
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
solution
In 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