摘要
本文研究了长江口底质泥沙吸附 Zn^(2+)的热力学,结果表明吸附等温线为L—4型并符合 Langmuir吸附等温式。本文用固相表面不同的活性点位解释了L—4型等温线的形成原因。
This paper studied the thermodynamic of Znz+ adsorption on Changjiang estuarine bottom sediment. The results indicated that adsorption isotherm is L-4 type and suits for Langmuir isotherm equation. The formation of L- 4 isotherm is discussed by means of different active site of sediment surface.
出处
《阜阳师范学院学报（自然科学版）》
1996年第2期20-22,共3页
Journal of Fuyang Normal University(Natural Science)
