摘要
为了探讨土壤粘粒表面Pb2+吸附-解吸的不可逆性特征,采用一次平衡法研究了陕西4种土壤粘粒对Pb2+的吸附和解吸特征。结果表明,在恒定pH条件下,残留吸附常数Kd与吸附常数Ka的比值称为吸附-解吸的不可逆性特征参数,Kd/Ka=1,表示吸附-解吸过程是可逆的;Kd/Ka≠1,表示该过程不可逆;在不同解吸溶液中,供试土壤粘粒表面Pb2+Kd/Ka值由大到小依次表现为N aNO3、草酸、柠檬酸,不可逆程度大小与此相同。在不同pH条件下,供试土壤粘粒表面Pb2+络合常数log Kiant与解吸常数log Kidnt的比值也可作为过程不可逆性特征参数;在不同介质中,其绝对值由大到小依次为N aNO3、柠檬酸、草酸,不可逆程度大小与此相反。
In order to investigate the irreversibility of the adsorption and desorption of Pb^2+ on soil clays,one equilibrium method was used to study the characteristics of the adsorption and desorption of Pb^2+ on soil clays in Shaanxi. The results were that the ratio of residual adsorption constant Kd to adsorption constant Ka was defined as the irreversible parameter of adsorption-desorption for Pb^2+ on the soil clay. If Kd/Ka= 1 ,the process of adsorption and desorption was reversible. If Kd/Ka≠1 ,the process of adsorption and desorption was irreversible. The ratio Kd/Ka of soil clays showed the feature of NaNO3〉oxalic acid〉citric acid at a constant pH,the irreversible degree showed the same sequence. So,concerning pH, the ratio of log K^intd/log Kinta (the intrinsic desorption constant/surface intrinsic complexation constant) Pb^2+ on soil clays was defined as the parameter of irreversible,the ratio showed NaNO3〉 citric acid〉 oxalic acid in different mediums ,the irreversible degree was just the opposite.
出处
《西北农林科技大学学报(自然科学版)》
CSCD
北大核心
2007年第1期127-132,共6页
Journal of Northwest A&F University(Natural Science Edition)
基金
西北农林科技大学重点专项基金项目