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Soil Carbon and Nitrogen Mineralization

Influence of Drying Temperature

^a USDA-ARS, 808 E. Blackland Rd, Temple, TX 76502
^b Dep. of Soil & Crop Sciences, Texas A&M University, Texas Agricultural Experiment Station, College Station, TX 77843
^c USDA-ARS, 1420 Experiment Station Road, Watkinsville, GA 30677-2373

View larger version (30K): [in a new window]   Fig. 1. Rate of CO2 evolution during the first 4 d of incubation after drying at 40, 60, and 100°C and then rewetting.

View larger version (18K): [in a new window]   Fig. 2. Nitrogen mineralized after 24 d in soils dried at 40, 60, or 100°C following rewetting compared with 24-d N mineralization in soils that were kept continuously moist.

View larger version (35K): [in a new window]   Fig. 3. Nitrogen mineralized (NH4+–N, NO2––N, NO3––N) after 24 d in soils kept continuously moist vs. soils that were dried and rewetted.