From f1a4fa6bf2966b17a59be791f43df10bae19ba48 Mon Sep 17 00:00:00 2001
From: Benjamin Faigle <benjamin.faigle@posteo.de>
Date: Wed, 16 Oct 2013 09:31:06 +0000
Subject: [PATCH] add 3D L-method for 2p and subTimeStepping to Changelog.
git-svn-id: svn://svn.iws.uni-stuttgart.de/DUMUX/dumux/trunk@11667 2fb0f335-1f38-0410-981e-8018bf24f1b0
---
CHANGELOG | 8 ++++++++
1 file changed, 8 insertions(+)
diff --git a/CHANGELOG b/CHANGELOG
index f891bc41a6..46cd6af45d 100644
--- a/CHANGELOG
+++ b/CHANGELOG
@@ -22,6 +22,10 @@ Differences Between DuMuX 2.3 and DuMuX 2.4
the fluid phase is admitted to consist of two components.
. el2p: poroelasticity equations for one solid phase and two immiscible
fluid phases.
+
+ - A three-dimensional implementation of the MPFA L-method is added and made
+ available for the decoupled 2p models. It also allows for simulation on
+ an adaptive grid.
- The MPNC model now allows to drop the assumptions of local thermal and/or
chemical equilibrium. Dropping the local chemical equilibrium assumption
@@ -39,6 +43,10 @@ Differences Between DuMuX 2.3 and DuMuX 2.4
incorporated into the local residual in a weak sense. Only for mixed
Dirichlet/Neumann conditions and for the MPNC model, they still are
incorporated in a strong sense.
+
+ - The sequential models can use a sub-timestepping in the transport scheme, if
+ the property "SubCFLFactor" is chosen smaller than "CFLFactor", which in
+ that case specifies the CFL factor used in the pressure equation.
- All fully-implicit porous-media models now provide the possibility to write
the velocities to the VTK output. This can be achieved by setting the
--
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