LINEAR STOCHASTIC-MODELS FOR MINERAL LIBERATION

Authors
Citation
Rp. King, LINEAR STOCHASTIC-MODELS FOR MINERAL LIBERATION, Powder technology, 81(3), 1994, pp. 217-234
Citations number
26
Categorie Soggetti
Engineering, Chemical
Journal title
ISSN journal
00325910
Volume
81
Issue
3
Year of publication
1994
Pages
217 - 234
Database
ISI
SICI code
0032-5910(1994)81:3<217:LSFML>2.0.ZU;2-1
Abstract
This paper provides a clearly defined procedure for the calculation of the liberation spectrum that can be expected when any two-phase or po rphyry three-phase ore is comminuted in a ball mill or an open-circuit continuous mill. All the data that are required by the model are read ily obtained by suitable image analysis of the original ore. The model accommodates both random and non-random fracture patterns although, i n the latter case, the model is not entirely predictive at present and requires some measurements to be made on the comminuted ore. A linear stochastic process is used to characterize the mineralogical texture of the ore. This model of the ore texture can be used to predict the l iberation spectrum in particles of any size after comminution of the o re. The model is parameter-free and is not limited to textures having convex grain structures nor to convex particles. The model is extended to include the effects of different brittleness of the mineral compon ents and fracture along the grain boundaries which lead to non-random fracture patterns. The model predicts that modest amounts of grain-bou ndary fracture will not increase liberation in minerals having exponen tially distributed linear intercept lengths in each phase. The model i s extended to multicomponent ores. Examples calculations are given for a binary ore having exponentially distributed linear intercepts throu gh both phases. An exponentially distributed porphyry ore with two val uable mineral phases is analyzed up to the calculations of the linear grade distribution as a function of particle size. The calculated dist ribution of linear grades for this three-phase ore cannot be stereolog ically transformed to the distribution of volumetric grades because no suitable transformation kernel has yet been determined.