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首页> 外文期刊>Applied and environmental soil science >In Situ Generated Colloid Transport of Cu and Zn in Reclaimed Mine Soil Profiles Associated with Biosolids Application
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In Situ Generated Colloid Transport of Cu and Zn in Reclaimed Mine Soil Profiles Associated with Biosolids Application

机译:与生物固体施用相关的矿山复垦土壤中铜和锌的原位胶体迁移

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摘要

Areas reclaimed for agricultural uses following coal mining often receive biosolids applications to increase organic matter and fertility. Transport of heavy metals within these soils may be enhanced by the additional presence of biosolids colloids. Intact monoliths from reclaimed and undisturbed soils in Virginia and Kentucky were leached to observe Cu and Zn mobility with and without biosolids application. Transport of Cu and Zn was observed in both solution and colloid associated phases in reclaimed and undisturbed forest soils, where the presence of unweathered spoil material and biosolids amendments contributed to higher metal release in solution fractions. Up to 81% of mobile Cu was associated with the colloid fraction, particularly when gibbsite was present, while only up to 18% of mobile Zn was associated with the colloid fraction. The colloid bound Cu was exchangeable by ammonium acetate, suggesting that it will release into groundwater resources.
机译:煤矿开采后被垦殖为农业用途的地区通常接受生物固体施用,以增加有机质和肥力。通过额外存在生物固体胶体,可以增强这些土壤中重金属的运输。从弗吉尼亚州和肯塔基州的经过开垦和未扰动的土壤中提取完整的块料,以观察使用和不使用生物固体的情况下铜和锌的迁移率。在开垦和未扰动的森林土壤中,溶液和胶体相关相中都观察到了铜和锌的迁移,未风化的弃土材料和生物固形物的存在促使溶液中的金属释放量增加。高达81%的活动性Cu与胶体部分有关,特别是当存在菱锰矿时,而只有高达18%的活动性Zn与胶体部分有关。胶体结合的铜可通过乙酸铵交换,表明它将释放到地下水资源中。

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