Hydrological attributes of terrains (Water Overlay): Difference between revisions

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[[Terrain]]s in a project have a number of hydrological properties which can influence the flow of water in a project. Because there is always both surface and underground terrain defined for the entirety of the project area, all cells are affected by all properties of terrains, unless a [[hydrological attributes of constructions (Water Overlay)|construction]] is present with overwriting values.
[[Terrain]]s in a project have a number of hydrological properties which can influence the flow of water in a project. Because there is always both surface and underground terrain defined for the entirety of the project area, all cells are affected by all properties of terrains, unless a [[hydrological attributes of constructions (Water Overlay)|construction]] is present with overwriting values.
{{terrain attributes|suppresscategory=true|allowselflinks=true|
{{:terrain water (Water Overlay)}}
{{:terrain root depth m (Water Overlay)}}
{{:terrain water evaporation factor (Water Overlay)}}
{{:terrain water storage percentage (Water Overlay)}}
{{:terrain ground infiltration md (Water Overlay)}}
{{:terrain water manning (Water Overlay)}}
}}


{| class="wikitable"
{{article end
! Icon
|notes=
! Attribute
! Unit
! Type
! Description
|-
|
|[[Terrain_water_(Water_Overlay)|WATER]]
|boolean
|Surface
|Whether the specified terrain is a water terrain.
|-
|
|[[Terrain_root_depth_m_(Water_Overlay)|ROOT_DEPTH_M]]
|m
|Surface
|The depth of the roots of this surface terrain, relative to the surface. Water can be drawn from the underground and evaporated if the roots can reach it.
|-
|[[File:waterwizard_icon_evaporation_factor.png]]
|[[Terrain_water_evaporation_factor_(Water_Overlay)|WATER_EVAPORATION_FACTOR]]
|factor
|Surface
|How fast this terrain can evaporate water from the underground. The [[weather (Water Overlay)|weather]] evaporation speed is multiplied by this factor to determine the rate of evaporation.
|-
|
|[[Terrain_water_storage_percentage_(Water_Overlay)|WATER_STORAGE_PERCENTAGE]]
|fraction
|Underground
|The percentage (as a fraction) of the underground volume which can be filled with water. A lower percentage means the underground will be able to store less water, and the saturated zone will rise higher with the same amount of water in the underground layer.
|-
|[[File:waterwizard_icon_water_infiltration.png]]
|[[Terrain_ground_infiltration_md_(Water_Overlay)|GROUND_INFILTRATION_MD]]
|m/day
|Surface
|The speed at which water can flow vertically from the surface to the underground unsaturated zone.
|-
|[[File:waterwizard_icon_water_infiltration.png]]
|[[Terrain_ground_infiltration_md_(Water_Overlay)|GROUND_INFILTRATION_MD]]
|m/day
|Underground
|The speed at which water can flow vertically from the underground unsaturated zone to the underground saturated zone, and horizontally through across the saturated zone.
|-
|[[File:waterwizard_icon_manning.png]]
|[[Terrain_water_manning_(Water_Overlay)|WATER_MANNING]]
|s/(m<sup>1/3</sup>)
|Surface
|The Gauckler–Manning coefficient of the terrain.
|}
==Notes==
* In general, surface terrain attributes can be overridden by [[hydrological attributes of constructions (Water Overlay)|attributes of construction]]s on the surface, even when the attribute values of the construction are set to 0.
* In general, surface terrain attributes can be overridden by [[hydrological attributes of constructions (Water Overlay)|attributes of construction]]s on the surface, even when the attribute values of the construction are set to 0.
}}


{{WaterOverlay terrain attribute nav}}
{{WaterOverlay terrain attribute nav}}
[[Category:Water Module]]
[[Category:Water Module]]

Revision as of 07:30, 3 September 2020

Terrains in a project have a number of hydrological properties which can influence the flow of water in a project. Because there is always both surface and underground terrain defined for the entirety of the project area, all cells are affected by all properties of terrains, unless a construction is present with overwriting values.

Icon Attribute Unit Layer Range Description
WATER nominal Surface Whether this Terrain Type represents a form of water (and what type).
Waterwizard icon water root depth m.png ROOT_DEPTH_M m Surface The depth of the roots of the terrain type. This depth is used to determine whether evaporation will occur from the groundwater.
Waterwizard icon evaporation factor.png WATER_EVAPORATION_FACTOR factor Surface How fast this terrain can evaporate water from the ground. The weather's evaporation speed is multiplied by this factor to determine the rate of evaporation.
Waterwizard icon water storage.png WATER_STORAGE_PERCENTAGE fraction (m3/m3) Ground The percentage (as a fraction) of the ground layer volume which can be filled with water. A lower percentage means the ground layer will be able to store less water, and the saturated zone will rise higher with the same amount of water in the ground layer.
Waterwizard icon water infiltration.png GROUND_INFILTRATION_MD m/day Surface 0 to 10 The speed at which water can flow vertically from the surface to the unsaturated zone.
Waterwizard icon water infiltration.png GROUND_INFILTRATION_MD m/day Ground 0 to 10 The speed at which water can flow vertically from the surface to the unsaturated zone.
Waterwizard icon manning.png WATER_MANNING s/(m1/3) Surface The Gauckler–Manning coefficient of the terrain, which is a measure of surface roughness. Used in the surface flow computation of the Water Overlay.

Notes

  • In general, surface terrain attributes can be overridden by attributes of constructions on the surface, even when the attribute values of the construction are set to 0.
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Terrain attributes
Ground infiltration md •  Hydraulic conductivity md •  Hydraulic conductivity with thickness md •  Root depth m •  Water •  Water evaporation factor •  Water manning •  Water microrlief m •  Water storage percentage
Related
Building attributes • Hydrological features • Hydraulic structures • Model attributes • Results • Simulation data
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