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首页> 外文期刊>Asian Journal of Chemistry: An International Quarterly Research Journal of Chemistry >Effect of Land Use on Adsorption and Fractionation of Copper in High Andean Andisols
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Effect of Land Use on Adsorption and Fractionation of Copper in High Andean Andisols

机译:土地利用对高安第斯山甲ls中铜的吸附和分离的影响

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The presence of high concentrations of copper in soil generates risk of entry into food chain, causing adverse effects. To elucidate its behaviour and prevent potential toxic risks in High Andean soils of Rio "Las Piedras"sub-basin, we assessed availability, the different chemical species of this metal and the adsorption-desorption phenomena occurring in soil phases. We estimated the effect of land use change from forest to crop and pasture on physical, chemical properties, the soil organic matter quality, adsorption phenomena and speciation of copper. In these soils highlights strong acidity, presence of allophanes, high content of organic carbon, high cationic exchange capacity, sandy-loam texture and low bulk density. Organic matter quality was estimated from humification degree determined by different humification index. Crop use change improves quality and increased humified organic matter, opposite effect occurred in pasture. Adsorption phenomenon of copper was evaluated by Freundlich adsorption isotherms, K values were 266.81 (forest), 1103.06 (crop) and 691.19 (pasture); n values corresponded to 1.40, 1.19 and 1.27, denoting change in retention strength as adsorption capacity. The colloidal complex of these soils is not saturated with copper in the dose range used (50-300 mg kg~(-1)). Improvement in soil organic matter quality causes increase on copper adsorption process. The chemical speciation of copper in this High Andean soils reveals predominance of fraction bound to organic matter. The mobility factor increases on pasture soil but decreases on crop soil.
机译:土壤中高浓度的铜存在进入食物链的风险,从而造成不利影响。为了阐明其行为并防止在“ Las Piedras”里约热内卢的安第斯高山土壤中发生潜在的毒性危险,我们评估了其有效性,该金属的不同化学种类以及在土壤相中发生的吸附-解吸现象。我们估计了从森林到作物和牧场的土地利用变化对物理,化学性质,土壤有机质,吸附现象和铜形态的影响。在这些土壤中突出显示出强酸度,存在Allophanes,高有机碳含量,高阳离子交换容量,沙壤土质地和低堆积密度。通过由不同的腐殖化指数确定的腐化度来估计有机物质量。作物使用方式的改变提高了品质,增加了腐殖质的有机质,而在牧场上则相反。用弗氏吸附等温线评估铜的吸附现象,K值为266.81(森林),1103.06(作物)和691.19(草场)。 n值对应于1.40、1.19和1.27,表示保留强度的变化为吸附容量。这些土壤的胶体复合物在所用剂量范围(50-300 mg kg〜(-1))中没有被铜饱和。土壤有机质的改善导致铜吸附过程的增加。在这种高安第斯山脉土壤中,铜的化学形态表明,与有机物结合的部分占主导地位。牧草土壤的迁移率增加,而农作物土壤的迁移率下降。

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