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利用多元统计技术研究城市化地区(华南)人类活动和自然过程对地下水砷的影响。

Impact of human activity and natural processes on groundwater arsenic in an urbanized area (South China) using multivariate statistical techniques.

机构信息

Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang, 050061, China,

出版信息

Environ Sci Pollut Res Int. 2014 Nov;21(22):13043-54. doi: 10.1007/s11356-014-3269-x. Epub 2014 Jul 5.

Abstract

Anthropogenic factors resulted from the urbanization may affect the groundwater As in urbanized areas. Groundwater samples from the Guangzhou city (South China) were collected for As and other parameter analysis, in order to assess the impact of urbanization and natural processes on As distribution in aquifers. Nearly 25.5 % of groundwater samples were above the WHO drinking water standard for As, and the As concentrations in the granular aquifer (GA) were generally far higher than that in the fractured bedrock aquifer (FBA). Samples were classified into four clusters by using hierarchical cluster analysis. Cluster 1 is mainly located in the FBA and controlled by natural processes. Anthropogenic pollution resulted from the urbanization is responsible for high As concentrations identified in cluster 2. Clusters 3 and 4 are mainly located in the GA and controlled by both natural processes and anthropogenic factors. Three main mechanisms control the source and mobilization of groundwater As in the study area. Firstly, the interaction of water and calcareous rocks appears to be responsible for As release in the FBA. Secondly, reduction of Fe/Mn oxyhydroxides and decomposition of organic matter are probably responsible for high As concentrations in the GA. Thirdly, during the process of urbanization, the infiltration of wastewater/leachate with a high As content is likely to be the main source for groundwater As, while NO3 (-) contamination diminishes groundwater As.

摘要

人为因素城市化可能会影响地下水砷在城市地区。从广州市(华南)采集地下水样本进行砷和其他参数分析,以评估城市化和自然过程对含水层中砷分布的影响。近 25.5%的地下水样本中砷的浓度超过了世界卫生组织饮用水砷标准,而颗粒含水层(GA)中的砷浓度普遍远高于基岩裂隙含水层(FBA)。通过使用层次聚类分析将样品分为四个类群。第 1 类主要位于 FBA 中,受自然过程控制。城市化带来的人为污染导致第 2 类中砷浓度升高。第 3 类和第 4 类主要位于 GA 中,受自然过程和人为因素的共同控制。研究区地下水砷的来源和迁移受三种主要机制控制。首先,水与钙质岩石的相互作用似乎是 FBA 中砷释放的原因。其次,Fe/Mn 氢氧化物的还原和有机物的分解可能是 GA 中砷浓度高的原因。第三,在城市化过程中,高砷含量的废水/渗滤液的渗透可能是地下水砷的主要来源,而硝酸盐(NO3(-))污染会降低地下水中的砷含量。

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