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DEFINICIÓN

  • Root hydraulic conductivity is a measure of how easily water can flow through a plant's roots. It's calculated as the rate of water flow divided by the difference in water potential and the root surface area. This is a property of the roots themselves, not influenced by their size.

    Creado: 9/19/23

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URI

http://aims.fao.org/aos/agrovoc/c_37237

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RDF/XML TURTLE JSON-LD Creado 20/11/11, última modificación 20/9/23