| Literature DB >> 15621233 |
Anandi Krishnan1, Arwen Wilson, Jacqueline Sturgeon, Christopher A Siedlecki, Erwin A Vogler.
Abstract
A systematic study of water-air (liquid-vapor, LV) interfacial tension gamma(lv) of blood plasma and serum derived from four different mammalian species (human, bovine, ovine and equine) reveals nearly identical concentration-dependence (dgamma(lv)/dlnC(B); where C(B) is plasma/serum dilution expressed in v/v concentration units). Comparison of results to a previously-published survey of purified human-blood proteins further reveals that dgamma(lv)/dlnC(B) of plasma and serum is surprisingly similar to that of purified protein constituents. It is thus concluded that any combination of blood-protein constituents will be substantially similar because dgamma(lv)/dlnC(B) of individual proteins are very similar. Experimental results are further interpreted in terms of a recently-developed theory emphasizing the controlling role of water in protein adsorption. Accordingly, the LV interphase saturates with protein adsorbed from bulk solution at a fixed weight-volume concentration ( approximately 436 mg/mL) independent of protein identity or mixture. As a direct consequence, dgamma(lv)/dlnC(B) of purified proteins closely resembles that of mixed solutions and does not depend on the relative proportions of individual proteins comprising a mixture. Thus variations in the plasma proteome between species are not reflected in dgamma(lv)/dlnC(B) nor is serum different from plasma in this regard, despite being depleted of coagulation proteins (e.g. fibrinogen). A comparison of pendant-drop and Wilhelmy-balance tensiometry as tools for assessing protein gamma(lv) shows that measurement conditions employed in the typical Wilhelmy plate approach fails to achieve the steady-state adsorption state that is accessible to pendant-drop tensiometry.Entities:
Mesh:
Substances:
Year: 2005 PMID: 15621233 DOI: 10.1016/j.biomaterials.2004.09.016
Source DB: PubMed Journal: Biomaterials ISSN: 0142-9612 Impact factor: 12.479