Impacts of vertical variation of coal seam structure on hydraulic fracturing and resultant gas and water production: A case study on the Shizhuangnan Block, Southern Qinshui Basin, China

Guoqiao Yang, Wenhui Hu, Shuheng Tang, Zhuoming Zhou, Zhen-duo Song
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Abstract

Hydraulic fracturing plays a vital role in the development of coalbed methane (CBM). Coal seam structures can, however, affect the fracturing operations, further affecting gas and water production from the coal seam. Within the research area—the Shizhuangnan Block, Southern Qinshui Basin, China—three types of coal body textures are relevant, including original, cataclastic, and granulated structure. This research describes the impacts of different coal seam types on fracturing operations and gas and water production. The results show that different types of coal seams have different impacts on hydraulic fracturing and the resultant production of gas and water. The coal seams are classified according to the vertical variation characteristics of the coal seam structures. The first type of coal seam (Type I) only develops the original and cataclastic coal structure. The effects of fracturing reconstruction for Type I are good. A high degree of coal breakage and fracture formation is observed. Gas production from CBM wells in Type I coalbeds is usually high because the water in the coal reservoir can be discharged smoothly at an early stage. The second type of coal seam (Type II) develops an additional layer of granulated coal compared with Type I. During the fracturing process, breakage of the coal seam is obvious, and the granulated coal can easily produce fine-grained coal that can block the pores and fractures, which causes an increase and fluctuation of oil pressure and can affect the effectiveness of fracturing. The gas production curve from CBM wells in Type II coal seams is mostly bimodal and water production depends on whether the pulverized coal blocks the pores and fractures. The third type of coal seam (Type III) develops two additional layers of granulated coal compared with Type I, with a greater proportion of granulated coal present. A low degree of coal breakage and fracture formation is observed, and fractures are easily blocked by pulverized coal. The effects of fracturing reconstruction for Type III are bad. Forming an effective seepage channel in this type of coal seam and extending the fracture to the far end is difficult. The gas production from CBM wells in Type III coal seams is usually low, and water production is generally low during the whole drainage period.
煤层构造垂向变化对水力压裂及产气产水的影响——以沁水盆地南部石庄南区块为例
水力压裂在煤层气开发中起着至关重要的作用。然而,煤层构造会影响压裂作业,进而影响煤层气的产气和产水。在秦水盆地南部石庄南地块研究区内,具有原生、碎裂、粒状三种煤体结构类型。本文描述了不同煤层类型对压裂作业和产气产水的影响。结果表明,不同类型的煤层对水力压裂及由此产生的气、水的影响不同。根据煤层构造的垂向变化特征对煤层进行了分类。第一类煤层(ⅰ型)只发育原始碎裂煤结构。ⅰ型压裂改造效果较好。观察到煤的高度破碎和裂缝形成。I型煤层煤层气井的产气量通常较高,因为煤储层中的水在开采初期能够顺利排出。第二类煤层(II型)在ⅰ型煤层的基础上多发育一层颗粒煤。在压裂过程中,煤层破碎明显,颗粒煤容易产生细粒煤,细粒煤会堵塞孔隙和裂缝,导致油压升高和波动,影响压裂效果。II型煤层煤层气井产气曲线多为双峰型,产水量取决于煤粉是否堵塞孔隙和裂缝。第三种煤层(III型)比I型多出两层颗粒煤,颗粒煤的比例更大。煤破碎和裂隙形成程度低,裂隙容易被煤粉堵塞。ⅲ型压裂改造效果较差。在这类煤层中形成有效的渗流通道并将裂隙延伸到远端是困难的。III型煤层的煤层气井产气量通常较低,整个抽采期的产水量普遍较低。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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