Specifying the topology of the river link via a cross-section is the first step in setting up the GN1D model.
Edit Cross Section
Opens the cross-section editor
Clear Cross Section
Deletes the cross-section.
Common Controls
These parameters are common with the GAT (Analytical Tool) saturated connection model.
Transmissivity
The rate at which groundwater flows horizontally in an aquifer. The transmissivity for horizontal flow of an aquifer with saturated thickness and horizontal conductivity is:
For an unconfined aquifer, d is the average saturated thickness.
Specific yield
A ratio indicating the volumetric fraction that an aquifer will yield when all water is allowed to drain out of it under the force of gravity:
is the volume of water drained
is the total volume of the aquifer material
River to No-flow Boundary
The distance from the left and right hand river banks to the groundwater no-flow boundary
Model Parameters
Additional parameters saturated zone, which are required for the finite difference scheme.
Divisions per Bank
The number of subdivisions per bank.
Aquifer Floor
The z-coordinate of the aquifer basement (no-flow boundary). Uses the coordinate system defined by the cross section.
Init. Height Method
The method by which the initial groundwater table height is calculated. The two options are:
Input
Height at t = 0
1.3.1 Option 1: Input
Init. Height
The initial groundwater table height in the coordinate system of the cross section.
Option 2: Height at t = 0
The initial groundwater table height is set to the initial river stage.
Infiltration Parameters
Unsaturated zone parameters
Init. Soil Moisture
The initial soil moisture content of the unsaturated zone as volumetric fraction of the total volume.
Sat. Soil Moisture
The saturated soil moisture content as a volumetric fraction.
Field soil moisture is the amount of water that will be retained in the soil if it is allowed to drain under the force of gravity. It can be calculated as:
Field Soil Moisture = Sat. Soil Moisture – Specific Yield
Field soil moisture is displayed in the user interface but is not editable.
Field Soil Moisture
Field soil moisture is displayed in the user interface but is not editable.
Field soil moisture is the amount of water that will be retained in the soil if it is allowed to drain under the force of gravity. It can be calculated as:
Field Soil Moisture = Sat. Soil Moisture – Specific Yield
Saturated Vertical hydraulic conductivity
The saturated vertical hydraulic conductivity.
Average Suction
The average suction at the wetted front.
Soil Evaporation Parameters
Parameters for setting the maximum depth at which evapotranspiration can occur.
Extinction Depth
Sets the method by which the evapotranspiration extinction depth will be calculated. The extinction depth is the maximum depth below the ground surface at which evapotranspiration can occur. The two options are:
Calculation Depth
Input Depth
Option 1: Calculation Depth
The evapotranspiration extinction depth is estimated from soil type and ground cover.
Soil Type
The soil type
Ground Cover
The type of ground cover
Option 2: Input Depth
The evapotranspiration extinction depth is input by the user.
Depth
The maximum depth below the ground surface at which evapotranspiration can occur.