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首页> 外文期刊>Geochemistry: Interdisciplinary Journal for Chemical Problems of the Geosciences and Geoecology >Screening of residual contamination at a former uranium heap leaching site,Thuringia,Germany
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Screening of residual contamination at a former uranium heap leaching site,Thuringia,Germany

机译:在德国图林根州一个以前的铀堆浸场中残留污染物的筛选

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Uranium mining in the former German Democratic Republic was extensive during the period 1946-1990 with a total production of over 200 kt of uranium.About half of the uranium production originated from the Ronneburg operations and heap leaching at the Gessenhalde site,where low-grade black shale uranium ores were leached,in operation in 1970-1989.The area is remediated since the mid-nineties but residual contamination is still seen as exemplified by the effects on vegetation.The purpose of this study is to provide general information about residual contamination and its soil and water geochemistry.Uppermost,in the investigated area,is sandy loam(10-30% loam)overlaying glacial clay that may have a thickness of several meters.On top of the glacial clay a perched groundwater table can be found.Soil was sampled in a grid layout pattern down to the glacial clay and water samples from the perched groundwater table have been collected(0.22mum filter size).Soil concentrations were found to be elevated for V,Cr,Cd,Ni,Cu,Zn,As,Mo,W,Th,U,and Cd when comparing the average and median values with the content for a typical soil,derived from periglacial sediments of(sandy)loam in Saxony.Iron precipitates are extensive and a hardpan is present in the unsaturated zone and identified by X-ray diffraction(XRD)as goethite.The goethite is presumed to be the main scavenger of metals at the site.The hardpan is enriched,compared to the "normal" soil of the area,with regard to elements present as sulphides in the black shales;the elements Cd,Ni,As,and U were preferentially enriched in the hardpan.Two different types of samples could be distinguished using Zr normalization.This was interpreted as soil with more or less extensive Fe precipitation.Dissolved Fe concentration is in most cases low,an indication that the Fe precipitates are stable under the current environmental conditions.Water concentrations for many elements(e.g.Ni,Cu,Zn,Al,F,Pb,and U)strongly correlated with decreasing pH.In the future,the situation in this area with regard to soil and water contamination will improve due to the ongoing wash out and the limited pool of residual contaminants.
机译:在1946年至1990年期间,前德意志民主共和国的铀矿开采十分广泛,铀的总产量超过200 kt。铀产量的大约一半来自Ronneburg矿场和Gessenhalde矿场(低品位)的堆浸黑页岩铀矿浸出后于1970-1989年投入运行。该地区自90年代中期开始得到修复,但残留污染仍被视为对植被的影响。本研究的目的是提供有关残留污染的一般信息在研究区域的最上方是砂壤土(10-30%壤土)覆盖的冰川黏土,厚度可能为几米。在冰川黏土的顶部可以找到栖息的地下水位。以网格布局的方式取样土壤,直至冰河粘土,并从栖息的地下水位收集了水样(0.22微米滤池尺寸)。当比较平均值和中位数与典型土壤(由砂质壤土的冰川沉积物衍生)的含量进行比较时,对V,Cr,Cd,Ni,Cu,Zn,As,Mo,W,Th,U和Cd进行征收在萨克森州,铁沉淀物大量存在,并且在非饱和区中存在硬盘,并通过X射线衍射(XRD)鉴定为针铁矿。该针铁矿被认为是该部位的主要金属清除剂。相对于该地区“正常”土壤,在黑色页岩中以硫化物形式存在; Cd,Ni,As和U元素在硬质岩中优先富集。通过Zr归一化可以区分两种不同类型的样品这被解释为具有或多或少的大量Fe沉淀物的土壤。在大多数情况下,溶解的Fe浓度很低,表明在当前环境条件下,Fe沉淀物是稳定的。许多元素(如Ni,Cu,Zn, Al,F,Pb和U)与pH值降低密切相关。未来,由于持续的冲洗和残留污染物的数量有限,该地区土壤和水污染的状况将得到改善。

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