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CHANGE Project
Climate Change Narrative Game Education
Teacher Notes: Chemistry Unit – Ocean Acidification
Lesson Time: 50 minutes
14 minutes slides/36 minutes lab
Instructor Note: These notes include a “sample lesson” that is intended to provide an example
of how this information could be presented to a classroom. The sample lesson is written in a
conversational tone and often does not follow the normal rules of writing (we don’t talk the way
we write). If you are very familiar with the topic, then the CHANGE team recommends that you
quickly skim through the material to make sure there are no surprises or changes. If you
relatively new to this material, then a more careful reading is in order.
Each section of the lesson includes the anticipated time that you will spend on each
subject (to the nearest minute, rounded up). The time estimates are intended as a tool to help you
manage the classroom, and are not a hard and fast rule. If your students are asking very fruitful
questions in a section that wasn’t allotted enough time, allow the questions (within reason). You
can make this time up by asking fewer questions later or by abbreviating topics that were
partially covered by the earlier questions.
Sample Lesson
Overview: (est. time: 1 min)
Today we’re going to talk about the chemistry
behind ocean acidification and then do some lab work so
you’ll see first-hand what the effects will be. The
processes behind ocean acidification are pretty
straightforward and would have been well understood by chemists 100 years ago. We’re also
going to talk about some of the basic chemistry that goes on all around us so that we can
understand the phenomenon of ocean acidification.
pH Scale: (est. time: 3 min)
QUESTION: By a show of hands, how many of you went
swimming in a pool over the summer?
ANTICIPATED RESPONSE: (most hands will raise)
QUESTION: Does anyone know what the pH of a
swimming pool is supposed to be kept at? (A few students will be responsible for caring for their
pool, but they probably don’t remember the exact numbers)
ANTICIPATED RESPONSE: Somewhere between 7 and 8
TEACHER FEEDBACK: Your pH should be between 7.2 and 7.8, and anyone that has had to
take care of a pool will tell you that you have to add chemicals about every week to keep it
where it should be.
In case you don’t know what pH is, it’s the standard scale that everyone uses to measure
acidity. We define a pH of 7 as neutral, because that’s the pH we find in absolutely pure water.
In real life, water isn’t pure though, and the ocean has a pH of 8.2. All pH numbers lower than 7
are acidic and numbers higher than 7 are called alkaline or basic. Every whole number step
means that the substance is either 10 times more acidic or basic, depending on which way you’re
going. So, I’ve given you a bunch of numbers that describe acids and bases, but did you know
that humans have a built-in ability to identify acids and bases?
We can tell how acidic or basic something is by its taste. Acids are sour and bases are
bitter. That doesn’t mean that everything that isn’t pH balanced tastes bad. Sour candies are
incredibly popular, and with the exception of a few that are just ridiculous, they taste pretty
good, right? If you look at the pH scale, you see that lemons have a pH of 2 and oranges are at 3.
The reason most people don’t just peel a lemon and eat it is that they are 10 times more acidic
and therefore 10 times more sour than an orange.
QUESTION: Someone that’s gone swimming in the ocean, on top of being salty, does the ocean
water taste sweet, sour, or bitter?
ANTICIPATED RESPONSE: Bitter
TEACHER FEEDBACK: Isn’t that interesting? Things don’t start to taste too sour to eat until
the pH gets down to about 2, but a pH of 8, which is barely alkaline already tastes pretty bitter.
QUESTION: Does anybody want to take a guess why that is?
ANTICIPATED FEEDACK: (Possible that no hands will raise, the answer isn’t obvious)
Because ocean water can kill us.
TEACHER FEEDBACK: Generally speaking, if we describe something as very sour or bitter,
we aren’t talking about something delicious that we want to eat more of. Almost everything
that’s edible by humans falls in the pH range of 2 to 8. This doesn’t mean you should go around
tasting random things, especially when you know better, because with some poisons even a taste
is enough to kill you. Most things with a pH outside the 2 to 8 range is probably going to make
you sick.
Natural Carbon Cycle: (est. time: 3 min)
In the natural world, you see a states of dynamic
equilibrium all over the place. Plants take in carbon
dioxide and water to produce oxygen and carbohydrates.
Carbohydrates are pretty much what their name suggests.
They are chains of carbon atoms bound to the chemical elements of water. We call short
carbohydrate chains sugars, and longer chains, like the ones in potatoes, are complex
carbohydrates. The ones that are extremely long are ones that humans can’t break down, and we
call them dietary fibers. Most solid plant material, like wood, is made up of densely packed
carbohydrate fibers.
Animals, do the reverse chemical reaction of plants. They take in oxygen by breathing
and eat the carbohydrates from plants. Then they release the energy from the carbohydrates by
breaking them back into carbon dioxide and water. Some animals, like koalas can survive
without having to drink water. Think about it, carbohydrates are, by definition, chemically made
up of half carbon and half water. Animals that digest dense fibers like wood and leaves are
getting a lot of their water by breaking them down.
When you look at all the inputs and outputs of carbon in the ecosystem, it gets
complicated quickly. But, in general, when plants die and are buried before they get eaten, that
carbon is sequestered from the ecosystem. When volcanos erupt, they pump carbon dioxide out
of the Earth into the atmosphere. We know that the amount of carbon dioxide and oxygen in the
atmosphere varies over geologic time periods. And, looking at the records in the rocks and
fossils, we know that a lot of this variation is due to the types and concentrations of plants and
animals, but sometimes it’s from major volcanic events, like super volcanos.
Human Caused CO2 in the Environment: (est. time: 2
min)
When we dig fossil fuels, like coal and oil, out of
the ground and burn it for fuel, we are using carbon that
had been sequestered from the atmosphere and re-
releasing it into the ecosystem as carbon dioxide. Now let me ask a question to see if you can
put it all together.
QUESTION: Because billions of people use fossil fuels to power their day, unnaturally adding
carbon dioxide to the atmosphere, what do you think is happening to the amount of carbon
dioxide dissolved in the oceans?
ANTICIPATED RESPONSE: It’s going up.
FOLLOW-UP QUESTION: Okay, that was too easy. Let’s try this one…Several countries are
trying to find economical ways of fixing carbon. Fixing carbon is where you do something to
lock it into rocks and other material, or somehow bury it to remove it from the ecosystem. Kind
of like drilling for oil, but in reverse. What will happen to the ocean if they are successful?
ANTICIPATED RESPONSE: (Give them time to think it through) The carbon dioxide in the
ocean will go down?
TEACHER FEEDBACK: Exactly! Nature will maintain its equilibrium, so if we start removing
the carbon dioxide from the air, more will come out of the ocean to re-establish equilibrium.
Ocean Acidification (est. time: 2 min)
It turns out that somewhere between a quarter and a third
of the carbon dioxide being added to the atmosphere finds
its way into the ocean. Then some of the dissolved
carbon dioxide reacts with water to make carbonic acid.
That’s the reason why CO2, which is odorless and tasteless, can change the flavor of a soda and
also drops its pH to about 3. We are slowly making our oceans more acidic. Since we started
measuring their pH about a hundred years ago, the ocean dropped its pH from 8.3 down to 8.2.
That doesn’t sound like a lot, but remember that for every whole number it goes down, it’s 10
times more acidic. Because the production rate of CO2 is increasing, scientists expect that we’ll
drop to a pH of 7.9 by the year 2100.
But, it’s not all bad news. Did you know that not all carbon dioxide is created equally?
If I grow several trees in my backyard so I can use them for firewood in the winter, the carbon in
the wood came from the atmosphere. When I burn the wood, I’m just releasing carbon dioxide
that came out of the air to begin with. In this scenario, as long as I plant as many trees as I cut
down, there are no global warming or ocean acidification concerns. If, on the other hand, I pull
oil and coal out of the ground and burn them, then there is a concern. Their carbon had been
locked out of the ecosystem for millions of years.
Effects of Ocean Acidification: (est. time: 2 min)
When the pH of the ocean changes, we have
measurable proof that we are changing our environment.
Beyond, that, why do we care? Because Corals and
crustaceans. Corals are a required habitat for at least part of the life cycle for most sea life and
crustaceans are at the base of the food web.
Building a shell that is just barely safe from dissolving is metabolically inexpensive.
Unfortunately, nature’s propensity to reward metabolically efficient species through the process
of evolution might be catastrophic for us. We’re already seeing shells and corals growing much
more slowly, and in some places outright dissolving. Unless the human civilization changes
something, we are going to find out just how resilient the oceans are during your lifetime.
Having said all that, most industrialized nations are working hard to keep the future safe.
I don’t know what the final answer will be, but it most likely will be the result of many small
steps and individual choices that we make. Maybe you demand that smokestacks get torn down
and replaced with wind and solar farms. Maybe, as a society, we decide that we’re done using
gasoline in our cars because going electric isn’t that much more expensive. Maybe one of you
has the answer.
Summary: (est. time: 1 min)
Before we move on to our lab, does anyone have
questions about ocean acidification, dynamic equilibrium
or anything else?