Hydraulic conductivity with thickness md (Terrain Attribute): Difference between revisions
Jump to navigation
Jump to search
Created page with "{{terrain attributes | <onlyinclude> {{terrain attributes|type=row|overlay=Water |attribute=HYDRAULIC_CONDUCTIVITY_WITH_THICKNESS_MD |unit=m2/day |layer=ground |description=The hydraulic conductivity (symbolically represented as KD) is defined as the speed by which water moves through the saturated layer horizontally, multiplied with the layer thickness. |icon=waterwizard_icon_water_hydraulic_conductivity.png }}</onlyinclude> }}" |
No edit summary |
||
| (6 intermediate revisions by 2 users not shown) | |||
| Line 1: | Line 1: | ||
{{terrain attributes | {{terrain attributes | ||
| <onlyinclude> | | <onlyinclude> | ||
{{terrain attributes|type=row | {{terrain attributes|type=row | ||
|attribute=HYDRAULIC_CONDUCTIVITY_WITH_THICKNESS_MD | |attribute=HYDRAULIC_CONDUCTIVITY_WITH_THICKNESS_MD | ||
|unit=m2/day | |unit=m2/day | ||
|layer= | |layer=Ground | ||
|description= | |description=This attribute represents the horizontal hydraulic conductivity (KD) of the saturated layer multiplied by the layer thickness. | ||
|icon=waterwizard_icon_water_hydraulic_conductivity.png | |icon=waterwizard_icon_water_hydraulic_conductivity.png | ||
}}</onlyinclude> | }}</onlyinclude> | ||
}} | }} | ||
{{Terrain attribute details | |||
| static= | |||
| usages= * [[Terrain hydraulic conductivity with thickness md (Water Overlay)]] | |||
| specifics= | |||
| notes= | |||
| references= | |||
| seealso=* [[Terrain Attributes]] | |||
| api=* [[Api session event editor terraintype]] | |||
* [[Api session event editor terraintype set attribute]] | |||
* [[Api session event editor terraintype set attributes]] | |||
}} | |||
[[Category:Terrain]] | |||
Latest revision as of 09:18, 10 July 2026
| Icon | Attribute | Unit | Layer | Range | Description |
|---|---|---|---|---|---|
| |
HYDRAULIC_CONDUCTIVITY_WITH_THICKNESS_MD | m2/day | Ground | This attribute represents the horizontal hydraulic conductivity (KD) of the saturated layer multiplied by the layer thickness. |