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Research on gas occurrence regularity in Fengcheng Mining Area of Jiangxi Province

机译:江西凤城矿区瓦斯赋存规律研究

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摘要

The hazard of coal and gas outburst and the utilization of coalbed methane, continuously promotes research on the characteristics of methane distribution. As an important coal production base in China, Fengcheng Mining Area not only is serious in coal and gas outburst but also is one of the most promising coalbed methane development zones, so it is of significance to research on gas occurrence regularity. Based on the analysis of gas data collected from geological exploration and coal mining, the research reveals that: the gas occurrence regularity vary significantly between north limb and south limb of Fengcheng syncline. In north limb, with the increase of the depth of coal seam, gas content of coal seam tend to increase, the relative gas emission rate and the absolute gas emission rate tend to increase, the intensity of coal and gas outbursts tend to increase. But in south limb, the gas contents of coal seam are very low, far below the gas contents in north limb under the same depth. The controlling factors to gas occurrence regularity are discussed in this paper. The features of coal quality, the overlying lithology of coal seam and coal body structure in Fengcheng Mining Area are all favorable to gas generation and gas preservation. Under these conditions, in north limb, with the increase of coal seam's depth and overlying pressure of coal seam, the risk of gas hazard increase, which cause the gas occurrence regularity in north limb of Fengcheng syncline. But in south limb, the Eocene strata of Paleocene is directly overlying above Longtan coal-bearing strata of the Permian, which means that the coal seams of south limb have ever been strongly uplifted and exposed to ground so as to be weathered and eroded for a long time, and a large amount of gas is released, thus the gas contents of B4 coal seam in south limb are very low.
机译:煤与瓦斯突出的危害以及煤层气的利用,不断推动着甲烷分布特征的研究。作为中国重要的煤炭生产基地,凤城矿区不仅煤与瓦斯突出严重,而且是最有前途的煤层气开发区之一,对研究瓦斯发生规律具有重要意义。通过对地质勘探和煤矿开采的瓦斯资料的分析,发现:凤城向斜向北,南向的瓦斯赋存规律有较大差异。在北肢,随着煤层深度的增加,煤层瓦斯含量趋于增加,相对瓦斯率和绝对瓦斯率趋于增加,煤与瓦斯突出强度趋于增加。但是在南肢,煤层的瓦斯含量很低,在相同深度下远低于北肢的瓦斯含量。讨论了影响瓦斯发生规律的因素。凤城矿区煤质特征,上覆煤层岩性和煤体结构都有利于天然气的产生和瓦斯的保存。在这种情况下,随着煤层深度的增加和煤层上覆压力的增加,在北肢,瓦斯灾害的危险性增加,导致凤城向斜向北肢的瓦斯发生规律。但是在南肢,古新世始新世地层直接覆盖在二叠纪龙潭含煤地层之上,这意味着南肢的煤层曾被强烈抬升并暴露于地面,以使其风化和侵蚀。时间长,释放出大量的瓦斯,因此南肢的B4煤层瓦斯含量很低。

著录项

  • 来源
    《Energy Exploration & Exploitation》 |2014年第3期|591-599|共9页
  • 作者单位

    School of Earth and Environment, Anhui University of Science and Technology, Huainan 232001, China,Mine Geology Committee, China Coal Society, Huainan 232001, China;

    School of Surveying, Anhui University of Science and Technology, Huainan 232001, China;

    School of Surveying, Anhui University of Science and Technology, Huainan 232001, China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Fengcheng Mining Area; B4 coal seam; Mining depth; Erosion of coal seam; Gas emission;

    机译:凤城矿区;B4煤层;开采深度;煤层侵蚀;气体排放;

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