AN INVESTIGATION OF THE DELIQUESCENCE OF FERRICOPIAPITE AND THE ONSET OF DELIQUESCENCE OF EPSOMITE CRYSTAL FACES OF DIFFERING MILLER INDICES
Deliquescence is the process whereby a solid interacts with a humid atmosphere and begins to dissolve when the partial pressure of H2O in the atmosphere exceeds the partial pressure of H2O at which the solid is in equilibrium at a given temperature. Deliquescence of sulfate minerals poses a risk to...
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| Language: | en en |
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2011
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| Online Access: | http://hdl.handle.net/1974/6274 |