Hydropedology and Preferential Flow in the Tasmanian Texture-Contrast Soils-Reference-Cited by-同舟云学术

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Hydropedology and Preferential Flow in the Tasmanian Texture-Contrast Soils

Published:2013-10-18 Issue:4 Volume:12 Page:vzj2013.03.0051
ISSN:1539-1663
Container-title:Vadose Zone Journal
language:en
Short-container-title:Vadose Zone Journal

Author:

Hardie Marcus¹²,Doyle Richard¹²,Cotching William³,Holz Greg¹,Lisson Shaun¹⁴

Affiliation:

1. Tasmanian Institute of Agriculture; Hobart Tasmania 7001 Australia

2. School of Agricultural Science, Univ. of Tasmania; Sandy Bay Tasmania 7001 Australia

3. Tasmanian Institute of Agriculture, Univ. of Tasmania; Burnie Tasmania Australia

4. CSIRO Ecosystems Sciences; Univ. of Tasmania; Hobart Tasmania 7001 Australia

Publisher

Wiley

Subject

Soil Science

Link

http://onlinelibrary.wiley.com/wol1/doi/10.2136/vzj2013.03.0051/fullpdf

Reference81 articles.

1. Macropores and water flow in soils;Beven;Water Resour. Res.,1982

2. The formation of duplex soils on hillslopes in the Sydney Basin, Australia;Bishop;Geoderma,1980

3. Ferrolysis, a hydromorphic soil forming process;Brinkman;Geoderma,1970

4. Restricting layers, flow paths, and correlation between duration of soil saturation and soil morphological features along a hillslope with an altered soil water regime in western Victoria;Brouwer;Aust. J. Soil Res.,2002

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