The nature of letsoku and related clayey soils, traditionally used by indigenous Southern
African communities for a wide range of purposes, was explored. Thirty-nine samples were
collected from Botswana, Lesotho, Swaziland, South Africa and Zimbabwe. They were
analysed to determine their composition and physical properties. Structured interviews were
used to establish the purpose of use and the location of sourcing sites. The samples were in the
form of either powder or rocks, and some were supplied as dry rolled clay balls. Cosmetic
applications were almost universally indicated. However, other functions, related to artwork,
medicinal use, cultural symbolism and traditional beliefs, were also mentioned. The samples
covered a wide range of colours from bright red to yellow, but also from off-white to black,
with some having a light grey colour. It was therefore not surprising that the mineral
composition of the letsoku samples also varied widely. A black sample, and the yellow and
reddish pastel-coloured samples, contained significant quantities of the corresponding, colourimparting
iron oxides. Clay minerals featured prominently, although kaolinite and muscovite
were more often encountered as the dominant minerals than smectites. All the samples
contained silica and in some instances the content exceeded 90 % m/m SiO2. The presence of
high contents (more than 40 % m/m) of gibbsite in the samples from Venda represents a new
finding for clayey soils in traditional usage. / Thesis (PhD)--University of Pretoria, 2017. / Chemical Engineering / PhD / Unrestricted
| Identifer | oai:union.ndltd.org:netd.ac.za/oai:union.ndltd.org:up/oai:repository.up.ac.za:2263/67817 |
| Date | January 2017 |
| Creators | Morekhure-Mphahlele, Refilwe |
| Contributors | Focke, Walter Wilhelm, u96276313@tuks.co.za |
| Publisher | University of Pretoria |
| Source Sets | South African National ETD Portal |
| Language | English |
| Detected Language | English |
| Type | Thesis |
| Rights | © 2018 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. |
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