Change of Trace Element Contents of Purple Soil in the Three Gorges Reservoir Region

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  • 1. College of Environment and Planning, Liaocheng University, Liaocheng, Shandong 252059;
    2. Department of Urban and Resources Sciences, Nanjing University, Nanjing, Jiangsu 210093

Received date: 2005-05-22

  Revised date: 2006-06-23

  Online published: 2006-09-20

Abstract

As a case study of purple soil on typical slope lands in the Three Gorges Reservoir region, this paper primarily explores trace element contents in purple soil and their changes under the different grades as well as the different land-use types. The result shows that the contents of Fe, Mn, Ni, Zr, Sr and Ti in purple soil in the Three Gorges Reservoir region are higher than the background values of purple soil (A layer) in China and the average value of all the soil (A layer) in Sichuan, that of Mo is very rich, but those of Zn and Pb are lower relatively than the ones of Sichuan and China. Contents of Pb, Cu and Co are decreasing along with grade increase among some grades. By contraries, the contents of Zr and Cr are increasing. The contents of Cu, Pb, Co, Ti, Zr, Ni, Cr, Sr, etc. in purple soil have some correlations with the changes of slope grades. Difference of trace element contents is remarkable between cultivated land and uncultivated land. The man-made activities are primary factors leading to the changes of trace element contents of purple soil in the Three Gorges Reservoir region.

Cite this article

DONG Jie, YANG Da-Yuan, ZHOU Bin, CHEN Ke-Feng, XU Qin-Mian . Change of Trace Element Contents of Purple Soil in the Three Gorges Reservoir Region[J]. SCIENTIA GEOGRAPHICA SINICA, 2006 , 26(5) : 592 -596 . DOI: 10.13249/j.cnki.sgs.2006.05.592

References

[1] 周天骧. 新疆哈密盆地土壤中微量元素的因子分析[J]. 地理科学, 1990, 10 (3):280~285.
[2] 朱颜明, 霍文毅, 陈定贵. 大兴安岭泥炭微量元素分布特征及其环境意义[J]. 地理科学, 1997, 17 (2):158~162.
[3] 陶澍, 曹军, 李本纲, 等. 深圳市土壤微量元素含量成因分析[J]. 土壤学报, 2001, 38 (2):248~255.
[4] 王冬艳, 许文良, 冯宏, 等. 吉林省西部草地土壤的化学元素含量及其特征研究[J]. 地理科学, 2002, 22 (6): 763~768.
[5] 王金达, 刘景双, 于君宝, 等. 沼生植物过渡金属元素含量季节变化特征——以三江平原典型湿地植物为例[J]. 地理科学, 2003, 23 (2):213~217.
[6] 刘光德, 李其林, 黄昀. 三峡库区面源污染现状与对策研究[J].长江流域资源与环境, 2003, 12 (5):462~466.
[7] 许峰, 蔡强国, 吴淑安, 等. 三峡库区坡地生态工程控制土壤养分流失研究[J]. 地理研究, 2000, 19 (3):303~310.
[8] 张芸, 朱诚, 于世永. 长江三峡大宁河流域3000年来的环境演变与人类活动[J]. 地理科学, 2001, 21 (3): 267~271.
[9] 范月娇. 基于遥感和GIS一体化技术的三峡库区土地利用变化研究[J]. 地理科学, 2002, 22 (5):593~597.
[10] 中国科学院成都分院土壤研究室. 中国紫色土(上篇)[M]. 北京:科学出版社, 1991. 1~340.
[11] 何毓蓉(主编). 中国紫色土(下篇)[M]. 北京:科学出版社, 2003. 1~406.
[12] 郑度,申元村. 坡地过程及退化坡地恢复整治研究——以三峡库区紫色土坡地为例[J]. 地理学报, 1998, 53 (2):116~122.
[13] 蔡强国, 吴淑安. 紫色土陡坡地不同土地利用对水土流失过程的影响[J]. 水土保持通报, 1998, 18 (2):1~8,35.
[14] 黄丽, 丁树文, 张光远, 等. 三峡库区紫色土坡地的耕作利用方式与水土流失初探[J]. 华中农业大学学报, 1998, 17 (1):45~49.
[15] 许峰, 蔡强国, 吴淑安. 等高植物篱在南方湿润山区坡地的应用——以三峡库区紫色土坡地为例[J]. 山地学报, 1999, 17 (3):193~199.
[16] 史志华, 蔡崇法, 丁树文, 等. GIS在三峡库区土壤肥力综合评价中的应用[J]. 土壤侵蚀与水土保持学报, 1999, 5 (1):74~78,96.
[17] 黄闰泉, 刘贵开, 袁传武, 等. 三峡库区坡面农林复合结构对土壤养分分布的影响[J]. 水土保持学报, 2000, 14 (3):41~45.
[18] 王玉宽, 文安邦, 张信宝. 长江上游重点水土流失区坡耕地土壤侵蚀的137Cs法研究[J]. 水土保持学报, 2003, 17 (2):77~80.
[19] 谭钦文, 尹黎明, 卢玉东, 等. 三峡库区紫色土陡坡耕地土壤侵蚀量预测模型研究[J]. 国土与自然资源研究, 2004, (1):19~21.
[20] 何太蓉, 姜洪涛, 杨达源, 等. 长江三峡库区现代坡地剥蚀速率研究[J]. 地理科学, 2004, 24 (1):89~93.
[21] 四川省丰都县地方志编纂委员会. 丰都县志[M]. 成都: 四川科技出版社, 1991. 47~65.
[22] 郉光喜, 朱建国. 土壤微量元素与稀土元素化学[M]. 北京: 科学出版社, 2003. 27~51.
[23] 魏复盛(主编). 中国土壤元素背景值[M]. 北京: 中国环境科学出版社, 1990. 87~493.
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