通过对弗罗茨瓦夫(波兰西南部)维达瓦河的化学和同位素研究证明河流在限制污染移动方面的作用

IF 2.6 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Chemie Der Erde-Geochemistry Pub Date : 2023-09-01 DOI:10.1016/j.chemer.2023.125975
Marta Trałka , Marek Błachowicz , Marta Jakubiak
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引用次数: 0

摘要

本文介绍了对浅层地下水和地表水进行化学和同位素研究的结果,以确定人工灌溉区附近的污染程度。该研究采用了在河流周围详细取样的方法,以捕捉污染物流向并确定环境状况。在河道两侧、河底和河道直接取样。通过对河底压力的测量,可以确定河水在哪一段排入或渗入地下水,再结合化学和同位素分析,就可以确定这项研究的目的。结果表明,研究区域的河流性质主要是中性的,其次是排水性的,但这并不意味着每个点的地下水污染程度。由于采用了取样方法,还可以确定氧化还原过程的深度和水中硫的来源,硫主要来自降水和其他人为来源。化学测试表明,浅层地下水的水质一般,根据测量点的位置不同,人为改造的程度也不同。这些初步结果证明这种取样方法适用于其他研究,并表明有必要进行更详细的化学分析。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

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Role of rivers in restricting pollution movement, as evidenced by chemical and isotopic research on the Widawa River in Wrocław (SW Poland)

This article presents results of chemical and isotopic studies of shallow groundwater and surface waters in order to determine the degree of their contamination near to artificial irrigation fields. The study applied the methodology of detailed sampling around the river in order to capture the direction of pollutant flow and to determine the state of the environment. Samples were taken on both sides of the river, from its bottom and directly from the river. Thanks to bottom pressure measurements, it was possible to determine in what section the river drains or infiltrates groundwater, which, combined with chemical and isotope analyses, made it possible to determine the aims of this study. As it turns out, the nature of the river in the study area is mainly neutral and in lesser extent draining, which does not translate into the degree of groundwater pollution at every point. Due to the sampling methodology used, it was also possible to determine the depth of redox processes and the origin of sulfur in water, which comes mainly from precipitation and other anthropogenic sources. Chemical tests indicate an average quality of shallow groundwater, anthropogenically transformed to varying degrees depending on the location of measurement point. These preliminary results support the applicability of this sampling methodology to other studies and indicate the need to perform more detailed chemical analysis.

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来源期刊
Chemie Der Erde-Geochemistry
Chemie Der Erde-Geochemistry 地学-地球化学与地球物理
CiteScore
7.10
自引率
0.00%
发文量
40
审稿时长
3.0 months
期刊介绍: GEOCHEMISTRY was founded as Chemie der Erde 1914 in Jena, and, hence, is one of the oldest journals for geochemistry-related topics. GEOCHEMISTRY (formerly Chemie der Erde / Geochemistry) publishes original research papers, short communications, reviews of selected topics, and high-class invited review articles addressed at broad geosciences audience. Publications dealing with interdisciplinary questions are particularly welcome. Young scientists are especially encouraged to submit their work. Contributions will be published exclusively in English. The journal, through very personalized consultation and its worldwide distribution, offers entry into the world of international scientific communication, and promotes interdisciplinary discussion on chemical problems in a broad spectrum of geosciences. The following topics are covered by the expertise of the members of the editorial board (see below): -cosmochemistry, meteoritics- igneous, metamorphic, and sedimentary petrology- volcanology- low & high temperature geochemistry- experimental - theoretical - field related studies- mineralogy - crystallography- environmental geosciences- archaeometry
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