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中国鄂尔多斯盆地东部临兴地区深部煤层气储层纳米级孔隙结构特征及其对CH₄吸附的影响

Nanoscale Pore Structure Characteristics of Deep Coalbed Methane Reservoirs and Its Influence on CH₄ Adsorption in the Linxing Area, Eastern Ordos Basin, China.

作者信息

Gao Xiang-Dong, Wang Yan-Bin, Wu Xiang, Li Yong, Ni Xiao-Ming, Zhao Shi-Hu

机构信息

School of Earth Science, East China University of Technology, Nanchang, Jiangxi 30013, China.

College of Geoscience and Surveying Engineering, China University of Mining and Technology, Beijing 100083, China.

出版信息

J Nanosci Nanotechnol. 2021 Jan 1;21(1):43-56. doi: 10.1166/jnn.2021.18444.

Abstract

The high gas content of deep coal seams is a driving force for the exploration and development of deep coalbed methane (CBM). The nanoscale pores, which are the main spaces for adsorption and storage of CBM, are closely related to the burial depth. Based on integrated approaches of vitrinite reflectance (), maceral composition, scanning electron microscope (SEM), proximate analysis, fluid inclusion test, low-temperature N₂ adsorption-desorption, and CH₄ isothermal adsorption, the nanoscale pore structure of coals recovered at depths from 650 to 2078 m was determined, and its influence on the CH₄ adsorption capacity was discussed. The results show that the coal rank has a good linear relationship with the current burial depth of the coal seams; that is, the influences of the burial depth on the coals can be reflected by the influences of the coal rank on the coals. With the increase in the coal rank, the moisture and volatile content decrease, and the fixed carbon content increases. The variation in the pore volume and specific surface area with the increase in the coal rank can be divided into two stages: the rapid decline stage (when 0.75%< < 1.0%), dominated by the compaction and gelatinization, and the slow decline stage (when 1.0%< < 1.35%), characterized by the low stress sensitivity and the mass production of secondary pores. The percentage of micropores increases throughout the process. When 10 nm is taken as the boundary, the nanoscale pores show different fractal features. When < 1.0%, the fractal dimension (FD) of the micropores is close to 3. When > 1.0%, the FD of the micropores is close to 2. This indicates that with the increase in the degree of coalification, the surface of the micropores is simpler. The above results show that the gas adsorption capacity of coal first slightly decreases (when 0.75% < < 1.0%) and then increases (when 1.0% < < 1.35%), and the coincident results are shown in the Langmuir volume (VL) test results.

摘要

深部煤层的高瓦斯含量是深部煤层气(CBM)勘探开发的驱动力。纳米级孔隙是煤层气吸附和储存的主要空间,与埋藏深度密切相关。基于镜质体反射率、煤岩组成、扫描电子显微镜(SEM)、工业分析、流体包裹体测试、低温N₂吸附-脱附和CH₄等温吸附等综合方法,确定了在650至2078米深度开采的煤的纳米级孔隙结构,并讨论了其对CH₄吸附能力的影响。结果表明,煤阶与煤层当前埋藏深度具有良好的线性关系;即,埋藏深度对煤的影响可通过煤阶对煤的影响来反映。随着煤阶的增加,水分和挥发分含量降低,固定碳含量增加。孔隙体积和比表面积随煤阶增加的变化可分为两个阶段:快速下降阶段(当0.75%<<1.0%时),以压实和胶结作用为主;缓慢下降阶段(当1.0%<<1.35%时),以低应力敏感性和次生孔隙大量产生为特征。整个过程中微孔百分比增加。以10纳米为界时,纳米级孔隙呈现不同的分形特征。当<1.0%时,微孔的分形维数(FD)接近3。当>1.0%时,微孔的FD接近2。这表明随着煤化程度的增加,微孔表面更简单。上述结果表明,煤的瓦斯吸附能力先略有下降(当0.75%<<1.0%时),然后增加(当1.0%<<1.35%时),朗缪尔体积(VL)测试结果也显示出一致的结果。

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