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Soil Temperature Change over Time during Infiltration

Dep. of Soil Science, North Dakota State Univ., P.O Box 5638, Fargo, ND 58105

View larger version (47K): [in a new window]   Fig. 1. Schematic of infiltration transient temperature (ITT) evaluation column.

View larger version (40K): [in a new window]   Fig. 2. Maximum temperature change on wetting along infiltration transient temperature (ITT) columns of Fargo soil at several initial water contents for thermocouple (TC) locations as shown in Fig. 1.

View larger version (33K): [in a new window]   Fig. 3. Maximum temperature change on wetting along infiltration transient temperature (ITT) columns of Glyndon soil at several initial water contents for thermocouple (TC) locations as shown in Fig. 1.

View larger version (33K): [in a new window]   Fig. 4. Temperature profiles during water infiltration into Fargo soil at (a) 0.00 and (b) 0.04 g g–1 initial water contents.

View larger version (33K): [in a new window]   Fig. 5. Temperature profiles during water infiltration into Glyndon soil at (a) 0.00 and (b) 0.04 g g–1 initial water contents.

View larger version (32K): [in a new window]   Fig. 6. Modeled temperature profiles generated from simulated water infiltration into Fargo soil at (a) 0.00 and (b) 0.04 g g–1 initial water contents.

View larger version (31K): [in a new window]   Fig. 7. Modeled temperature profiles generated from simulated water infiltration into Glyndon soil at (a) 0.00 and (b) 0.04 g g–1 initial water contents.

View larger version (18K): [in a new window]   Fig. 8. Calculated temperatures at z = 4.0 cm due to evaporation/condensation only (no heat of wetting effect) for Fargo soil at 0.00 g g–1 initial water content.