首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Geochemical mapping in polluted floodplains using in situ X-ray fluorescence analysis, geophysical imaging, and statistics: Surprising complexity of floodplain pollution hotspot
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Geochemical mapping in polluted floodplains using in situ X-ray fluorescence analysis, geophysical imaging, and statistics: Surprising complexity of floodplain pollution hotspot

机译:使用原位X射线荧光分析,地球物理成像和统计数据的地球化学映射:洪泛区污染热点令人惊讶的复杂性

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This study is focused on a pollution hotspot in a floodplain impacted by uranium mining in the second half of the 20th century. To image the internal structure of the hotspot, we performed surface gamma activity mapping, in situ X-ray fluorescence spectroscopic analysis (XRF) using a portable instrument and manually obtained sediment cores, and electric resistivity imaging of the shallow subsurface with the help of electric resistivity tomography (ERT) and dipole electromagnetic profiling (DEMP). We used two approaches aimed at deciphering the origin of the pollution hotspot: (i) surface pollution mapping and (ii) identification of the deeper lying lithogenetic units. The description of the floodplain subsurface was supported by optically stimulated luminescence (OSL) dating. The surface mapping approach was found insufficient to visualise the hotspot and understand its origin. We recognised deposition non-linear in time (or temporally independent) of younger over-bank fines, including mining pollutants over considerably older channel sediments. Our work documents the value of dense geochemical mapping for documentation of fluvial pollution (accessible by portable XRF) as well as the need to understand the structure of the floodplain subsurface (accessible by electric resistivity imaging) and thereby rationalise the hotspot internal structure.
机译:本研究专注于20世纪下半叶由铀矿业影响的洪泛区的污染热点。为了以热点的内部结构,我们使用便携式仪器进行表面伽马活动映射,原位X射线荧光光谱分析(XRF),并手动获得沉积物芯,以及浅地下的电阻率成像在电动方面的帮助下电阻率断层扫描(ERT)和偶极电磁分析(DEMP)。我们使用了两种旨在破译污染热点的起源的方法:(i)表面污染映射和(ii)识别更深的躺线型岩性单位。通过光学刺激的发光(OSL)约会,支持泛洪平面地下的描述。发现表面映射方法不足以可视化热点并理解其起源。我们在更年轻的过境罚款中识别沉积非线性(或时间上独立),包括在相当较老的频道沉积物上采矿污染物。我们的工作记录了熔狼污染文件的密集地球化学映射的价值(便携式XRF可访问)以及了解泛洪平地下的结构(可通过电阻率成像可访问),从而合理化热点内部结构。

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