Literature DB >> 5089916

The validity of the Ussing flux ratio equation in a three-dimensionally inhomogeneous membrane.

T L Schwartz.   

Abstract

Derivations of the Ussing flux ratio equation have, until now, required the membrane to be both bounded by parallel planes and homogeneous, except in the transmembrane direction. These constraints have been necessary for the theoretical demonstration that the equation is independent of membrane parameters in the absence of carriers, coupling, solvent drag, or "single-file" diffusion. In a new derivation, the flux ratio equation is shown to be valid in this kind of diffusion regime without regard to the three-dimensional structure of the membrane. Thus the constraints on both membrane homogeneity and membrane geometry are shown to be unnecessary. The general use of this equation to differentiate between simple, uncoupled diffusion and other membrane transport phenomena is thus placed on a firmer base. However, as in earlier derivations, it is necessary that isopotential, isobaric, constant concentration surfaces exist sufficiently close to the membrane on both of its sides.

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Year:  1971        PMID: 5089916      PMCID: PMC1483975          DOI: 10.1016/S0006-3495(71)86238-0

Source DB:  PubMed          Journal:  Biophys J        ISSN: 0006-3495            Impact factor:   4.033


  3 in total

1.  THE RELATIONSHIP OF USSING'S FLUX-RATIO EQUATION TO THE THERMODYNAMIC DESCRIPTION OF MEMBRANE PERMEABILITY.

Authors:  T HOSHIKO; B D LINDLEY
Journal:  Biochim Biophys Acta       Date:  1964-03-30

2.  Some aspects of the application of tracers in permeability studies.

Authors:  H H USSING
Journal:  Adv Enzymol Relat Subj Biochem       Date:  1952

3.  Isotope flows and flux ratios in biological membranes.

Authors:  O Kedem; A Essig
Journal:  J Gen Physiol       Date:  1965-07       Impact factor: 4.086

  3 in total
  1 in total

1.  Tracer flux ratios: a phenomenological approach.

Authors:  D C Dawson
Journal:  J Membr Biol       Date:  1977-03-23       Impact factor: 1.843

  1 in total

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