VPD Equation:
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Vapor Pressure Deficit (VPD) is the difference between the amount of moisture in the air and how much moisture the air can hold when it's saturated. It's a key parameter in agriculture, meteorology, and HVAC systems.
The calculator uses the VPD equation:
Where:
Explanation: VPD represents the "drying power" of the air, showing how far the current conditions are from saturation.
Details: VPD is crucial for understanding plant transpiration rates, predicting evaporation, and designing climate control systems. It affects crop growth, building comfort, and industrial processes.
Tips: Enter SVP in kPa and RH as a percentage (0-100%). Both values must be valid (SVP > 0, RH between 0-100).
Q1: What are typical VPD values for plants?
A: Most plants thrive at VPD between 0.8-1.2 kPa, though optimal ranges vary by species and growth stage.
Q2: How does temperature affect VPD?
A: Temperature influences SVP - warmer air can hold more moisture, increasing potential VPD at the same RH.
Q3: Why is VPD better than RH alone?
A: VPD accounts for both temperature and humidity, giving a more complete picture of atmospheric moisture conditions.
Q4: What's the relationship between VPD and evaporation?
A: Higher VPD generally means faster evaporation rates as the air can absorb more moisture.
Q5: How is VPD used in greenhouse management?
A: Growers adjust VPD to optimize plant transpiration, nutrient uptake, and prevent diseases from overly humid conditions.