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SORPTION AND DESORPTION CHARACTERISTICS OF CADMIUM BY FOUR DIFFERENT SOILS IN NORTHEAST CHINA
作者姓名:ZHANG  Lei  SONG  Feng-bin
作者单位:1. Northeast Institute of Geography and Agricultural Ecology,Chinese Academy of Sciences,Changchun 130012,P. R. China; 2. The Graduate School of Chinese Academy of Sciences,Beijing 100039,P. R. China
基金项目:Under the auspices of the K ey Projectof K now ledge Innovation Program of C hinese A cadem y of Sciences (N o.K ZC X 1-SW -19)
摘    要:1IN TR O D U C TIO NA s a persistentand toxic pollutant, cadm ium (C d) canresultin m any adverse health effects in a variety oftis-suesand organssuch asthe lung,kidney,urinary,blad-der,pancreas,breast and prostate (SA TA R U G etal.,2003).C adm ium in so…

关 键 词:中国  东北地区  土壤化学    吸附作用  土壤污染
文章编号:1002-0063(2005)04-0343-05
收稿时间:2005-05-20

Sorption and desorption characteristics of cadmium by four different soils in northeast China
ZHANG Lei SONG Feng-bin.SORPTION AND DESORPTION CHARACTERISTICS OF CADMIUM BY FOUR DIFFERENT SOILS IN NORTHEAST CHINA[J].Chinese Geographical Science,2005,15(4):343-347.
Authors:Zhang Lei  Song Feng-bin
Institution:(1) Northeast Institute of Geography and Agricultural Ecology, Chinese Academy of Sciences, 130012 Changchun, P. R. China;(2) The Graduate School of Chinese Academy of Sciences, 100039 Beijing, P. R. China
Abstract:Four soils, phaeozem (PM), saline-alkali soil (SA), meadow albic bleached soil (MA) and dark brown forest soil (DB) from Northeast China were used to examine the sorption and desorption characteristics of Cd and pH influence on it. According to sorption experiment without pH control, the order of amount of absorbed Cd by soils was: SA>PM>DB>MA. The results from non-linear fitting method showed that Langmuir and Freundrich models were more adaptable than Temkin model in describing the sorption data. The maximum sorption amounts from Langmuir model were: PM>SA>MA>DB. Exponential equation for PM and SA and quadratic equation for MA and DB were suitable to fit the desorption data. The order of average desorption percentage was: MA>DB>PM>SA. The amounts of sorption by PM, DB and MA reached the maximum in pH 9.0, while sorption by SA was linearly increased in the experimental range of pH 3.3-11.4. In uniform pH, however, Cd sorption by SA was the minimum among four soils, which indicated that the more amounts of Cd absorbed by SA in isotherm sorption were ascribed to the higher soil pH. The higher sorption of Cd in PM resulted from the higher percentage of organic matter and clay components.
Keywords:cadmium  soil  sorption  desorption  Northeast China
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