Experimental studies show that changes in wettability of mineral grain surface affects seriously the dispersive stability of the mineral pulp as a suspension system.
实验研究表明，矿粒表面润湿性的变化严重地影响其悬浮液的分散稳定性，矿粒的疏水化往往伴随着明显的絮凝，此种絮凝无法用dlvo理论解释。
Experimental studies show that changes in wettability of mineral grain surface affects seriously the dispersive stability of the mineral pulp as a suspension system.
实验研究表明，矿粒表面润湿性的变化严重地影响其悬浮液的分散稳定性，矿粒的疏水化往往伴随着明显的絮凝，此种絮凝无法用dlvo理论解释。
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