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Diffstat (limited to 'Master/texmf-dist/doc/latex/mitthesis/MIT-thesis-template/chapter1.tex')
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1 files changed, 12 insertions, 11 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..1f2acd20a6d 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: 1.06, 2024/07/09 % Documentation: https://ctan.org/pkg/mitthesis @@ -7,11 +7,11 @@ \lipsum[1-2] Postremo aliquos futuros suspicor, qui me ad alias litteras vocent, genus hoc scribendi, etsi sit elegans, personae tamen et dignitatis esse negent~\cite{DKE1969,ww1920,kirk2288a,churchill1948,gibbs1863}. -\section[A section discussing the first issue: \(J/\psi\)]{A section discussing the first issue: \ifpdftex\(\bm{J}/\bm{\psi}\)\else{\(\symbfup{J/\psi}\)}\fi} +\section[A section discussing the first issue: \(J/\psi\)]{A section discussing the first issue: \ifpdftex\(\bm{J}/\bm{\psi}\)\else{\(\symbfit{J/\psi}\)}\fi} 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 \\ |