• 中文核心期刊
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韩城矿区构造煤储层物性差异特征

张晓辉, 要惠芳, 李伟

张晓辉, 要惠芳, 李伟. 韩城矿区构造煤储层物性差异特征[J]. 煤矿安全, 2014, 45(4): 176-179.
引用本文: 张晓辉, 要惠芳, 李伟. 韩城矿区构造煤储层物性差异特征[J]. 煤矿安全, 2014, 45(4): 176-179.
ZHANG Xiaohui, YAO Huifang, LI Wei. The Difference of Physical Properties of Tectonic Coal Reservoirs in Hancheng Block[J]. Safety in Coal Mines, 2014, 45(4): 176-179.
Citation: ZHANG Xiaohui, YAO Huifang, LI Wei. The Difference of Physical Properties of Tectonic Coal Reservoirs in Hancheng Block[J]. Safety in Coal Mines, 2014, 45(4): 176-179.

韩城矿区构造煤储层物性差异特征

The Difference of Physical Properties of Tectonic Coal Reservoirs in Hancheng Block

  • 摘要: 采用手标本观察、扫描电镜、压汞法、低温氮吸附和等温吸附试验等方法,综合分析了韩城矿区块构造煤储层煤体结构、孔隙系统、渗透性、甲烷吸附能力等物性差异特征。研究表明:构造运动引起煤岩宏观变形变质,碎裂煤、碎粒煤、鳞片煤、糜棱煤发育;微观-超微观视域内煤颗粒搬运、堆积,煤岩组分剪切变形、揉流褶皱,微米级范围内脆性、脆韧性、韧性煤层流变特征突出;构造变形程度增大,中孔比例升高,孔径配置由并联转化为串联,开放型孔逐步转化为细颈瓶型孔,渗流孔隙比例下降,吸附孔隙比例大幅升高,渗透性降低。但在富水文地质单元条件下,后生矿物充填易导致弱变形煤渗透率下降,加之裂隙由开启渐趋闭合,张性转换为压性、压剪性,孔隙系统及渗流特性的非均质性明显增强;弱变形碎裂煤比表面积至强变形糜棱煤差异量达7.476 3 m2/g,纳米级孔隙氮吸附量由0.698 2 mL/g增至9.354 3 mL/g,甲烷吸附能力显著提升。
    Abstract: Appling hand specimens, scanning electron microscope, low-temperature nitrogen and isothermal adsorption experiment methods, it studies the difference of physical properties of deformed coal reservoirs in Hancheng Block, including coal body structure, pore system, permeability capacity and absorption ability. The results indicate that tectonic movement can cause coal macro deformation and metamorphism, development of cataclastic coal, granulated coal, flack coal and mylonitic coal. It shows obvious features in the particle transportation and accumulation, shear deformation and corrugation of coal composition in the vision of microscopic to super-microscopic, and brittle rheology, brittle-ductile rheology and ductile rheology at micron level; with the intense of deformation, mesopore enlarges further, pore structure characteristics convert parallel into series, open-end pores changes to thin-neck-bottle-shaped pores gradually, percolation pore decrease, adsorption pore elevates and reservoirs permeability become poor. In the condition of geohydrologic element abundance, mineral substance fill stratification of weak deformation coal and cause permeability decline, while open tensile fractures transforming to close shear fractures, increasing the anisotropy of coal pore system and seepage characteristics; strong altered coal has larger surface area than weak altered coal, the difference can be 7.476 3 m2/g and the nitrogen adsorbance of nano-pore rise from 0.698 2 mL/g to 9.354 3 mL/g, its adsorption ability of CH4 increases obviously.
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  • 发布日期:  2014-04-19

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