From a40eab950360c2b50e0dd3f252c70da4173eccee Mon Sep 17 00:00:00 2001
From: Menno Fraters <menno.fraters@outlook.com>
Date: Fri, 17 Jan 2020 11:38:00 -0800
Subject: [PATCH] fix fieldstone manual latex compilation.

---
 gravity.tex                         | 4 ++--
 oldies.tex                          | 2 +-
 python_codes/fieldstone_59/text.tex | 2 +-
 python_codes/gravity_01/text.tex    | 4 ++--
 4 files changed, 6 insertions(+), 6 deletions(-)

diff --git a/gravity.tex b/gravity.tex
index 7e18def99..732ce595f 100644
--- a/gravity.tex
+++ b/gravity.tex
@@ -207,10 +207,10 @@
 \textrm{for} \; l=0,1,2,3,... \; \textrm{and} \; m=-l,-l+1,...,l-1,l
 \label{eq:spha5}
 \end{equation}
-The phase factor (−1) , introduced originally by Condon and Shortley, is convenient for
+The phase factor (-1) , introduced originally by Condon and Shortley, is convenient for
 applications in quantum mechanics. Note that eq. (\ref{eq:spha4}) implies that
 \[
-Y_l^{−m} (\theta, \phi) = (−1)^m Y_l^m (\theta,\phi)^∗ 
+Y_l^{-m} (\theta, \phi) = (-1)^m Y_l^m (\theta,\phi)^* 
 \]
 where the star means complex conjugation.
 
diff --git a/oldies.tex b/oldies.tex
index c6e5d5fba..1fb04821a 100644
--- a/oldies.tex
+++ b/oldies.tex
@@ -131,7 +131,7 @@
 
 \begin{center}
 \includegraphics[height=6cm]{images/history/nesb99}\\
-{\captionfont 1989: Model geometry, boundary conditions and 3-D ¢nite element mesh used in 
+{\captionfont 1989: Model geometry, boundary conditions and 3-D finite element mesh used in 
 the calculations. The circles denote a free-slip condition. The arrow denotes the velocity 
 applied in some calculations to the southern boundary of the Tyrrhenian domain to simulate 
 the motion of the African plate. The springs represent the buoyant restoring force applied 
diff --git a/python_codes/fieldstone_59/text.tex b/python_codes/fieldstone_59/text.tex
index 87109c50d..9f64ad0bc 100644
--- a/python_codes/fieldstone_59/text.tex
+++ b/python_codes/fieldstone_59/text.tex
@@ -127,7 +127,7 @@
 $p$ is the grain size exponent, $Q$ is the activation energy for the creep 
 mechanism at stake (J$\cdot$mol$^{-1}$ ), $p$ is the hydrostatic pressure (MPa), 
 $V$ the activation volume (m$^3\cdot$mol$^{-1}$), 
-$R$ is the gas constant (J$\cdot$K$^{−1}\cdot$mol$^{-1}$), and $T$ the absolute temperature (K). 
+$R$ is the gas constant (J$\cdot$K$^{-1}\cdot$mol$^{-1}$), and $T$ the absolute temperature (K). 
 The effect of $pV$ is assumed to be very small \cite{dust01} 
 and is ignored for the remainder of this work.
 
diff --git a/python_codes/gravity_01/text.tex b/python_codes/gravity_01/text.tex
index 40449b1d9..bc53c47ba 100644
--- a/python_codes/gravity_01/text.tex
+++ b/python_codes/gravity_01/text.tex
@@ -10,7 +10,7 @@
 The horizontal spacing between nodes is $hx$ and the vertical spacing is $hy$.
 
 \begin{center}
-\includegraphics[width=7cm]{/home/cedrict/Desktop/FIELDSTONE/fieldstone/python_codes/gravity_01/images/drawing}
+\includegraphics[width=7cm]{python_codes/gravity_01/images/drawing}
 \end{center}
 
 Assume that this domain is filled with a rock type which 
@@ -65,7 +65,7 @@
 measured at each gravimeter at the surface. 
 
 \begin{center}
-\includegraphics[width=12cm]{/home/cedrict/Desktop/FIELDSTONE/fieldstone/python_codes/gravity_01/solution.pdf}
+\includegraphics[width=12cm]{python_codes/gravity_01/solution.pdf}
 \end{center}