source: tags/ORCHIDEE_1_9_5/ORCHIDEE/src_parameters/constantes_soil.f90 @ 8

!$Header: /home/ssipsl/CVSREP/ORCHIDEE/src_parameters/constantes_soil.f90,v 1.11 2010/04/06 14:38:48 ssipsl Exp $
!IPSL (2006)
! This software is governed by the CeCILL licence see ORCHIDEE/ORCHIDEE_CeCILL.LIC
!-
MODULE constantes_soil
!!--------------------------------------------------------------------
!! "constantes_soil" module contains public data for the soils
!!--------------------------------------------------------------------
  USE constantes
!-
  IMPLICIT NONE
!-
! Dimensioning parameters
!-
! Number of soil level
  INTEGER(i_std),PARAMETER :: ngrnd=7
! Number of diagnostic levels in the soil
  INTEGER(i_std),PARAMETER :: nbdl=11
!MM : if you want to compare hydrology variables with old TAG 1.6 and lower, 
!     you must set the Number of diagnostic levels in the soil to 6 :
!  INTEGER(i_std),PARAMETER :: nbdl=6
! Number of levels in CWRR
  INTEGER(i_std),PARAMETER :: nslm=11
! Number of soil types
  INTEGER(i_std),PARAMETER :: nstm=3
!-
!- Parameters for soil thermodynamics
!-
! Average Thermal Conductivity of soils
  REAL(r_std),PARAMETER :: so_cond = 1.5396
! Average Heat capacity of soils
  REAL(r_std),PARAMETER :: so_capa = 2.0514e+6
!-
! Values taken from : PIELKE,'MESOSCALE METEOROLOGICAL MODELING',P.384
! Dry soil heat capacity was decreased and conductivity increased.
!-
! Dry soil Heat capacity of soils
!*REAL(r_std),PARAMETER :: so_capa_dry = 1.35e+6
  REAL(r_std),PARAMETER :: so_capa_dry = 1.80e+6
! Dry soil Thermal Conductivity of soils
!*REAL(r_std),PARAMETER :: so_cond_dry = 0.28
  REAL(r_std),PARAMETER :: so_cond_dry = 0.40
!-
! Wet soil Heat capacity of soils
  REAL(r_std),PARAMETER :: so_capa_wet = 3.03e+6
! Wet soil Thermal Conductivity of soils
  REAL(r_std),PARAMETER :: so_cond_wet = 1.89
!-
! Thermal Conductivity of snow
  REAL(r_std),PARAMETER :: sn_cond = 0.3
! Snow density for the soil thermodynamics
  REAL(r_std),PARAMETER :: sn_dens = 330.0
! Heat capacity for snow
  REAL(r_std),PARAMETER :: sn_capa = 2100.0_r_std*sn_dens
!-
! Constantes from the Choisnel hydrology
!-
! Wilting point (Has a numerical role for the moment)
  REAL(r_std),PARAMETER :: qwilt = 5.0
! Total depth of soil reservoir (for hydrolc)
  REAL(r_std),SAVE :: dpu_cste=2.0_r_std
! The minimal size we allow for the upper reservoir (m)
  REAL(r_std),PARAMETER :: min_resdis = 2.e-5
! Diffusion constant for the slow regime
! (This is for the diffusion between reservoirs)
  REAL(r_std),PARAMETER :: min_drain = 0.001
! Diffusion constant for the fast regime
  REAL(r_std),PARAMETER :: max_drain = 0.1
! The exponential in the diffusion law
  REAL(r_std),PARAMETER :: exp_drain = 1.5
! Transforms leaf area index into size of interception reservoir
  REAL(r_std),SAVE      :: qsintcst = 0.1
! Maximum quantity of water (Kg/M3)
  REAL(r_std),PARAMETER :: mx_eau_eau = 150.
!-
! Constant in the computation of resistance for bare  soil evaporation
  REAL(r_std),PARAMETER :: rsol_cste = 33.E3
! Scaling depth for litter humidity (m)
!SZ changed this according to SP from 0.03 to 0.08, 080806
  REAL(r_std),PARAMETER :: hcrit_litter=0.08_r_std
!-
! Parameters for soil type distribution
!-
! Default soil texture distribution in the following order :
!    sand, loam and clay
  REAL(r_std),DIMENSION(nstm),SAVE :: soiltype_default = &
 & (/ 0.0, 1.0, 0.0 /)
!-
! Parameters specific for the CWRR hydrology.
!-
! Van genuchten coefficient n
  REAL(r_std),PARAMETER,DIMENSION(nstm) :: nvan = &
 & (/ 1.89_r_std, 1.56_r_std, 1.31_r_std /)
!!$! Van genuchten coefficient a (cm^{-1})
!!$  REAL(r_std),PARAMETER,DIMENSION(nstm) :: avan = &
!!$ & (/ 0.036_r_std, 0.036_r_std, 0.036_r_std /)
!TdO
! Van genuchten coefficient a (mm^{-1})
  REAL(r_std),PARAMETER,DIMENSION(nstm) :: avan = &
  & (/ 0.0075_r_std, 0.0036_r_std, 0.0019_r_std /) 
! CWRR linearisation
  INTEGER(i_std),PARAMETER :: imin = 1
! number of interval for CWRR
  INTEGER(i_std),PARAMETER :: nbint = 100
! number of points for CWRR
  INTEGER(i_std),PARAMETER :: imax = nbint+1
! Residual soil water content
  REAL(r_std),PARAMETER,DIMENSION(nstm) :: mcr = &
 & (/ 0.065_r_std, 0.078_r_std, 0.095_r_std /)
! Saturated soil water content
  REAL(r_std),PARAMETER,DIMENSION(nstm) :: mcs = &
 & (/ 0.41_r_std, 0.43_r_std, 0.41_r_std /)
! Total depth of soil reservoir (m)
  REAL(r_std),SAVE,DIMENSION(nstm) :: dpu = &
 & (/ 2.0_r_std, 2.0_r_std, 2.0_r_std /)
  ! dpu must be constant over the different soil types
! Hydraulic conductivity Saturation (mm/d)
  REAL(r_std),PARAMETER,DIMENSION(nstm) :: ks = &
 & (/ 1060.8_r_std, 249.6_r_std, 62.4_r_std /)
! Soil moisture above which transpir is max
  REAL(r_std),PARAMETER,DIMENSION(nstm) :: pcent = &
 & (/ 0.5_r_std, 0.5_r_std, 0.5_r_std /)
! Max value of the permeability coeff at the bottom of the soil
  REAL(r_std),PARAMETER,DIMENSION(nstm) :: free_drain_max = &
 & (/ 1.0_r_std, 1.0_r_std, 1.0_r_std /)
! Volumetric water content field capacity
  REAL(r_std),PARAMETER,DIMENSION(nstm) :: mcf = &
 & (/ 0.32_r_std, 0.32_r_std, 0.32_r_std /)
! Volumetric water content Wilting pt
  REAL(r_std),PARAMETER,DIMENSION(nstm) :: mcw = &
 & (/ 0.10_r_std, 0.10_r_std, 0.10_r_std /)
! Vol. wat. cont. above which albedo is cst
  REAL(r_std),PARAMETER,DIMENSION(nstm) :: mc_awet = &
 & (/ 0.25_r_std, 0.25_r_std, 0.25_r_std /)
! Vol. wat. cont. below which albedo is cst
  REAL(r_std),PARAMETER,DIMENSION(nstm) :: mc_adry = &
 & (/ 0.1_r_std, 0.1_r_std, 0.1_r_std /)
! Matrix potential at saturation (mm)
  REAL(r_std),PARAMETER,DIMENSION(nstm) :: psis = &
 & (/ -300.0_r_std, -300.0_r_std, -300.0_r_std /)
! Time weighting for discretisation
  REAL(r_std),PARAMETER :: w_time = 1.0_r_std
!-
! Diagnostic variables
!-
! The lower limit of the layer on which soil moisture (relative)
! and temperature are going to be diagnosed.
! These variables are made for transfering the information
! to the biogeophyical processes modelled in STOMATE.
!-
  REAL(r_std),DIMENSION(nbdl),SAVE :: diaglev 
!-------------------------
END MODULE constantes_soil