diff --git a/nass-uniaxial-model.org b/nass-uniaxial-model.org
index 57d4634..07a3a32 100644
--- a/nass-uniaxial-model.org
+++ b/nass-uniaxial-model.org
@@ -85,6 +85,15 @@
 (setq org-export-before-parsing-hook '(org-ref-glossary-before-parsing
                                        org-ref-acronyms-before-parsing))
 #+END_SRC
+#+begin_src emacs-lisp
+(org-export-define-derived-backend 'my-org 'org
+:translate-alist '((link . nil)(latex-fragment . nil)(latex-environment . nil)(special-block . nil)
+(table . nil)
+(property-drawer . nil)))
+#+end_src
+#+begin_src emacs-lisp
+(org-export-to-file 'my-org "text.org")
+#+end_src
 
 * Notes                                                             :noexport:
 Prefix is =uniaxial=
@@ -6184,5 +6193,5 @@ colors = colororder;
 * Footnotes
 
 [fn:3]DLPVA-100-B from Femto with a voltage input noise is $2.4\,nV/\sqrt{\text{Hz}}$
-[fn:2]Mark Product L-22D geophones are used with a sensitivity of $88\,\frac{V}{m/s} and a natural frequency of $\approx 2\,\text{Hz}$
+[fn:2]Mark Product L-22D geophones are used with a sensitivity of $88\,\frac{V}{m/s}$ and a natural frequency of $\approx 2\,\text{Hz}$
 [fn:1]Mark Product L4-C geophones are used with a sensitivity of $171\,\frac{V}{m/s}$ and a natural frequency of $\approx 1\,\text{Hz}$
diff --git a/nass-uniaxial-model.pdf b/nass-uniaxial-model.pdf
index c6edb8f..8cc5981 100644
Binary files a/nass-uniaxial-model.pdf and b/nass-uniaxial-model.pdf differ
diff --git a/nass-uniaxial-model.tex b/nass-uniaxial-model.tex
index 1d3940d..a80604e 100644
--- a/nass-uniaxial-model.tex
+++ b/nass-uniaxial-model.tex
@@ -1,4 +1,4 @@
-% Created 2024-05-02 Thu 12:04
+% Created 2024-11-05 Tue 13:26
 % Intended LaTeX compiler: pdflatex
 \documentclass[a4paper, 10pt, DIV=12, parskip=full, bibliography=totoc]{scrreprt}
 
@@ -38,7 +38,7 @@
  pdftitle={Nano Active Stabilization System - Uniaxial Model},
  pdfkeywords={},
  pdfsubject={},
- pdfcreator={Emacs 29.3 (Org mode 9.6)}, 
+ pdfcreator={Emacs 29.4 (Org mode 9.6)}, 
  pdflang={English}}
 \usepackage{biblatex}
 
@@ -213,7 +213,7 @@ For further analysis, 9 ``configurations'' of the uniaxial NASS model of Figure
 \end{figure}
 \chapter{Disturbance Identification}
 \label{sec:uniaxial_disturbances}
-To quantify disturbances (red signals in Figure \ref{fig:uniaxial_model_micro_station_nass}), three geophones\footnote{Mark Product L-22D geophones are used with a sensitivity of \$88$\backslash$,\frac{V}{m/s} and a natural frequency of \(\approx 2\,\text{Hz}\)} are used.
+To quantify disturbances (red signals in Figure \ref{fig:uniaxial_model_micro_station_nass}), three geophones\footnote{Mark Product L-22D geophones are used with a sensitivity of \(88\,\frac{V}{m/s}\) and a natural frequency of \(\approx 2\,\text{Hz}\)} are used.
 One is located on the floor, another one on the granite, and the last one on the micro-hexapod's top platform (see Figure \ref{fig:uniaxial_ustation_meas_disturbances}).
 The geophone located on the floor was used to measure the floor motion \(x_f\) while the other two geophones were used to measure vibrations introduced by scanning of the \(T_y\) stage and \(R_z\) stage (see Figure \ref{fig:uniaxial_ustation_dynamical_id_setup}).