Clay movement in a saline-sodic soil toposequence

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.

Author dc:creator

• Nathan, Muhammad

• Sodic soils; Soils, Salts in; Soils -- South Australia -- Lofty, Mount, Ranges, Region

Language dc:language.iso

en

Handle dc:identifier.uri

http://hdl.handle.net/2440/109032

OAI identifier oai:identifier

oai:digital.library.adelaide.edu.au:2440/109032