| Literature DB >> 1864084 |
Abstract
The stability of unilamellar vesicles during freeze-thaw cycles strongly depends on the Ca2+ concentration in the aqueous solution. Experiments performed at equal ionic strengths with Na+ and Ca2+ solutions indicate that the effect observed is specific for Ca2+. This is interpreted to be a consequence of the adsorption of Ca2+ on the vesicle bilayers. The variation of lipid and Ca2+ concentrations indicates that stability is achieved at a particular Ca2+/lipid ratio of 8 mol/mol above which vesicles are stable. The stability appears to be mainly conferred by the external Ca2+ in both slow and rapid cycles, independent of the ionic vesicle content. However, internal Ca2+ seems to increase the stability according to the F/T cycle rate to some extent in the absence of Ca2+ in the external solution.Entities:
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Year: 1991 PMID: 1864084 DOI: 10.1016/0011-2240(91)90033-k
Source DB: PubMed Journal: Cryobiology ISSN: 0011-2240 Impact factor: 2.487