From b214ffe805f59718711a9e3a3fe92a6ab4c22670 Mon Sep 17 00:00:00 2001 From: Luca Heltai Date: Wed, 26 Feb 2025 16:55:13 +0100 Subject: [PATCH] Apply suggestions from code review Co-authored-by: Marc Fehling --- doc/doxygen/references.bib | 7 +++++-- examples/step-34/doc/intro.dox | 2 +- 2 files changed, 6 insertions(+), 3 deletions(-) diff --git a/doc/doxygen/references.bib b/doc/doxygen/references.bib index 02a9be6983..8e43ce46e9 100644 --- a/doc/doxygen/references.bib +++ b/doc/doxygen/references.bib @@ -377,7 +377,8 @@ @book{Newman1977, author = {J. N. Newman}, title = {Marine Hydrodynamics}, - journal = {}, + url = {https://mitpress.mit.edu/9780262534826/marine-hydrodynamics/}, + publisher = {The MIT Press}, year = 1977 } @@ -385,7 +386,9 @@ @article{HeltaiBangerthKronbichler-2021, author = {Luca Heltai and Wolfgang Bangerth and Martin Kronbichler and Andrea Mola}, journal = {Transactions on Mathematical Software}, - month = {December}, + month = dec, + url = {https://dl.acm.org/doi/10.1145/3468428}, + doi = {10.1145/3468428}, number = {4}, pages = {1--30}, title = {Propagating geometry information to finite element computations}, diff --git a/examples/step-34/doc/intro.dox b/examples/step-34/doc/intro.dox index 6e46d1528d..fc67913ff4 100644 --- a/examples/step-34/doc/intro.dox +++ b/examples/step-34/doc/intro.dox @@ -680,4 +680,4 @@ $\phi = -x/2$. In the test problem, the flow is unitary in each coordinate direction, i.e., $(1,1)$ in dimension two and $(1,1,1)$ in dimension #3#, so the appropriate exact solution on the surface of the sphere is the superposition of the above solution with the analogous solutions along the other axes, or $\phi = -(x + y)$ in dimension two and $\phi = \frac{1}{2}(x + y + z)$ in dimension three. \ No newline at end of file +(x + y)$ in dimension two and $\phi = \frac{1}{2}(x + y + z)$ in dimension three. -- 2.39.5