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📄 gw_no3.f

📁 水文模型的原始代码
💻 F
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      subroutine gw_no3
      
!!    ~ ~ ~ PURPOSE ~ ~ ~
!!    this subroutine estimates groundwater contribution to
!!    streamflow

!!    ~ ~ ~ INCOMING VARIABLES ~ ~ ~
!!    name        |units         |definition
!!    ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~
!!    alpha_bf(:) |days          |alpha factor for groundwater recession curve
!!    alpha_bfe(:)|none          |Exp(-alpha_bf(:))
!!    deepst(:)   |mm H2O        |depth of water in deep aquifer
!!    ihru        |none          |HRU number
!!    gw_delaye(:)|none          |Exp(-1./(delay(:)) where delay(:) is the 
!!                               |groundwater delay (time required for water
!!                               |leaving the bottom of the root zone to reach
!!                               |the shallow aquifer; units-days)
!!    gw_revap(:) |none          |revap coeff: this variable controls the amount
!!                               |of water moving from the shallow aquifer to
!!                               |the root zone as a result of soil moisture
!!                               |depletion
!!    gw_spyld(:) |m**3/m**3     |specific yield for shallow aquifer
!!    gwht(:)     |m             |groundwater height
!!    gwqmn(:)    |mm H2O        |threshold depth of water in shallow aquifer
!!                               |required before groundwater flow will occur
!!    pet_day     |mm H2O        |potential evapotranspiration on current day
!!                               |in HRU
!!    rchrg(:)    |mm H2O        |amount of water entering shallow aquifer on
!!                               |previous day in HRU
!!    rchrg_dp(:) |none          |recharge to deep aquifer: the fraction of
!!                               |root zone percolation that reaches the deep
!!                               |aquifer
!!    revapmn(:)  |mm H2O        |threshold depth of water in shallow aquifer
!!                               |required to allow revap to occur
!!    sepbtm      |mm H2O        |percolation from bottom of soil profile for
!!                               |the day in HRU
!!    shallst(:)  |mm H2O        |depth of water in shallow aquifer
!!    ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~

!!    ~ ~ ~ OUTGOING VARIABLES ~ ~ ~
!!    name        |units         |definition
!!    ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~
!!    deepst(:)   |mm H2O        |depth of water in deep aquifer
!!    gw_q(:)     |mm H2O        |groundwater contribution to streamflow from
!!                               |HRU on current day
!!    gwht(:)     |m             |groundwater height
!!    gwseep      |mm H2O        |amount of water recharging deep aquifer on
!!                               |current day in HRU
!!    rchrg(:)    |mm H2O        |amount of water recharging both aquifers on
!!                               |current day in HRU
!!    revapday    |mm H2O        |amount of water moving from the shallow 
!!                               |aquifer into the soil profile or being taken
!!                               |up by plant roots in the shallow aquifer
!!    shallst(:)  |mm H2O        |depth of water in shallow aquifer
!!    ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~

!!    ~ ~ ~ LOCAL DEFINITIONS ~ ~ ~
!!    name        |units         |definition
!!    ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~
!!    j           |none          |HRU number
!!    rchrg1      |mm H2O        |amount of water entering shallow aquifer on
!!                               |previous day
!!    ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~

!!    ~ ~ ~ SUBROUTINES/FUNCTIONS CALLED ~ ~ ~
!!    Intrinsic: Max

!!    ~ ~ ~ ~ ~ ~ END SPECIFICATIONS ~ ~ ~ ~ ~ ~
!!    revap is subtracted and rchrg is delayed (johnson, 1977)

      use parm

      integer :: j
      real :: rchrgn1, revapn, gwseepn

      j = 0
      j = ihru

      rchrgn1 = 0.
      rchrgn1 = rchrg_n(j)
      if (rchrgn1 < 1.e-6) rchrgn1 = 0.0

!! compute nitrate aquifer loading from recharge for current day
      rchrg_n(j) = 0.
      rchrg_n(j) = (1.- gw_delaye(j)) * percn(j) + gw_delaye(j)
     &                                                   * rchrgn1
      shallst_n(j) = shallst_n(j) + rchrg_n(j)

      if (shallst_n(j) < 1.e-6) shallst_n(j) = 0.0
      if (shallst(j) < 1.e-6) shallst(j) = 0.0
      if (gw_q(j) < 1.e-6) gw_q(j) = 0.0
      if (revapday < 1.e-6) revapday = 0.0
      if (gwseep < 1.e-6) gwseep = 0.0

!! compute nitrate groundwater contribution to streamflow for day
      xx = shallst(j) + gw_q(j) + revapday + gwseep 
      if (xx > 1.) then
        xx = shallst_n(j) / (shallst(j) + gw_q(j) + revapday + gwseep) 
      else
        xx = 0.
      end if
      if (xx < 1.e-6) xx = 0.0
      no3gw(j) = xx * gw_q(j)

      revapn = xx * revapday
      gwseepn = xx * gwseep

      revapn = amax1(1.e-6,revapn)
      gwseepn = amax1(1.e-6,gwseepn)

!! subtract nitrate losses from the shallow aquifer
      shallst_n(j) = shallst_n(j) - no3gw(j) - revapn - gwseepn
      shallst_n(j) = amax1 (0., shallst_n(j))

!! compute nitrate losses in the groundwater
      shallst_n(j) = shallst_n(j) * gw_nloss(j)
      shallst_n(j) = amax1(0., shallst_n(j))
  
      return
      end

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