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Aerobically respiring organisms consume oxygen and can produce carbon dioxide. In the specified respirometer model, a suitable carbon dioxide absorbent is kept separate from the organisms. With that gas accounted for, a decrease in the system’s gas amount can support an oxygen-uptake measurement under the stated apparatus conditions.
Video by Michael Ralph. The demonstration explains the shared respirometer model. For this GCSE core practical, apply the specified temperature comparison, water bath, organism controls and ethical requirements.
Viewing focus: Explain the gas balance in an oxygen-use respirometer
After watching, attempt these questions before opening the answers. You can also use the written lesson below.
After watching 1: Why account for produced carbon dioxide?
It can offset the gas decrease caused by oxygen uptake. The gas balance depends on consumption and production.
After watching 2: Why use a matched temperature control?
Gas changes can occur without respiration. Separate physical changes from the intended biological signal.
What you'll be able to do
Aerobically respiring organisms consume oxygen and can produce carbon dioxide. In the specified respirometer model, a suitable carbon dioxide absorbent is kept separate from the organisms. With that gas accounted for, a decrease in the system’s gas amount can support an oxygen-uptake measurement under the stated apparatus conditions.
A marker’s movement is not automatically an oxygen volume. Use the instrument’s calibration or the appropriate capillary cross-sectional area to convert displacement where the model allows it. Check the direction of movement and what it means for the actual apparatus rather than memorising a left or right direction.
Use the approved small organisms, water-bath temperatures and ethical handling. Keep organism amount, condition and observation interval comparable. Allow apparatus and organisms to equilibrate appropriately and record actual temperature. A temperature change can alter gas pressure or volume without metabolism.
Check seals and use an appropriate matched control to account for physical effects. Record raw experimental and control readings with their signs and apply the specified correction. The centre controls absorbent handling and organism welfare; this is preparation for supervised work rather than a home apparatus-building task.
Divide corrected calibrated oxygen uptake by elapsed time. If organism amounts differ, use a justified mass or organism-number normalisation. State the measured units and avoid comparing a millimetre-per-minute displacement directly with a cubic-centimetre-per-minute volume rate.
Use independent repeats and describe variation. A higher rate at one temperature supports a local response under the tested conditions, not a universal unlimited temperature effect. Substrate, oxygen availability, activity, organism state and the measurement model can influence the result.
Attempt these problems on paper before opening the worked reasoning. Explain your steps as well as giving a final answer.
Common mistakes to avoid
Key takeaways
Question 1: The same uptake comes from 0.50 g of organisms. Find the mass-normalised rate.
0.12 cm³ min⁻¹ g⁻¹.
Check the assessed scope and practical or mathematical requirements.
An external explanation or interactive activity to use alongside the lesson. It may include extension material.
Close the notes and answer from memory. Revisit any explanation you cannot yet reconstruct.
Test yourself
Answer a few questions, then review anything you missed.
Start with the quiz above to check the key ideas. You can also choose another topic from the practice library.