吉布斯等温线
吸附
表面张力
埃
电解质
热力学
化学
离子
膜
结晶学
物理化学
物理
有机化学
电极
生物化学
出处
期刊:Acs Symposium Series
日期:1981-05-21
卷期号:: 1-9
被引量:94
标识
DOI:10.1021/bk-1981-0153.ch001
摘要
In the early 1950's Professor Samuel Yuster at the University of California, Los Angeles (UCLA) conceived the idea of using the Gibbs adsorption equation as a guideline to find techniques for producing fresh water from brines (1,2). The Gibbs equation is given by: U = -( l/vRT ) (∂σ/∂1na)T,Ar (1) where U is the adsorption of solute per unit area of surface, ∂ is the number of ions into which the electrolyte can dissociate, R is the gas constant, T is the absolute temperature, σ is the surface tension of the solution, a is the activity of the solute, and Ar is the area of the surface of the solution. According to this equation, brines in contact with air or other hydrophobic surfaces, will have a layer of relatively pure water, 3 or 4 Angstroms thick, adjacent to the interface. Therefore it should be possible to 'skim off this fresh
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