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黑土和棕壤对铜的吸附研究
引用本文:于颖,周启星,王新,任丽萍.黑土和棕壤对铜的吸附研究[J].应用生态学报,2003,14(5):761-765.
作者姓名:于颖  周启星  王新  任丽萍
作者单位:中国科学院沈阳应用生态研究所陆地生态过程重点实验室,沈阳110016
基金项目:国家杰出青年科学基金项目 ( 2 0 2 2 5 72 2 ),中国科学院知识创新重要方向项目 (KZCX2 SW 416),中国科学院沈阳应用生态研究所创新重大资助项目
摘    要:研究了黑土与棕壤对Cu吸附的热力学和动力学特性.结果表明,在实验所采用Cu^2+浓度范围内,黑土和棕壤对CU^2+的吸附量均随着加入Cu^2+浓度的增加而增加,但黑土对cu^2+的吸附固定能力明显高于棕壤.在吸附平衡液Cu^2+浓度为95mg·kg^-时,棕壤对cu^2+的吸附量接近3720mg·kg^-1,黑土对Cu^2+的吸附量高达6076mg·kg^-1,最大CuCl2浓度(400mg·kg^-1)时,黑土和棕壤对Cu^2+的吸附量分别达到6159.0和4736.6mg·kg^-1.两种土壤对Cu^2+的吸财等量线与Freundlich和Temkin方程均有较好的拟合性,可以用Freundlich方程对其吸附行为进行描述.Langmuir方程不适宜描述两种土壤对Cu^2+的等温吸附过程.黑土和棕壤对Cu^2+的吸附均较快,最初2min内就可以达到平衡后吸附量的90%以上,在15-20min左右吸附基本达到平衡.描述黑土和棕壤动力学过程的最优模型为双常数速率方程,其次为一级动力学方程和Elovich方程。

关 键 词:天山山地  土壤(类)重金属  污染评价  生态风险  多元统计  
文章编号:1001-9332(2003)05-0761-05
修稿时间:2002年9月27日

Cu adsorption by phaeozem and burazem
YU Ying,ZHOU Qixing,WANG Xin,REN Liping.Cu adsorption by phaeozem and burazem[J].Chinese Journal of Applied Ecology,2003,14(5):761-765.
Authors:YU Ying  ZHOU Qixing  WANG Xin  REN Liping
Institution:Key Laboratory of Terrestrial Ecological Process, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China. yyuhelen@hotmail.com
Abstract:Studies on the thermodynamics and kinetics of copper (Cu2+) adsorption by phaeozem and burozem showed that that the adsorption of Cu2+ by these two soils was increased with the increasing concentration of Cu2+ within the range of Cu2+ concentrations used in the experiment, but the amount of Cu2+ adsorbed and fixed on phaeozem was much higher than that on burozem. When the test Cu2+ concentration in adsorption equilibrium was 95 mg.kg-1, its adsorption by burozem was nearly 3720 mg.kg-1, whereas by phaeozem was as high as 6076 mg.kg-1. Under the highest CuCl2 treatment of 400 mg.kg-1, Cu2+ adsorbed by phaeozem and burozem was 6159.0 mg.kg-1 and 4736.6 mg.kg-1, respectively. The adsorption of Cu2+ by the test soils could significantly conform to the Freundlich and Temkin equation, while Langmuir equation was not applicable to describe the isothermal adsorption processes of Cu2+ by the two soils. The adsorption of Cu2+ by the test soils was very rapid, which could reach its balance after 15-20 min. The adsorption within the first 2 min at its beginning stage accounted for 90% of the Cu equilibrium adsorption. The adsorptive rate of Cu2+ by phaeozem was decreased more quickly than that by burozem with the time. The two-constant equation was the optimal model to describe the adsorption of Cu2+. The other models in point were first-order dynamic equations and Elovich equations, whereas parabolic diffusion equations were not suitable ones.
Keywords:Cu  Phaeozem  Burozem  Adsorption  Thermodynamics  Chemical kinetics  
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