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Erosion phenomena on Round Island, Mauritius

Mini-dissertation (MSc)--University of Pretoria, 2015.

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Other Authors: Sumner, P.D. (Paul)
Format: Thesis
Language:English
Published: University of Pretoria 2015
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access_status_str Open Access
author2 Sumner, P.D. (Paul)
author_browse Sumner, P.D. (Paul)
author_facet Sumner, P.D. (Paul)
collection Thesis
dc_rights_str_mv © 2015 University of Pretoria. All rights reserved. The copyright in this work vests in the University of Pretoria. No part of this work may be reproduced or transmitted in any form or by any means, without the prior written permission of the University of Pretoria.
description Mini-dissertation (MSc)--University of Pretoria, 2015.
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institution University of Pretoria (South Africa)
language English
last_indexed 2026-06-10T12:39:29.036Z
license_str Other — see source repository
provenance_str_mv Harvested via OAI-PMH from UPSpace — University of Pretoria Institutional Repository
publishDate 2015
publishDateRange 2015
publishDateSort 2015
publisher University of Pretoria
publisherStr University of Pretoria
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spelling oai:repository.up.ac.za:2263/46214 Erosion phenomena on Round Island, Mauritius Sumner, P.D. (Paul) Boojhawon, Ravindra Bean, Tamsyn A. Round Island Erosion Mapping Soils Bullies UCTD Mini-dissertation (MSc)--University of Pretoria, 2015. Round Island is a 219 hectares islet north of the Mauritian mainland and has been classified as a Nature Reserve since 1957. The island has been subjected to human influence in the form of land degradation through introduced grazing animals (goats and rabbits) which has detrimentally affected the floral and faunal ecology of the island. Since the removal of the grazers, intensive conservation management has been undertaken to restore Round Island’s unique ecological status. The aim of this research project was to investigate erosion phenomena at specific study sites on Round Island through field-based classification and mapping procedures and describe physical soil characteristics. A modified version of the SARCCUS (1981) Erosion Classification system was used to classify linear erosion forms in the field, based on morphometric parameters. The effect of rock hardness was also assessed to determine lithological controls on bedrock-incised erosion features. Given the size of Round Island and the extensive nature of erosion, five study sites were chosen for the soil and erosion assessment. An additional two gully networks, ‘camp’ and ‘big’ gully were chosen to allow the investigation of an entire erosion system. Soils are thin and discontinuous, with a sandy texture and are poorly sorted. The Helipad habitat has the coarsest soils indicative of wind erosion where the deflation of fines leaves a coarser gravel pavement. No significant differences are found between sites for soil physical properties, with the exception of pH where the Summit has a significantly lower pH than the Helipad (Mann- Whitney U test, z= -2.21, p= 0.03) and Rock Slab (Mann- Whitney U test, z= -2.93, p< 0.01) habitat regions. No linear erosion forms are found on the soils of Round Island, however bedrock incised rills and gullies extensively occur. The Summit, Rock Slab and Palm Savannah habitats represent erosion processes along a profile gradient on the steep, convex western slope. The Summit habitat is subject predominantly to sheetwash and wind erosion, with the presence of two bedrock-incised rills of moderate severity. The Rock Slab region is predominated by parallel, shallow bedrock rills and gullies running downslope with moderate and slight severity, respectively. Soil and vegetation cover is highly variable within the region. Downslope, the Palm Savannah region is subject to moderate gully erosion with an irregular morphology. Soil is transported during rainfall within the gully channels where it is ultimately lost to sea. The two large gully systems, ‘camp’ and ‘big’ gully represent erosion of the highest severity on Round Island. The gullies have their starting points on the mid- upslope regions as rills, which increase in width and depth downslope, as indicated by decreasing width: depth ratios. The gullies have their end point at sea, both with a severity of very severe bedrock-gully erosion. During periods of intense rainfall the bedrock-incised gullies act as transport channels for sediment which is ultimately lost to sea. Little sediment is able to remain and this is exemplified by a lack of vegetation. This is a natural cycle where conservation efforts will remain ineffective. In addition to morphology, rock hardness was assessed using a Schmidt Hammer for the bedrock incised forms. The rate of erosion of the bedrock dominated channels depends on various factors such as rock strength, sediment supply and grain size. The predominant rock type on Round Island is tuff which is a relatively weak volcanic rock, as indicated by low mean Schmidt Hammer R-values, implicating higher expected bedrock erosion rates. tm2015 Zoology and Entomology MSc Unrestricted 2015-07-02T11:07:18Z 2015-07-02T11:07:18Z 2015/04/22 2015 Mini Dissertation Bean, TA 2015, Erosion phenomena on Round Island, Mauritius, MSc Mini-dissertation, University of Pretoria, Pretoria, viewed yymmdd <http://hdl.handle.net/2263/46214> A2015 http://hdl.handle.net/2263/46214 en © 2015 University of Pretoria. All rights reserved. The copyright in this work vests in the University of Pretoria. No part of this work may be reproduced or transmitted in any form or by any means, without the prior written permission of the University of Pretoria. application/pdf University of Pretoria
spellingShingle Round Island
Erosion
Mapping
Soils
Bullies
UCTD
Erosion phenomena on Round Island, Mauritius
title Erosion phenomena on Round Island, Mauritius
title_full Erosion phenomena on Round Island, Mauritius
title_fullStr Erosion phenomena on Round Island, Mauritius
title_full_unstemmed Erosion phenomena on Round Island, Mauritius
title_short Erosion phenomena on Round Island, Mauritius
title_sort erosion phenomena on round island mauritius
topic Round Island
Erosion
Mapping
Soils
Bullies
UCTD
url http://hdl.handle.net/2263/46214