作者: Leonard J. Warren
DOI: 10.1016/0301-7516(85)90012-2
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摘要: Abstract Laboratory batch flotation tests were carried out on a deslimed (+6 μm) sulfiderich cassiterite ore, an ultrafine fraction (−6 of ore and bituminous coal. Chemical conditions kept constant but the water recovery was varied by changing height froth column rate depth removed. The floatable mineral in each system then found to be linearly related weight recovered. intercept regression line axis, where is zero, interpreted as due true flotation. entrainment contribution proportional slope line. In this way contributions overall separated.