by Larry D. Jacobson, Professor and Extension Agricultural Engineer | University of Minnesota
Presented at the 2015 Minnesota Statewide High Tunnel Conference.
1. Presented at MN Statewide High Tunnel
Conference, Feb 17, 2015.
Arrowwood Lodge, Baxter, MN
Larry D Jacobson, Professor and
Extension Agricultural Engineer
Dept of Bioproducts & Biosystems Engineering
University of Minnesota, St.Paul, MN
Understanding High Tunnel
Ventilation in Detail
2. Presentation Outline
Ventilation principles
Natural vs. Mechanical
High Tunnel application
Manual Control
Automated Control
(by temperature)
3. Ventilation or Air Exchange of High
Tunnels Needed to Remove Heat &
Moisture
4. Suggested Temperatures in High
Tunnels for Selected Crops
Table 2. Approximate Temperatures for Best Growth and Quality of Selected Vegetable Crops.*
Temperature (ºF)
Crop
Maximum Optimum Minimum
85 55-75 45 Onion, Garlic
75 60-65 40 Beet, Broccoli, Cabbage, Chard, Radish
75 60-65 45 Carrot, Lettuce, Pea, Potato Snap Bean,
Lima Bean
80 60-70 50
90 65-75 60 Cucumber
80 70-75 65 Tomato, Sweet Pepper
95 70-85 65 Eggplant, Hot Pepper, Okra
*Adapted from Knott's Handbook for Vegetable Growers. Lorenz and Maynard. 1988. P 70.
6. Air expands as it is heated and can absorb more moisture.
Warm Air Holds More Moisture
7. Two Different Ventilation
Systems used in HT
Natural Ventilation
Driving Forces –
Thermal Buoyancy
Wind
Mechanical Ventilation
Driving Force –
Exhaust Fans
14. Manual Control of sidewall Inlets
Management Tools for
managing opening size
(controlling air exchange)
High-low thermometers
Remote thermometer
(read out in home/office)
19. Summary
Natural Ventilation is probably preferred in
High Tunnels because of lower cost and
difficulty to seal up all the leaks so
mechanical ventilation will work properly
Temperature control is primary need for
ventilation or air exchange, moisture control
secondary
Manual ventilation control challenging but
possible
Simple aid might be remote thermometer
Automated controller for sidewall inlets would
yield tighter temperature control
A 10-degree C (18 F) rise in air temperature roughly doubles the amount of moisture air can hold (over the range of normal air temperatures). Illustration: morning fog ‘burns off’ or disappears as the air warms up (even though the amount of moisture in the air is basically the same). As the day goes on, the air warms up and takes on additional moisture (from the ground, plants, etc.). But, when it cools off again in the evening, it loses ability to hold moisture and may become ‘saturated’ (foggy) again.
Warming air increases the air’s ability to hold water vapor and visa versa.