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An Integrated Approach to Identify Water Resources for Human Consumption in an Area Affected by High Natural Arsenic Content

机译:天然砷含量高的地区识别人类消耗水资源的综合方法

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This study concerns the occurrence of arsenic in the groundwater system of the Cimino-Vico volcanic area (central Italy), different parts of which are currently widely used for local drinking water supply and for irrigation. The system shows a complex groundwater circulation, including a continuous basal aquifer, discontinuous perched aquifers, groundwater flows at high altitude, and local interactions with rising thermal fluids. Data on arsenic contents in 250 water samples from springs and wells and in 68 samples from rock outcrops were measured and combined with already existing information. Results highlight that arsenic concentrations of groundwater are influenced by type of aquifer, groundwater flow path, arsenic content of the aquifer rocks, and interaction with fluids rising from depth. Waters circulating in the Vico volcanics, one of the prominent rock units of the area, have high concentrations of arsenic, both for the basal and the perched aquifers. A large fraction of the waters associated with this rock unit have arsenic contents higher than 10 μg/L (82 percent for basal, 40 percent for perched). In contrast, waters circulating in the Cimino volcanics have lower arsenic contents: 30 percent of the basal and 10 percent of the perched aquifers have arsenic concentrations greater than 10 μg/L. Through an integrated approach, including leaching tests to investigate the arsenic behavior concerning the water-rock interaction and a geostatistical modeling of data, it has been possible to identify and tentatively quantify suitable water resources that have arsenic content not exceeding the quality standards for human consumption.
机译:这项研究涉及Cimino-Vico火山区(意大利中部)的地下水系统中砷的发生,该地区的不同部分目前广泛用于当地饮用水供应和灌溉。该系统显示出复杂的地下水循环,包括连续的基础含水层,不连续的栖息含水层,高海拔地区的地下水流以及与上升的热流体的局部相互作用。测量了来自泉水和水井的250个水样以及来自岩层的68个样品中的砷含量数据,并将其与现有信息结合起来。结果表明,地下水中砷的浓度受含水层类型,地下水流径,含水层岩石中砷含量以及与深层流体相互作用的影响。在维科火山中循环的水是该地区最重要的岩石单元之一,无论是基底含水层还是栖息含水层,其砷含量都很高。与该岩石单元相关的大部分水的砷含量都高于10μg/ L(基础为82%,栖息为40%)。相反,在奇米诺火山中循环的水的砷含量较低:30%的基础层和10%的栖息含水层中的砷浓度大于10μg/ L。通过一种综合方法,包括浸出试验以研究与水-岩相互作用有关的砷行为以及数据的地统计学模型,已经可以识别和初步量化砷含量不超过人类消费质量标准的水资源。

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