You’re offline. This is a read only version of the page.
Please wait...
×
Error
X
Toggle navigation
Download Center
Download Center
MIKE 2025
Scientific Publications
Knowledge Base
Contact Support
Contact Sales
Contact Sales
Service and Maintenance Agreements
Knowledge Articles
All
Forums
Knowledge Articles
Search Filter
Knowledge Articles
Forums
Knowledge Articles
Search all support and community content
Sign in
DHI Group
MIKE Powered by DHI
DHI Training Portal
Metocean Data Portal
Bathymetrics Data Portal
MIKE Cloud Admin
Home
Access Denied
FEFLOW
Darcy Flux (nodal)
Darcy Flux (nodal)
Posted
Wed, 19 Apr 2017 18:12:34 GMT
by
Steffen Beck-Broichsitter
Represent the Darcy fluxes in m/d the saturated and/or the unsaturated conditions or rather the saturated and/or the unsaturated hydraulic conductivity?
Best regards from Northern Germany!
Posted
Wed, 26 Apr 2017 07:36:06 GMT
by
Björn Kaiser
The Richards equation is reduced to the Darcy equation within domains where the system is saturated. The Darcy flux in the Data Panel can be used to plot the vector in both saturated and unsaturated domains.
You must be signed in to post in this forum.