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https://hdl.handle.net/2440/91783
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DC Field | Value | Language |
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dc.contributor.author | Bald, M. | - |
dc.coverage.spatial | Kanmantoo Province, Mount Lofty Ranges, South Australia | en |
dc.date.issued | 2012 | - |
dc.identifier.uri | http://hdl.handle.net/2440/91783 | - |
dc.description | This item is only available electronically. | en |
dc.description.abstract | A soil profile exhibiting strong textural differentiation between surface and subsurface horizons at Keyneton, South Australia, was sampled for quantitative and qualitative analyses of the processes responsible for development. From constant resistant mineral ratios throughout the profile it was concluded that the soil had formed from uniform parent material, suggesting that pedological processes had heavily influenced formation. Particle size distribution, clay mineralogy determined by XRD, and microstructural features indicated that clay accumulation in the subsurface was accompanied by a greater intensity of weathering in the surface horizons. The presence of void argillans in the B horizon provided strong evidence for the translocation of clay. Mass balance calculations showed significant volumetric expansion and mass gain throughout the entire profile, but greatest in the B horizons. Al, Fe, Na and Si were all gained in large quantities. The results indicate that clay translocation by illuviation is a dominant process in the development of textural differentiation, with some clay likely to have formed in situ. | en |
dc.language.iso | en | en |
dc.subject | Honours; Geology; Alfisol; Natric Palexeralf; texture contrast soil; duplex; red-brown earth; pedogenesis; clay translocation; eluviation; illuviation; weathering; mass balance | en |
dc.title | Development of textural differentiation in soils: a quantitative analysis | en |
dc.type | Thesis | en |
dc.contributor.school | School of Physical Sciences | en |
dc.provenance | 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 author of this thesis and do not wish it to be made publicly available, or 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/legals | en |
dc.description.dissertation | Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical cinches, 2012 | - |
Appears in Collections: | School of Physical Sciences |
Files in This Item:
File | Description | Size | Format | |
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01frontGeoHon.pdf | Title page, abstract & contents | 184.27 kB | Adobe PDF | View/Open |
02wholeGeoHon.pdf | Whole thesis (as available) | 10.09 MB | Adobe PDF | View/Open |
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