diff --git a/bench/barite/README.org b/bench/barite/README.org
index bce368b0f..180c3c4de 100644
--- a/bench/barite/README.org
+++ b/bench/barite/README.org
@@ -24,15 +24,13 @@ celestite; following diffusion of $BaCl_2$ celestite dissolution
 occurs Dissolution of celestite and the successive release of
 $SO_4^{2-}$ into solution causes barite to precipitate:
 
-#+begin_src tex
-$ \mathrm{Ba}^{2+}_{\mathrm{(aq)}} + \mathrm{SrSO}_{4, \mathrm{(s)}} \rightarrow \mathrm{BaSO}_{4,\mathrm{(s)}} + \mathrm{Sr}^{2+}_{\mathrm{(s)}} $
-#+end_src
+```\mathrm{Ba}^{2+}_{\mathrm{(aq)}} + \mathrm{SrSO}_{4, \mathrm{(s)}} \rightarrow \mathrm{BaSO}_{4,\mathrm{(s)}} + \mathrm{Sr}^{2+}_{\mathrm{(s)}}```
 
 Reaction rates are calculated using a general kinetics rate law for
 both dissolution and precipitation based on transition state
 theory:
 
-$ \frac{\mathrm{d}m_{m}}{\mathrm{d}t} = -\mathrm{SA}_m k_{\mathrm{r},m} (1-\mathrm{SR}_{m})$
+```\frac{\mathrm{d}m_{m}}{\mathrm{d}t} = -\mathrm{SA}_m k_{\mathrm{r},m} (1-\mathrm{SR}_{m})```
 
 
 where $\mathrm{d}m\,(\mathrm{mol/s})$ is the rate of a mineral phase