Abstract
The response of a particle to mineral processing is influenced to an important degree by its shape — i.e. its ratio of surface to volume. If one gram of a solid of S.G. 1.0 could be crushed into equi-dimensional particles just passing through a 200-mesh sieve these, if cubic, would have a combined area of 674 cm2 ; if oblong 562 and if composed of platy flakes some 2,700. A typical mineral sand would have an area of 922 cm2. The surface of a particle is, so to speak, the door to its interior. The bigger the surface vis-à-vis volume, the faster is the rate of reaction and the greater its potential (surface) energy. A sphere has the minimum surface for its volume, and a thin flat plate the minimum volume for its surface. This surface is available for:
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(a)
Frictional retardation of the particle.
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(b)
Acting as a transition area between solid substrate and fluid surroundings of particle.
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(c)
Introducing heat or chemicals to the interior of the particle.
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(d)
Displaying the contents of the particle.
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(e)
Contributing to the pseudo-viscosity of a pulp (total friction per unit volume).
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(f)
Stoichiometric reaction.
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(g)
Protecting the contents of the particle it encloses.
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© 1965 Elsevier Publishing Company Limited
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Pryor, E.J. (1965). Laboratory Sizing Control. In: Mineral Processing. Springer, Dordrecht. https://doi.org/10.1007/978-94-010-2941-4_8
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DOI: https://doi.org/10.1007/978-94-010-2941-4_8
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