首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Effects of waterlogging on the solubility of antimony and arsenic in variously treated shooting range soils
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Effects of waterlogging on the solubility of antimony and arsenic in variously treated shooting range soils

机译:涝渍对锑和砷的溶解度,各种处理射击射游土壤

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摘要

This study examined a release of two metalloids: Sb and As into pore water from five shooting range soils under oxidized and waterlogged conditions, in a 140-day incubation experiment. The total concentrations of Sb and As in soils were in the ranges: 4.15-89.6 and 2.23-9.22 mg kg(-1), respectively. Soils were treated with green waste compost and deferrisation sludge prior to incubation. Additionally, the effects of treatment with acid and lime were examined. Pore water was collected 5 times with MacroRhizon suction samplers and examined on Sb and As concentrations. Antimony speciation in pore water involved Sb(III) and Sb(V) which were assayed by ICP-MSHCLP. Additionally, five operationally defined fractions of Sb and As in soil solid phase were determined by sequential extraction before and after incubation. Data showed that waterlogging considerably reduced final Sb concentrations in pore water, irrespectively of the kind of pre-treatment, except for a temporal increase in Sb solubility in two soils. On the contrary, As was usually more intensively released under anoxic conditions, particularly from compost-treated soils. The concentrations of Sb(III) were negligible in pore water of oxidized soils, while their share in pore water of waterlogged soils was considerable and tended to increase with prolonged incubation. The highest concentrations of Sb(III) in pore water were found in waterlogged acid-treated soils, and also in limed soils. The mechanisms involved in the changes of Sb and As solubility were discussed. Sequential extraction did not provide satisfactory results consistent with hypothesized processes running in waterlogged soils.
机译:本研究检测了两种金属氢化物:Sb,在氧化和涝渍条件下,来自五个拍摄范围土壤的孔隙水,在140天的孵育实验中。 Sb的总浓度和土壤中的总浓度分别为:4.15-89.6和2.23-9.22 mg kg(-1)。在孵育之前,用绿色废物堆肥和脱气污泥​​处理土壤。另外,检查了处理与酸和石灰的影响。用大火凹吸样器收集孔隙水5次,并在Sb上检查和浓度。孔隙水中的锑形态涉及通过ICP-MSHCLP测定的Sb(III)和Sb(V)。另外,通过在孵育之前和之后序列提取来确定五个可操作定义的Sb和土壤固相的级分。数据显示,除了在两种土壤中的Sb溶解度的时间增加外,水涝可显着降低孔隙水中的最终Sb浓度。相反,正如在缺氧条件下更强烈地释放,特别是从堆肥处理的土壤中释放。氧化土的孔隙水中的Sb(III)的浓度可忽略不计,而其在涝渍土的孔隙水中的份额相当可观,并且随着延长孵育而增加。在含水酸处理的土壤中发现孔隙水中的最高浓度的Sb(III),也发现了含有含量的酸性土壤。讨论了SB变化和溶解度的机制。顺序提取没有提供令人满意的结果,这与涝渍土中的假设工艺一致。

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