...
首页> 外文期刊>The Science of the Total Environment >High resolution spatial and temporal evolution of dissolved gases in groundwater during a controlled natural gas release experiment
【24h】

High resolution spatial and temporal evolution of dissolved gases in groundwater during a controlled natural gas release experiment

机译:受控的天然气释放实验中地下水中溶解气体的高分辨率时空演化

获取原文
获取原文并翻译 | 示例

摘要

Fugitive gas comprised primarily of methane (CH4) with traces of ethane and propane (collectively termed C1–3) may negatively impact shallow groundwater when unintentionally released from oil and natural gas wells. Currently, knowledge of fugitive gas migration, subsurface source identification and oxidation potential in groundwater is limited. To advance understanding, a controlled release experiment was performed at the Borden Research Aquifer, Canada, whereby 51m3of natural gas was injected into an unconfined sand aquifer over 72days with dissolved gases monitored over 323days. During active gas injection, a dispersed plume of dissolved C1–3evolved in a depth discrete and spatially complex manner. Evolution of the dissolved gas plume was driven by free-phase gas migration controlled by small-scale sediment layering and anisotropy. Upon cessation of gas injection, C1–3concentrations increased to the greatest levels observed, particularly at 2 and 6m depths, reaching up to 31.5, 1.5 and 0.1mg/L respectively before stabilizing and persisting. At no time did groundwater become fully saturated with natural gas at the scale of sampling undertaken. Throughout the experiment the isotopic composition of injected methane (δ13C of −42.2‰) and the wetness parameter (i.e. the ratio of C1to C2+) constituted excellent tracers for the presence of fugitive gas at concentrations >2mg/L. At discrete times C1–3concentrations varied by up to 4 orders of magnitude over 8m of aquifer thickness (e.g. from <0.01 to 30mg/L for CH4), while some groundwater samples lacked evidence of fugitive gas, despite being within 10m of the injection zone. Meanwhile, carbon isotope ratios of dissolved CH4showed no evidence of oxidation. Our results show that while impacts to aquifers from a fugitive gas event are readily detectable at discrete depths, they are spatially and temporally variable and dissolved methane has propensity to persist.
机译:当无意中从石油和天然气井中释放时,主要由甲烷(CH4)以及痕量乙烷和丙烷(统称为C1-3)组成的逸散性气体可能会对浅层地下水产生负面影响。当前,对地下气体逸散气体迁移,地下源识别和氧化潜力的了解有限。为了进一步了解,在加拿大Borden Research含水层进行了控释实验,其中在72天的时间内将51立方米的天然气注入到无限制的砂层中,并在323天的时间内监测了溶解气体。在注入活性气体期间,溶解的C1-3的分散羽以深度离散和空间复杂的方式演化。溶解气柱的演化是由自由相气体运移驱动的,该相移由小规模的沉积物分层和各向异性控制。停止注气后,C1–3浓度增加到观察到的最大水平,尤其是在2m和6m深度处,在稳定并持续之前分别达到31.5、1.5和0.1mg / L。在所进行的采样范围内,地下水绝不会完全被天然气饱和。在整个实验过程中,注入的甲烷的同位素组成(δ13C为-42.2‰)和湿度参数(即C1与C2 +的比)构成了在浓度> 2mg / L的逃逸性气体存在时的极好的示踪剂。在离散时间,C1-3浓度在8m的含水层厚度中变化高达4个数量级(例如,CH4的浓度从<0.01到30mg / L),而某些地下水样品尽管在注入区的10m以内,但仍缺乏挥发性气体的证据。 。同时,溶解的CH4的碳同位素比没有显示出氧化的迹象。我们的结果表明,尽管在离散深度很容易检测到逃逸性气体事件对含水层的影响,但它们在空间和时间上都是可变的,溶解的甲烷具有持续存在的倾向。

著录项

  • 来源
    《The Science of the Total Environment》 |2018年第may1期|1178-1192|共15页
  • 作者单位

    G360 Institute for Groundwater Research, College of Engineering & Physical Sciences, University of Guelph,Energy and Environment Research Initiative, Department of Earth, Ocean and Atmospheric Science, University of British Columbia;

    G360 Institute for Groundwater Research, College of Engineering & Physical Sciences, University of Guelph;

    Department of Geoscience, University of Calgary;

    Energy and Environment Research Initiative, Department of Earth, Ocean and Atmospheric Science, University of British Columbia;

    G360 Institute for Groundwater Research, College of Engineering & Physical Sciences, University of Guelph;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Methane; Natural gas; Groundwater; Energy; Hydraulic fracturing; Stable carbon isotopes;

    机译:甲烷;天然气;地下水;能源;水力压裂;碳同位素稳定;

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号