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A new method to measure copper binding affinity of DOM and its application to soil solutions with DOM of varying quality

机译:一种测量DOM铜结合亲和力的新方法及其在不同品质中的土壤溶液中的应用

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Copper (Cu) complexation by dissolved organic matter (DOM) mobilises Cu in soils, but the role of DOM quality in this process is still not clarified. Differences in DOM quantity and quality (aromaticity, total DOM acidity and Cu mobilising potential, CuMP) were analysed in the soil solutions of thirteen uncontaminated topsoils. Solutions were obtained using different extraction methods, from soils incubated for different times. A one-step resin exchange method was developed to measure the CuMP (mmol Cu/kg DOC) of DOM at pCu 11.3 and pH 7.0, representative for conditions in neutral-pH uncontaminated soils. The CuMP varied tenfold and followed the order water extract >0. 01M CaCl<,2> extract > pore water. Soil solutions from soils kept dry for a long time or subjected to drying-wetting cycles had high dissolved organic carbon (DOC) concentrations with low DOM aromaticity and CuMP. Prolonged incubations decreased DOC concentrations and increased aromaticity and Cu affinity of DOM. A significant positive correlation between the specific UV-absorption (SUVA), indicating aromaticity, and CuMP was found for all DOM samples (R<'2>=0.58). For one soil, soil samples were taken from different depths and pore water was immediately extracted. The CuMP and SUVA of DOM was smallest for the solution of the deepest soil layer (40-60cm). It was concluded that both quantity and quality of DOM has to be taken into account when predicting Cu mobilisation in soils.
机译:溶解有机物(DOM)铜(Cu)络合在土壤中调动Cu,但仍未澄清DOM质量在该过程中的作用。在13个未污染的表土的土壤溶液中分析了DOM数量和质量(芳香性,总Dom酸度和Cu动员潜力,崩溃)的差异。使用不同的萃取方法获得溶液,从孵育不同时间孵育的土壤获得。开发了一种单级树脂交换方法以测量PCU 11.3和pH7.0的DOM的凹凸(Mmol Cu / kg Doc),代表中性-P-pH未污染土壤的条件。凹陷多样化,并随后秩序水提取物> 0。 01M CaCl <,2>提取物>孔隙水。来自土壤的土壤溶液长时间保持干燥或进行干燥润湿循环,具有高溶解的有机碳(DOC)浓度,具有低Dom芳香性和凹陷。延长孵育降低了DOC浓度和DOM的芳香性和Cu亲和力。针对所有DOM样品(R 1 2> = 0.58)发现特异性紫外线吸收(SUVA),表明芳香性和陷阱之间的显着正相关性。对于一块土壤,土壤样品取自不同的深度,并立即提取孔隙水。 DOM的凹槽和SUVA对于最深的土壤层(40-60cm)的溶液最小。结论是,在预测土壤中的Cu动员时,必须考虑DOM的数量和质量。

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