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Using GIS to understand the environmental chemistry of manganese contaminated soils, Kgwakgwe area, Botswana

机译:使用GIS了解博茨瓦纳Kgwakgwe地区锰污染土壤的环境化学

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This study aimed at establishing the spatial distribution of manganese (Mn) and iron (Fe) within the periphery of a manganese oxide (Mn oxide) ore abandoned mine. Four hundred soil samples were obtained from a 4 km~2 area close to the Kgwakgwe Mn oxide ore abandoned mine, Kanye, South eastern Botswana. The determination of Fe and Mn concentrations after acid digestion of samples was performed on a Varian Spectra AA-220 FS atomic absorption spectrometer (Varian, Australia) equipped with a deuterium background correction. Laboratory results were processed using Geographical Information Systems (GIS), and Remote Sensing (RS) techniques with the integrated Land and Water Information System (1LWIS), Geosoft Oasis Montaj and ArcGIS software packages. Microsoft Excel was used for statistical and graphical presentation of data analyses. The range of concentration levels of Fe in soils was from 1116 μg g~(-1) to 870766 μg g~(-1) with a mean of 17593 μg g~(-1) and for Mn in soils was 35 μg g~(-1) to 24907 μg g~(-1) with a mean of 1088 μg g~(-1). The gridded soil maps for Fe and Mn show anomalies in different parts of the study area. Where Mn is high, the Fe is low and vice versa. Manganese was high at the mine workings and in the northwestern part of the study area. Iron on the other hand is very low in the mine working area and is high on the northern part of the study area. Suggestions are advanced for the Mn interplay in the soils and environment around the Kgwakgwe abandoned Mn oxides ore mine.
机译:这项研究旨在确定锰矿(Mn氧化物)矿石废弃矿井周边锰(Mn)和铁(Fe)的空间分布。从位于博茨瓦纳东南部坎耶的Kgwakgwe锰氧化物废弃矿山附近的4 km〜2区域中获得了400个土壤样品。样品酸解后,在配有氘背景校正的Varian Spectra AA-220 FS原子吸收光谱仪(澳大利亚瓦里安)上测定铁和锰的浓度。实验室结果使用地理信息系统(GIS)和遥感(RS)技术以及集成的土地和水信息系统(1LWIS),Geosoft Oasis Montaj和ArcGIS软件包进行处理。 Microsoft Excel用于数据分析的统计和图形表示。土壤中铁的浓度范围为1116μgg〜(-1)至870766μgg〜(-1),平均值为17593μgg〜(-1),土壤中的Mn为35μgg〜。 (-1)至24907μgg〜(-1),平均值为1088μgg〜(-1)。 Fe和Mn的栅格化土壤图显示了研究区域不同区域的异常。当Mn高时,Fe低,反之亦然。锰在矿山和研究区域的西北部含量很高。另一方面,铁在矿山的工作区域非常低,而在研究区域的北部则很高。提出了关于Kgwakgwe废弃的Mn氧化物矿山周围土壤和环境中Mn相互作用的建议。

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