Separate carbon gain, water loss and an efficiency ratio
Stomata connect internal leaf gas spaces to the atmosphere. Guard-cell osmotic and turgor changes alter pore opening, affecting CO2 entry and water-vapor escape. The same opening can therefore support carbon uptake and impose a water cost. Cuticle, boundary layers and leaf structure also influence exchange.
Learning outcome: Compare g = 0.2, 0.6 and 1 at D = 2, retaining A, E and their ratio separately. Then change D at fixed g and identify which feedback the imposed static comparison prevents.
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Connect plant tissues, transport, developmental signals and reproductive origins to complete quantitative evidence with explicit resource and model boundaries.
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At g = 0.6 and D = 2, A = 12/0.8 = 15 µmol CO2/m²/s and E = 6 mmol H2O/m²/s. A/E = 2.5 µmol CO2/mmol H2O. At D = 3 with g unchanged, E becomes 9 and the ratio falls to about 1.667.
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Does a higher carbon-per-water ratio necessarily imply more total carbon gained?
Experiment
Compare g = 0.2, 0.6 and 1 at D = 2, retaining A, E and their ratio separately. Then change D at fixed g and identify which feedback the imposed static comparison prevents.
Compare carbon uptake and water loss under a changed atmosphere
Worked teaching model · synthetic values · Original steady comparison: net assimilation A=20 g/(0.2+g)µmol CO2/m²/s and transpiration E=5 gD mmolH2O/m²/s. Temperature/light/CO2 fixed; no true optimal-control or universal species response implied.
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Opening stomata can raise carbon uptake while increasing water loss under the stated atmosphere.
At fixed conductance, a larger vapor-pressure deficit raises modeled water loss without changing the supplied carbon curve. Actual stomata can respond, and ABA, hydraulics, temperature and light complicate this static comparison. Ratio efficiency is not automatically maximum growth.
Solid: Supplied saturating carbon response. Axes rescale to the current range; use labeled values rather than comparing graph heights across settings.
| Relative conductance | Supplied saturating carbon response (Assimilation µmol CO2/m²/s) |
|---|---|
| 0.2 | 10.00000 |
| 0.4 | 13.33333 |
| 0.6000000000000001 | 15.00000 |
| 0.8 | 16.00000 |
| 1 | 16.66667 |
| Quantity | Value | Unit |
|---|---|---|
| Net carbon assimilation | 15 | µmol CO2/m²/s |
| Water loss | 6 | mmolH2O/m²/s |
| Instantaneous assimilation / water loss | 2.500000 | µmol CO2/mmolH2O |
Retain prior predictions, settings and quantities in the notebook. These are original supplied/calculated comparisons, not physical specimen observations or laboratory participation.
Opening stomata can raise carbon uptake while increasing water loss under the stated atmosphere.
At fixed conductance, a larger vapor-pressure deficit raises modeled water loss without changing the supplied carbon curve. Actual stomata can respond, and ABA, hydraulics, temperature and light complicate this static comparison. Ratio efficiency is not automatically maximum growth.
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At g = 0.4 and D = 1, calculate A, E and A/E.
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