ABSTRACT Prior to this study, phosphogypsum (PG) stockpiles at the Eshidiya mine in Jordan were thought to be potentially enriched with potentially toxic metals and radionuclides, resulting in possible environmental degradation of the surrounding ecosystem. In order to investigate this phenomenon, enrichment levels and distribution patterns of metals (e.g. Zn, Cd, V) and radionuclides in the underlying soils, alluvium, and yellow marl bedrock were determined and compared against those in the PG stockpiles. The 226 Ra, 210 Pb, and 238 U in soil reached peak concentrations of 1.5 pCi/g, 2.0 pCi/g, and 1.1 pCi/g, respectively. These elemental concentrations are similar to their concetrations in the uncontaminated soils, whereas the concentrations of these elements exhibit higher concentrations in PG and are as follows: 226 Ra= 18 pCi/g, 210 Pb= 19 pCi/g, and 238 U= 4 pCi/g . The elements Cd, Zn, and V have maximum concentrations of 3 mg kg −1 , 69 mg kg −1 and 62 mg kg −1 , respectively, in the soil9s layer. These elemental concentrations are relatively lower than in uncontaminated soil and the PG. The degrees of mobility of the determined elements in soils were classified into three categories: elements with high mobility are Se, Mn, Pb, and Cr; those with moderate mobility are Co, Ni, As, Hg, Cu, V, and Zn; and those with low mobility are U, Cd, 210 Pb, 226 Ra, and 238 U. Following correlation analysis, R-mode factor analysis was applied in conjunction with mineralogy to understand the geochemical variability of the soil. Four main meaningful factors were extracted: a detrital quartz factor, a clay minerals factor, a carbonate factor, and a terrigenous minerals factor. To investigate the spatial distribution patterns of the elements, a contour mapping technique was applied, allowing the following conclusions: (1) The elements 210 Pb, 226 Ra, and U exhibit similar distribution patterns; (2) Cd and Cu show similar distribution patterns; (3) As and V exhibit similar distribution patterns; and (4) no observed trend was observed for Cr. Generally, the results revealed that potentially toxic metals and radionuclides are not contaminated in soils related to the phosphogypsum stockpiles, and the soils of the Eshidiya area do not contain potentially toxic metals and radionuclide concentrations that threaten the surrounding ecosystem.
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