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The fracture and autogenous comminution of quartzite

Bibliography: p.103-116.

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Bibliographic Details
Main Author: Kanellopoulos, Achilles Constantine
Other Authors: Ball, Anthony
Format: Thesis
Language:English
Published: Centre for Materials Engineering 2016
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access_status_str Open Access
author Kanellopoulos, Achilles Constantine
author2 Ball, Anthony
author_browse Ball, Anthony
Kanellopoulos, Achilles Constantine
author_facet Ball, Anthony
Kanellopoulos, Achilles Constantine
author_sort Kanellopoulos, Achilles Constantine
collection Thesis
description Bibliography: p.103-116.
format Thesis
id oai:open.uct.ac.za:11427/18008
institution University of Cape Town (South Africa)
language eng
last_indexed 2026-06-10T12:35:29.805Z
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
publishDateSort 2016
publisher Centre for Materials Engineering
publisherStr Centre for Materials Engineering
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source_str UCTD — University of Cape Town Open Access Repository
spelling oai:open.uct.ac.za:11427/18008 The fracture and autogenous comminution of quartzite Kanellopoulos, Achilles Constantine Ball, Anthony Materials Engineering Bibliography: p.103-116. Comminution is the process which aims at increasing the surface area and the resultant liberation of a particular constituent from the mass of a solid. The autogenous mill uses tumbling to effect comminution, but instead of special milling bodies being added, pebbles of the material to be comminuted are used. The autogenous comminution process utilises less than 0,1 per cent of the energy input. The principal objective of the present work was to analyse autogenous milling behaviour in terms of the individual comminuting mechanisms and to establish the inter-relationships between the main process variables, namely rock petrography, size distribution of the feed, applied load, relative velocity and environment. In this manner the optimisation of the process and an improvement of its efficiency was sought. In addition the establishment of testing procedures to predict the autogenous milling behaviour of a given type of rock was aimed. In the present work the gold bearing Witwatersrand quartzite was used, although the findings are applicable to other types of rocks. Since fracture phenomena are involved in all comminuting mechanisms of impact-compression, chipping and abrasion, slow compression and Brazilian tests were performed. The grain size and the mineral composition of the rock has been found to have a large influence on the local stresses required for these processes. Indeed the results show that the fragility and therefore ease of comminution increases with increasing grain size of the quartzite. Brazilian tests on drill cores of varying diameters may allow the prediction of the critical size of rock of the mill feed which can survive in a mill of given characteristics. 2016-03-21T19:01:59Z 2016-03-21T19:01:59Z 1978 Doctoral Thesis Doctoral PhD http://hdl.handle.net/11427/18008 eng application/pdf Centre for Materials Engineering Faculty of Engineering and the Built Environment University of Cape Town
spellingShingle Materials Engineering
Kanellopoulos, Achilles Constantine
The fracture and autogenous comminution of quartzite
thesis_degree_str Doctoral
title The fracture and autogenous comminution of quartzite
title_full The fracture and autogenous comminution of quartzite
title_fullStr The fracture and autogenous comminution of quartzite
title_full_unstemmed The fracture and autogenous comminution of quartzite
title_short The fracture and autogenous comminution of quartzite
title_sort fracture and autogenous comminution of quartzite
topic Materials Engineering
url http://hdl.handle.net/11427/18008
work_keys_str_mv AT kanellopoulosachillesconstantine thefractureandautogenouscomminutionofquartzite
AT kanellopoulosachillesconstantine fractureandautogenouscomminutionofquartzite