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Interaction between Osmotic- and Pressure-induced Water Flow in Plant Roots
When the pressure gradient across a root alters, there is often an apparent change in the permeability of the root to water. Fiscus (Plant Physiol. 1975. 55: 917-922) has suggested that this can be explained by a simple two-compartment model which takes into account rates of solute uptake into the x...
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| 1. autor: | |
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| Format: | Artigo |
| Język: | Inglês |
| Wydane: |
1976
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| Hasła przedmiotowe: | |
| Dostęp online: | https://ncbi.nlm.nih.gov/pmc/articles/PMC542110/ https://ncbi.nlm.nih.gov/pubmed/16659562 |
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