Mineralogical impact on the compaction of residual gabbro soils in the construction of Platinum Tailings Storage Facilities

dc.contributor.advisorDippenaar, Matthys Alois
dc.contributor.emailjase.tunnell@gmail.comen_US
dc.contributor.postgraduateTunnell, Jason
dc.date.accessioned2024-07-11T10:02:32Z
dc.date.available2024-07-11T10:02:32Z
dc.date.created2024-09-01
dc.date.issued2023-12-05
dc.descriptionDissertation (MSc (Engineering Geology))--University of Pretoria, 2023.en_US
dc.description.abstractOver the past decade, there have been 45 tailings storage facility (TSF) disasters worldwide, resulting in fatalities, serious environmental damage, and the destruction of entire ecosystems. These failures often stem from substandard design or operational practices. Many TSFs are constructed in regions associated with intrusive mafic rocks such as gabbro, norite, pyroxenite, and anorthosite, which are commonly found alongside platinum group metals in areas like the Bushveld Igneous Complex in South Africa and the Great Dyke in Zimbabwe. The stability of these structures can be significantly influenced by the residual soils present at the construction sites. Residual soils, both cohesive and non-cohesive, contain varying quantities of different minerals, which can impact the compaction characteristics and, consequently, the stability of the TSF foundations. Cohesive soils rich in clay minerals, such as kaolinite and smectite, exhibit properties that can hinder effective soil compaction. The expansive nature of smectite due to its ability to absorb large amounts of water and host free exchangeable cations, counteracts the compaction process, reducing soil stability. Soil compaction is a complex process influenced by several factors, including compaction effort, method, water content, particle size distribution, and mineralogy. This study aimed to analyse these factors using a series of laboratory tests, including foundation indicators, MOD AASHTO compaction testing, and X-ray diffraction analysis, on residual soils from two TSF construction sites. The findings revealed that soils with high clay content tend to retain more water and have a higher optimum water content, adversely affecting their compaction properties. This study highlights the critical need to consider the mineralogical composition and weathering effects of residual soils in the design and construction of TSFs. By improving our understanding of these factors, we can enhance the stability of TSF foundations, reducing the likelihood of future failures. The insights gained from this research highlight the importance of thorough geotechnical assessments in the successful design and maintenance of TSF’s.en_US
dc.description.availabilityUnrestricteden_US
dc.description.degreeMSc (Engineering Geology)en_US
dc.description.departmentGeologyen_US
dc.description.facultyFaculty of Natural and Agricultural Sciencesen_US
dc.description.sdgSDG-09: Industry, innovation and infrastructureen_US
dc.identifier.citation*en_US
dc.identifier.doi10.25403/UPresearchdata.26236304en_US
dc.identifier.otherS2024en_US
dc.identifier.urihttp://hdl.handle.net/2263/96932
dc.language.isoenen_US
dc.publisherUniversity of Pretoria
dc.rights© 2023 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.
dc.subjectUCTDen_US
dc.subjectSustainable Development Goals (SDGs)en_US
dc.subjectMinerologyen_US
dc.subjectGreat Dyke
dc.subjectIgneous Bushveld Complex
dc.subjectTailings
dc.subjectMineralogical impact
dc.subject.otherSDG-09: Industry, innovation and infrastructure
dc.subject.otherNatural and agricultural sciences theses SDG-09
dc.titleMineralogical impact on the compaction of residual gabbro soils in the construction of Platinum Tailings Storage Facilitiesen_US
dc.typeDissertationen_US

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