Difference of Soil Nutrient between Topsoil and Subsoil and its Influencing Factors

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Abstract:

Taking the representative alluvial plain of the Yellow River-Fengqiu county as example, difference of available K (AK), total (TK) and total (TP) between topsoil and subsoil and corresponding factors was studied. The result shows that average content of AK in topsoil is lower than it in subsoil, spatial variation of AK in topsoil is similar with it in subsoil. TK in topsoil shows more randomness than in subsoil. TP in topsoil has a stronger spatial correlation than in subsoil. The spatial distribution of TK and TP are quite consistent with landform in topsoil and subsoil, but AK does not have this trend. The difference of TK between two layers is related with surface deposit and irrigation condition. AK is mainly affected by surface deposit and farming intensity such as fertilization. The difference of TP is unrelated with elevation, the distance to the Yellow River, roads and water channel and residential areas.

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561-565

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December 2012

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© 2013 Trans Tech Publications Ltd. All Rights Reserved

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[1] Pu, Y.L., Xie, D.L., Qu, M., Yang, J. H (2010) Effects of land use and landscape position on soil nutrient in hilly region of Chongqing West. J. Journal of Soil and Water Conservation. 24(5): 1009-2242.

Google Scholar

[2] Zheng, B. J,. Wang, Z.F., Tan, X. L (2008) Effects of land use patterns on the physic-chemical properties of the soil profile in purple hilly areas. J. Journal of Southwest University (Natural Science Edition) 30(3): 101-106.

Google Scholar

[3] Liu, X. J., Xu, X. N., Chen, X. L (2009) Study on the content of four metal elements in different forest soil. J. Journal of Soil and Water Conservation 23(1): 127-131.

Google Scholar

[4] Bewket W., Stroosnijer L (2003) Effects of agroecological land use succession on soil properties in Chemoga watershed, Blue Nile basin, Ethiopia. J. Geoderma 111(1): 85-88.

DOI: 10.1016/s0016-7061(02)00255-0

Google Scholar

[5] Zhang, Q.Y., Li, F.D., Liu, M.Y. (2006) Effect of land use on soil properties in debris flow bottomland: A case study at Xiaojiang basin, Yunnan. J. Wuhan University Journal of Natural Sciences 11(4): 870-874.

DOI: 10.1007/bf02830179

Google Scholar

[6] T. M. Burgess, R. Webster (1980) Optimal interpolation and isarithmic mapping of soil properties. J. Journal of Soil Science 31(2): 315-331.

DOI: 10.1111/j.1365-2389.1980.tb02084.x

Google Scholar

[7] Qu, K.Y., Dai, L.M., Feng, H. M. (2009) Soil fertility characteristics of main forest types in easten mountain areas of Liaoning. J. Chinese Journal of Soil Science. 40: 558-562.

Google Scholar

[8] Shepherd, T.G., Saggar, S., Newman, R.H. (2001) Tillage-indued changes to soil structure and organic carbon fractions in New Zealand soil. J. Australian Journal of Soil Research. 39(3): 465-589.

DOI: 10.1071/sr00018

Google Scholar