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Using Stable Carbon Isotopes to Monitor for Potential Leakage of CO2 at an Enhanced Coal Bed Methane Recovery Site in Marshall County, WV.

机译:在西弗吉尼亚州马绍尔县,使用稳定的碳同位素监测增强的煤层气回收站中二氧化碳的潜在泄漏。

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摘要

Enhanced coal bed methane recovery, also known as ECBM, is a carbon capture and storage method in which carbon dioxide is injected into depleted gas formations (specifically unmineable coal beds) to aid in coal bed methane recovery for industrial uses. Produced natural gas, shallow groundwater, and soil vadose gas samples were collected at the CONSOL Energy Inc. CO2 Sequestration Pilot Test Site located in Marshall County, WV to test the feasibility using carbon isotope signatures to detect potential leakage of CO2 into overlying formations. CO2 was injected into the Upper Freeport coal seam at a depth of 396 m below valley bottom surface intermittently from September 2009 to December 2013. Water and gas samples were collected for isotopic analysis over a 12-month period (August 2013-August 2014). One set of water and gas samples collected in August 2013 was during an extended period of injection. The rest of the samples were collected during times the system was down or during the post-injection monitoring period that began in January 2014. The distinct carbon isotope signatures of the injected CO2, soil CO2, and coal bed CO2 allows us to use delta 13C as a natural tracer to detect any potential leakage from the injection coal bed into the overlying coal bed, aquifers and shallow soil zone. The range of the carbon isotope values observed in each of the overlying systems (i.e. overlying Pittsburgh coal seam, groundwater aquifer and shallow soil) indicate carbon originated from natural sources and processes within individual systems. There appears to be no influence of the injected CO2 on the delta13C values of the overlying systems. The initial results indicate that there was no significant leakage of CO2 from the Upper Freeport coal seam to the overlying formations at the time of sampling.
机译:增强的煤层气回收,也称为ECBM,是一种碳捕获和存储方法,其中将二氧化碳注入贫化的天然气层(特别是不可开采的煤层)中,以辅助工业用途的煤层气回收。在CONSOL Energy Inc.位于西弗吉尼亚州马歇尔县的CO2封存试验场,收集了生产的天然气,浅层地下水和土壤渗碳气体样品,以测试利用碳同位素特征检测CO2潜在泄漏到上层地层的可行性。从2009年9月至2013年12月,在谷底表面以下396 m处间歇性地向上游Freeport煤层注入CO2。在12个月内(2013年8月至2014年8月)收集了水和天然气样品进行同位素分析。 2013年8月收集的一组水和气样品处于延长的注入期。其余样本是在系统停机时或在2014年1月开始的注入后监控期间收集的。注入的CO2,土壤CO2和煤层CO2的独特碳同位素特征使我们可以使用δ13C作为一种天然示踪剂,可以检测从注煤层到上覆煤层,含水层和浅层土壤区域的任何潜在泄漏。在每个上覆系统(即上覆匹兹堡煤层,地下水蓄水层和浅层土壤)中观察到的碳同位素值范围均表明碳源自自然资源和各个系统中的过程。注入的二氧化碳似乎对上覆系统的δ13C值没有影响。初步结果表明,在采样时,从上自由港煤层到上覆地层没有明显的CO2泄漏。

著录项

  • 作者

    Meier, Bethany.;

  • 作者单位

    West Virginia University.;

  • 授予单位 West Virginia University.;
  • 学科 Geology.;Environmental health.;Geochemistry.
  • 学位 M.S.
  • 年度 2014
  • 页码 45 p.
  • 总页数 45
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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