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镉在喀斯特环境水文循环中的行为。

Cadmium behavior in a karst environment hydrological cycle.

机构信息

Geology Department, Federal University of Ouro Preto, Ouro Preto, MG, Brazil.

Geology Department, Federal University of Minas Gerais, Ouro Preto, MG, Brazil.

出版信息

Environ Sci Pollut Res Int. 2020 Mar;27(9):8965-8979. doi: 10.1007/s11356-020-07894-2. Epub 2020 Feb 10.

Abstract

Karst regions are important water providers, supplying approximately 25% of the world population. These areas present higher vulnerability to contamination due to hydrodynamics, which hampers the natural depuration of these waters until reaching the underground environment. High concentrations of cadmium (Cd) are observed in the São Miguel watershed, state of Minas Gerais, Brazil. This toxic element is generally and predominantly released into the atmosphere by burning materials that have Cd in their composition, potentially contaminating surface and groundwater. Therefore, the objective of the study is to map Cd concentrations in the hydrological cycle of the São Miguel karst watershed and, through natural background level values (NBL 90%) of rainwater, surface water and groundwater, to understand the seasonal behavior of this element, and to identify the most vulnerable areas to contamination. To achieve this goal, rainwater, surface, and groundwater seasonal monitoring were conducted in 87 sampling stations. A total of 335 samples were collected, distributed over a watershed area of 520 km. Concentrations of cadmium above 1 μg/L were found in 21.49% of samples during the rainy season. The origin and distribution of Cd were related to rainfall. For rainwater samples, 90% presented Cd concentration of 3.06 μg/L. When these waters precipitate, they contaminate surface waters (NBL 90% = 1.50 μg/L) and groundwater (NBL 90% = 2.81 μg/L). This study presented a hydrochemical cycle map and proposed NBL values of Cd for surface water and groundwater, helping to understand how the environment is contaminated by this element.

摘要

喀斯特地区是重要的水源地,为全球约 25%的人口提供水源。由于水动力作用,这些地区更容易受到污染,阻碍了这些水的自然净化,直到它们到达地下环境。巴西米纳斯吉拉斯州圣米格尔流域的水中镉(Cd)浓度较高。这种有毒元素通常主要是通过燃烧含有 Cd 的物质释放到大气中,可能会污染地表水和地下水。因此,本研究的目的是绘制圣米格尔喀斯特流域水文循环中的 Cd 浓度图,并通过雨水、地表水和地下水的自然背景水平值(NBL 90%)来了解该元素的季节性行为,并识别最易受污染的区域。为了实现这一目标,在 87 个采样站进行了雨水、地表水和地下水的季节性监测。共采集了 335 个样本,分布在 520 平方公里的流域面积上。在雨季,有 21.49%的样本中发现 Cd 浓度超过 1μg/L。Cd 的来源和分布与降雨有关。对于雨水样本,90%的 Cd 浓度为 3.06μg/L。当这些水沉淀时,它们会污染地表水(NBL 90%=1.50μg/L)和地下水(NBL 90%=2.81μg/L)。本研究绘制了一个水文化学循环图,并提出了地表水和地下水 Cd 的 NBL 值,有助于了解环境如何受到该元素的污染。

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