What Can Groundwater Monitoring Tell Us About Gas Migration? A Numerical Modeling Study

IF 2 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Groundwater Pub Date : 2023-10-01 DOI:10.1111/gwat.13358
Kartik Jain, Cole J.C. Van De Ven, K. Ulrich Mayer
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Abstract

Groundwater monitoring to measure a variety of indicator parameters including dissolved gas concentrations, total dissolved gas pressure (TDGP), and redox indicators is commonly used to evaluate the impacts of gas migration (GM) from energy development in shallow aquifer systems. However, these parameters can be challenging to interpret due to complex free-phase gas source architecture, multicomponent partitioning, and biogeochemical reactions. A series of numerical simulations using a gas flow model and a reactive transport model were conducted to delineate the anticipated evolution of indicator parameters following GM in an aquifer under a variety of physical and biogeochemical conditions. The simulations illustrate how multicomponent mass transfer processes and biogeochemical reactions create unexpected spatial and temporal variations in several analytes. The results indicate that care must be taken when interpreting measured indicator parameters including dissolved hydrocarbon concentrations and TDGP, as the presence of dissolved gases in background groundwater and biogeochemical processes can cause potentially misleading conclusions about the impact of GM. Based on the consideration of multicomponent gas partitioning in this study, it is suggested that dissolved background gases such as N2 and Ar can provide valuable insights on the presence, longevity and fate of free-phase natural gas in aquifer systems. Overall, these results contribute to developing a better understanding of indicators for GM in groundwater, which will aid the planning of future monitoring networks and subsequent data interpretation.

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地下水监测能告诉我们什么是气体迁移?数值建模研究。
地下水监测用于测量各种指标参数,包括溶解气体浓度、总溶解气体压力(TDGP)和氧化还原指标,通常用于评估浅层含水层系统能源开发对气体迁移(GM)的影响。然而,由于复杂的自由相气源结构、多组分分配和生物地球化学反应,这些参数的解释可能具有挑战性。使用气流模型和反应输运模型进行了一系列数值模拟,以描绘在各种物理和生物地球化学条件下,含水层中GM后指标参数的预期演变。模拟说明了多组分传质过程和生物地球化学反应如何在几种分析物中产生意想不到的空间和时间变化。结果表明,在解释包括溶解碳氢化合物浓度和TDGP在内的测量指标参数时必须小心,因为背景地下水和生物地球化学过程中溶解气体的存在可能会导致关于GM影响的潜在误导性结论。基于本研究中对多组分气体分配的考虑,认为溶解的背景气体如N2和Ar可以为含水层系统中自由相天然气的存在、寿命和命运提供有价值的见解。总的来说,这些结果有助于更好地了解地下水中的转基因指标,这将有助于规划未来的监测网络和随后的数据解释。这篇文章受版权保护。保留所有权利。
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来源期刊
Groundwater
Groundwater 环境科学-地球科学综合
CiteScore
4.80
自引率
3.80%
发文量
0
审稿时长
12-24 weeks
期刊介绍: Ground Water is the leading international journal focused exclusively on ground water. Since 1963, Ground Water has published a dynamic mix of papers on topics related to ground water including ground water flow and well hydraulics, hydrogeochemistry and contaminant hydrogeology, application of geophysics, groundwater management and policy, and history of ground water hydrology. This is the journal you can count on to bring you the practical applications in ground water hydrology.
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