Quantifying batch consistency for yeast respiration experiments
Weigh 20 spheres individually after draining surface moisture (transfer with forceps to dry filter paper for ~30 s before weighing). Enter mass in grams — e.g. 0.0475. Tab between cells.
Descriptive statistics for the batch. The coefficient of variation (CV) is the most useful single measure of uniformity — it expresses the spread relative to the mean and is dimensionless, so different batches can be directly compared.
The chart on the left shows each sphere sorted from lightest to heaviest, with mean ± 1 SD shaded. The histogram on the right shows how masses cluster around the mean.
Sorted lightest to heaviest. Calcium alginate hydrogels are ~98% water, so we assume density ≈ 1.02 g/mL to convert mass to volume, then to radius assuming spherical geometry.
Each circle represents one sphere, rendered at approximately true size (1 mm ≈ 4 px). Spread should be visually subtle for a uniform batch.
For a sphere: V = m/ρ, r = (3V/4π)1/3, SA = 4πr², and SA:V = 3/r. The smallest and largest spheres differ in surface-area-to-volume ratio — the key geometric quantity governing diffusion.
Your experimental design uses 8 spheres per condition at 0, 20, 40 and 60 °C in 0.01 M bicarbonate buffer (pH 8.3) for 45 min. We need to ask: given the variation in individual sphere mass, how much variation should we expect between conditions purely from sampling, before any biology even happens?
When 8 spheres are pooled into a single condition, the relative variation in total mass shrinks by a factor of √8 ≈ 2.83 (assuming spheres are picked independently). This is the central limit theorem at work.
Simulated random draws of 8 spheres (sampled with replacement from your 20), repeated 2000 times:
Two physical processes drive the pH change in this experiment, and they respond differently to temperature:
| Temperature | Yeast metabolic rate (Q₁₀ ≈ 2) | CO₂ diffusion coefficient (in water) | Likely outcome |
|---|---|---|---|
| 0 °C | ≈ 0.25× the 20 °C rate | ≈ 0.52× the 20 °C value | Very little CO₂ produced; minimal pH change. |
| 20 °C | baseline (1×) | baseline (1×) | Moderate, measurable pH drop. |
| 40 °C | ≈ 4× the 20 °C rate | ≈ 1.6× the 20 °C value | Largest pH drop — typically the optimum for S. cerevisiae. |
| 60 °C | brief activity, then thermal death (>55 °C) | ≈ 2.4× the 20 °C value | Small early pH change, then plateaus as yeast die. |
Imagine two scenarios for how CO₂ release rate depends on sphere geometry:
For most VCE practicals with these spheres, scenario 1 dominates and mass uniformity is the relevant metric. Scenario 2 is worth discussing with students as a way to motivate why SA:V appears so often in biology.