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Regularities of Cu, Pb and Zn adsorption by chernozems of the South of Russia

机译:俄罗斯南部黑钙土吸附铜,铅和锌的规律

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The parameters of Cu 2+ , Pb 2+ and Zn 2+ adsorption by chernozems of the south of Ru ssia and their particle - size fractions were studied. The adsorption capacity of chernozems for Cu 2+ , Pb 2+ , and Zn 2+ depending on the particle - size distribution decreased in the following sequence: clay loamy ordinary chernozem ~ clay loamy southern chernoz em loamy southern chern o zem loamy sandy southern chernozem. According to the parameters of the adsorption by the different particle - size fractions ( C max and k ), the heavy metal cations form a sequence analogous to that obtained for the entire soils: Cu 2+ ≥ Pb 2+ Zn 2+ . The parameters of the heavy metal adsorption by similar particle - size fractions separated from different soils decreased in the following order: clay loamy chernozem loamy chernozem loamy sandy chernozem. The r a tio between the content of exchangeable cations displaced from the soil adsorbing complex (SAC) into the solution and the content of adsorbed HMs decreased with the in creasing concentration of adsorbed HMs. These values could be higher (for Cu 2+ and Pb 2+ ), equal, or lo w er than 1 (for Zn 2+ ) and depend on the properties of HMs. At the first case, this was due to the diss o lution of readily soluble salts at low HM concentrations in the SAC. In the latter case, this was related to the adsorption of associated forms HMs and the formati on of new phases localized on the surface of soil particles at high HM conce n trations in the SAC.
机译:研究了俄罗斯南部黑钙土吸附Cu 2+,Pb 2+和Zn 2+的参数及其粒径分数。黑质对Cu 2+,Pb 2+和Zn 2+的吸附能力随颗粒大小的分布而降低,其顺序依次为:粘土壤土普通黑钙土〜粘土壤土南部黑钙土>壤质南部黑钙土>壤质沙土南部的黑黑石。根据不同粒径分数(C max和k)的吸附参数,重金属阳离子形成的序列类似于整个土壤所获得的序列:Cu 2+≥Pb 2+> Zn 2+。从不同土壤中分离出的相似粒度分数的重金属吸附参数按以下顺序降低:粘土壤土黑钙土>壤土黑钙土>壤土沙土黑钙土。从土壤吸附复合物(SAC)转移到溶液中的可交换阳离子的含量与吸附的HMs的含量之间的关系随着吸附的HMs浓度的增加而降低。这些值可能更高(对于Cu 2+和Pb 2+),等于或更低(对于Zn 2+),并且取决于HMs的特性。在第一种情况下,这是由于在SAC中以低HM浓度溶解了易溶盐。在后一种情况下,这与在SAC中高HM浓度下吸附相关形式的HM和在土壤颗粒表面定位的新相的形成有关。

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