Movement of Elements between Soil and its Source Rock a Case Form Limestone Soil in Suzhou City, Anhui Province, China

Song Chen

doi:10.4028/www.scientific.net/AMR.610-613.2904

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HomeAdvanced Materials ResearchAdvanced Materials Research Vols. 610-613Movement of Elements between Soil and its Source...

Movement of Elements between Soil and its Source Rock a Case Form Limestone Soil in Suzhou City, Anhui Province, China

Abstract:

The limestone soils and its source rock samples had been collected from Suzhou area for the testing about major and trace elements. The concentration value have been compared with the background and the migration coefficient(K) of element form source rock to soil have been calculated, the result showed: the elements Ca and Th are enrichment, the Al is loss seriously, the Ti, V, Cr, Mn, Zn, Rb, Sr., Zr, and Pb are basic fairly with the background value; the K, Cu, Fe and As are slightly higher than the soil background values; The elements Si, Ti, Mn, Zr, Pb and Th have high K in subsoil layer; the element Fe, Cr, As and Rb have the least K in subsoil layer; the element Al, V, Cu and Zn can be showed disorder with the more high migration coefficient in topsoil.

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Periodical:

Advanced Materials Research (Volumes 610-613)

Pages:

2904-2907

DOI:

https://doi.org/10.4028/www.scientific.net/AMR.610-613.2904

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Online since:

December 2012

Authors:

Song Chen

Keywords:

Limestone Soil, Movement of Element, Source Rock, Suzhou Area

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References

[1] X. L. Xu, S. Q. Dai and J. Y. Liu: Earth Science, Vol.30(2005),pp.168-176.

Google Scholar

[2] S. Q. Ni, Q. L. Hou and Y. W. Ju: Science China D: Earth science, Vol.39(2009),pp.488-496.

Google Scholar

[3] Chinese Environmental Protection Administration: Elemental background values of soils in China (Environmental Science Press of China,Beijing,1990)

Google Scholar

[4] G. L. Dongye, W. W. Zhao: Acta Pedologica Sinica, Vol.45(2008),P.876-880.

Google Scholar

[5] Y. M. Wen, S. Q. Zeng and S. R. Pan: Chinese Geographical Science,Vol.5(1995),pp.316-324.

Google Scholar