| Literature DB >> 6713942 |
Abstract
The permeability of the membrane of the rat megakaryocytopoietic cell to dimethyl sulfoxide was measured to assess its availability to the intracellular compartment. The method used was osmotic, and measured the initial loss of cell water followed by a reswelling to isotonic volume when cells were placed in culture media containing 0.6 M DMSO. Values for the hydraulic coefficient, Lp, the permeability of the membrane to DMSO, wRT , and the reflection coefficient were calculated from the equations of Kedem and Katchalsky . The average value at 25 degrees C for Lp was 0.46 micron min-1 atm1 ; wRT was 9.3 micron min-1, and the reflection coefficient was 0.65. At these cell volumes, 50% equilibration occurred in 5 sec. Cells equilibrated in 0.6 M DMSO increased their volume of osmotically inactive water. Coupled with this phenomenon of stabilization of water was a reduction in the hydraulic coefficient by 50%. These findings are discussed in the context of current hypotheses about cellular viability during freezing and thawing in the presence and absence of cryoprotectants.Entities:
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Year: 1984 PMID: 6713942 DOI: 10.1016/0011-2240(84)90204-9
Source DB: PubMed Journal: Cryobiology ISSN: 0011-2240 Impact factor: 2.487