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Quantitative measurement of pore flux and radius

Because the theory is relatively simple and well developed, the tip collection mode has been employed extensively for quantitative measurements of pore flux and radius. [Pg.362]

These techniques involving the measurement of membrane permeability to a fluid (liquid or gas) lead to a mean pore radius (usually the effective hydraulic radius Th) whose quantitative value is often highly ambiguous. The flux of a fluid through a porous material is sensitive to all structural aspects of the material [129]. Thus, in spite of the simplicity of the method, the interpretation of flux data, even for the simplest case of steady state, is subject to uncertainties and depends on the models and approximations used. [Pg.102]


See other pages where Quantitative measurement of pore flux and radius is mentioned: [Pg.356]    [Pg.233]    [Pg.242]    [Pg.356]    [Pg.233]    [Pg.242]    [Pg.1507]   
See also in sourсe #XX -- [ Pg.336 ]




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