Use Siunitx package for dealing with units (#129)

It is complicated :
[1] The International System of Units (si), https://www.bipm.org/en/
measurement-units/.
[2] International System of Units from nist, http://physics.nist.gov/cuu/Units/
index.html.

And one will never get it right (space or not, half-space?) nor
consistent so using that instead.

I am not sure how times and hours, when to write digits and when in
letter so I did not change much..

Did not touch the tables as ebooks on github actions seems to break when
you look at them funny.

Co-authored-by: Cedric <ced@awase.ostal>
This commit is contained in:
cedounet
2023-06-28 19:30:12 +01:00
committed by GitHub
parent 0614fe7d8f
commit 4637c29a37
25 changed files with 334 additions and 318 deletions

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@@ -29,7 +29,7 @@ extensible and can be stretched.
\end{center}
\end{table}
At around 60°C (140°F) the microbes in your dough start to die.
At around \qty{60}{\degreeCelsius} (\qty{140}{\degF}) the microbes in your dough start to die.
There are rumors that until this happens the microbes produce
a lot of \ch{CO2}, resulting in the dough's expansion. However, this temperature
is reached quickly. Furthermore, stress makes the microbes
@@ -37,19 +37,19 @@ enter sporulation mode in order to focus on spreading genetics.
More research should be done here to validate or invalidate this
claim.
At 75°C (167°F) the surface of your dough turns into a gel. It
At \qty{75}{\degreeCelsius} (\qty{167}{\degF}) the surface of your dough turns into a gel. It
holds together nicely and is still extensible. This gel is essential
for oven spring as it retains the gas of your dough very well.
At around 100°C (212°F) the water starts to evaporate out of your
At around \qty{100}{\degreeCelsius} (\qty{212}{\degF}) the water starts to evaporate out of your
dough. If this weren't the case, your dough would taste soggy and
doughy. The higher hydration your dough has, the more water your bread
still contains after the bake. The crumb is going to taste a bit
more moist. The consistency will be different.
Another often undervalued step is the evaporation of acids. At
118°C (244°F) the acetic acid in your dough starters to evaporate.
Shortly after at 122°C (252°F) the lactic acid begins evaporating.
\qty{118}{\degreeCelsius} (\qty{244}{\degF}) the acetic acid in your dough starters to evaporate.
Shortly after at \qty{122}{\degreeCelsius} (\qty{252}{\degF}) the lactic acid begins evaporating.
This is crucial to understand and opens a door to many interesting
ways to influence your final bread's taste. As more and more water
begins to evaporate the acids in your dough become more concentrated.
@@ -78,9 +78,9 @@ acid? How would the taste change?
As the temperature increases
the crust thickens. The Maillard reaction kicks in, further deforming
proteins and starches. The outside of your dough starts to become
browner and crisper. This process begins at around 140°C (284°F)
browner and crisper. This process begins at around \qty{140}{\degreeCelsius} (\qty{284}{\degF})
Once the temperature increases even more to around 170°C (338°F),
Once the temperature increases even more to around \qty{170}{\degreeCelsius} (\qty{338}{\degF}),
the caramelization process begins. The remaining sugars the microbes
did not convert yet start to brown and darken. You can keep baking
for as long as you like to achieve the crust color that you
@@ -92,7 +92,7 @@ darker crust.}.
The best method to know that your dough is done is to take
the temperature of your dough. You can use a barbecue thermometer
to measure it. Once the core temperature is at around 92°C (197°F),
to measure it. Once the core temperature is at around \qty{92}{\degreeCelsius} (\qty{197}{\degF}),
you can stop the baking process. This is typically not done though
as the crust hasn't been built yet\footnote{The thermometer is
especially important when using a large loaf pan. It is sometimes
@@ -135,13 +135,13 @@ loses its ability to contain gas as the temperature heats
up. The dough stops increasing in size. The steam plays
an important role as it condenses and evaporates on top
of your dough. The surface temperature is rapidly increasing
to around 75°C (160°F). At this temperature the gel starts
to around \qty{75}{\degreeCelsius} (\qty{160}{\degF}). At this temperature the gel starts
to build. This gel is still extensible and allows expansion.
Without the steam, the dough would never enter the gel stage,
but instead directly go to the Maillard reaction zone. You
want your dough to stay in this gel stage as long as possible
to achieve maximum expansion\footnote{You can remove your
dough from the oven after 5 minutes to see the gel. You will notice
dough from the oven after 5~minutes to see the gel. You will notice
that it holds the dough's structure. It has a very interesting consistency.}.
\begin{figure}[!htb]
@@ -246,7 +246,7 @@ For the inverted tray you will need the following tools:
These are the steps to follow with the inverted tray method:
\begin{enumerate}
\item Preheat the oven to around 230°C (446°F) and
\item Preheat the oven to around \qty{230}{\degreeCelsius} (\qty{446}{\degF}) and
preheat one of the trays.
\item Bring water to boil.
\item Place your loaves on a piece of parchment paper. You
@@ -266,9 +266,9 @@ to the oven.
water bowl. I~have added rocks to it, as it helps
to improve the steam even further. This is optional.
\item Close the oven.
\item After 30 minutes remove the top tray. Also remove the bowl with water.
\item After 30~minutes remove the top tray. Also remove the bowl with water.
\item Finish baking your bread until you have reached your desired
crust color. In my case this is another 15--25 minutes typically.
crust color. In my case this is another 15--25~minutes typically.
\end{enumerate}
\section{Conclusions}