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 metric in agriculture and environmental science for understanding plant stress and transpiration rates.
The calculator uses the VPD equation:
Where:
Explanation: The equation calculates the difference between the actual water vapor pressure and the saturation water vapor pressure at a particular temperature.
Details: VPD is crucial for understanding plant water relations, optimizing greenhouse environments, and predicting evapotranspiration rates in ecosystems.
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. Values below 0.4 kPa may indicate too much humidity, while above 1.6 kPa may cause plant stress.
Q2: How is SVP determined?
A: SVP is temperature-dependent and can be calculated using the Arden Buck equation or looked up in standard tables.
Q3: Why is VPD better than RH alone?
A: VPD accounts for both temperature and humidity, giving a more accurate measure of the driving force for evaporation.
Q4: What's the relationship between VPD and transpiration?
A: Higher VPD increases transpiration rates as plants lose more water to the drier air.
Q5: How does VPD affect plant growth?
A: Optimal VPD promotes healthy stomatal opening for photosynthesis while preventing excessive water loss.