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

✍ Scribed by Jean-Yves Lapointe; Marilène Gagnon; Simon Poirier; Pierre Bissonnette


Book ID
110111713
Publisher
Cambridge University Press
Year
2002
Tongue
English
Weight
79 KB
Volume
542
Category
Article
ISSN
0022-3751

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