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张士灌区土壤中镉形态的探讨
引用本文:陈涛,吴燕玉,孔庆新,谭方.张士灌区土壤中镉形态的探讨[J].生态学报,1985,5(4):300-306.
作者姓名:陈涛  吴燕玉  孔庆新  谭方
作者单位:中国科学院林业土壤研究所 (陈涛,吴燕玉,孔庆新),中国科学院林业土壤研究所(谭方)
摘    要:本文研究了张士灌区土壤中镉的形态。交换态占78%,可给态占18%,不溶态和碱溶态只占3—4%。在田间酸性土壤中,Cl~-是无机配位体的主要成分。镉主要与Cl~-络合而形成CdCl]~-和CdCl_2。土壤中加入石灰和钙、镁、磷肥、HCO_3~-增多,镉与之生成Cd(HCO_3)_2沉淀。在长期淹水状况下,S~-增多,镉与S~-产生CdS沉淀,难以被水稻吸收。


STUDY ON CADMIUM FORMS IN SOILS IN ZHANG-SHI IRRIGATION AREA
Chen Tao.STUDY ON CADMIUM FORMS IN SOILS IN ZHANG-SHI IRRIGATION AREA[J].Acta Ecologica Sinica,1985,5(4):300-306.
Authors:Chen Tao
Institution:Institute of Forestry and Soil Science; Academia Sinica
Abstract:The forms of Cd in soils of Zhang-Shi Irrigation Area were reported in this paper. 78%of Cd existed in the soils is in exchangable form, 18%is in available form and only 3-4%is in insoluble form and in alkali-soluble form.In acid soils Cr is the major constituent of inorganic ligands which is incorporated with Cd to formCCdCl]-and CdCl2.In the case of adding limes and Ca-Mg-P fertilizers, the concentration of HCO3-in soils was increased and Cd(HCO3)2was formed and precipitated. In another case when the soil...
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