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Assessment of shallow aquifer remediation capacity under different groundwater management conditions in CGS field

机译:CGS田不同地下水管理条件下浅层含水层修复能力评价

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摘要

Because of unknown faults and fractures in the overlying rock, CO2 stored deep underground may move upward, and the intrusion may impact shallow groundwater quality. After leakage of CO2 has ceased, the affected aquifer may show remediation capacity under natural conditions and injections and extractions. In this study, the reactive transport modeling software TOUGHREACT was used to simulate the remediation capacity of a study aquifer. The simulation results show that the intrusion of leaked CO2 would decrease the pH of the target aquifer and trigger the dissolution of calcite minerals. After CO2 leakage has ceased, the pH would increase as would the concentration of Ca because of the dissolution of calcite along the flow path. Scenario simulation results of amelioration of groundwater quality by water injection and extraction show that single injection is the best option and a combination approach of injection and extraction could control the range of the affected area. The pH value should not be regarded as the single indicator for remediation capacity assessment. Parameter sensitive analysis results show that the rates of injection and extraction affect the repair results significantly.
机译:由于上覆岩石中未知的断层和裂缝,储存在地下深处的CO2可能会向上移动,并且侵入可能会影响浅层地下水水质。在二氧化碳泄漏停止后,受影响的含水层在自然条件下以及注入和提取后可能显示出修复能力。在这项研究中,反应性传输建模软件TOUGHREACT被用来模拟研究含水层的修复能力。模拟结果表明,泄漏的CO2侵入将降低目标含水层的pH值并触发方解石矿物的溶解。在二氧化碳泄漏停止后,由于方解石沿流动路径的溶解,pH值将随着钙浓度的升高而增加。通过注水和抽水改善地下水质量的方案模拟结果表明,单注是最佳选择,注水和抽水相结合的方法可以控制受影响区域的范围。 pH值不应视为补救能力评估的单一指标。参数敏感性分析结果表明,注入和提取的速率显着影响修复结果。

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