A Slice of Science

By Simon Shapiro

Watching "The Great British Baking Show" recently, I was intrigued by the judges' comments. They would glance at piece of bread and immediately say
"You proofed it for too long" (or not long enough)
"You kneaded it too much" (or not enough)
"Overbaked" (or underbaked)
"Oven was too hot" (or too cool)
"The wrong flour"
"Too much liquid"

They really seemed to know all about the process and what can go wrong. (It sounded complex and lots could go wrong).

That led me to wondering about the science behind baking bread. Humans have been baking bread for thousands of years. At its simplest, all you do is mix flour and water, and bake it. But it gets more complicated and there's a lot of science involved.

Nathan Myhrvold, a physicist and former Microsoft Chief Technology Officer, founded Intellectual Ventures Lab, which performs scientific experiments with food. Last year they published Modernist Bread, a 6-volume 2642-page book about bread. It reflects information from 1,600 experiments.

Want more dough? As for a raise. 

Flour and water and 18 minutes of baking will get the flat bread called matzah.  Most people who eat this for a week find it boring, to say the least. Comparisons to cardboard are common.

Jews are required to eat matzah and no leavened bread for the seven days of the Passover festival.

The easiest and quickest leavened bread is soda bread. You make this by adding baking soda or baking powder to the mix. Baking soda is simply sodium bicarbonate (NaHCO₃). When it's mixed with an acid, the reaction releases carbon dioxide gas. Common acids in bread recipes include cream of tartar, lemon juice, yogurt, buttermilk, cocoa and vinegar. You have to get the right balance of acid and baking soda. If you have too little acid, unreacted baking soda will taste metallic and bitter. Baking powder makes life easier. It consists of baking soda pre-mixed with dry acid. Adding liquid is all you need to add to get little bubbles of gas. (See it for yourself: add water to some baking powder and watch it fizz; add water to some baking soda - no fizz until you add lemon juice).

It's not as quick and easy, but  using yeast to get the carbon dioxide bubbles tastes better and is more versatile for getting different bread textures. Yeast is a single celled fungus that feeds on sugar and transforms it into alcohol and carbon dioxide gas.

Yeast cells at a magnification of 400

  Where does the sugar come from? Adding water to flour allows enzymes in the flour to convert starch within the flour into sugars.

What else do we need?

We need some sort of framework to capture the carbon dioxide bubbles. The best material for this is gluten. Gluten consists of long, elastic protein chains, which form rubbery networks, perfect for capturing gas. It's a lot like a balloon. Handily, wheat flour contains two proteins, glutenin and gliadin which, when combined with water, form gluten.

 The more protein in the flour, the more gluten it has. That's why cake flour and bread flour are different. Bread needs much more gluten than cakes do. Bread flour has about twice as much protein as cake flour. This video

has a great demonstration of the difference and really shows the elastic property of gluten.

Most bread recipes mix the dry and wet ingredients and then leave the dough for an hour or two to do its magic: breaking down the starch to form sugar, which feeds the yeast cells, giving off bubbles of carbon dioxide which are captured in the gluten network. The dough will rise to about double its original volume. This is called proofing.

Then you knead the dough by repeatedly folding at and squashing it. This helps develop the gluten network to make it stronger and more elastic. Some recipes repeat the process of letting the dough rise and kneading it - sometimes several times.

Now we're cooking!

It's time to bake. As the dough heats up in the oven, the carbon dioxide bubbles expand. New bubbles are also formed because the alcohol (remember that yeast produces both carbon dioxide and alcohol) and the water which the starch absorbed, both vaporize. So the dough rises again. This is called "oven spring".

Illustration of heat transfer from Modernist Bread, The Cooking Lab

Heat is transferred from the outside of the loaf through "heat pipes". Adjacent bubbles transfer heat from the outer side by water boiling on that side and steam condensing on the inner side, releasing heat to start vapourising the next bubble in the "pipe". The rising heat kills the yeast cells, hardens the gluten network and caramelizes sugars on the crust of the loaf.

If the experiment was successful, you now have a hot, crusty, delicious loaf of bread.

Full disclosure: I haven't yet put any of my newly discovered information to the test of actually baking bread. But I will!


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What happens to creatures that live in the ocean if seawater becomes more acidic? This fun activity, excerpted from The Big Green Book of the Big Blue Sea (Kids Can Press), is an easy to do, seeing-is-believing demonstration.

Humpty Dumpty Coral

Excess carbon dioxide from burning fossil fuels, is gradually making the oceans more acidic. How might more acidic waters affect coral reefs? See for yourself.

You Will Need

an egg

500 ml (2 c.) white vinegar

a large glass container (to hold the vinegar)

plastic wrap

1.     Break the egg neatly in half. Reserve the egg white and yolk for another purpose (like breakfast!).

2.     Measure the vinegar into your container. Place the two halves of the eggshell in the vinegar. Cover the container with plastic wrap.

3.     Watch what happens when you place the shells in the vinegar. Do you see bubbles forming around the shells?

4.     Leave the container in an area where it won’t be disturbed. Then check on your eggshells three days later. Where did they go?

What’s Going On?

Eggshells are made out of calcium carbonate, the same mineral that coral polyps use to make their shells. Vinegar — an acid — reacts with the calcium carbonate, removing the carbon from the shell. The carbon combines with oxygen to make the gas carbon dioxide. Those are the bubbles you saw rising from the egg.

With no carbon left in the shell, the shell literally dissolves and disappears. What you see floating in the vinegar is just the soft membrane that lines the eggshell. It is similar to the soft bodies of the corals. Like the egg membranes, the coral bodies would float off without their calyces. They’d be totally vulnerable to predators.

What’s Happening Now?

Despite their tiny size, corals build structures that are so gigantic they can even be seen from space! To do so, they need just the right conditions. They need water that is the right temperature, clarity and acidity. They need to remain undisturbed. And they need the right kind of base to lay the foundation for the reef.

Today, reefs are at risk all over the world. Global warming, ocean acidification, pollution and habitat destruction are all taking their toll. So people are lending corals a helping hand. The Reef Ball Foundation, for example, is a non-profit organization dedicated to building artificial reefs.

The foundation makes ball-shaped, concrete structures. They lower them in waters where an existing reef has been damaged. Teams of scientists hand “plant” about 500 corals per day onto each structure. The scientists then monitor the growth and health of the corals until the reefs re-establish themselves. The process can take 3–5 years. Since their founding in 1993, the Reef Ball Foundation has helped rebuild coral reefs in more than 70 countries.

 

The Big Green Book of the Big Blue Sea has been longlisted for the Information Book Award from the Vancouver Children's Roundtable.