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3 changes: 3 additions & 0 deletions docs/source/conf.py
Original file line number Diff line number Diff line change
Expand Up @@ -57,3 +57,6 @@
html_static_path = ['_static']
html_css_files = ['conf.css']

# load mathjax so render math in 'HTML-CSS' which is searchable in browser
mathjax_path = "https://cdn.mathjax.org/mathjax/latest/MathJax.js?config=TeX-AMS-MML_HTMLorMML"

6 changes: 3 additions & 3 deletions docs/source/intro.rst
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Expand Up @@ -622,7 +622,7 @@ nanophytoplankton:

Z = \psi \cdot p_{phy} \cdot \mathrm{C}_{phy}

$\psi$ is the calcite production ratio that incorporates the ratio of
:math:`\psi` is the calcite production ratio that incorporates the ratio of
calcium carbonate producers to total nanophytoplankton and the :math:`CaCO_3`:POC
ratio in coccolithophorids. The latter is assumed to be 1.

Expand Down Expand Up @@ -829,7 +829,7 @@ The silica dissolution rate :math:`\rho_{Si}^T` follows the temperature dependen
\paragraph{Calcium carbonate pool (:math:`\mathrm{CaCO}_{3\,det}`)}
Nanophytoplankton loses :math:`CaCO_3` to the detrital :math:`CaCO_3` compartment
via excretion, respiration, aggregation and grazing. Dissolution of
:math:`CaCO$_3` leads to an increase in :math:`\mathrm{DIC}` and alkalinity (see section
:math:`CaCO_3` leads to an increase in :math:`\mathrm{DIC}` and alkalinity (see section
:ref:`sec_carbchem`).

.. math::
Expand Down Expand Up @@ -900,7 +900,7 @@ function (:math:`f_T`, see Eq. :eq:`eq_arr`).
Dissolved Organic Carbon (:math:`\mathrm{DOC}`)
-----------------------------------------------

$\mathrm{DOC}$ sources are carbon excretion by nanophytoplankton, diatoms and
:math:`\mathrm{DOC}` sources are carbon excretion by nanophytoplankton, diatoms and
heterotrophs, and degradation of :math:`\mathrm{C}_{det}`. Remineralization of :math:`\mathrm{DOC}` leads
to a transfer of carbon from :math:`\mathrm{DOC}` to :math:`\mathrm{DIC}`.

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