← Year 9 Earth and space

Where does the carbon in a tree go?

Photosynthesis moves carbon from the atmosphere into living things; respiration and decomposition move it back. These huge flows nearly balance, so the air's CO₂ stays steady until something upsets them.

A big gum tree can weigh many tonnes. Almost all of that mass came out of the air.

You know the four spheres. This lesson follows carbon between two of them.

WidthMore contexts, same idea.
EngageCommit to a prediction before you test anything. A wrong guess is fine: it shows you what to look for.

Engage: where does a tree's mass come from?

Where does most of the mass of a tree come from?

ExploreTry it on the board and compare what happens with your prediction.

Explore: switch the flows

First press Run 10 years with everything on. Then switch Respiration and decomposition off and run again. Then switch it back on, switch Photosynthesis off, and run again. Press Start again whenever you like.

Try it yourselfYour edits are saved in this browser.

Make the CO₂ in the air fall, then make it rise, by switching processes on and off.

Use the board. This ticks when you get there.

ExplainUse the particle model to explain what you saw.

Explain: two flows, opposite directions

In your book: draw the atmosphere and biosphere as boxes, with arrows for photosynthesis, respiration and decomposition, labelled with their direction.

Which way does each process move carbon?

Photosynthesis
A kangaroo breathing out
Fungi rotting a fallen log
A tree respiring at night
Grass growing

With every process on, why did the CO₂ in the air stay steady?

If a large forest is cleared and burned, what happens to the carbon flows?

Elaborate TypicalUse the same idea in a new context.

Elaborate: a carbon atom's journey

Put a carbon atom's journey in order.

CO₂ in the air
Taken in by a grass leaf in photosynthesis
Eaten by a kangaroo, part of its body
The kangaroo dies and fungi decompose it
Respired by the fungi back into the air as CO₂

Elaborate WiderUse the same idea in a new context.

Elaborate: seasons in the air

Measurements of CO₂ in the air in the Northern Hemisphere dip every northern summer and rise every winter. Why?

EvaluateLook back at your first ideas and what changed.

Evaluate: look back

Write one sentence: "At first I thought… Now I think… because…"

Revision summary

For teachers

Students explain photosynthesis and respiration (including decomposition) as opposite flows of carbon between the atmosphere and biosphere, and explain balance between them (AC9S9U03, node 3, a hinge node). About 22 minutes.

Open the teacher guide: answers, solutions, slides and a worksheet.

Students will be able to

Before class

A concept tutorial for introducing or revising the idea. Set the width with ?width=minimum, typical (default) or wider.

The hinge is representing each process as a directional flow between spheres. The misconception that plants are made from soil is raised in Engage.

Board notes: stores in billions of tonnes of carbon (GtC); the air starts at a balanced 280 ppm (before 1800). Photosynthesis takes about 120 GtC a year; respiration and decomposition return about the same; the oceans exchange about 80 each way. Switching a process off is a "what if": with respiration and decomposition off, plants draw the air's CO₂ down within years; with photosynthesis off, it climbs. The model's numbers are rounded and its rules simple (plants take up a little more CO₂ when there is more of it).

Running the lesson

  1. Engage: count how many chose the soil.
  2. Explore: ask what happened in each run, and why.
  3. Explain: the balance question is the checkpoint.

The hard part (on purpose)

Seeing photosynthesis and respiration as flows of carbon that nearly balance. When a student says only animals respire, ask whether plant cells need energy at night.

When students get stuck

Stretch and support

Stretch: If photosynthesis and respiration nearly balance, how did fossil fuels form?

Support: Give a two-box diagram (atmosphere, biosphere) with three blank arrows to label.

Where it leads

Next: burning fossil fuels (node 4). Later: the greenhouse effect (Year 10).

What each step is for

Now you can
Next lesson4. What does burning fossil fuels do to the carbon cycle?Fossil fuels are carbon taken out of the cycle and stored in the geosphere over millions of years. Burning them returns it to the atmosphere in years, faster than plants and oceans can take it back, so CO₂ in the air rises.