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中国贵州省高煤阶煤裂隙网络扩展机制与三维重构特征试验研究

Experimental Study of the Fracture Network Expansion Mechanism and Three-Dimensional Reconstruction Characteristic of High-Rank Coal in Guizhou Province, China.

作者信息

Liu Wei, Pan Zihao, Zhang Xiong, Wei Yuanlong, Zhao Lingyun, Zhu Xuanshi, Zhao Youzhou, Guo Qiang

机构信息

State Key Laboratory of Coal Mine Disaster Dynamics and Control, Chongqing University, Chongqing400044, China.

Key Laboratory of Unconventional Natural Gas Evaluation and Development in Complex Tectonic Areas, Ministry of Natural Resources, Guiyang500081, China.

出版信息

ACS Omega. 2023 Feb 7;8(7):6361-6375. doi: 10.1021/acsomega.2c06497. eCollection 2023 Feb 21.

Abstract

To better understand the fracture propagation characteristics and spatial distribution pattern of a high-rank coal reservoir during hydraulic fracturing, a true triaxial physical simulation device was used to conduct a hydraulic fracturing experiment on large-sized raw coal from Zhijin, Guizhou Province, China. Computed tomography technology was used to scan the three-dimensional morphology of the fracture network before and after fracturing, then AVIZO software was used to reconstruct the internal fractures of the coal sample, and fractal theory was used to quantify the fractures. The results show that (1) the sudden increase of the pump pressure curve and acoustic emission signal is an important identification feature of hydraulic fractures, and the in situ stress difference coefficient plays a leading role in the complexity of coal and rock fractures. (2) When a hydraulic fracture encounters a primary fracture in the process of expansion, the opening of the primary fracture, the penetration, bifurcation, and turning of the hydraulic fracture are the main reasons for the formation of complex fractures, and the existence of a large number of primary fractures is the basis for the formation of complex fractures. (3) The fracture shape of coal hydraulic fracturing can be divided into three categories: complex fracture, plane fracture + cross fracture, and inverted T-shaped fracture. The fracture shape is closely related to the original fracture shape. The research results of this paper provide strong theoretical and technical support for coalbed methane mining design such as Zhijin high-rank coal reservoirs.

摘要

为了更好地了解高煤级煤储层水力压裂过程中的裂缝扩展特征和空间分布规律,采用真三轴物理模拟装置对取自中国贵州省织金的大尺寸原煤进行了水力压裂实验。利用计算机断层扫描技术扫描压裂前后裂缝网络的三维形态,然后使用AVIZO软件重建煤样内部裂缝,并运用分形理论对裂缝进行量化。结果表明:(1)泵压曲线和声发射信号的突然增大是水力裂缝的重要识别特征,原地应力差系数对煤岩裂缝的复杂性起主导作用。(2)水力裂缝在扩展过程中遇到原生裂缝时,原生裂缝的开启以及水力裂缝的穿透、分支和转向是形成复杂裂缝的主要原因,大量原生裂缝的存在是形成复杂裂缝的基础。(3)煤水力压裂的裂缝形态可分为复杂裂缝、平面裂缝+交叉裂缝和倒T形裂缝三类。裂缝形态与原始裂缝形态密切相关。本文的研究成果为织金高煤级煤储层等煤层气开采设计提供了有力的理论和技术支持。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/305e/9947985/10725ad75771/ao2c06497_0002.jpg

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