This subroutine reads in soil data.
READS IN:
CLODSZ Soil clod size index NDSOIL Number of depths in soil (number of soil layers) REFDPT Reference depth (m) IRESDU Is there residue on the surface? (1=T, 0=F) Z0SOIL Roughness length in meters 0.003 is typical for clear ground 0.01 is typical for ground with residue BD Bulk density SANDFC Sand fraction SILTFC Silt fraction CLAYFC Clay fraction QRTZFC Quartz fraction in fractions of total weight DPE Air entry potential (J/kg) (optional). If 0 is entered it is calculated by G. Cambbell's equations. DBX Exponent in the soil moisture release curve (optional). DAKS Saturating water conductivity (optional). ZSOIL Depth of nodes in soil (m) (ZOSOIL in output) IDOROC Does rock layer exist? (1=T, 0=F) IROCLY The NDSOIL layer where rock starts AKROCK Rock thermal conductivity CPROCK Rock heat capacity DELD Convergence criteria of diff. equation solutionIn code: "DELD is the tolerance on sum D(JZ) in newt-raphson soil eqs--1.e-5-1.e-7 Should be at least 1.e-5 to get storage change to match fluxes." DRHSFC Value to match soil water flow equations with canopy vapor flow equations
In code: "Tolerance on matching sfc rel hum from cpy vapor eqs with rel hum from soil eqs. Determines how close ecpy and wcpys are. 0.001 is small and 0.01 is usually acceptable." RHSLOP Value to match soil water flow equations with canopy vapor flow equations
In code: "RHSLOP is the change of rhsfc below value from cpy vapor eqs to get slope of rhsfc vs soil evap for newt-raph iteration in soil eqs."
COMPUTES:
DGEOM Geometric diameter SGEOM Geometric standard deviation A-ESOIL Coefficients for soil thermal conductivity calc. PE Air entry potential (j/kg) AKS Saturated hydraulic conductivity (kg s m-3) FC1-5 AKSMMH Saturated hydraulic conductivity (mm/hr)Return to cupidg2