Leaf Temperature Infrared Thermometry & Crop Water Stress Index (CWSI) Sensing
📅 2026-08-29
🏷️ Phyto-Sensing & Thermography
✍️ Inwoovation AgTech Research
1. Why Ambient Air Temperature Is Insufficient
In high-wire greenhouse steering, crops are active thermodynamic heat exchangers. Under intense radiation (\(> 600 \text{ W/m}^2\)), active transpiration evaporatively cools the foliage, causing leaf temperature (\(T_{leaf}\)) to be 2°C to 4°C cooler than ambient air (\(T_{air}\)). Conversely, when roots experience water stress or high root zone EC, stomata close, eliminating latent heat loss and elevating \(T_{leaf}\) up to 3°C above air temperature.
2. Stefan-Boltzmann Law & Infrared Radiometry
Thermal Radiation (E, W/m²) = ε × σ × (T_leaf_Kelvin)⁴
• ε = Leaf Emissivity (0.97 - 0.98 for plant cuticle)
• σ = Stefan-Boltzmann Constant (5.67037 × 10⁻⁸ W m⁻² K⁻⁴)
Crop Water Stress Index (CWSI) = [(T_leaf − T_air) − ΔT_lower] / [ΔT_upper − ΔT_lower]
CWSI scales strictly between 0 and 1:
- CWSI = 0.0 – 0.2 (Optimal Hydration): Maximum transpiration cooling (\(\Delta T_{lower}\) baseline); stomata fully open.
- CWSI = 0.3 – 0.5 (Mild Generative Stress): Controlled mild deficit steering, stimulating fruit sugar accumulation without vegetative collapse.
- CWSI > 0.6 (Critical Drought Stress): Stomatal closure (\(\Delta T_{upper}\) threshold); immediate irrigation trigger required.
3. Integrating IR Leaf Sensors with VPD Control
Calculating Leaf-to-Air VPD (VPD_leaf) using actual contact/IR thermopile data provides 100% true physiological feedback, preventing catastrophic over-ventilation during sudden sun breaks in spring and autumn.
🌡️ Calculate True Leaf-to-Air VPD Now
Compute precise vapor pressure differentials with custom leaf temperature offsets.
Open Interactive VPD Engine →