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dc.creatorGourgoulianis, K. I.en
dc.creatorHatzoglou, C.en
dc.creatorMolyvdas, P. A.en
dc.date.accessioned2015-11-23T10:28:55Z
dc.date.available2015-11-23T10:28:55Z
dc.date.issued2005
dc.identifier10.1016/j.mehy.2004.06.011
dc.identifier.issn0306-9877
dc.identifier.urihttp://hdl.handle.net/11615/28131
dc.description.abstractThe small amount of liquid that, under physiological conditions, is presented in the pleural cavity has been the focus of extensive research for more than a century. However, there are still unanswered questions and considerable controversies about the nature of the forces governing its movement into and out of the pleural cavity. Early in the 20th century has been proposed that pleural fluid turnover is simple based on the balance between hydraulic and colloid osmotic pressures existing across the pleura membranes. This original hypothesis has not been validated by data accumulating over the last 20 years. Pleural tissues and renal proximal tubules present high water permeability, small transepithelial electrical resistance (22.02 Omega cm(2)) and the same cation transportation such as Na+ channels, Na+-K+ ATPase channels, and Na+-H+ exchanger. In contrast to previous conflicting theories concerning pleura fluid movement, the same functional characteristics suggest the hypothesis that physiology of pleura is similar to proximal tubules. (C) 2004 Elsevier Ltd. All rights reserved.en
dc.sourceMedical Hypothesesen
dc.source.uri<Go to ISI>://WOS:000225481400017
dc.subjectPERMEABILITYen
dc.subjectABSORPTIONen
dc.subjectEFFUSIONen
dc.subjectMedicine, Research & Experimentalen
dc.titleFunctional similarities between pleura and the renal proximal tubule - membrane and cellular considerationsen
dc.typejournalArticleen


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