It is introduced that the calculating principle and the math model of the equilibrium constant method for calculating the equilibrium distribution of species of water solution.
介绍了基于平衡常数法的水溶液平衡组分分布的计算原理及其数学模型。
Increase of concentration of solution and flow velocity brought about rise of adsorption rate constant and "quasi-equilibrium" adsorption amount.
溶液浓度、流速提高，吸附速率常数及“准平衡”吸附量随之加大。
Increase of concentration of solution and flow velocity brought about rise of adsorption rate constant and "quasi-equilibrium" adsorption amount.
溶液浓度、流速提高，吸附速率常数及“准平衡”吸附量随之加大。
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