Water-use efficiency
Water-use efficiency refers to the ratio of plant biomass to water lost by transpiration, can be defined either at the leaf, at the whole plant or a population/stand/field level:
- leaf level : photosynthetic water-use efficiency, which is defined as the ratio of the rate of net CO2 carbon assimilation to the rate of transpiration or stomatal conductance, then called intrinsic water-use efficiency
- plant level : water-use efficiency of productivity, which is typically defined as the ratio of dry biomass produced to the rate of transpiration.
- field level : based on measurements of CO2 and water fluxes over a field of a crop or a forest, using the eddy covariance technique
Intrinsic water-use efficiency Wi usually increases during soil drought, due to stomatal closure and a reduction in transpiration, and is therefore often linked to drought tolerance. Observations from several authors have however suggested that WUE would rather be linked to different drought response strategies, where
- low WUE plants could either correspond to a drought tolerance strategy, for example by anatomical adaptations reducing vulnerability to xylem cavitation, or to a drought avoidance/water spender strategy through a wide soil exploration by roots or a drought escape strategy due to early flowering
- whereas high WUE plants could correspond to a drought avoidance/water saving strategy, through drought-sensitive, early closing stomata.
Water-use efficiency is also a much studied trait in Plant ecology, where it has been used already in the early 20th century to study the ecological requirements of Herbaceous plants or forest trees, and is still used today, for example related to a drought-induced limitation of tree growth