土壤砷的化学形态及其含量
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CHEMICAL FORMS AND CONTENT OF ARSENIC IN SOME SOILS OF CHINA
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    摘要:

    砷是自然界普遍存在的重要元素之一.砷的化合物一般具有毒性.土壤中砷是来源于成土母岩.岩石在风化过程中,原生矿物遭到分解,次生矿物不断形成,在这过程中,土壤从中得到砷的补给,并且大部分与Fe、Al、Ca等离子结合成难溶性砷化物.

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    In this paper chemical forms and content of soil arsenic are discussed based on analytical data of thirteen soil samples collected from ten provinces of China. Part of the procedures of fractionation of phosphorus in soil proposed by Chang and Jackson (1937 ) were adopted in the experiment for the separation of arsenic in soil. Forms of arsenic separated from the soils were adsorbed-, Al-, Fe-, Ca- and oceluded-arsenates. Analytical results showed that the contents oaf the five arsenates mentioned above in the total contents of arsenic of the soils were 0-21.3%,1.1-9.0%, 1.0-16.3%, 2.5-45.8% and 32.0-86.3% respectively. It was also revealed that chemical forms of soilarsenic and its contents seemed to be closely related to the geographical distribution of soil types. With the zonal distribution of the soils in China, the occluded-arsenate was gradually decreasing, but the adsorbed and Ca-arsenates were gradually increasing from the south to the north and from the east to the west.

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李勋官.土壤砷的化学形态及其含量[J].土壤学报,1982,19(4):360-366. Li Xun-guan. CHEMICAL FORMS AND CONTENT OF ARSENIC IN SOME SOILS OF CHINA[J]. Acta Pedologica Sinica,1982,19(4):360-366.

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  • 在线发布日期: 2013-02-25
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