algebraic equation
actual soil evaporation
boundary conditions for solute transport
canopy water balance
drainage
soil hydraulic properties in one-domain flow
solute concentration in canopy and rain
solute loss due to biodegradation
upper boundary condition for unsaturated water flow
vertical water flow in saturated zone
water uptake by roots
dynamic equation
crop cover
soil hydraulic properties in two-domain flow
partial differential equation
bottom boundary condition for unsaturated water flow
soil temperature
solute transport
unsaturated soil water flow