Zonal Seepage in Coal Seams Generated by Hydraulic Fracturing Under Gas Pressure Attenuation: Characteristics and Affecting Factors

IF 4.8 2区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Cun Zhang, Chenxi Liu, Wuyan Xu, Yixin Zhao, Ziyu Song, Lei Zhang
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Abstract

Hydraulic fracturing causes the fracture zone phenomenon in a coal seam. The effectiveness of coalbed methane (CBM) extraction is determined by the seepage characteristics of various fracture zones under gas pressure attenuation by gas extraction in coal seams. Based on this, this paper developed a zonal seepage test device for hydraulic fracturing coal, designed a series and parallel test method for intact coal sample, microfracture coal sample and penetration fracture coal sample. This method can simulate the migration process of CBM in different disturbance areas near the wellbore in the initial stage of hydraulic fracturing (transverse seepage) and the migration process of CBM from the matrix to the wellbore in the later stage (longitudinal seepage). On this basis, the seepage characteristics of the complex zonal phenomenon produced by hydraulic fracturing under the condition of gas pressure attenuation were studied. A series and parallel permeability model combining Klinkenberg effect, expansion effect and effective stress was established. This model can well describe the series and parallel permeability variation law with gas pressure. It indicated that the adsorption expansion effect and effective stress have an impact on the coal matrix during the longitudinal seepage process, which restricts the seepage of both natural and artificial fractures. Artificial fractures are less impacted by the expansion effect and effective stress during the transverse seepage process, which makes them the primary seepage channel. Combined with the extraction data and the permeability model, the gas production trend in the Qinshui Basin is divided into two stages: transverse seepage dominant stage and longitudinal seepage dominant stage.

Abstract Image

瓦斯压力衰减下水力压裂产生的煤层带状渗流:特征和影响因素
水力压裂造成煤层中的断裂带现象。煤层气抽采效果取决于煤层中瓦斯抽采在瓦斯压力衰减下各断裂带的渗流特性。基于此,本文开发了水力压裂煤层分区渗流试验装置,设计了完整煤样、微裂缝煤样和贯穿裂缝煤样的串联和并联试验方法。该方法可以模拟水力压裂初期煤层气在井筒附近不同扰动区域的迁移过程(横向渗流)和后期煤层气从基质向井筒的迁移过程(纵向渗流)。在此基础上,研究了气体压力衰减条件下水力压裂产生的复杂地带现象的渗流特征。结合克林肯贝格效应、膨胀效应和有效应力,建立了串并联渗透率模型。该模型能够很好地描述随气体压力变化的串并联渗透率变化规律。研究表明,在纵向渗流过程中,吸附膨胀效应和有效应力对煤基质有影响,从而限制了天然裂缝和人工裂缝的渗流。人工裂缝在横向渗流过程中受膨胀效应和有效应力的影响较小,因此成为主要渗流通道。结合开采数据和渗透率模型,将沁水盆地的产气趋势划分为两个阶段:横向渗流主导阶段和纵向渗流主导阶段。
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来源期刊
Natural Resources Research
Natural Resources Research Environmental Science-General Environmental Science
CiteScore
11.90
自引率
11.10%
发文量
151
期刊介绍: This journal publishes quantitative studies of natural (mainly but not limited to mineral) resources exploration, evaluation and exploitation, including environmental and risk-related aspects. Typical articles use geoscientific data or analyses to assess, test, or compare resource-related aspects. NRR covers a wide variety of resources including minerals, coal, hydrocarbon, geothermal, water, and vegetation. Case studies are welcome.
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