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SPATIAL—TEMPORAL VARIATION OF HEAVY METAL ELEMENTS CONTENT IN COVERING SPIL OF RECLAMATION AREA IN FUSHUN COAL MINE
引用本文:YUJun-bao LIUJing-shuang 等.SPATIAL—TEMPORAL VARIATION OF HEAVY METAL ELEMENTS CONTENT IN COVERING SPIL OF RECLAMATION AREA IN FUSHUN COAL MINE[J].中国地理科学,2002,12(3):268-272.
作者姓名:YUJun-bao  LIUJing-shuang
作者单位:ChangchunInstitueofGeography,theChineseAcademyofSciences,Changchun130012,P.R.China
摘    要:Grid method is employed for sampling covering soil at the test field,which is reclamation area filled by coal mining wastes for cropland in the Fushun coal mine,Liaoning Province,the Northeast China.The soil samples are taken at different locations,including three kinds of covering soil,three different depths of soil layers and four different covering ages of covering soil.The spatial-temporal variation of heavy metal element content in reclamation soil is stud-ied.The results indicate that the content of heavy metal elements is decreasing year after year,the determinant reason why the content of heavy metal elements at 60cm depth layer is higher than that at 30cm depth layer and surface is fertiliz-er and manure application;the metal elements mainly come from external environment;there is no metal pollution coming from mother material (coal mining wastes)in plough layer of covering soil.

关 键 词:土壤  重金属元素  时空分布  复垦  抚顺煤矿
收稿时间:30 May 2010

Spatial-temporal variation of heavy metal elements content in covering soil of reclamation area in fushun coal mine
Jun-bao Yu,Jing-shuang Liu,Jin-da Wang,Zhong-gen Li,Xue-lin Zhang.Spatial-temporal variation of heavy metal elements content in covering soil of reclamation area in fushun coal mine[J].Chinese Geographical Science,2002,12(3):268-272.
Authors:Jun-bao Yu  Jing-shuang Liu  Jin-da Wang  Zhong-gen Li  Xue-lin Zhang
Institution:(1) Key Laboratory of Marginal Sea Geology, Chinese Academy of Sciences, 510301 Guangzhou, GD, People’s Republic of China;(2) South China Sea Institute of Oceanology, Chinese Academy of Sciences, 510301 Guangzhou, GD, People’s Republic of China;(3) Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, 510640 Guangzhou, GD, People’s Republic of China;
Abstract:Grid method is employed for sampling covering soil at the test field, which is reclamation area filled by coal mining wastes for cropland in the Fushun coal mine, Liaoning Province, the Northeast China. The soil samples are taken at different locations, including three kinds of covering soil, three different depths of soil layers and four different covering ages of covering soil. The spatial-temporal variation of heavy metal element content in reclamation soil is studied. The results indicate that the content of heavy metal elements is decreasing year after year; the determinant reason why the content of heavy metal elements at 60cm depth layer is higher than that at 30cm depth layer and surface is fertilizer and manure application; the metal elements mainly come from external environment; there is no metal pollution coming from mother material (coal mining wastes) in plough layer of covering soil.
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