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Alteration of the soil mantle by strip mining in the Namaqualand Strandveld

Thesis (MScAgric (Soil Science))--University of Stellenbosch, 2005.

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Main Author: Prinsloo, H. P.
Other Authors: Fey, M. V.
Format: Thesis
Language:English
Published: Stellenbosch : University of Stellenbosch 2008
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access_status_str Open Access
author Prinsloo, H. P.
author2 Fey, M. V.
author_browse Fey, M. V.
Prinsloo, H. P.
author_facet Fey, M. V.
Prinsloo, H. P.
author_sort Prinsloo, H. P.
collection Thesis
dc_rights_str_mv University of Stellenbosch
description Thesis (MScAgric (Soil Science))--University of Stellenbosch, 2005.
format Thesis
id oai:scholar.sun.ac.za:10019.1/1918
institution Stellenbosch University (South Africa)
language English
last_indexed 2026-06-10T12:43:27.297Z
license_str Other — see source repository
provenance_str_mv Harvested via OAI-PMH from SUNScholar — Stellenbosch University Repository
publishDate 2008
publishDateRange 2008
publishDateSort 2008
publisher Stellenbosch : University of Stellenbosch
publisherStr Stellenbosch : University of Stellenbosch
record_format dspace
source_str SUNScholar — Stellenbosch University Repository
spelling oai:scholar.sun.ac.za:10019.1/1918 Alteration of the soil mantle by strip mining in the Namaqualand Strandveld Prinsloo, H. P. Fey, M. V. Ellis, F. University of Stellenbosch. Faculty of Agrisciences. Dept. of Soil Science. Dissertations -- Soil science Theses -- Soil science Strip mining -- Environmental aspects -- South Africa -- Namaqualand Strip mining -- Environmental aspects -- South Africa -- Strandveld Plant-soil relationships -- South Africa -- Namaqualand Abandoned mined lands reclamation -- South Africa -- Namaqualand Soil science -- South Africa -- Namaqualand Soil management -- South Africa -- Namaqualand Botany -- South Africa -- Strandveld Thesis (MScAgric (Soil Science))--University of Stellenbosch, 2005. The purpose of this study was to investigate and identify the occurrence of specific soil properties that may be important for vegetation functioning and the possible effect of the loss of or changes in these properties on rehabilitation success on the sandy coastal plains of the West Coast, South Africa. The study area covered approximately 9 400 ha on the Namaqualand coast in the vicinity of Brand-se-Baai (31º18'S 17º54'E), approximately 350 km north of Cape Town and 70 km north-west of the nearest town, Lutzville. A soil survey was done to reveal the presence of important pedological features. The 20 soil profiles surveyed are situated within six vegetation communities. Pedological features such as surface water repellency, permeable apedal subsurface horizons, subsurface impediments such as cemented (calcrete or dorbank) hardpans and significantly more clayey (cutanic, luvic) horizons were identified. A comparative study between rehabilitated and natural soils indicates that mining operations result in the formation of saline sand tailings, stripped of a large portion of the clay and organic matter fraction. The natural leaching of solutes, over a period of 25 months, is sufficient to lower salinity of the tailings to levels comparable to natural soils. This leaching can also results in lowering of soil fertility. Removal of the dorbank and the dense neocutanic horizon in the western side of the mine, loss of topographical features such as small dune systems and heuweltjies, destruction of natural soil profile morphology and the lowering of organic carbon and clay plus silt fraction can have detrimental effects on attempts at rehabilitation of this area to a natural condition similar to that which preceded the mining operation. Infiltration fingering and deep percolation results in the development of an aquifer below the reach of shallow-rooted desert shrubs. A method of water acquisition by vegetation through water distillation is investigated as a possible solution to the apparent discontinuum between the shallow root systems and deeper-lying aquifer. Volumetric water content measurements indicated that precipitation of 29.5 mm, over a period of 10 days, did not result in any variation at 235 mm, 360 mm and 900 mm depths. An average volumetric water content increase of 0.4 mm per night was measured in the first 23.5 cm of soil surface. This amount is a significant source of water that can explain the shallow root distribution. Water vapour movement due to temperature gradients can explain the diurnal volumetric water content fluctuations observed. Further studies are necessary to determine to what extent the depth of water infiltration influences the capacity of subsurface dew to provide plants with a nocturnal water source. Findings of this study can be summarised into two concepts namely: • Heuweltjies, small dune systems, and variation in depth of cemented hardpans are the main features that contribute to pedosphere variation and possibly to biodiversity. • Pedogenic features such as topsoil hydrophobicity, and cemented dorbank and dense more clayey (cutanic, luvic) subsurface horizons are important components of a soil water distillation process that could be a driving force behind vegetation functioning in this region. Mine activities result in the loss of certain pedogenic features and soil properties that that could be key ingredients to ecosystem functioning. The inability to recognise their significance and ignorance thereof when planning rehabilitation methods might prevent sustainable restoration of the environment. Masters 2008-07-24T10:40:18Z 2010-06-01T08:36:37Z 2008-07-24T10:40:18Z 2010-06-01T08:36:37Z 2005-03 Thesis http://hdl.handle.net/10019.1/1918 en University of Stellenbosch application/pdf Stellenbosch : University of Stellenbosch
spellingShingle Dissertations -- Soil science
Theses -- Soil science
Strip mining -- Environmental aspects -- South Africa -- Namaqualand
Strip mining -- Environmental aspects -- South Africa -- Strandveld
Plant-soil relationships -- South Africa -- Namaqualand
Abandoned mined lands reclamation -- South Africa -- Namaqualand
Soil science -- South Africa -- Namaqualand
Soil management -- South Africa -- Namaqualand
Botany -- South Africa -- Strandveld
Prinsloo, H. P.
Alteration of the soil mantle by strip mining in the Namaqualand Strandveld
title Alteration of the soil mantle by strip mining in the Namaqualand Strandveld
title_full Alteration of the soil mantle by strip mining in the Namaqualand Strandveld
title_fullStr Alteration of the soil mantle by strip mining in the Namaqualand Strandveld
title_full_unstemmed Alteration of the soil mantle by strip mining in the Namaqualand Strandveld
title_short Alteration of the soil mantle by strip mining in the Namaqualand Strandveld
title_sort alteration of the soil mantle by strip mining in the namaqualand strandveld
topic Dissertations -- Soil science
Theses -- Soil science
Strip mining -- Environmental aspects -- South Africa -- Namaqualand
Strip mining -- Environmental aspects -- South Africa -- Strandveld
Plant-soil relationships -- South Africa -- Namaqualand
Abandoned mined lands reclamation -- South Africa -- Namaqualand
Soil science -- South Africa -- Namaqualand
Soil management -- South Africa -- Namaqualand
Botany -- South Africa -- Strandveld
url http://hdl.handle.net/10019.1/1918
work_keys_str_mv AT prinsloohp alterationofthesoilmantlebystripmininginthenamaqualandstrandveld