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Controls on Gas Content and Carbon Isotopic Abundance of Methane in Qinnan-East Coal Bed Methane Block, Qinshui Basin, China

机译:沁水盆地沁南东煤层气区块甲烷气体含量和碳同位素丰度的控制

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摘要

Qinnan-East Block is one newly planned coal bed methane (CBM) exploration area in the Qinshui Basin, China, and research on the accumulation of gas in this block is quite limited. In this study, on the basis of a series of laboratory experiments and the latest exploration data, the gas content and carbon isotopic ratio of methane [delta C-13(CH4)] in the No. 3 coal seam of Permian Shanxi Formation in Quinan-East.Block were investigated, and then the correlations between delta C-13(CH4) and vitrinite reflectance, burial depth, gas content, reservoir pressure, and gas adsorption saturation were analyzed; then, the mechanism controlling the gas bearing properties and the distribution of delta C-13(CH4) in the study area were addressed. It turns out that the gas content in the study area ranges from 2.87 to 24.63 m(3)/t with an average of 13.78 m(3)/t, the CBM reservoir pressure ranges from 0.86 to 5.96 MPa with an average of 3.09 MPa, the reservoir pressure gradient ranges from 0.11 to 1.06 MPa/100 m with an average of 0.49 MPa/100 m, and the gas saturation ranges from 12.34 to 117.76% with an average of 67.58%; the gas content, CBM reservoir pressure, and gas saturation increase with an increase in burial depth.delta C-13(CH4) of naturally desorbed methane from the No. 3 coal seam varies from -28.89 to -53.27%o with an average of -36.48%o and increases with an increase in vitrinite reflectance and burial depth. The carbon isotopic abundance of CBM is mainly controlled by the thermodynamic equilibrium fractionation in the formation of CBM and the kinetic disequilibrium fractionation in the transport of CBM delta C-13(CH4) rises in a nearly logarithmic form with the increase in CBM content, reservoir pressure, and gas saturation. The geological controls on gas bearing properties of the coal seam are vitrinite reflectance and effective burial depth, which are similar to those of the carbon isotopic abundance of methane. The outcomes may benefit the exploration of CBM in the study area.
机译:沁南东区是中国沁水盆地的一个新规划的煤层气勘探区,该区天然气成藏的研究十分有限。本研究基于一系列的实验室实验和最新的勘探数据,研究了奎南二叠系山西组三煤层中甲烷[δC-13(CH4)]的气体含量和碳同位素比。研究了East.Block,然后分析了δC-13(CH4)与镜质反射率,埋深,气体含量,储层压力和气体吸附饱和度之间的相关性;然后,研究了控制气藏性质的机制和δC-13(CH4)在研究区内的分布。结果表明,研究区域的天然气含量为2.87至24.63 m(3)/ t,平均为13.78 m(3)/ t,煤层气储层压力为0.86至5.96 MPa,平均为3.09 MPa。 ,储层压力梯度范围为0.11〜1.06 MPa / 100 m,平均为0.49 MPa / 100 m,气体饱和度为12.34〜117.76%,平均为67.58%;随着埋深的增加,瓦斯含量,煤层气储层压力和瓦斯饱和度也随之增加。3号煤层天然解吸甲烷的δC-13(CH4)变化范围为-28.89至-53.27%o,平均值为-36.48%o并随镜质体反射率和埋深的增加而增加。煤层气的碳同位素丰度主要受煤层气形成过程中的热力学平衡分馏和煤层气δC-13(CH4)运移的动力学不平衡分馏的影响,随着煤层气含量的增加,储层的增加压力和气体饱和度。煤层含气性的地质控制为镜质体反射率和有效埋深,与甲烷的碳同位素丰度相似。结果可能有益于研究区域中煤层气的勘探。

著录项

  • 来源
    《Energy & fuels》 |2017年第2期|1502-1511|共10页
  • 作者单位

    China Univ Min & Technol Beijing, Coll Geosci & Surveying Engn, Beijing 100083, Peoples R China|Shanxi Jincheng Anthracite Min Grp Co Ltd, State Key Lab Coal & CBM Comining, Jincheng 048000, Shanxi, Peoples R China;

    China Univ Min & Technol Beijing, Coll Geosci & Surveying Engn, Beijing 100083, Peoples R China|Shanxi Jincheng Anthracite Min Grp Co Ltd, State Key Lab Coal & CBM Comining, Jincheng 048000, Shanxi, Peoples R China;

    China Univ Geosci, Fac Earth Resources, Wuhan 430074, Hubei, Peoples R China|Shanxi Jincheng Anthracite Min Grp Co Ltd, State Key Lab Coal & CBM Comining, Jincheng 048000, Shanxi, Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);
  • 原文格式 PDF
  • 正文语种 eng
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  • 入库时间 2022-08-18 00:39:29

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