Definition:
Condition dans laquelle la force de succion des racines des plantes ne parvient pas à compenser une pression atmosphérique de 15 bars, ce qui fait que l’eau restante est maintenue dans les particules du sol. En d’autres termes, c’est l’humidité minimale du sol nécessaire pour éviter le flétrissement définitif d’une plante.
Source:
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Food and Agriculture Organization of the United Nations, AQUASTAT Web Site
AQUASTAT. 2009. Adapted from: FAO. 2002. Irrigation Manual Volume I Module 4 – Crop Water Requirements and Irrigation Scheduling. Developed by: Andreas P. Savva and Karen Frenken. FAO, Harare