土壤地下水系统中运输,迁移和转化的特征和数值模拟
Rongrong Ying1, Bin Yang2, Meng Chen1
1Nanjing Institute of Environmental Sciences, Ministry of Ecology and Environment, Nanjing 210042, PR China.
Journal of hazardous materials
|April 28, 2024
概括
了解土壤和地下水中的 (Cr) 迁移是修复的关键. 管理水表深度可以限制Cr Cr.
科学领域:
- 环境科学 环境科学
- 地质化学 地质化学
- 水文地质学 水文地质学
背景情况:
- 地表 (Cr) 污染对环境构成重大风险.
- 了解土壤地下水系统中的Cr迁移对于有效的补救策略至关重要.
研究的目的:
- 为了研究在模拟污染现场的3D迁移和转变.
- 分析地下水流量和水表深度对Cr.行为的影响.
- 评估Cr的固定和分散模式.
主要方法:
- 一个三维 (3D) 沙箱实验模拟了珍珠河三角洲 (PRD) 的典型Cr污染地点.
- 在雨量和地下水流量组合下,研究Cr的迁移和转变.
- 应用一个反应式运输模型来模拟Cr的保留和形态分布.
主要成果:
- 形成了一个复杂的3D流场,受水表深度的影响,促进了Cr的迁移和分散.
- 低水平面条件扩大了下流,增加了垂直的Cr迁移和深层土壤污染.
- (VI) 的减少导致了土壤中约75%的总Cr固定.
- 在8年的时间里,Cr迁移并向下游扩散了15米,这表明地下水的运输量很大.
结论:
- 水平面深度是影响土壤地下水系统中迁移模式的关键因素.
- 管理水表深度可以是一个可行的策略,以尽量减少垂直迁移和地下污染.
- 反应式运输建模准确地预测了Cr的保留和分布,有助于风险评估和补救计划.
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