Photosynthesis Rate and Light Response Calculator

Calculate net photosynthesis rate at any light intensity using the rectangular hyperbola model.
Find light compensation and saturation points.

Photosynthesis Rate Results

The light response curve

The rate of photosynthesis depends on light intensity, but not linearly. Two distinct regions:

  • At low light: each photon adds proportionally to photosynthesis (quantum-yield-limited)
  • At high light: the enzymes (especially Rubisco) become rate-limited, no matter how much extra light

The rectangular hyperbola captures this:

A_net = (Amax × I) ÷ (I + Ik) − Rd

Where:

  • A_net: net CO₂ assimilation (µmol CO₂/m²/s)
  • Amax: maximum gross photosynthetic rate at light saturation
  • I: incident light intensity (µmol photons/m²/s PAR)
  • Ik: light intensity at which photosynthesis is half-maximum
  • Rd: dark respiration rate (CO₂ released even in darkness)

The “net” part is important. Plants respire 24/7.
They consume CO₂ via photosynthesis and produce CO₂ via mitochondrial respiration, and the net A is the balance between the two.

The two critical light thresholds

Light Compensation Point (LCP): the light intensity at which net A = 0.
Photosynthesis exactly balances respiration, so below LCP the plant is losing carbon. For most plants LCP falls between 10 and 50 µmol/m²/s. Bright office lighting runs 5 to 15 (see the PAR reference below), so an office is marginal at best and usually sits below the point where a plant breaks even, which is exactly why the ones on desks slowly decline.

Light Saturation Point: the light intensity above which further increases give little or no additional photosynthesis.

There are two conventions here and they give very different numbers, which is worth knowing before you compare a figure to a textbook. The strict definition is the light at which gross A reaches 90% of Amax, which works out at nine times Ik. Field tables normally quote something lower, the light beyond which the extra gain stops being measurable in practice, and that sits closer to 75% of Amax, or three times Ik. The calculator reports both. The saturation column in the table below uses the practical convention.

Plant type LCP (µmol/m²/s) Saturation point Amax (µmol/m²/s)
Deep shade plants (forest understory) 1-5 100-300 2-6
Shade-tolerant (Hosta, Calathea) 5-15 200-400 5-10
Sun plants (tomato, lettuce, most vegetables) 15-30 600-1,200 15-25
C₃ crops (wheat, rice, soybean) 20-40 1,000-1,500 25-40
C₄ crops (corn, sugarcane, sorghum) 30-50 1,800-2,500 40-60
Tropical sun plants 40-60 2,000+ 50-80

PAR, the units that matter for plants

Plants use PAR (Photosynthetically Active Radiation), the 400-700 nm band.
That is roughly the visible spectrum, excluding ultraviolet and infrared. PAR is measured in µmol photons/m²/s, the number of photons landing on a square meter each second.

Reference PAR values:

  • Full sunlight at noon (clear day): 1,800-2,200 µmol/m²/s
  • Sunset / heavy overcast: 50-400 µmol/m²/s
  • Bright office lighting: 5-15 µmol/m²/s (no plant grows in this)
  • Indoor grow lights (LED, mid-tier): 200-800 µmol/m²/s
  • Greenhouse on cloudy day: 300-600 µmol/m²/s
  • Direct sun under shade cloth (50% shade): 900-1,100 µmol/m²/s

A common confusion: lux (commonly cited in indoor light meters) and PAR are not interchangeable. Lux is weighted to human eye sensitivity (peaks at green, where plants don’t care). For converting:

  • Sunlight: 1 PAR µmol/m²/s ≈ 54 lux
  • Cool white LED: 1 PAR ≈ 70 lux
  • Warm LED: 1 PAR ≈ 55 lux

So 10,000 lux of sunlight ≈ 185 PAR; 10,000 lux of cool LED ≈ 143 PAR.

C₃ vs C₄ photosynthesis

The most important distinction in plant biochemistry:

Pathway Where common Optimum temp Water efficiency
C₃ (most plants) Cool/moderate climates, low light 15-25°C Lower (loses water faster)
C₄ Tropical, hot/dry climates 30-45°C 2x higher than C₃
CAM Deserts, succulents High day temp 4-10x higher than C₃

C₄ plants concentrate CO₂ near Rubisco using PEP carboxylase, reducing photorespiration losses. This is why corn (C₄) thrives at high light and temperature while wheat (C₃) actually does better in cooler conditions. The agricultural implication: C₄ crops dominate the tropics.

Quantum yield, the molecular efficiency

At low light, each photon absorbed converts to chemistry with some quantum yield φ. Theoretical maximum is 1 photon → 1 CO₂ fixed, but actual values are roughly:

  • C₃ plants: 0.045-0.060 mol CO₂/mol photons
  • C₄ plants: 0.055-0.075

So at low light, a C₄ plant is about 25% more efficient per photon. This is invisible at high light where Rubisco saturates, but matters in shaded or seasonal conditions.

Photoinhibition, when too much light damages plants

Above 1,500-2,000 µmol/m²/s, especially alongside heat or drought stress, plants can experience photoinhibition.
Light damages the Photosystem II complex faster than the plant can repair it, and the leaf shows wilting, burn, or chlorosis. This is why:

  • Greenhouse growers use shade cloth even on sunny days
  • Indoor growers don’t crank LED to maximum
  • Forest plants underneath gaps experience leaf burn when overstory is removed

Repairing the damaged D1 protein in Photosystem II is the rate-limiting step in recovery, and it takes hours to days.

Practical greenhouse and indoor growing application

For commercial indoor crops (lettuce, herbs, cannabis):

  • Lettuce: DLI (Daily Light Integral) target 12-17 mol/m²/day. At 200 PAR for 18 hours that is 13 mol/m²/day
  • Tomato: DLI target 20-30 mol/m²/day, which needs 400-500 PAR for 14-16 hours
  • Cannabis in flower: DLI target 35-45 mol/m²/day, which needs 800-1,200 PAR for 12 hours
  • Microgreens: DLI target 6-10 mol/m²/day, met at 100-150 PAR

DLI is not PAR. PAR is the instantaneous photon flux; DLI is that flux added up over the whole photoperiod, so the units are mol/m²/day rather than µmol/m²/s. Get the two mixed up and you will over-light a crop by an order of magnitude. The conversion is DLI = PAR × hours × 3,600 ÷ 1,000,000.

Above DLI saturation, you get diminishing returns and risk photoinhibition. Below DLI threshold, plants stretch, thin out, and yield collapses.

Environmental modifiers

The simple light response curve ignores temperature, CO₂, water, and nutrients. In reality:

  • CO₂ enrichment (1,000-1,400 ppm in greenhouses) raises Amax by 20-40% in C₃ plants
  • Temperature affects Amax (Q10 ≈ 2 around the optimum)
  • Water stress closes stomata, which cuts CO₂ uptake and so caps Amax
  • Nitrogen deficiency reduces Rubisco, lowering Amax
  • Diurnal patterns: Amax is often higher midday than morning/afternoon at the same PAR

A full plant model uses the Farquhar-von Caemmerer-Berry biochemical model, which incorporates all these. The simple hyperbola here is a useful first approximation.

Bottom line

For sun-grown crops, you’re optimizing for high Amax and operating near light saturation (1,000-1,500 PAR for C₃, 2,000+ for C₄). For indoor crops, target the species-specific DLI (Daily Light Integral) rather than instantaneous PAR.
The light compensation point matters most when you are working out whether a low-light location can support growth at all. Below LCP the plant is just respiring and starving.


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