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Onset of water stress, hysteresis in plant conductance, and hydraulic lift: Scaling soil water dynamics from millimeters to meters
Author(s) -
Siqueira Mario,
Katul Gabriel,
Porporato Amilcare
Publication year - 2008
Publication title -
water resources research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.863
H-Index - 217
eISSN - 1944-7973
pISSN - 0043-1397
DOI - 10.1029/2007wr006094
Subject(s) - hydraulic conductivity , soil water , environmental science , soil science , scaling , water content , lift (data mining) , diurnal cycle , mesoscale meteorology , hydrology (agriculture) , geotechnical engineering , atmospheric sciences , geology , meteorology , mathematics , geometry , physics , computer science , data mining
Estimation of water uptake by plants and subsequent water stress are complicated by the need to resolve the soil‐plant hydrodynamics at scales ranging from millimeters to meters. Using a simplified homogenization technique, the three‐dimensional (3‐D) soil water movement dynamics can be reduced to solving two 1‐D coupled Richards' equations, one for the radial water movement toward rootlets (mesoscale, important for diurnal cycle) and a second for vertical water motion (macroscale, relevant to interstorm timescales). This approach allows explicit simulation of known features of root uptake such as diurnal hysteresis in canopy conductance, hydraulic lift, and compensatory root water uptake during extended drying cycles. A simple scaling analysis suggests that the effectiveness of the hydraulic lift is mainly controlled by the root vertical distribution, while the soil moisture levels at which hydraulic lift is most effective is dictated by soil hydraulic properties and surrogates for atmospheric water vapor demand.