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现代地质 ›› 2015, Vol. 29 ›› Issue (2): 331-336.

• 地下水污染与防治 • 上一篇    下一篇

压裂液在煤层中的运移模拟研究

侯宏冰,陈立,郭晓静,马琳娜   

  1. (中国地质科学院 水文地质环境地质研究所,河北 石家庄 050061)
  • 出版日期:2015-04-21 发布日期:2015-06-09
  • 作者简介:侯宏冰,男,助理研究员,博士研究生,1976年出生,水文地质工程地质专业,主要从事地下水数值模拟研究。Email:houhongbing@gmail.com。
  • 基金资助:

    国家科技支撑计划项目(2012BAJ11B04);中国地质调查局地质调查项目(12120114011701)。

Migration Simulation Research on Hydro-fracturing Fluid in Coal Bed

HOU Hong-bing, CHEN Li, GUO Xiao-jing, MA Lin-na   

  1. (Institute of Hydrogeology and Environmental Geology,Chinese Academy of Geology Sciences, Shijiazhuang, Hebei  050061,China)
  • Online:2015-04-21 Published:2015-06-09

摘要:

为给山西省临县三交区块的地下水环境保护提供科学依据,运用地下水数值模拟技术对压裂液在煤层中的运移进行了预测。在分析研究区地质结构的基础上,建立了水文地质概念模型,将山西组3#煤层概化为一个承压含水层,其上覆二叠系砂岩、泥岩作为隔水层,下伏的泥岩、砂岩互层作为隔水层,并确定了地下水系统的边界条件。运用地下水模型软件(Feflow)对研究区内的压裂液在煤层中的运移进行了模拟和预测,预测结果表明,压裂液在煤层中的的运移范围在煤层压裂影响范围以内,即压裂井周围300  m范围内。

关键词: 煤层气, 压裂液, 污染, 三交区块, 山西临县

Abstract:

To provide scientific foundation for the protection of groundwater environment in Sanjiao block of Lin County in Shanxi Province, the groundwater numerical simulation was conducted to predict the migration of hydro-fracturing fluid in coal bed. A hydrogeological conceptual model was set up based on the analysis of geological structure. The 3# group coal bed within Shanxi Formation was conceptualized as  a confined aquifer, overlaid by Permian sandstone and mudstone and underlaid by interbeds of mudstone and sandstone functioning as quitards. In addition, groundwater boundary conditions were confirmed. Migration of hydro-fracturing fluid in coal bed of the study area was modeled and predicted. Results indicate that the migration range of hydro-fracturing fluid in the coal bed is within coal hydro-fracturing impact limits, about 300 meters around fractured well.

Key words: coal-bed gas, hydro-fracturing fluid, pollution, Sanjiao block, Lin County in Shanxi Province

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