User Tools

Site Tools


start:hype_model_description:aquifier

Differences

This shows you the differences between two versions of the page.

Link to this comparison view

Both sides previous revision Previous revision
Next revision
Previous revision
start:hype_model_description:aquifier [2020/03/11 09:08]
cpers [Deep percolation delay and aquifer recharge]
start:hype_model_description:aquifier [2024/02/21 10:07] (current)
cpers [Deep processes]
Line 1: Line 1:
 ====== Deep processes ====== ====== Deep processes ======
  
-There are two model options for processes deep below ground; regional groundwater flow and aquifers. The regional groundwater flow model simulates groundwater flow between subbasins, but no explicit storage of deep groundwater. The aquifer model simulates aquifer storage and delay before regional groundwater reaches the destination. +There are two model options for processes deep below ground; regional groundwater flow and aquifers. The regional groundwater flow model simulates groundwater flow between subbasins, but no explicit storage of deep groundwater. The aquifer model simulates aquifer storage and delay before regional groundwater reaches the destination. ​Another model option related to groundwater flow, although not classified as deep processes by HYPE is the option for recharge and discharge classes within a subbasin ([[start:​hype_model_description:​hype_land#​recharge_-_discharge_model|read more here]]). ​
 ===== Regional groundwater flow ===== ===== Regional groundwater flow =====
  
Line 15: Line 14:
 ==== Soil addition of regional groundwater flow ==== ==== Soil addition of regional groundwater flow ====
  
-The groundwater flow to be added to the bottom layer (and mixed) is added in the class loop portion of the code. If the layer then becomes full of water, it will be pressed into the layer above and mixed, etc. Please note that if downstream subbasin is much smaller than the upstream subbasin, groundwater inflows can become large. If part of the groundwater flow is to go to the outlet lake in the subbasin this is added to the volume of the lake in the routing part of the code.+The groundwater flow to be added to the bottom layer (and mixed) is added in the class loop portion of the code. If the layer then becomes full of water, it will be pressed into the layer above and mixed, etc. Please note that if downstream subbasin is much smaller than the upstream subbasin, groundwater inflows can become large. ​
  
 ==== Regional groundwater to outlet lake ==== ==== Regional groundwater to outlet lake ====
  
-With an input variable in GeoData.txt,​ an outlet lake may be flagged to receive inflow from the regional groundwater. The coefficient (//​grwtolake//​) specifies the portion of the produced regional groundwater flow which is led to the subbasins outlet lake. +With an input variable in GeoData.txt,​ an outlet lake may be flagged to receive inflow from the regional groundwater. The coefficient (//​grwtolake//​) specifies the portion of the produced regional groundwater flow which is led to the subbasins outlet lake. The part of the groundwater flow that is to go to the outlet lake is added to the lake volume in the routing part of the code.
  
  
Line 25: Line 24:
  
 ^Section ^Symbol ^Parameter/​Data ^File ^ ^Section ^Symbol ^Parameter/​Data ^File ^
-|Soil regional groundwater flow creation| |//grwtolake, grwdown//​|[[start:​hype_file_reference:​geodata.txt|GeoData.txt]]|+|Soil regional groundwater flow creation| |//grwolake, grwdown//​|[[start:​hype_file_reference:​geodata.txt|GeoData.txt]]|
 |:::​|//​rcgrw//​ |//​rcgrw//​|[[start:​hype_file_reference:​par.txt|par.txt]]| |:::​|//​rcgrw//​ |//​rcgrw//​|[[start:​hype_file_reference:​par.txt|par.txt]]|
 |:::​|//​wp(k)//​|//​wcwp,​ wcwp1, wcwp2, wcwp3//​|:::​| |:::​|//​wp(k)//​|//​wcwp,​ wcwp1, wcwp2, wcwp3//​|:::​|
Line 39: Line 38:
  
 ===== Aquifers ===== ===== Aquifers =====
 +
 +Aquifers are large water bodies covering several subbasins and located below the soillayers simulated by HYPE. They recieve water by percolation from land and river classes, and they return flow to a river (Figure 1). They can also be used as a water source for abstraction. The aquifer is a large water body that can have a passive volume partaking in mixing but not return flow (Figure 2).
 +
 +|{{:​start:​hype_model_description:​HYPE_box_picture_v3_aquifer.png?​400|}}|
 +|Figure 1 Water flows of aquifer.|
 +
 +|{{:​start:​hype_model_description:​aquifer2.png?​400|}}|
 +|Figure 2 Structure of an aquifer.|
 +
  
 ==== Deep percolation ==== ==== Deep percolation ====
Line 61: Line 69:
 ==== Deep percolation delay and aquifer recharge ==== ==== Deep percolation delay and aquifer recharge ====
  
-Deep percolation from soil and rivers in all recharge subbasins of an aquifer is added together. This total deep percolation (//qperc//) is delayed before it recharges the aquifer (//qrech//).+Deep percolation from soil and rivers in all recharge subbasins of an aquifer is added together. This total deep percolation (<​m>​q_{perc}<​/m>) is delayed before it recharges the aquifer (<​m>​q_{rech}<​/m>).
  
 <m> q_{rech}(t) = (1-coeff) * q_{perc}(t) + coeff * q_{rech}(t-1) </m> <m> q_{rech}(t) = (1-coeff) * q_{perc}(t) + coeff * q_{rech}(t-1) </m>
Line 71: Line 79:
 ==== Return flow from aquifer ==== ==== Return flow from aquifer ====
  
-Outflow from the aquifer depends on the water in the aquifer (//vol//) and a rate. The rate is determined by a aquifer property (//​retrate//​) and a regional adjustment parameter (//​aqretcor//,​ parameter region dependent).+Outflow from the aquifer depends on the water in the aquifer (//vol//) (not including passive volume) and a rate. The rate is determined by a aquifer property (//​retrate//​) and a regional adjustment parameter (//​aqretcor//,​ parameter region dependent).
  
  
Line 77: Line 85:
 \\ \\
  
-The outflow may be divided between several receiving subbasins (//​retfrac//​). The water is added to the inflow ​of the main river of these subbasins.+The outflow may be divided between several receiving subbasins (//​retfrac//​). The receiving subbasins may or may not be different from the subbasin recharging the aquifer. The specified fraction of outflow ​is added to the inflow ​to the main river of these subbasins.
  
-The return flow is added to the main river of the receiving subbasin.+It is possible ​to simulate that (part of) the aquifer'​s outflow leads to outside ​of the modelled domain (sum of retfrac less than 1). It is possible to simulate addition of water (from aquifers) from outside the model domain to the model as aquifer recharge by upscaling the recharge calculated for an aquifer in the model set-up (sum of retfrac larger than one).
  
 ==== Nutrient processes related to aquifers ==== ==== Nutrient processes related to aquifers ====
  
-The organic nitrogen, particulate phosphorus, and organic carbon in water percolating from soil and river stay in the soil/river, while temperature,​ inorganic nitrogen and SRP follow the water to the aquifer. Inorganic nitrogen is subjected to denitrification in the aquifer (see Chapter [[start:​hype_model_description:​hype_np_soil#​denitrification|Nitrogen and phosphorus in land routines - Denitrification]]).+For most models the organic nitrogen, particulate phosphorus, and organic carbon in water percolating from soil and river stay in the soil/river, while temperature,​ inorganic nitrogen and SRP follow the water to the aquifer. ​In the case of a model using the simplified soil model based on travel time through soil and half life of pollutants (i.e. using load as input to HYPE) all substances follow the water to the aquifer.  
 + 
 +Inorganic nitrogen is subjected to denitrification in the aquifer (see Chapter [[start:​hype_model_description:​hype_np_soil#​denitrification|Nitrogen and phosphorus in land routines - Denitrification]]). For other substances an exponential decay can be applied in the aquifer. The process is goverened by the model parameter //decay// (e.g. ''​ppdecaq''​),​ which denote the half life of the substance in days. The decay will decrease the concentration (//conc//) of the substance in the aquifer. 
 + 
 +<m> conc = conc *  2 ^ {-ts/decay} </​m>​ 
 +where //ts// is length of time step in days. 
 + 
 +==== Abstraction from aquifers ==== 
 + 
 +Aquifers can be used for abstraction of water. The abstraction is defined through PointSourceData for a subbasin. The water is removed from the aquifer below that subbasin. Water is taken from the aquifer water volume. This means that also water from the passive volume can be removed.
  
 ==== Links to file reference ==== ==== Links to file reference ====
Line 89: Line 106:
 ^Section ^Symbol ^Parameter/​Data ^File ^ ^Section ^Symbol ^Parameter/​Data ^File ^
 |Aquifers| |//aquid, subid, parreg//​|[[start:​hype_file_reference:​aquiferdata.txt|AquiferData.txt]]| |Aquifers| |//aquid, subid, parreg//​|[[start:​hype_file_reference:​aquiferdata.txt|AquiferData.txt]]|
-|:::​|:::​|//​basedepth,​ inidepth, porosity, area//|:::|+|:::​|:::​|//​basedepth, passivedep, inidepth, porosity, area//|:::|
 |Deep percolation|<​m>​rc_{grw}</​m>​ calculated from|//​rcgrw,​ rcgrwst, aqpercorr//​|[[start:​hype_file_reference:​par.txt|par.txt]]| |Deep percolation|<​m>​rc_{grw}</​m>​ calculated from|//​rcgrw,​ rcgrwst, aqpercorr//​|[[start:​hype_file_reference:​par.txt|par.txt]]|
 |:::​|//​wp//​|//​wcwp,​ wcwp1, wcwp2, wcwp3//​|:::​| |:::​|//​wp//​|//​wcwp,​ wcwp1, wcwp2, wcwp3//​|:::​|
Line 100: Line 117:
 |Nutrient processes related to aquifers| |//​topdepth,​ temp, conc_IN, conc_SP//​|[[start:​hype_file_reference:​aquiferdata.txt|AquiferData.txt]]| |Nutrient processes related to aquifers| |//​topdepth,​ temp, conc_IN, conc_SP//​|[[start:​hype_file_reference:​aquiferdata.txt|AquiferData.txt]]|
 |:::​|:::​|//​denitaq,​ hsatINs, wcep, wcfc, wcwp//​|[[start:​hype_file_reference:​par.txt|par.txt]]| |:::​|:::​|//​denitaq,​ hsatINs, wcep, wcfc, wcwp//​|[[start:​hype_file_reference:​par.txt|par.txt]]|
 +|:::​|//​decay//​|//​ondecaq,​ spdecaq, ppdecaq, ocdecaq, ssdecaq, aedecaq, t1decaq//​|[[start:​hype_file_reference:​par.txt|par.txt]]|
  
  
Line 117: Line 135:
 | ::: | ::: | nutrient processes related to aquifers | | ::: | ::: | nutrient processes related to aquifers |
 | ::: | set_percolation_concentration | nutrient processes related to aquifers | | ::: | set_percolation_concentration | nutrient processes related to aquifers |
 +| [[http://​hype.sourceforge.net/​doxy-html/​namespacenpc__soil__processes.html|npc_soil_processes (npc_soil_proc.f90)]]| soil_denitrification | nutrient processes related to aquifers |
 +| [[http://​hype.sourceforge.net/​doxy-html/​namespacegeneral__functions.html|general_functions (general_func.f90)]]| exponential_decay | ::: |
  
  
  
  
start/hype_model_description/aquifier.1583914084.txt.gz · Last modified: 2023/11/16 14:28 (external edit)