Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang, China.
Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang, China; Hebei and China Geological Survey Key Laboratory of Groundwater Remediation, Shijiazhuang, China.
Sci Total Environ. 2020 Jan 20;701:134777. doi: 10.1016/j.scitotenv.2019.134777. Epub 2019 Oct 31.
High concentration of manganese (Mn) in groundwater is a major concern because of its harmful to human health, and the origin of which in urbanized areas is often complicated. The present study aims to delineate spatial distributions of groundwater Mn in various aquifers and in areas with different urbanization levels in the Pearl River Delta (PRD), and to identify the origins of groundwater Mn in this region. Nearly 400 groundwater samples collected, and 14 chemicals were analyzed. The results show that approximately 20% groundwater in granular aquifers showed elevated-Mn (>0.4 mg/L), and was more than two times of that in fissured aquifers, while that in karst aquifers was absent. The proportions of elevated-Mn groundwater in urbanized areas and peri-urban areas were higher than that in non-urbanized areas. The decomposition of organic matter and reduction of Fe (hydr)oxides in sediments with reducing condition was likely to be the main factor controlling elevated-Mn groundwater in granular aquifers at a regional scale. By contrast, elevated-Mn groundwater in fissured aquifers was likely mainly affected by the urbanization accompanied with the leakage of low-oxygen domestic sewage and the industrialization accompanied by the leakage of industrial wastewater. In addition, Mn-rich surface water was also probably an important source for groundwater Mn in river network areas. Therefore, it is necessary to make a long-term monitoring for groundwater Mn in granular aquifers, especially in urbanized areas and river network areas, because of the high proportion of elevated-Mn.
地下水高浓度锰 (Mn) 是一个主要关注点,因为它对人体健康有害,而城市化地区锰的来源往往很复杂。本研究旨在描绘珠江三角洲 (PRD) 不同含水层和不同城市化水平地区地下水 Mn 的空间分布,并确定该地区地下水 Mn 的来源。采集了近 400 个地下水样本,并分析了 14 种化学物质。结果表明,约 20%的颗粒状含水层地下水呈现高锰 (>0.4 mg/L),是裂隙含水层的两倍多,而岩溶含水层则不存在。城市化地区和城郊地区高浓度地下水的比例高于非城市化地区。在区域尺度上,沉积物中有机物的分解和还原性条件下 Fe(hydr)氧化物的还原可能是控制颗粒状含水层高浓度地下水的主要因素。相比之下,裂隙状含水层中高浓度的地下水可能主要受城市化的影响,伴随着低氧生活污水的泄漏,以及工业化的影响,伴随着工业废水的泄漏。此外,富锰地表水也是河网地区地下水 Mn 的一个重要来源。因此,由于高浓度地下水 Mn 的比例较高,有必要对颗粒状含水层,特别是城市化地区和河网地区的地下水 Mn 进行长期监测。