Abstract
A soil–plant hydraulic model shows that the degree of isohydricity is constrained by below-ground hydraulic limitations and that the shape of plant water potential (WP) curve depends on soil hydraulics.
Publication types
-
Letter
-
Research Support, Non-U.S. Gov't
MeSH terms
-
Adaptation, Physiological / physiology*
-
Biological Transport / physiology*
-
Droughts*
-
Plant Transpiration / physiology*
-
Soil / chemistry*
-
Water / chemistry*