title: The presence of local osmotic gradients can account for the water flux driven by the Na+-glucose cotransporter.
authors.affiliation: Groupe de recherche en transport membranaire, Physics Department, Université de Montréal, Montréal, QC, Canada H3C 3J7. jean-yves.lapointe@umontreal.ca
authors.forename: Jean-Yves
authors.initials: JY
authors.lastname: Lapointe
authors.forename: Marilène
authors.initials: M
authors.lastname: Gagnon
authors.forename: Simon
authors.initials: S
authors.lastname: Poirier
authors.forename: Pierre
authors.initials: P
authors.lastname: Bissonnette
mesh_terms: D000818:Animals; D004058:Diffusion; D006801:Humans; D008562:Membrane Glycoproteins / Q000378:metabolism*; D009004:Monosaccharide Transport Proteins / Q000378:metabolism*; D009995:Osmosis; D051269:Sodium-Glucose Transporter 1; D014867:Water / Q000378:metabolism*
chemical_list: D008562:Membrane Glycoproteins; D009004:Monosaccharide Transport Proteins; C495674:SLC5A1 protein, human; D051269:Sodium-Glucose Transporter 1; D014867:Water