and adsorption of asphaltene is not obvious.

(5)沥青质沉积吸附造成的储层伤害特征研究(5) Study on the characteristics of reservoir damage caused by asphaltene deposition and adsorption

由于岩石矿物类型、储层温度、水湿条件等因素对沥青质的沉积吸附过程有着不同的影响,因此为进一步研究不同模拟条件下沥青质沉积吸附过程对储层孔隙度、渗透率等的影响,本节研究了由于储层岩石矿物性质变化造成的黏土矿物含量及体积变化、以及模型的孔隙度及渗透率的变化。Since rock mineral types, reservoir temperature, water-humidity conditions and other factors have different effects on asphaltene deposition and adsorption process, in order to further study the influence of asphaltene deposition and adsorption process on reservoir porosity and permeability under different simulation conditions , this section studies the clay mineral content and volume changes caused by changes in the mineral properties of reservoir rocks, as well as the changes in porosity and permeability of the model.

①沥青质含量与体积的变化① Changes in content and volume of asphaltene

如图7和图9所示为不同模拟条件下沥青质沉积、吸附造成的储层伤害模型,在沥青质沉积过程中,沥青质以分散的聚集体的形式悬浮于储层孔隙当中,而在沥青质的吸附过程中,悬浮的沥青质聚集体在岩石矿物的吸附作用下按照最大吸附容量和吸附能力的不同附着于岩石矿物的表面。如表3所示为不同沉积条件下模型中沥青质含量及体积的变化情况。Figure 7 and Figure 9 show the reservoir damage model caused by asphaltene deposition and adsorption under different simulation conditions. During asphaltene deposition, asphaltene is suspended in the reservoir pores in the form of dispersed aggregates, while in During the adsorption process of asphaltenes, suspended asphaltene aggregates adhere to the surface of rock minerals under the adsorption of rock minerals according to the difference of maximum adsorption capacity and adsorption capacity. Table 3 shows the changes of asphaltene content and volume in the model under different deposition conditions.

表3不同条件下沥青质的沉积量及体积变化Table 3 The deposition amount and volume change of asphaltene under different conditions

由图7和表3可以看出,沥青质沉积过程中,高温条件下的原始模型和低温条件下的原始模型的孔隙度分别由原始的26.38%下降为25.52%和25.69%。沥青质聚集体的析出,虽然以固体颗粒的形式悬浮于原油体系当中,将其视为固相,孔隙度虽有一定程度的下降,但是沥青质聚集体的沉积并不对储层的有效孔隙度和渗透率产生明显的影响。悬浮的沥青质聚集体在氢键、偶极—偶极作用、离子交换等作用下吸附于不同类型岩石矿物的表面,从而储层物性产生明显的影响,由表3所示为不同条件下沥青质沉积吸附后沥青质的沉积量、吸附量及体积变化,其中蒙脱石、伊利石、绿泥石、高岭石、石英砂、其它类型岩石矿物和沥青质的密度分别为2.35kg/m3,2.75kg/m3,2.75kg/m3,2.62kg/m3,2.65kg/m3,2.65kg/m3和1.2kg/m3It can be seen from Fig. 7 and Table 3 that during the process of asphaltene deposition, the porosity of the original model under high temperature conditions and the original model under low temperature conditions decreased from the original 26.38% to 25.52% and 25.69%, respectively. Although the precipitation of asphaltene aggregates is suspended in the crude oil system in the form of solid particles, it is regarded as a solid phase, and although the porosity decreases to a certain extent, the deposition of asphaltene aggregates does not affect the effective porosity of the reservoir. have a significant impact on permeability. Suspended asphaltene aggregates are adsorbed on the surface of different types of rock minerals under the action of hydrogen bond, dipole-dipole interaction, ion exchange, etc., so that the physical properties of the reservoir are significantly affected, as shown in Table 3. The deposition amount, adsorption amount and volume change of asphaltene after mass deposition and adsorption, among which the densities of montmorillonite, illite, chlorite, kaolinite, quartz sand, other types of rock minerals and asphaltene are respectively 2.35kg/m 3 , 2.75kg/m 3 , 2.75kg/m 3 , 2.62kg/m 3 , 2.65kg/m 3 , 2.65kg/m 3 and 1.2kg/m 3 .

表4不同条件下沥青质沉积吸附后沥青质的沉积量、吸附量及体积变化Table 4 The deposition amount, adsorption amount and volume change of asphaltene after asphaltene deposition and adsorption under different conditions

由表4可知,沥青质的沉积体积随初始模型的孔隙体积变化而变化,其中原始模型80℃和180℃条件下的沉积体积分别为69010个体素和55081个体素。由于模拟过程中最大吸附容量和吸附平衡常数是最主要的两个限定条件,模拟结束后,干燥条件下,除80℃原始模型的沉积量大于模型岩石矿物对沥青质的最大吸附量外,其它不同模型在干燥条件下,岩石矿物的最大吸附量都明显高于沥青质的沉积量,说明干燥条件下,沥青质发生沉积后,储层岩石矿物表面有较多的吸附位点提供给未被吸附的沥青质聚集体。而水湿条件下,由于水膜的存在使得沥青质在岩石表面的吸附过程更好的满足Langmuir等温吸附模型,说明水膜的存在使得沥青质在岩石矿物表面的吸附过程更接近于单层吸附过程,水膜的存在有效的抑制了沥青质在岩石矿物表面的吸附过程,另一方面,水湿条件下,各类岩石矿物的最大吸附容量明显降低,储层岩石矿物表面提供的有效吸附位点减少。It can be seen from Table 4 that the deposition volume of asphaltenes varies with the pore volume of the initial model, and the deposition volumes of the original model at 80°C and 180°C are 69010 voxels and 55081 voxels, respectively. Since the maximum adsorption capacity and adsorption equilibrium constant are the two most important limiting conditions in the simulation process, after the simulation, under dry conditions, except that the deposition amount of the original model at 80 °C is greater than the maximum adsorption amount of asphaltene by the model rock minerals, other Under dry conditions, the maximum adsorption capacity of rock minerals in different models is significantly higher than that of asphaltene deposition, indicating that under dry conditions, after asphaltene deposition occurs, there are more adsorption sites on the surface of reservoir rock minerals for the undisturbed. Adsorbed asphaltene aggregates. Under water-wet conditions, the adsorption process of asphaltene on the rock surface better satisfies the Langmuir isothermal adsorption model due to the existence of the water film, indicating that the existence of the water film makes the adsorption process of asphaltene on the rock mineral surface closer to monolayer adsorption. The existence of water film effectively inhibits the adsorption process of asphaltene on the surface of rock minerals. On the other hand, under water-wet conditions, the maximum adsorption capacity of various rock minerals is significantly reduced, and the effective adsorption sites provided by the surface of rock minerals in the reservoir point reduction.

②孔隙度和渗透率变化② Changes in porosity and permeability

沥青质沉积过程中,被视为堵塞物的沥青质聚集体虽然从原油体系中不断析出造成了孔隙度的降低,但是该过程中沥青质基本以悬浮的形式存在于储层孔隙当中,因此被视为固相时,沥青质聚集体并没有在孔隙中形成有效的堵塞而影响储层渗透率;而岩石矿物对于沥青质的吸附过程,一方面使得储层的有效孔隙度下降,另一方面附着于岩石矿物表面的沥青质改变的储层岩石的孔喉结构,进一步降低了储层的渗透率。During the process of asphaltene deposition, although asphaltene aggregates, which are regarded as plugs, are continuously precipitated from the crude oil system, resulting in a decrease in porosity, the asphaltene basically exists in the reservoir pores in the form of suspension during this process, so it is called When treated as a solid phase, the asphaltene aggregates did not form an effective plug in the pores to affect the reservoir permeability; while the adsorption process of rock minerals for asphaltene, on the one hand, decreased the effective porosity of the reservoir, on the other hand Asphaltenes attached to rock mineral surfaces alter the pore-throat structure of reservoir rocks, further reducing reservoir permeability.

表5不同类型储层伤害过程中模型孔隙参数变化Table 5 Changes of model pore parameters during different types of reservoir damage

由表5可以看出,沥青质的沉积吸附给储层造成了明显的二次伤害,其中80℃干燥模拟冷凝液条件下,储层渗透率先由589.76×103μm2下降为552.12×103μm2,孔隙度由26.38%下降为23.42%,储层伤害后渗透率和孔隙度分别下降了6.38%和11.22%。水湿环境对于沥青质沉积吸附有明显的抑制作用,其中180℃模拟冷凝液模型水湿条件下沥青质沉积吸附后,渗透率由589.76×103μm2下降为582.90×103μm2,降幅仅为1.16%。因此温度条件及水湿环境对于稠油注汽高压井的储层伤害过程起着重要的控制作用。It can be seen from Table 5 that the deposition and adsorption of asphaltene has caused obvious secondary damage to the reservoir. Under the condition of dry simulated condensate at 80°C, the reservoir permeability first decreased from 589.76×10 3 μm 2 to 552.12×10 3 μm 2 , the porosity decreased from 26.38% to 23.42%, and the permeability and porosity decreased by 6.38% and 11.22% respectively after reservoir damage. The water-wet environment has a significant inhibitory effect on asphaltene deposition and adsorption. After asphaltene deposition and adsorption under the water-humidity condition of the simulated condensate model at 180 °C, the permeability decreased from 589.76×10 3 μm 2 to 582.90×10 3 μm 2 . Just 1.16%. Therefore, temperature conditions and water-humidity environment play an important role in controlling the reservoir damage process of heavy oil steam injection high-pressure wells.

Claims (6)

1. a kind of heavy crude reservoir asphaltene deposits absorption damage analogy method based on digital cores model, which is characterized in that packet Include following steps:
Step 1, it is based on true reservoir two-dimensional signal, based on improved mixed algorithm and clustering algorithm building containing a variety of rock forming minerals Digital cores model;
Step 2, it is obtained under different simulated conditions by laboratory experiment, the deposition and asphalitine of asphalitine are in different type rock The absorption situation of stone mineral surfaces;
Step 3, the deposition fraction of the different crude oils asphalitine under different simulated conditions obtained by laboratory experiment, contains original On the basis of a variety of rock forming mineral digital cores models, deposition asphalitine is placed in interstitial space occupy-place in proportion, output is heavy Digital cores model after product asphalitine;
Step 4, the adsorpting characteristic based on asphalitine under different simulated conditions on different type rock forming mineral surface, will be deposited on hole The asphalitine in gap space is placed in different types of rock forming mineral surface, output absorption according to the adsorpting characteristic that laboratory experiment obtains Digital cores model after asphalitine.
2. the heavy crude reservoir asphaltene deposits absorption damage analogy method based on digital cores model according to claim 1, It is characterized in that, true reservoir two-dimensional signal includes casting body flake, rock grain size distribution, clay mineral point in the step 1 Cloth, clay mineral attitude Characteristics, specific model construction step include:
The first step considers the total content of clay mineral, in deposition process when constructing fundamental digital core model using process method In, according to the size distribution situation of true reservoir, the radius of deposited particles is randomly choosed, the size of deposited particles is not only by original Deposited particles size distribution determine that while the additional ratio considered between clay mineral and reservoir sandstone particle is high meeting Deposition process is simulated on the basis of energy environment and the maximum whereabouts simulation principle of gravitional force gradient, and combines true core hole Degree, the porosity of selection compacting factor domination number word core model;
Second step, it is unstable to neighborhood by it by the space occupy-place of unit bodies pixel, i.e. point, line and face occupy-place three types Property percentage contribution assign weight, wherein face is 5, o'clock is 2 while be 3;When choosing cross-over unit body image vegetarian refreshments, the body is calculated Unstability percentage contribution S on pixel and neighborhood mass point, line and face, and based on energy value decline in simulated annealing Process, introduce cross-over unit body image vegetarian refreshments percentage contribution parameter S instable to its neighborhoodd, to the commutative of exchange point Property judged, improve the validity of cross-over unit body image vegetarian refreshments, wherein SdFor nothing relevant to system capacity in simulation process Because of sub-value:
Sd=N × β (E0-Ei/△Emax) (1)
In formula, N is the number for the neighborhood contact point that unit body image vegetarian refreshments influences, dimensionless;β be unit body image vegetarian refreshments to neighborhood not Stability coefficient, dimensionless;E0For the primary power of system, dimensionless;EiFor the energy of system after i-th cooling, dimensionless; ΔEmaxFor initial model and the energy differences of the model reference system based on reservoir rock two-dimensional signal, dimensionless, initial model Refer to the fundamental digital core model of process method building;
Third step, using improved mixed algorithm construct initial number core model the step of be:
1. the reference model based on reservoir rock two-dimensional signal is established, using fundamental digital core model that process method constructs as changing Into the initial model of hybrid algorithm, initial temperature is set, and calculates the relevant parameter of initial system, includes auto-correlation function, line Property path function, fractal characteristic function and energy value;
2. calculating the 26 space occupy-places pair of cross-over unit body image vegetarian refreshments on the basis of guaranteeing simulated annealing temperature-fall period randomness The instable percentage contribution S of neighborhood;Work as S>SdWhen, it is believed that the unstable degree of the point is higher, can be used as the friendship of system update It changes a little;Work as S<SdWhen, then repeatedly step is 2.;
3. calculating the relevant parameter of system after cross-over unit body image vegetarian refreshments, including single-point probability function, auto-correlation function, linear road Diameter function, fractal function and energy value calculate and the energy differences Δ E that does not exchange preceding system;As Δ E<When 0, more new system;When ΔE>When 0, judge whether system updates according to Metropolis criterion, i.e., receives system under certain Probability Condition more Newly;System update condition is unsatisfactory for after if it is determined that, then return step is 2.;
4. loop termination condition in judging judges whether system capacity difference is less than the minimum energy of setting under the conditions of same temperature Measure difference;Simultaneously to avoid system from just cooling down, system capacity rises and immediately leads to the cooling that interior circulation terminates and generates, and passes through Set the failure rate f of system updatefAvoid the appearance of the phenomenon, wherein:
In formula, NfFor the number for the update failure for causing system capacity to be gone up;N is the total degree of system update;
Work as ffAfter certain value, then cooling processing is carried out, temperature-fall period is taken etc. than cooling profiles, and return step is 2.;
5. being less than setting when analog process temperature is reduced to final set temperature or with the system capacity difference DELTA E of last time cooling When value, entire simulation process is terminated;
As constraint condition, statistical function used in simulated annealing includes:Single-point probability function P (r), auto-correlation letter Number, linear path function and fractal function, carry out annealing simulation to initial system using auto-correlation function and linear path function, After model has certain fractal characteristic, the further constraint reestablishing model of fractal function is introduced;
4th step, class ball rock particles after hybrid algorithm is rebuild in initial number core model and construct in process method The original spherical rock particles of fundamental digital core model compares and takes the two supplementary set, and initial number core model is tentatively drawn It is divided into rock matrix phase, hole phase and clay mineral phase three categories;
5th step counts the clay mineral group in initial number core model by Hoshen-Kopelman algorithm And division, wherein the probability occupied by M phase is c, the probability occupied by T-phase is 1-c, for each of lattice occupy-place i, when When it is occupied by M phase, then a group label is assigned to the occupy-placeWherein α is the characteristic symbol of group label, and t is group The label of the number of label, a certain discrete point is indicated by a series of natural numbers:
Only one natural number is the accurate marker of group α in this set of natural numbers, this is labeled asAnd the value is set (3) minimum value of all natural numbers in, the relationship between other each groups labels are then provided by following set of integers:
Wherein, onlyIt is positive integer element, which is the number of M phase in group, is clocked when carrying out t deutero-albumose, if group Middle M phase number is less than the M phase number of last time labeling process group α, then the difference is expressed as to the T-phase of corresponding t times group α Number, other elements in (4) are all negative integer, are reflectedIt is marked with other groupsRelationship,WithRelationship use Formula (5) indicates:
Inspection is judged whether discrete point has the adjacent discrete point being scanned, if adjacent discrete point is T-phase, will currently be judged to Dialysis scatterplot assigns the label of new group;If there is an adjacent discrete point assigned group label, then by current grid with Adjacent discrete point assigns identical label;If there is more than one adjacent discrete point has assigned group label, and group mark Remember different, then assign discrete points all in group to identical label, finally clay mineral phase in statistics and partitioning model The number and size of group;
6th step, biggish connection group are the clay mineral base that group size is greater than neighboring matrix particle size in clay phase Group, by K-means algorithm to the larger-size clay mineral group of clay mineral phase group in initial number core model into Row divides, and specific step is as follows:
1. reading the set of data sample;
2. setting the number k of sample clustering, random selection k number is according to sample as initial data sample cluster centre;
3. calculating Euclidean distance, each data are calculated in data sample to the European geometric distance of each cluster centre, then basis Data are divided into cluster corresponding to corresponding different cluster centres according to far and near distance by minimal error sum-of-squares criterion function In the middle;
4. cluster centre is updated, using the mean value of data all in each cluster center new as each cluster, and accidentally with minimum Poor sum-of-squares criterion recalculates the value of new cluster centre;
5. iteration differentiates, by step 4. in the numerical value that is calculated compare with the preceding numerical value being once calculated, if the two Difference is less than or equal to preset critical value, then stops iteration, otherwise re-start step and be 3. iterated;
6. output data sample and cluster result, cluster centre, size including each cluster;
7th step, when the discrete point on clay mineral group boundary is single rock particles, then by the clay mineral group division To hand over form, explanation form is distributed mainly in rock particles, in the formal distribution of single discrete point;When clay mineral group It is then particle surface by the clay mineral phase group division when adjacent discrete point on boundary is single rock matrix particle and hole Filling form;
When the adjacent discrete point on clay mineral group boundary is multiple rock matrix particles and hole, then by the clay mineral base Group is divided into intergranular filling form;
The clay mineral group of explanation form, particle surface filling form and intergranular filling form is respectively labeled as A, B, C;Most The distribution of different structure clay mineral group and the distribution of different types of clay mineral group are obtained eventually;
8th step obtains clay mineral in initial number core model based on Hoshen-Kopelman algorithm and K-means algorithm Group size and distributed number, and the clay mineral types of radicals and distributed number that are divided by structure, in conjunction with true storage Layer clay content and distribution and main clay mineral design feature, by clay mineral phase group size and design feature by mould Clay mineral in type assigns corresponding clay property, obtains the digital cores model of the distribution of rock forming mineral containing multicomponent.
3. the heavy crude reservoir asphaltene deposits absorption damage analogy method based on digital cores model according to claim 1, It is characterized in that, laboratory experiment includes under simulation initial reservoir and different working conditions, when reservoir temperature, pressure in the step 2 When fluid and injection fluid properties change in power, layer, the variation of the asphaltene deposits amount in crude oil;Asphalitine is in rock mine The Adsorption law and adsorpting characteristic on object surface, adsorbance, absorption constant including asphalitine on different type rock forming mineral surface And maximum adsorption capacity.
4. the heavy crude reservoir asphaltene deposits absorption damage analogy method based on digital cores model according to claim 1, It is characterized in that, obtaining the deposition that the digital cores model after output deposition asphalitine refers to simulation asphalitine in the step 3 Process, steps are as follows:
The first step obtains the pore volume of digital cores by the original digital cores model containing a variety of rock forming minerals;
Second step, deposition fraction and step 1 of the crude oil studies on asphaltene obtained based on step 2 under different simulated conditions are obtained The pore volume containing a variety of rock forming mineral component number core models, calculate it is original contain a variety of rock forming mineral digital cores models Asphaltene deposits amount in hole;
Third step is containing the smallest unit bodies pixel in a variety of rock forming mineral component number core models with what step 1 obtained Basic deposition analogue unit, will need the asphalitine deposited to deposit analogue unit substantially as maximum analog unit, randomly places Deposition process in interstitial space occupy-place, until completing all asphalitines.
5. the heavy crude reservoir asphaltene deposits absorption damage analogy method based on digital cores model according to claim 1, It is characterized in that, obtaining the absorption that the digital cores model after output adsorptive pitch matter refers to simulation asphalitine in the step 4 Process, steps are as follows:
The first step, the digital cores model containing a variety of rock forming minerals after reading asphaltene deposits;
Second step, the laboratory experiment obtained based on step 2 is as a result, the absorption of input different type rock forming mineral at different conditions The equilibrium constant and maximum adsorption capacity parameter;
Third step is determined original containing a variety of rock forming mineral groups by the Hoshen-Kopelman group division and statistic algorithm The radical amount and size of different type rock forming mineral in score word core model, by different type rock forming mineral to asphalitine Adsorpting characteristic relationship determine the adsorbance of different type rock forming mineral surface asphalitine;
4th step, in conjunction with original containing all kinds of rock forming mineral group sizes and reality in a variety of rock forming mineral component number core models The maximum adsorption capacity of different type rock forming mineral surface asphalitine under difference simulated conditions obtained in testing, rock in computation model The total adsorption capacity of stone ore object group;
5th step, when the maximum adsorption capacity of rock forming mineral group is greater than the deposition quality of asphalitine, rock forming mineral surface Asphaltene adsorption ratio determines that the asphalitine on all kinds of rock forming mineral surfaces is always adsorbed according to adsorpting characteristic constant under simulated conditions Amount is controlled by the deposition of asphalitine;When the maximum adsorption capacity of rock forming mineral group is less than or equal to the deposition quality of asphalitine When, the Asphaltene adsorption ratio on rock forming mineral surface is come true according to the maximum adsorption capacity of rock forming minerals all kinds of under simulated conditions Fixed, the adsorbance that the asphalitine on all kinds of rock forming mineral surfaces is total is then controlled by maximum adsorption capacity;
6th step calculates " the absorption distance " of asphalitine and clay and sorts, wherein the absorption ratio of " absorption distance " with each clay Example is related;
7th step calculates the adjacent pores occupy-place of rock forming mineral group boundary according to the Convenient stable criterion of the space occupy-place Stability, asphalitine is placed in the higher hole occupy-place of priority level by " absorption distance ", if clay reaches maximum Adsorption capacity and simulation process terminates when having met total adsorbance, otherwise continues to be simulated by the above process.
6. the heavy crude reservoir asphaltene deposits absorption damage analogy method based on digital cores model according to claim 1, It is characterized in that, damaging pitch in the digital cores model of front and back by comparing heavy crude reservoir asphaltene deposits under different simulated conditions Matter is further ground in the variation of the adsorption volume on rock forming mineral surface, the variation of the porosity and permeability of digital cores model Study carefully influence of the heavy crude reservoir asphalitine damage front and back to Microstructure of Reservoirs.
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