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-rw-r--r--Master/texmf-dist/doc/latex/mitthesis/MIT-thesis-template/chapter1.tex21
1 files changed, 11 insertions, 10 deletions
diff --git a/Master/texmf-dist/doc/latex/mitthesis/MIT-thesis-template/chapter1.tex b/Master/texmf-dist/doc/latex/mitthesis/MIT-thesis-template/chapter1.tex
index cc7683744ec..481e96a4c4e 100644
--- a/Master/texmf-dist/doc/latex/mitthesis/MIT-thesis-template/chapter1.tex
+++ b/Master/texmf-dist/doc/latex/mitthesis/MIT-thesis-template/chapter1.tex
@@ -1,5 +1,5 @@
% From mitthesis package
-% Version: 1.04, 2023/10/19
+% Version: 1.05, 2023/11/03
% Documentation: https://ctan.org/pkg/mitthesis
@@ -11,7 +11,7 @@
We begin with some ideas from the literature \cite{Fong2015,sharpe1}.
-\begin{equation}
+\begin{equation}\label{eqn:1}
\frac{\partial}{\partial t}\left[\rho\bigl(e + \lvert\vec{u}\rvert^2\big/2\bigr)\right] + \nabla\cdot\left[\rho\bigl(h + \lvert\vec{u}\rvert^2\big/2 \bigr)\vec{u}\right]
={}-\nabla \cdot \vec{q} + \rho \vec{u}\cdot\vec{g}+ \frac{\partial}{\partial x_j}\bigl(d_{ji}u_i\bigr)
\end{equation}
@@ -37,7 +37,8 @@ We begin with some ideas from the literature \cite{Fong2015,sharpe1}.
\lipsum[4]
-\subsection{Subsection~eqn.~\eqref{eqn:WT1}}
+%% note use of \ref* here to avoid placing a nested link in the table of contents
+\subsection[Subsection~eqn.~(\ref*{eqn:WT1})]{Subsection~eqn.~\eqref{eqn:WT1}}
\lipsum[5-6]
\subsubsection{A subsubsection}
@@ -84,9 +85,9 @@ L(\ifpdftex\bm{A}\else\symbfup{A}\fi) = \begin{pmatrix}
\ce{SO4^2- + Ba^2+ -> BaSO4 v} \\[0.5em]
\ce{Zn^2+
<=>[+ 2OH-][+ 2H+]
-$\underset{\text{amphoteric hydroxide}}{\ce{Zn(OH)2 v}}$
+$\underset{\textrm{amphoteric hydroxide}}{\ce{Zn(OH)2 v}}$
<=>[+ 2OH-][+ 2H+]
-$\underset{\text{tetrahydroxozincate}}{\ce{[Zn(OH)4]^2-}}$
+$\underset{\textrm{tetrahydroxozincate}}{\ce{[Zn(OH)4]^2-}}$
}
\end{gather}
These examples of chemical formul\ae\ are copied directly from the documentation of the \texttt{mhchem} package, which was used to typeset them.
@@ -94,7 +95,7 @@ These examples of chemical formul\ae\ are copied directly from the documentation
\section{Baroclinic generation of vorticity\label{sec:stratified-flow}}
Substitution of the particle acceleration and application Stokes theorem leads to the \textit{Kelvin-Bjerknes circulation theorem}, for
-$\rho \neq \text{fn}(p)$:
+$\rho \neq \textrm{fn}(p)$:
\begin{align}
\frac{d\Gamma}{dt} &{}= \frac{d}{dt} \int_{\mathcal{C}} \mathbf{u} \cdot d\mathbf{r}\\
&{}= \int_{\mathcal{C}} \frac{D\mathbf{u}}{Dt} \cdot d\mathbf{r} + \underbrace{\int_{\mathcal{C}} \mathbf{u}\cdot d\biggl( \frac{d\mathbf{r}}{dt}\Biggr)}_{=\, 0} \\[-2pt]
@@ -130,11 +131,11 @@ Baroclinic generation of vorticity accounts for the sea breeze and various other
\\[-0.5em]
\toprule
\multicolumn{1}{@{\hspace*{1.5em}}c}{$x$\rule{0pt}{8pt}} &
-\multicolumn{1}{c}{$\text{erf}(x)$} &
-\multicolumn{1}{c!{\hspace*{3.em}}}{$\text{erfc}(x)$} &
+\multicolumn{1}{c}{$\textrm{erf}(x)$} &
+\multicolumn{1}{c!{\hspace*{3.em}}}{$\textrm{erfc}(x)$} &
\multicolumn{1}{c}{$x$} &
-\multicolumn{1}{c}{$\text{erf}(x)$} &
-\multicolumn{1}{c@{\hspace*{1.5em}}}{$\text{erfc}(x)$} \\ \midrule
+\multicolumn{1}{c}{$\textrm{erf}(x)$} &
+\multicolumn{1}{c@{\hspace*{1.5em}}}{$\textrm{erfc}(x)$} \\ \midrule
0.00 & 0.00000 & 1.00000 & 1.10 & 0.88021 & 0.11980 \\
0.05 & 0.05637 & 0.94363 & 1.20 & 0.91031 & 0.08969 \\
0.10 & 0.11246 & 0.88754 & 1.30 & 0.93401 & 0.06599 \\