Linking land subsidence to deep arsenic release in the Mekong Delta aquifer system

将地面沉降与湄公河三角洲含水层系统深层砷释放联系起来

• 批准号: 1313518
• 负责人: Steven Gorelick
• 金额: $ 25.64万
• 依托单位: Stanford University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2013
• 资助国家: 美国
• 起止时间: 2013-08-15 至 2016-07-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1313518&HistoricalAwards=false
• 关键词: Linking; land; subsidence; deep; arsenic

An estimated 100 million people living in floodplains in Asia are exposed to arsenic in groundwater that is derived from Himalayan sediments. Arsenic is a toxin linked to cancer and a variety of other serious ailments through direct ingestion of contaminated groundwater. Growing exploitation of these contaminated aquifers increases the number of people facing these health risks, and exposes still greater populations to the hazard of consuming agricultural products irrigated with arsenic-contaminated groundwater. Despite widespread awareness of the arsenic hazard, understanding of the relationship between groundwater exploitation and arsenic contamination remains limited, particularly in deep aquifers, which are increasingly providing a larger portion of total pumped groundwater.In this work, we focus on the Mekong Delta, where we have obtained a comprehensive, unique, unanalyzed dataset consisting of 42,000 dissolved arsenic measurements from southern Vietnam showing widespread contamination (1000 sq km) in deep aquifers (200m) that are used extensively for water supply. One hypothesis is that deep pumping has induced shallow dissolved arsenic or arsenic-mobilizing solutes to move deeper. However, preliminary analysis does not support this mechanism in the Mekong Delta given the observed widespread deep arsenic contamination in the presence of thick clay deposits that serve as relative vertical flow barriers. We hypothesize a previously unrecognized deep arsenic source mechanism in which water containing arsenic is expelled from storage in clays that compact when overlying and underlying deep aquifers are exploited. This work combines spatial statistical modeling of groundwater arsenic observations, 3D aquifer flow and compaction simulation, and remote measurement of land subsidence using satellite radar imagery (InSAR). Our goal is to explore the notion that deep groundwater arsenic may be due to the release of pore-waters containing arsenic trapped in clay beds deposited millions of years ago. This research has important implications to science and society. First, our formerly unrecognized contamination mechanism may be fundamental to understanding arsenic occurrence in aquifer systems and the associated health risks of deep groundwater exploitation. Our investigation will have implications for water resources development and human health in the arsenic-affected basins of Southeast Asia where some regions of planned deep aquifer exploitation may unknowingly expose people to deep-source arsenic. This work has consequences for analogous arsenic-affected aquifer systems in sedimentary basins around the world containing interbedded compressible clays that may harbor arsenic and other contaminants. Second, in terms of methods, the link between subsidence and arsenic release has significant potential as a reconnaissance tool, particularly in underdeveloped regions where the impacts of excessive pumping on land subsidence have not been recognized. The use of satellite radar to detect land deformation can serve as a means to identify areas where clay compaction and consequent arsenic release may be occurring.

据估计，生活在亚洲洪泛区的1亿人暴露于来自喜马拉雅沉积物的地下水中的砷。砷是一种毒素，通过直接摄入受污染的地下水，与癌症和其他各种严重疾病有关。对这些受污染的含水层的开采日益增加，使更多的人面临这些健康风险，并使更多的人面临消费用砷污染的地下水灌溉的农产品的危险。尽管人们普遍认识到砷的危害，但对地下水开采和砷污染之间关系的了解仍然有限，特别是在深层含水层中，这些含水层越来越多地提供了总抽取地下水的更大部分。在这项工作中，我们专注于湄公河三角洲，在那里我们获得了一个全面，独特，未经分析的数据集，包括42，越南南部的000个溶解砷测量结果显示，广泛用于供水的深层含水层（200米）中存在广泛的污染（1000平方公里）。一种假设是，深层抽水导致浅层溶解的砷或砷动员溶质移动到更深处。然而，初步分析并不支持这种机制在湄公河三角洲的观察到广泛的深砷污染存在的厚粘土沉积物，作为相对的垂直流动障碍。我们假设了一个以前未被认识到的深砷源机制，其中含有砷的水被驱逐出存储在粘土，紧凑时，上覆和下伏的深层含水层被开采。这项工作结合了地下水砷观测的空间统计建模，三维含水层流动和压实模拟，以及使用卫星雷达图像（干涉合成孔径雷达）的地面沉降遥感测量。我们的目标是探讨深层地下水砷可能是由于释放的孔隙水中的砷被困在粘土床沉积数百万年前的概念。 这项研究对科学和社会具有重要意义。首先，我们以前未认识到的污染机制可能是根本的了解砷发生在含水层系统和相关的健康风险的深层地下水开采。我们的调查将对东南亚受砷影响的盆地的水资源开发和人类健康产生影响，在这些盆地中，一些计划开采深层含水层的地区可能会在不知不觉中使人们暴露于深源砷。这项工作的后果类似砷影响的含水层系统在世界各地的沉积盆地含有层间可压缩粘土，可能窝藏砷和其他污染物。 其次，在方法方面，沉降与砷释放之间的联系作为一种侦察工具具有巨大的潜力，特别是在过度抽水对地面沉降的影响尚未得到认识的欠发达地区。利用卫星雷达探测土地变形可以作为一种手段，查明可能发生粘土压实和随之发生砷释放的地区。