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黄河冲积扇地表水和地下水痕量金属及其迁移:同位素和水化学证据。

Trace metal in surface water and groundwater and its transfer in a Yellow River alluvial fan: evidence from isotopes and hydrochemistry.

机构信息

Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China.

Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China.

出版信息

Sci Total Environ. 2014 Feb 15;472:979-88. doi: 10.1016/j.scitotenv.2013.11.120. Epub 2013 Dec 17.

Abstract

Metals are ubiquitous in the environment. The aim of sustainable management of the agro-ecosystem includes ensuring that water continues to fulfill its function in agricultural production, cycling of elements, and as a habitat of numerous organisms. There is no doubt that the influence of large-scale irrigation projects has impacted the regional surface-groundwater interactions in the North China Plain (NCP). Given these concerns, the aim of this study is to evaluate the pollution, identify the sources of trace metals, analyze the influence of surface-groundwater interactions on trace metal distribution, and to propose urgent management strategies for trace metals in the agriculture area in China. Trace metals, hydrochemical indicators (EC, pH, concentrations of Na(+), K(+), Mg(2+), Ca(2+), Cl(-), SO4(2-), and HCO3(-)) and stable isotopic composition (δ(18)O and δ(2)H) were determined for surface water (SW) and groundwater (GW) samples. Trace metals were detected in all samples. Concentrations of Fe, Se, B, Mn, and Zn in SW exceeded drinking water standards by 14.8%, 29.6%, 25.9%, 11.1%, and 14.8% higher, respectively, and by 3.8%, 23.1%, 11.5%, 11.5%, and 7.7% in GW. The pollution of trace metals in surface water was more serious than that in groundwater, and was also higher than in common irrigation areas in NCP. Trace metals were found to have a combined origin of geogenic and agriculture and industrial activities. Their distribution varied greatly and exhibited a certain relationship with the water flow direction, with the exception of a number of singular sites. Hydrochemical and environmental isotopic evidence indicates surface-groundwater interactions influence the spatial distribution of trace metal in the study area. Facing the ongoing serious pollution, management practices for source control, improved control technologies, and the construction of a monitoring net to warn of increased risk are urgently needed.

摘要

金属在环境中无处不在。农业生态系统可持续管理的目标包括确保水继续在农业生产、元素循环以及作为众多生物栖息地方面发挥其功能。毫无疑问,大规模灌溉项目的影响已经改变了华北平原(NCP)的区域地表水-地下水相互作用。鉴于这些担忧,本研究的目的是评估污染,确定痕量金属的来源,分析地表水-地下水相互作用对痕量金属分布的影响,并为中国农业区的痕量金属提出紧急管理策略。对地表水(SW)和地下水(GW)样品进行了痕量金属、水化学指标(EC、pH、Na(+)、K(+)、Mg(2+)、Ca(2+)、Cl(-)、SO4(2-)和 HCO3(-)浓度)和稳定同位素组成(δ(18)O 和 δ(2)H)的测定。所有样品中均检测到痕量金属。SW 中 Fe、Se、B、Mn 和 Zn 的浓度分别比饮用水标准高出 14.8%、29.6%、25.9%、11.1%和 14.8%,GW 中分别高出 3.8%、23.1%、11.5%、11.5%和 7.7%。地表水痕量金属污染比地下水更严重,也高于 NCP 常见灌溉区。痕量金属具有地球成因和农业及工业活动的综合来源。除了一些奇异点外,它们的分布差异很大,与水流方向存在一定关系。水化学和环境同位素证据表明地表水-地下水相互作用影响研究区痕量金属的空间分布。面对持续严重的污染,迫切需要采取源头控制、改进控制技术和建立监测网以预警风险增加的管理措施。

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