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
test_cases:two [2014/05/20 10:32]
grenier
test_cases:two [2015/01/09 16:10] (current)
grenier
Line 3: Line 3:
 Test Case T2 is a further step towards the full set of coupled equations. It is limited to the heat transfer equation solely with conduction and phase change.  Test Case T2 is a further step towards the full set of coupled equations. It is limited to the heat transfer equation solely with conduction and phase change. 
  
-{{:test_cases:equations1.jpg?300|}}+{{ equations1.jpg?300 }}
  
-The system consists of a 1D vertical soil column with heterogeneous porous medium properties and geothermal flux. A step temperature is imposed for a column initially in balance with geothermal flux.  +This test case is still under discussion. The system would consists of a 1D vertical soil column with heterogeneous porous medium properties and geothermal flux. A step temperature could be imposed for a column initially in balance with geothermal flux. We could deal with a fully saturated column or wait from later stages of the Benchmark dealing with a non saturated medium and for instance Richards equations. 
  
-{{:test_cases:t2geom.png?100|}}+{{ test_cases:t2geom.png?100 }} 
 + 
 +Please contact us if you are interested.