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A geochemical investigation of the Lake Sibiya system, Northern Zululand

Lake Sibaya (27°15'-21'25'S; 32°32'-32°44'E) is situated in the northern region of the Zululand coastal plain, and is remarkable in that it embodies a near-pristine· freshwater coastal lake preserving clear residual signs of its former estuarine origin. Despite the· fact that the lake constitutes pe...

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Main Author: Whyte, Stewart Rodney
Other Authors: Willis, James
Format: Thesis
Language:English
Published: Department of Geological Sciences 2016
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access_status_str Open Access
author Whyte, Stewart Rodney
author2 Willis, James
author_browse Whyte, Stewart Rodney
Willis, James
author_facet Willis, James
Whyte, Stewart Rodney
author_sort Whyte, Stewart Rodney
collection Thesis
description Lake Sibaya (27°15'-21'25'S; 32°32'-32°44'E) is situated in the northern region of the Zululand coastal plain, and is remarkable in that it embodies a near-pristine· freshwater coastal lake preserving clear residual signs of its former estuarine origin. Despite the· fact that the lake constitutes perhaps the most intensively studied of all freshwater bodies in South Africa, little is known .of its geochemical character. The objective of this study was therefore to conduct an investigation of the waters and sediments of the lake system, which might then provide a chemical baseline against which the future environmental quality of the system could be gauged, and in terms of which the current functioning of the ecosystem can be better understood. In line with this rationale, water and sediment samples were collected from each of fourteen sampling sites located along three transects running, variously, S-N, SW-NE and W-E across peripheral arms of the lake. Waters in direct contact with the sediments were thoroughly agitated with the sediments and thereafter decanted for analysis. Since the lake is purported to be fed almost exclusively by groundwater flow, water samples were collected from three groundwater . . wells located north-west of the lake. The Department of Water Affairs (DW AF) databases for groundwater chemistry, and for lake level and chemistry over the period 1980 to 1998, were used to supplement this data, and to provide an indication of any medium-term parameter changes. A water sample was also· collected from the non-perennial Mseleni River, although the river is known to contribute minimally to the lake volume. The majority of laboratory analyses were conducted within the Department of Geological Sciences at the University of Cape Town, adhering to standard analytical methods wherever possible.
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institution University of Cape Town (South Africa)
language eng
last_indexed 2026-06-10T12:33:01.081Z
license_str Not specified — see source repository
provenance_str_mv Harvested via OAI-PMH from UCTD — University of Cape Town Open Access Repository
publishDate 2016
publishDateRange 2016
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publisher Department of Geological Sciences
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spelling oai:open.uct.ac.za:11427/21695 A geochemical investigation of the Lake Sibiya system, Northern Zululand Whyte, Stewart Rodney Willis, James Fey, Martin V Environmental Geochemistry Lake Sibaya (27°15'-21'25'S; 32°32'-32°44'E) is situated in the northern region of the Zululand coastal plain, and is remarkable in that it embodies a near-pristine· freshwater coastal lake preserving clear residual signs of its former estuarine origin. Despite the· fact that the lake constitutes perhaps the most intensively studied of all freshwater bodies in South Africa, little is known .of its geochemical character. The objective of this study was therefore to conduct an investigation of the waters and sediments of the lake system, which might then provide a chemical baseline against which the future environmental quality of the system could be gauged, and in terms of which the current functioning of the ecosystem can be better understood. In line with this rationale, water and sediment samples were collected from each of fourteen sampling sites located along three transects running, variously, S-N, SW-NE and W-E across peripheral arms of the lake. Waters in direct contact with the sediments were thoroughly agitated with the sediments and thereafter decanted for analysis. Since the lake is purported to be fed almost exclusively by groundwater flow, water samples were collected from three groundwater . . wells located north-west of the lake. The Department of Water Affairs (DW AF) databases for groundwater chemistry, and for lake level and chemistry over the period 1980 to 1998, were used to supplement this data, and to provide an indication of any medium-term parameter changes. A water sample was also· collected from the non-perennial Mseleni River, although the river is known to contribute minimally to the lake volume. The majority of laboratory analyses were conducted within the Department of Geological Sciences at the University of Cape Town, adhering to standard analytical methods wherever possible. 2016-09-06T14:44:08Z 2016-09-06T14:44:08Z 1999 Master Thesis Masters MSc http://hdl.handle.net/11427/21695 eng application/pdf Department of Geological Sciences Faculty of Science University of Cape Town
spellingShingle Environmental Geochemistry
Whyte, Stewart Rodney
A geochemical investigation of the Lake Sibiya system, Northern Zululand
thesis_degree_str Master's
title A geochemical investigation of the Lake Sibiya system, Northern Zululand
title_full A geochemical investigation of the Lake Sibiya system, Northern Zululand
title_fullStr A geochemical investigation of the Lake Sibiya system, Northern Zululand
title_full_unstemmed A geochemical investigation of the Lake Sibiya system, Northern Zululand
title_short A geochemical investigation of the Lake Sibiya system, Northern Zululand
title_sort geochemical investigation of the lake sibiya system northern zululand
topic Environmental Geochemistry
url http://hdl.handle.net/11427/21695
work_keys_str_mv AT whytestewartrodney ageochemicalinvestigationofthelakesibiyasystemnorthernzululand
AT whytestewartrodney geochemicalinvestigationofthelakesibiyasystemnorthernzululand