石楼南区块煤孔隙结构及其对甲烷吸附特性的影响研究

    Study on pore structure of coal in south Shilou Block and its influence on methane adsorption characteristics

    • 摘要: 煤储层中孔隙结构的发育程度影响着煤体甲烷的吸附性能。以石楼南区块2#煤和3#煤为研究对象,通过低温N2吸附、低场核磁共振和显微CT等试验手段,定量表征了煤的孔隙结构特征;基于甲烷等温吸附试验,获得了甲烷吸附量的变化趋势,并分析了煤的孔隙结构与甲烷吸附量之间的关系。研究结果表明:SX−2煤样和SX−3煤样的孔隙特征有显著差异,SX−3煤样的微孔数量明显多于SX−2煤样,且其吸附能力优于SX−2煤样,2种煤样均以圆柱状孔隙和墨水瓶形孔隙居多,BET孔比表面积为0.6085~2.1155 m2/g,BJH孔体积为0.0026~0.0051 cm3/g,平均孔径为9.6431~17.0912 nm,SX−2煤样矿物含量明显高于SX−3煤样,煤的孔体积、孔比表面积与煤中矿物含量呈负相关关系;SX−2煤样的T2谱图呈现三峰分布,SX−3煤样的T2谱图呈现双峰分布,SX−3煤样相对SX−2煤样的孔隙空间分布更加集中,连通性更好;SX−2煤样的孔隙结构以大孔为主,而SX−3煤样的孔隙结构以微孔为主;2种煤样的裂缝体积主要由平均孔径大于1000 μm的裂缝提供,SX−2煤样的裂缝体积明显小于SX−3煤样;Langmuir模型能很好地描述研究区煤样的吸附行为,微孔对甲烷的吸附起主导作用,Langmuir体积与煤中矿物含量呈负相关关系,与煤的孔比表面积和孔体积呈正相关关系,SX−3煤样对甲烷的吸附优于SX−2煤样,SX−3煤样的Langmuir体积是SX−2煤样的2.1倍。

       

      Abstract: The development degree of pore structure in coal reservoir controls the adsorption performance of methane in coal. Taking the No.2 and No.3 coals in the south Shilou Block as the research objects, the pore structure characteristics of the coals were quantitatively characterized by experimental methods such as low-temperature N2 adsorption, low-field nuclear magnetic resonance and micro-CT. Based on the methane isotherm adsorption experiment, the changing trend of methane adsorption was obtained, and the relationship between the pore structure of coal and methane adsorption was analyzed. The results show that the pore characteristics of SX-2 coal and SX-3 coal are significantly different. The number of micropores in SX-3 coal is significantly greater than that of SX-2 coal, and its adsorption capacity is better than that of SX-2 coal. There are many cylindrical pores and ink bottle pores in coal, with BET pore specific surface area ranging from 0.608 5 to 2.115 5 m2/g, BJH pore volume ranging from 0.002 6 to 0.005 1 cm3/g, and average pore diameter ranging from 9.643 1 to 17.091 2 nm. The mineral content of coal is significantly higher than that of SX-3 coal. The pore volume and pore specific surface area of coal are negatively correlated with the mineral content in coal. The T2 spectrum of SX-2 coal shows a trimodal distribution, while that of SX-3 coal shows a bimodal distribution. The pore space distribution of SX-3 coal sample is more concentrated, and the pore connectivity is better. The pore structure of SX-2 coal is mainly macropores, and the pore structure of SX-3 coal is mainly micropores. The microcrack volume of the two coals is mainly provided by cracks with a size greater than 1 000 μm. The volume of microcracks in SX-2 coal is significantly smaller than that in SX-3 coal. The Langmuir model can well describe the adsorption behavior of coal in the study area. Micropores play a leading role in the adsorption of methane. The Langmuir volume is negatively associated with the mineral content in coal, and has a positive correlation with the pore specific surface area and pore volume of coal. The adsorption of methane by SX-3 coal is better than that by SX -2 coal, and the Langmuir volume of SX-3 coal is 2.1 times that of SX-2 coal sample.

       

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