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Effects of anions on the capacity and affinity of copper adsorption in two variable charge soils.

机译:阴离子对两种可变电荷土壤中铜吸附能力和亲和力的影响。

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Effects of nitrate (NO3-), chloride (Cl-), sulfate (SO42-), and acetate (Ac-) on Cu2+ adsorption and affinity of the adsorbed Cu2+ were evaluated in two Fe and Al enriched variable charge soils from Southern China. The maximum adsorption of Cu2+ (M, a parameter from the Langmuir isotherm model) in the presence of different anions decreased in the order Cl- > Ac- > NO3- > SO42- for both soils. The clayey loamy soil (mixed siliceous thermic Typic Dystrochrept, TTD), developed on the Arenaceous rock, adsorbed less Cu2+ than the clayey soil (kaolinitic thermic Plinthudults, KTP), derived from the Quaternary red earths, regardless of anion type present in the medium. The affinity of adsorbed Cu2+ to both soils could be characterized by the Kd (distribution coefficient) values and successive extraction of the adsorbed Cu2+ with 1-mol NH4Ac L-1. The log10Kd value was smaller for the TTD soil than for the KTP soil and decreased in the order of Cl- > NO3- > SO42- > Ac- at low initial Cu2+ concentrations (<=40 mg Cu2+ L-1), whereas at 80 mg Cu2+ L-1, the log10Kd value was similar for NO3-, SO4-2, and Ac-, but was slightly higher for Cl-. Complete extraction of Cu2+ adsorbed in the presence of Ac- was achieved. Influence of NO3- and SO42- on the affinity of adsorbed Cu2+ was similar, but the effects of Cl- depended on the initial Cu2+ concentrations. The extracted percentage of the adsorbed Cu2+ in the presence of NO3- or SO42- increased with increasing Cu2+ adsorption saturation. The presence of Cl-, NO3-, or SO42- markedly decreased the equilibrium solution pH for both soils with increasing initial Cu2+ concentrations, and the delta pH values at the highest Cu2+ level were 0.5, 0.63, and 0.55 U for the TTD soil and 0.79, 0.84, and 0.93 U for the KTP soil, respectively for the three anions. The presence of Ac- had a minimal influence on the equilibrium solution pH because of the buffering nature of the NaAc/HAc medium which buffered the released protons. The effects of anions on Cu2+ adsorption and affinity of the adsorbed Cu2+ were dependent on anion types and were apparently related to the altered surface properties caused by anion adsorption and/or the formation of anion-Cu2+ complexes..
机译:在中国南方的两种富含铁和铝的可变电荷土壤中,评估了硝酸盐(NO3-),氯化物(Cl-),硫酸盐(SO42-)和乙酸盐(Ac-)对Cu2 +吸附和吸附的Cu2 +亲和力的影响。对于两种土壤,在存在不同阴离子的情况下,Cu2 +的最大吸附(M,来自Langmuir等温线模型的参数)以Cl-> Ac-> NO3-> SO42-的顺序降低。黏土质壤土(混合的硅质热典型Typy Dyochochrept,TTD)在Arenaceous岩石上发育,吸附的Cu2 +比黏土(来自第四纪红土的高岭土质热土Plinthudults,KTP)少,而与介质中存在的阴离子类型无关。吸附的Cu2 +对两种土壤的亲和力都可以通过Kd(分布系数)值和用1-mol NH4Ac L-1连续萃取吸附的Cu2 +来表征。在较低的初始Cu2 +浓度(<= 40 mg Cu2 + L-1)下,TTD土壤的log10Kd值小于KTP土壤,且按Cl-> NO3-> SO42-> Ac-的顺序降低。以Cu2 + L-1为单位,NO3-,SO4-2和Ac-的log10Kd值相似,而Cl-的log10Kd值略高。在存在Ac-的情况下,可以完全提取所吸附的Cu2 +。 NO3-和SO42-对吸附的Cu2 +亲和力的影响相似,但Cl-的影响取决于初始Cu2 +浓度。在存在NO3-或SO42-的情况下,吸附的Cu2 +的提取百分比随Cu2 +吸附饱和度的增加而增加。随着初始Cu2 +浓度的增加,两种土壤中Cl-,NO3-或SO42-的存在均显着降低了平衡溶液的pH,而TTD土壤和最高Cu2 +水平下的δpH值分别为0.5、0.63和0.55U。 KTP土壤中的三种阴离子分别为0.79、0.84和0.93U。由于NaAc / HAc介质缓冲了释放的质子,因此Ac-的存在对平衡溶液pH的影响最小。阴离子对Cu2 +吸附和吸附的Cu2 +亲和力的影响取决于阴离子类型,并且显然与阴离子吸附和/或阴离子-Cu2 +络合物的形成引起的表面性能改变有关。

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