Claim · model-written summary
The authors explain diurnal trends by interdependence of leaf conductance and water potential.
- Taxon
- Picea abies
Picea abiest0 - Outcome
- observed trends in diurnal dynamicse0
- Qualifier
- interdependency of leaf conductance and water potentiale0
Not reportedMaterialGeneCompoundOrgan / stageInteractorInteractor roleSecond interactorSecond interactor roleTreatmentComparatorSettingDirectionValue
Organisms pictured · Representative pictures of the matched species, not figures from the paper.
Verbatim
e0“The observed trends in diurnal dynamics can be explained solely by the interdependency of leaf conductance and water potential.”
t0“Picea abies”
Title
U. Maier-Maercker Tree Physiology 1998. doi:10.1093/treephys/18.4.211
Other claims from this paper (11)
- Observation Early in drought, daily maximum photosynthesis and transpiration were relatively high.
- Association As humidity fell during the day, gas exchange dropped more steeply and earlier on successive drought days.
- Association Maximum stomatal aperture was greatly reduced below a soil water potential of -2000 hPa, despite humid air.
- Association At low soil water potential, photosynthesis and transpiration declined less steeply from daily maxima, with small max-min differences.
- Association In the field, daily transpiration and photosynthesis sums depended more on atmospheric conditions than soil water potential.
- Association In growth chambers, daily transpiration and photosynthesis sums fell continuously as soil dried, steeply to -2000 hPa and then slowly.
- Observation Predawn water potential fluctuated in the field but tended to fall over time.
- Observation Needle osmotic potential increased slightly over time in the field.
- Observation Growth chamber predawn water potential never exceeded -1.0 MPa despite saturated soil.
- Association With high average humidity, relatively high predawn water potential persisted until soil water potential reached -8000 hPa.
- Mechanism The authors state that stomata respond directly to the ratio of water supply to demand.