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构造复杂区深部煤储层可压性评价方法及应用——以沁水盆地H区块为例

Method and application of fracability of deep coal reservoirs in complex structural areas of Hengling Block, Qinshui Basin

  • 摘要: 我国深部煤层气资源丰富,但其高效开发受限于复杂的地质构造与储层条件。沁水盆地H区块深部煤储层在压裂改造中效果差异显著,现有评价方法难以适用。本研究旨在建立一套适用于构造复杂区的深部煤储层可压性综合评价方法,精准识别压裂“甜点区”,为深部煤层气藏的分类改造与高效开发提供理论依据与技术支撑。以H区块埋深1 352~1 921 m的15号煤层为研究对象,集成地质、测井、实验、压裂与排采工程等多源信息。通过煤岩力学性质分析、地应力场分析及相关实验手段,系统量化了裂缝发育程度、脆性指数、断裂韧性、地应力差异系数及煤体结构指数五大关键地质参数。采用层次分析法确定各参数权重,构建了综合可压性评价指数(FI)数学模型,实现了对研究区可压性的定量化评价与分区。研究结果表明:① 揭示了15号煤层的关键地质力学特征:天然裂缝发育指数为0.26~1.16,空间非均质性强;脆性指数主体分布于0.4以下;Ⅰ型与Ⅱ型断裂韧性分布规律一致;水平主应力差异系数为0.04~0.20;煤体结构以碎裂−碎粒煤为主。② 基于FI值将研究区划分为3类可压区域:Ⅰ类(FI>0.6,优选)、Ⅱ类(0.45<FI<0.6,良好)和Ⅲ类(FI<0.45,一般),并明确了其空间分布格局。③ 微地震监测与排采动态数据验证了分区的可靠性:Ⅰ类区单位压裂液量造缝长度最高(0.043 m/m3),压后158 d见气,稳产气量达4 044 m3/d;Ⅱ类区和Ⅲ类区单位压裂液量造缝长度分别为0.042 m/m3和0.037 m/m3,稳产气量依次为2 036 m3/d和1731 m3/d,清晰展现了可压性指数与开发效果的正相关性。本研究构建的“地质−工程”一体化可压性评价体系,能够有效克服传统方法的局限性,精准刻画构造复杂区深部煤储层的压裂潜力。该成果为深部煤层气开发的井位优化与差异化压裂方案设计提供了可靠的决策工具,对推动同类复杂储层的效益开发具有重要应用价值。

     

    Abstract: China possesses abundant deep coalbed methane (CBM) resources, but their efficient development is hindered by complex geological structures and reservoir conditions. The H Block in the Qinshui Basin exhibits significant variations in fracturing effectiveness within its deep coal reservoirs, for which existing evaluation methods are inadequate. This study aims to establish a comprehensive fracability evaluation methodology for deep coal reservoirs in structurally complex areas, to accurately identify fracturing "sweet spots", and to provide theoretical and technical support for the classified stimulation and efficient development of deep CBM resources. This research focuses on Coal Seam No. 15, with a burial depth of 13521921 m in the H Block. It integrates multi-source data including geology, logging, experimental tests, and fracturing engineering. Key geological parameters—fracture development degree, brittleness index, fracture toughness, in-situ stress difference coefficient, and coal structure index—were systematically quantified using coal mechanics tests, in-situ stress field analysis, and advanced techniques like CT scanning and XRMI imaging. The Analytic Hierarchy Process (AHP) was employed to determine parameter weights, leading to the construction of a mathematical model for a Comprehensive Fracability Index (FI), enabling quantitative evaluation and zoning of fracability within the study area. Results showed that ① The key geomechanical characteristics of Coal Seam No. 15 were revealed: the natural fracture development index ranges from 0.26 to 1.16, showing strong spatial heterogeneity; the brittleness index is primarily below 0.4; distributions of Type I and Type II fracture toughness are consistent; the horizontal principal stress difference coefficient is between 0.04 and 0.20; and the coal structure is dominated by fragmented-granular coal. ② Based on the FI values (0.35−0.76), the study area was classified into three fracability types: Type I (FI > 0.6, Preferred), Type II (0.45 < FI < 0.6, Good), and Type III (FI < 0.45, Fair), with their spatial distribution patterns clearly identified. ③ Microseismic monitoring and production data validated the zoning reliability: Type I areas achieved the highest fracture length per unit fluid volume (0.043 m/m3), with gas encountered 158 days after fracturing and a stable production rate of 4 044 m3/d. Type II and Type III areas showed values of 0.042 m/m3 and 0.037 m/m3, and stable production rates of 2 036 m3/d and 1731 m3/d, respectively, demonstrating a positive correlation between the fracability index and development outcomes. The established “geology-engineering” integrated fracability evaluation system effectively overcomes the limitations of traditional methods and accurately characterizes the fracturing potential of deep coal reservoirs in structurally complex areas. This achievement provides a reliable decision-making tool for well placement optimization and differentiated fracturing design in deep CBM development, holding significant application value for promoting the profitable development of similar complex reservoirs.

     

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