subroutine gwflow_soil(hru_id) !rtb gwflow !! ~ ~ ~ PURPOSE ~ ~ ~ !! this subroutine calculates the water exchange volume between the aquifer and the soil profile !! (exchange volumes are used in gwflow_simulate, in groundwater balance equations) use gwflow_module use soil_module, only : soil use hydrograph_module, only : ob use hru_module, only : gwsoilq use time_module, only : time implicit none integer, intent (in) :: hru_id ! |hru number integer :: k = 0 ! |counter integer :: s = 0 ! |solute counter integer :: jj = 0 ! |soil layer counter integer :: cell_id = 0 ! |cell in connection with the channel real :: hru_Q = 0. !m3 |volume transferred from cell to the soil profile real :: hru_soilz = 0. !m |thickness of HRU soil profile real :: vadose_z = 0. !m |thickness of cell vadose zone real :: poly_area = 0. !m2 |area of cell within the HRU real :: solmass(100) = 0. !g |solute mass transferred from cell real :: water_depth(100) = 0. !m |depth of groundwater in each soil layer real :: water_depth_tot = 0. !m |total depth of groundwater in the soil profile real :: sol_thick = 0. !m |thickness of soil layer real :: layer_fraction = 0. ! |fraction of saturated soil profile within the layer real :: layer_transfer = 0. ! |amount of water and solute transferred to the soil layer real :: hru_area_m2 = 0. !m2 |surface area of the hru real :: heat_flux = 0. !J |total groundwater heat flux transferred to HRU soils real :: soil_volm = 0. !m3 |volume of soil water in the layer real :: soil_heat = 0. !J |heat in the soil water of the layer !area of the HRU in m2 hru_area_m2 = ob(hru_id)%area_ha * 10000. !only proceed if gw-->soil exchange is active if (gw_soil_flag == 1) then !HRU soil thickness hru_soilz = soil(hru_id)%phys(soil(hru_id)%nly)%d / 1000. !m !loop through the grid cells connected to the HRU ------------------------------------------------------------- hru_Q = 0. do k=1,hru_num_cells(hru_id) !cell in connection with the HRU cell_id = hru_cells(hru_id,k) !only proceed if the cell is active if(gw_state(cell_id)%stat == 1) then !calculate the current thickness of the vadose zone (m) vadose_z = gw_state(cell_id)%elev - gw_state(cell_id)%head !thickness of vadose zone (m) !if water table is within the soil profile --> calculate groundwater volume (Q) to transfer; then transfer to soil layer hru_Q = 0. if(vadose_z < hru_soilz) then !water table is within the soil profile poly_area = gw_state(cell_id)%area * cells_fract(hru_id,k) !area of cell within HRU hru_Q = (hru_soilz - vadose_z) * poly_area * gw_state(cell_id)%spyd !m3 of groundwater to transfer to the soil profile !store for water balance calculations (in gwflow_simulate) gw_hyd_ss(cell_id)%soil = gw_hyd_ss(cell_id)%soil + (hru_Q*(-1)) !negative = leaving the aquifer gw_hyd_ss_yr(cell_id)%soil = gw_hyd_ss_yr(cell_id)%soil + (hru_Q*(-1)) !store for annual water gw_hyd_ss_mo(cell_id)%soil = gw_hyd_ss_mo(cell_id)%soil + (hru_Q*(-1)) !store for monthly water !heat if(gw_heat_flag == 1) then heat_flux = gwheat_state(cell_id)%temp * gw_rho * gw_cp * hru_Q !J if(heat_flux >= gwheat_state(cell_id)%stor) then heat_flux = gwheat_state(cell_id)%stor endif gw_heat_ss(cell_id)%soil = gw_heat_ss(cell_id)%soil + (heat_flux*(-1)) gw_heat_ss_yr(cell_id)%soil = gw_heat_ss_yr(cell_id)%soil + (heat_flux*(-1)) endif !determine which HRU soil layers are to receive groundwater water_depth = 0. water_depth_tot = 0. do jj=1,soil(hru_id)%nly sol_thick = soil(hru_id)%phys(jj)%thick / 1000. !mm --> m if((soil(hru_id)%phys(jj)%d/1000.) > vadose_z) then if(jj == 1) then !top layer water_depth(jj) = (soil(hru_id)%phys(jj)%d/1000.) - vadose_z else if(vadose_z > (soil(hru_id)%phys(jj-1)%d/1000.)) then !water table is within this layer water_depth(jj) = (soil(hru_id)%phys(jj)%d/1000.) - vadose_z else !water table is above this layer water_depth(jj) = sol_thick endif endif water_depth_tot = water_depth_tot + water_depth(jj) endif enddo !next soil layer !transfer the groundwater and the solute mass to the HRU soil layers do jj=1,soil(hru_id)%nly if(water_depth_tot > 0) then layer_fraction = water_depth(jj) / water_depth_tot else layer_fraction = 0. endif layer_transfer = (hru_Q*layer_fraction) / hru_area_m2 * 1000. !m3 --> mm soil(hru_id)%phys(jj)%st = soil(hru_id)%phys(jj)%st + layer_transfer !mm gwsoilq(hru_id) = gwsoilq(hru_id) + layer_transfer !store for hru output if (gw_solute_flag == 1) then do s=1,gw_nsolute !loop through the solutes layer_transfer = (solmass(s)*layer_fraction) / 1000. / ob(hru_id)%area_ha !g --> kg/ha hru_soil(hru_id,jj,s) = hru_soil(hru_id,jj,s) + layer_transfer !kg/ha (mass added to soil profile in nut_nlch, nut_solp, salt_lch, cs_lch) enddo endif if(gw_heat_flag == 1) then !heat transferred to HRU soil profile layer_transfer = (heat_flux * layer_fraction) !J !update temperature in soil layer soil_volm = (soil(hru_id)%phys(jj)%st/1000.) * hru_area_m2 !m3 of soil water soil_heat = soil(hru_id)%phys(jj)%tmp * gw_rho * gw_cp * soil_volm !J soil_heat = soil_heat + layer_transfer soil(hru_id)%phys(jj)%tmp = soil_heat / (gw_rho * gw_cp * soil_volm) endif enddo endif !check for water table in soil profile endif !check if cell is active enddo !go to next connected cell endif !check if gw-->soil transfer is active return end subroutine gwflow_soil