A THEORY OF CELL HYDRATION PREDICATED ON ADSORPTION OF WATER ON CELL PROTEINS.

Abstract

If it is postulated that cell hydration is governed by adsorption of water on cell proteins in accord with the Bradley adsorption isotherm and that the action of a solute in the surrounding solution is to lower the vapor pressure of the solution so that cell water adsorption is decreased by moving down the Bradley isotherm, then one may derive that cell volume (V) should be related to solute concentration (x) by the equation V = -Elog x + F where E and F are constants which are independent of type of solute. For a non-adsorbed solute, this agrees well with experimental data. For solutes which are adsorbed by cell proteins, a correction in the above equation may be necessary at higher solute concentrations, which is shown to be compatible with various experimental data. The types of experiments which are generally used to support the osmotic pressure theory of cell hydration agree equally well with the adsorption theory. The virtue of the adsorption theory is that, unlike the osmotic pressure theory of cell swelling, it is compatible with permeability of the cell membrane to solutes, which has been experimentally observed for various solutes. (Author)

Document Details

Document Type
Technical Report
Publication Date
Feb 17, 1967
Accession Number
AD0652376

Entities

People

  • Freeman W. Cope

Organizations

  • Naval Air Warfare Center Warminster

Tags

DTIC Thesaurus Topics

  • Adsorption
  • Cell Membrane
  • Cells
  • Equations
  • Experimental Data
  • Hydration
  • Isotherms
  • Membranes
  • Osmotic Pressure
  • Permeability
  • Vapor Pressure

Fields of Study

  • Chemistry

Readers

  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.
  • Calculus or Mathematical Analysis
  • Environmental Engineering