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Separation Of Chromite And Hematite

Vr and Vm and the total interaction energy Vt as a function of the interparticle separation for a suspension of colloidal mineral particles. a 0.25 to 2.00 181m. -40 mV corresponding to an approximate average value for the oxide mineral dispersion such as hematite or chromite at a natural pH of 7 to 8, Wang et al., 1992.

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