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Coalbed methane resources and reservoir characteristics of NO. II1 coal seam in the Jiaozuo coalfield, China

机译:煤层气资源及NO的储层特征中国焦作煤田II1煤层

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摘要

Jiaozuo coalfield is located in the northwest of Henan province, China, and Close to the Southern Qinshui coal basin. (lie most successfully commercial CBM resource developed area in China. The No. II1 coal seam is the main economic coal seam in Jiaozuo coalfield and its average thickness exceeds 5.36m. The maximum reflectance of vitrinite (R-0.max) No. II1 coal across the Jiaozuo is between 3.16% and 4.78%. The coalbody structure of the No. II1 coal seam changes greatly in different part and can be generally divided into 1 similar to 3 sub-layers. The micropores ill the No.II1 coal seam is the major pores, secondly are transitional pores, and then less macropores and mesopores. The No. II1 coal seam has stronger adsorption, and the reservoir natural permeability has all evident heterogeneity vary from 0.0001 to 83.71mD. High permeability region is often near fault structure or the boundary of fault block. The CBM genetic type is homologous thermal cracking gas of humic coal with high matunity. Gas content with the burial depth of 163 similar to 1070m varies very greatly from 4.65 to 45.75m(3)/t, with all average value of 18.3m(3)/t, and gradually increases from northeast to southwest. According to the latest evaluation for CBM resource in Jiaozuo coalfield, the existing total in-place CBM resources in the No. In coal seam with the depth of shallower than 2000 m are close to 1.2 x 10(12)m(3), most of them mainly distribute in the depth of 1000 similar to 1500 m. The existing total in-place CBM resources is dominated by the inferred CBM resource reserves (more than 70%), which distribute the undrilled places with few coal geological knowledge and deeper than 1000m. The resource concentration of the No. II1 coal,earn in Jiaozuo coalfield is in the range of (0.513-3.478)x10(8) m(3)/km(2), with an average value of 1.805x10(8) m(3)/km(2). Based on the CBM resource investigation and reservoir evaluation, the most prospective target zones for CBM production in Jiaozuo coalfield include Guhanshan coal mine, Jiulishan coal mine and the west part of Qiangnan coal district.
机译:焦作煤田位于中国河南省西北部,靠近沁水盆地南部。 (是中国最成功的商业煤层气资源开发区。II1煤层是焦作煤田的主要经济煤层,平均厚度超过5.36m。最大镜面反射率(R-0.max)II1煤层焦作地区的煤层在3.16%至4.78%之间,II1煤层的煤体结构在不同部分变化很大,大致可分为1个相似的3个子层。 II1煤层具有较强的吸附能力,储集层的天然渗透率均具有明显的非均质性,从0.0001到83.71mD不等;高渗透率区常在断层附近,是主要的孔隙,其次是过渡孔隙,其次是大孔隙和中孔。煤层气成因类型为高成熟度的腐殖质煤热裂解气,埋藏深度为163〜1070m的瓦斯含量在4.65至45.75m(3)/ t之间变化很大。所有平均值为18.3m(3)/ t,并从东北向西南逐渐增加。根据焦作煤田煤层气资源的最新评价,在深度小于2000 m的煤层中,现有的现地煤层气资源总量接近1.2 x 10(12)m(3)。它们主要分布在1000深度处,类似于1500 m。现有的现场煤层气资源总量以推断的煤层气资源储量(占70%以上)为主导,这些储量分布的未钻探区域煤地质知识很少,深度超过1000m。焦作煤田II1号煤的资源集中度在(0.513-3.478)x10(8)m(3)/ km(2)范围内,平均值为1.805x10(8)m( 3)/ km(2)。根据煤层气资源调查和储层评价,焦作煤田煤层气生产的最有前景目标地区包括孤汉山煤矿,九里山煤矿和Qian南煤区西部。

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