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Nathan, Muhammad Dept. of Soil and Water 2001 http://hdl.handle.net/2440/109032 In the Herrmanns sub-catchment in the Mt. Lofty Ranges (near Mt. Torrens) soil sodicity was the dominant factor in causing clay to disperse in the eroded area along the foot slopes, wheras in non-eroded areas of the mid-slopes and on the stream banks, the dispersive power of sodicity was attenuated by the flocculative power of other soil properties. Thesis (M.Ag.Sc.) -- University of Adelaide, Dept. of Soil and Water, 2002 en Sodic soils; Soils, Salts in; Soils -- South Australia -- Lofty, Mount, Ranges, Region Clay movement in a saline-sodic soil toposequence Theses This electronic version is made publicly available by the University of Adelaide in accordance with its open access policy for student theses. Copyright in this thesis remains with the author. This thesis may incorporate third party material which has been used by the author pursuant to Fair Dealing exceptions. If you are the owner of any included third party copyright material you wish to be removed from this electronic version, please complete the take down form located at: http://www.adelaide.edu.au/legalsopen.access