油气藏评价与开发

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碎裂煤中煤粉运移对孔渗影响的数值模拟研究

石慧1, 谢天成1, 刘子亮1, 蒋志坤1, 魏迎春1,2   

  1. 1.中国矿业大学(北京)地球科学与测绘工程学院,北京 100083;
    2.中国矿业大学(北京)煤炭精细勘探与智能开发全国重点实验室,北京 100083
  • 收稿日期:2024-09-19
  • 通讯作者: 魏迎春(1977—),女,博士,教授,主要从事煤与煤系矿产资源地质勘探与开发方面的教学和科研工作。地址:北京市海淀区学院路丁11号,邮政编码:100083。E-mail: wyc@cumtb.edu.cn
  • 作者简介:石慧(2001—),女,在读硕士研究生,从事煤层气开发地质研究。地址:北京市海淀区学院路丁11号,邮政编码:100083。E-mail: shih_forward@163.com
  • 基金资助:
    国家自然科学基金项目“不同类型构造煤储层中煤粉运移规律及其储层意义”(41972174); 国家自然科学基金项目“惰质组与镜质组大分子结构演化差异性及其动力学机制”(42042197)

Numerical simulation study on the influence of coal fines migration on porosity and permeability in cataclastic coal

SHI HUI1, XIE TIANCHENG1, LIU ZILIANG1, JIANG ZHIKUN1, WEI YINGCHUN1,2   

  1. 1. College of Geoscience and Surveying Engineering, China University of Mining and Technology (Beijing), Beijing 100083, China;
    2. State Key Laboratory for fine exploration and intelligent development of Coal Resources, China University of Mining and Technology (Beijing), Beijing 100083, China
  • Received:2024-09-19

摘要: 在煤层气排采过程中,储层中煤粉会发生运移,可能造成孔隙和喉道堵塞,导致渗透率下降,从而影响煤层气的产量。为了探究煤粉运移对碎裂煤储层孔渗的影响,建立了煤粉在孔喉通道内的运移—沉降数值模型,基于python(高级程序设计语言)编写了煤粉运移的数值模拟程序,模拟了煤粉在碎裂煤基质孔隙网络中的运移,探讨了煤粉运移过程中的碎裂煤储层孔渗变化规律以及煤粉运移对孔渗的影响。数值模拟结果表明:压差和煤粉粒度是影响储层孔渗的2个关键因素。模拟初始阶段,煤粉运移引起储层渗透率迅速降低,不同粒径煤粉颗粒运移、沉降和排出进一步受到压差的影响,煤粉粒度越大,在低压差、低流速条件下越难以启动运移,而在压差较大流速较高的情况下,则会发生运移。对比小粒径煤粉,大粒径煤粉颗粒更加容易堵塞有效孔隙,导致渗透率迅速下降。压差增加会使煤粉沉积位置向出口端转移,导致煤粉沉降范围变大。在煤粉粒径小于喉道半径的条件下,驱替压力存在一个阈值,当小于这个阈值时,渗透率的下降速度随着驱替压力的增大而增大;当大于这个阈值时,渗透率的下降速度会随着驱替压力的增大而降低。将数值模拟实验数据与关于煤粉运移的物理模拟实验结果相结合表明:模型的数值模拟结果与物理模拟实验中的煤粉运移过程中碎裂煤的渗透率变化和煤粉产出沉降情况一致。

关键词: 煤层气, 碎裂煤, 煤粉运移, 孔渗, 煤粉粒径, 数值模拟

Abstract: In the process of coalbed methane drainage, the coal fines in the reservoir will be migrated significantly. This phenomenon is likely to cause the effective circulation space of pores and throats to be blocked, resulting in a significant reduction in reservoir permeability. It has a very adverse effect on the final production of coalbed methane. In order to explore the influence of coal fines migration on the porosity and permeability of cataclastic coal reservoirs, aiming at the process of coal fines start-up, migration and deposition retention in reservoir channels, the pore size distribution characteristics of cataclastic coal were analyzed by low-field nuclear magnetic resonance and low-temperature liquid nitrogen adsorption, a three-dimensional pore network model was established, and a numerical model of migration and sedimentation of coal fines in pore throat channels was constructed. Combined with the previous mechanical model of coal fines start-up and the probability model of particle deposition and blockage in throat, monte Carlo method is used to simulate the migration and blockage of coal fines in reservoir pores. Based on the python language, a numerical simulation program for the migration of coal fines was written to simulate the migration of coal fines in the pore network of broken coal matrix. The variation law of porosity and permeability of cataclastic coal reservoir in the process of coal fines migration and the influence of coal fines migration on porosity and permeability are discussed. Through in-depth analysis of precise numerical models and advanced program simulation techniques, the internal mechanism of the far-reaching influence of pressure difference and coal fines particle size on coal fines output and model permeability is revealed. These two key factors not only play a significant role alone, but also their interaction is more complicated. Specifically, the particle size of coal fines directly affects its migration, sedimentation and output characteristics under different hydrodynamic conditions. Under the condition of low pressure difference and low flow velocity, large particle size coal fines is like a silent giant, which is difficult to be activated and start migration ; however, under the strong drive of high pressure difference and high flow velocity, these coal fines become active, but their migration is more likely to lead to the blockage of effective pores, resulting in a sharp decline in permeability. In addition, the increase of pressure difference is like a double-edged sword. On the one hand, it promotes the increase of coal fines output, on the other hand, it also accelerates the deterioration of permeability. It is worth noting that the settlement position of coal fines migrates to the outlet end with the increase of displacement pressure difference, and the increase of displacement pressure is accompanied by a significant increase in the proportion of small throats. Under the condition that the particle size of coal fines is constant and generally smaller than the throat radius, there is a subtle equilibrium point of the displacement pressure, that is, the threshold value. On both sides of this threshold value, the relationship between the permeability decline rate and the displacement pressure shows a completely different trend. In the drainage and depressurization stage of actual industrial production, the output characteristics and particle size distribution of coal fines have become important indicators for evaluating production efficiency and reservoir permeability changes. With the gradual increase of drainage intensity, the output intensity of coal fines experienced a process from initial slow growth to subsequent rapid decline. At the same time, the particle size distribution of coal fines also reached a maximum, covering a wide range from small particle size to large particle size. This phenomenon is particularly significant in the initial drainage stage. When the drainage intensity is still at a low level, only some small particle size coal fines migrates and outputs under the drive of fluid dynamics. In order to further explore this phenomenon, we used numerical simulation technology to simulate the actual situation of low drainage intensity by setting low pressure difference conditions. In the numerical simulation program, it can be concluded that in the case of low flow rate, small particle size coal fines can indeed migrate and produce, and at the same time, the decline rate of reservoir permeability is relatively gentle. The simulation results are highly consistent with the output of coal fines under the condition of low drainage intensity in actual production, which verifies the accuracy and reliability of numerical simulation technology in predicting the migration behavior of coal fines. Furthermore, the numerical simulation data are compared with the results of physical simulation experiments on the migration of coal fines. The simulation results of the model show that as the simulated drainage continues, the large-size coal fines will preferentially settle in the pores. The settlement of these large particles is like a channel barrier, which effectively blocks the pores and leads to a significant decrease in permeability. At the same time, the settlement probability of small particle size coal fines also increases rapidly. This makes the migration and production of coal fines more and more difficult, which shows that the number of coal fines produced decreases rapidly with time. In addition, the physical simulation experiment of coal fines migration in cataclastic coal reservoir also provides us with valuable reference information. The experimental results show that the decrease of permeability of coal samples is mainly concentrated in the early stage of water flooding, and the higher the fracture density is, the higher the average permeability is. Pores and fissures with a pore diameter greater than 1 000 nm become the main channels for coal fines migration and blockage. The coal fines further leads to a decrease in permeability by migrating and plugging connected pores with a pore size greater than 10 000 nm. This finding is consistent with the numerical simulation results, which further confirms the consistency between the permeability change and the coal fines production in the coal fines migration of the cataclastic coal reservoir. In the simulation program, the high drainage strength is simulated by setting the pressure difference compared with the high pressure difference. When the large particle size coal fines are added, the settlement position of the coal fines begins to increase compared with the low pressure difference, and the output decreases, concentrated at the outlet end. When the small particle size coal fines are added, the output of coal fines increases significantly, and the decrease of permeability of coal fines is reduced compared with that of large particle size coal fines. On the whole, the simulation results of the model are consistent with the output of coal fines after increasing the drainage intensity in actual production. The numerical simulation results show that the larger the particle size of the coal fines, the more concentrated the position of the settlement and blockage of the coal fines to the inlet end, and the smaller the position range of the deposition. When the pressure difference is low, the coal fines is mainly concentrated in the direction of the inlet end. With the increase of pressure difference, the settlement position of coal fines is close to the outlet end, and the range of settlement position becomes larger. In the visual physical simulation of coal fines migration in fractures, the deposition area of coal fines in the fracture throat gradually decreases from the inlet to the two ends of the vertical main migration direction and the main migration direction. In summary, the experimental results of numerical simulation are consistent with the permeability change of broken coal and the settlement of coal fines in the process of coal fines migration in physical simulation experiments.

Key words: coalbed methane, cataclastic coal, coal fines migration, pore permeability, particle size of coal fines, numerical simulation

中图分类号: 

  • TE357