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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| Vydáno v: | Plant Physiol |
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| Hlavní autor: | |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Oxford University Press
1976
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.govhttps://pmc.ncbi.nlm.nih.gov/articles/PMC542110/ https://ncbi.nlm.nih.govhttps://pubmed.ncbi.nlm.nih.gov/16659562/ https://ncbi.nlm.nih.govhttps://doi.org/10.1104/pp.57.5.738 |
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