Skip to main content

Browse the archive

https://gitlab.opengeosys.org/ogs/ogs.git
28 March 2024, 10:48:24 UTC
Revision 69ca768c760c492caa2a825fea3b9e22fa5d4c69 authored by Dmitri Naumov on 04 October 2023, 08:29:10 UTC, committed by Dmitri Naumov on 05 October 2023, 13:14:07 UTC 
[T/THM] Heat transport in stationary flow w/ ice
 
Presence of ice phase at slightly positive temperatures with shallow
sigmoid function for ice phase should not affect the results much but
only for amount of ice formed. In the simulation the initial ice volume
fraction is 0.0379... . Displacement and stress are read from previous
simulation's steady-state result.

Incorrect update of phi_fr_prev causes pressure to drop significantly in
the first step, which is unexpected, since everything is in equilibrium.
Temperature load starts only after 10 steps at t=10000s.
1 parent 277410a
Raw File
Tip revision: 69ca768c760c492caa2a825fea3b9e22fa5d4c69 authored by Dmitri Naumov on 04 October 2023, 08:29:10 UTC
[T/THM] Heat transport in stationary flow w/ ice
Tip revision: 69ca768
.codespellexclude 
* De Nevers N. Physical and chemical equilibrium for chemical engineers[M].
        "\tthe command must be run with its full path.\n\n"
        COO = 10,
              var dateA = new Date(a.created_at);
              var dateB = new Date(b.created_at);
              return dateB - dateA;
Malcom, M.A.M.(2018).Analysis of underground excavations in argillaceous hard
    auto Ket = local_K.template block<temperature_size, temperature_size>(
        Ket.noalias() +=
        title: '{Entwicklung mathematisch-mechanischer Modelle zur Beschreibung des
            Stoffverhaltens von Salzgestein in Abh{\"a}ngigkeit von der Zeit und der
            Temperatur auf der Grundlage von Laborversuchen mit begleitenden kontinuumsmechanischen
            Berechnungen nach der Methode der finiten Elemente}'
- _Dupuit J. Mouvement de l’eau a travers le terrains permeables. C. R. Hebd. Seances Acad. Sci., 45:92–96, 1857._
back to top