Soil Infiltration Characteristics under Different Land at Western Yunnan Plateau

Article Preview

Abstract:

On the basis of soil physical properties of three different land use types at western Yunnan plateau, the soil moisture infiltration characteristics in these three land use types were studied with the advanced double-rings method. The results showed that there were differences on soil bulk density, soil porosity, initial soil water infiltration rate and stable soil water infiltration rate. The bulk density of dry land is higher than that of forest land and grass land, which results in the physical properties and structure of forest land soil are better than those of non-forest land. For the initial infiltration, its order from high to low is forest land, dry land and grass land. Among different stands, it is showed that from the average infiltration rate and steady infiltration rate, its order from high to low was forest land, grass land and dry land.

You might also be interested in these eBooks

Info:

Periodical:

Advanced Materials Research (Volumes 884-885)

Pages:

694-697

Citation:

Online since:

January 2014

Export:

Price:

Permissions CCC:

Permissions PLS:

Сopyright:

© 2014 Trans Tech Publications Ltd. All Rights Reserved

Share:

Citation:

[1] Harden, C.P., Delmas Scruggs, P. Infiltration on mountain slopes: a comparison of three environments. Geomorphology, 55, 5–24(2003).

DOI: 10.1016/s0169-555x(03)00129-6

Google Scholar

[2] Ribolzi, O., Hermida, M., Karambiri, H., Delhoume, J.P., Thiombiano, L. Effects of aeolian processes on water infiltration in sandy Sahelian rangeland in Burkina Faso. Catena 67, 145–154(2006).

DOI: 10.1016/j.catena.2006.03.006

Google Scholar

[3] John D. Valiantzas. New linearized two-parameter infiltration equation for direct determination of conductivity and sorptivity[J]. Journal of Hydrology, 384(2): 1-13(2010).

DOI: 10.1016/j.jhydrol.2009.12.049

Google Scholar

[4] Philip J R. Hill slop infiltration divergent and convergent slops [J]. Water Resources Research, 27: 1035 1040(1991).

DOI: 10.1029/91wr00098

Google Scholar

[5] Fox, D.M., Bryan, R.B., Price, A.G. The influence of slope angle on final infiltration rate for interrill conditions. Geoderma 80, 18-194(1997).

DOI: 10.1016/s0016-7061(97)00075-x

Google Scholar

[6] Ninghu Su. Theory of infiltration: Infiltration into swelling soils in a material coordinate[J]. Journal of Hydrology, 395(1): 103-108(2010).

DOI: 10.1016/j.jhydrol.2010.10.019

Google Scholar

[7] Wang Guoliang, Liu Guobin, Zhou Shenglu. The effect of vegetation restoration on soil stable infiltration rates in small watershed of loess gully region[J]. Journal of Natural Resources, 18(5): 529-535(2003).

Google Scholar

[8] T.S. Moroke, O. Dikinya, C. Patrick. Comparative assessment of water infiltration of soils under different tillage systems in eastern Botswana[J]. Physics and Chemistry of the Earth, Parts A/B/C, Volume 34, Issues 4-5, 316-323(2009).

DOI: 10.1016/j.pce.2008.08.002

Google Scholar

[9] Carroll C, Merton L, Burger P. Impact o f vegetation cover and slope on runoff erosion, and water quality for field plots on a range of soil and spoil materials on central Queensland coal mines[J] . Australian Journal of Soil Research, 38( 2): 313-327(2000).

DOI: 10.1071/sr99052

Google Scholar

[10] Jiang Dingsheng. Soil erosion and governance model in Loess Plateau[M]. Beijing: China water conservancy and hydropower press, 27-44(1997).

Google Scholar