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J Physiol Volume 542, Number 1, 61-62, July 1, 2002 DOI: 10.1113/jphysiol.2002.013328
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Journal of Physiology (2002), 542.1, p. 61-62
© Copyright 2002 The Physiological Society
DOI: 10.1113/jphysiol.2002.013328

The presence of local osmotic gradients can account for the water flux driven by the Na+-glucose cotransporter

Jean-Yves Lapointe, Marilène Gagnon, Simon Poirier and Pierre Bissonnette

Groupe de recherche en transport membranaire, Physics Department, Université de Montréal, Montréal, QC, Canada H3C 3J7

Email: jean-yves.lapointe{at}umontreal.ca




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