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Assessing Indices for Predicting Potential Nitrogen Mineralization in Soils under Different Management Systems

Harry H. SchombergUSDA‐ARS J. Phil Campbell, Sr., Natural Resource Conservation Center Watkinsville GA 30677S. WiethölterEmpresa Brasileira de Pesquisa Agropecuária (Embrapa Trigo) Passo Fundo Rio Grande do Sul Brazil 99001‐970Timothy S. GriffinFriedman School of Nutrition Sci. and Policy, Tufts Univ. Boston MA 02111D. W. ReevesUSDA‐ARS J. Phil Campbell, Sr., Natural Resource Conservation Center Watkinsville GA 30677M. L. CabreraUniv. of Georgia Dep. of Crop and Soil Sciences Athens GA 30602D. S. FisherUSDA‐ARS J. Phil Campbell, Sr., Natural Resource Conservation Center Watkinsville GA 30677Dinku M. EndaleUSDA‐ARS J. Phil Campbell, Sr., Natural Resource Conservation Center Watkinsville GA 30677Jeff M. NovakUSDA‐ARS Coastal Plains Soil, Water, and Plant Res.Ctr. Florence SC 29501K. S. BalkcomUSDA‐ARS National Soil Dynamics Lab. Auburn AL 36832R. L. RaperUSDA‐ARS National Soil Dynamics Lab. Auburn AL 36832Newell R. KitchenUSDA‐ARS Cropping Systems and Water Quality Res. Unit Columbia MO 65211Martin A. LockeUSDA‐ARS National Sedimentation Lab. Oxford MS 38655K. N. PotterUSDA‐ARS Grassland Soil and Water Res. Lab. Temple TX 76502Robert C. SchwartzUSDA‐ARS Southern Plains Conserv.Production Rese. Lab. Bushland TX 79012Clinton C. TrumanUSDA‐ARS Southeast Watershed Res. Lab. Tifton GA 31793D. D. TylerUniv. of Tennessee Biosystems Engineering and Soil Science Dep. Jackson TN 38301
2009en
ABI

Annotatsiya

A reliable laboratory index of N availability would be useful for making N recommendations, but no single approach has received broad acceptance across a wide range of soils. We compared several indices over a range of soil conditions to test the possibility of combining indices for predicting potentially mineralizable N (N 0 ). Soils (0–5 and 5–15 cm) from nine tillage studies across the southern USA were used in the evaluations. Long‐term incubation data were fit to a first‐order exponential equation to determine N 0 , k (mineralization rate), and N 0 * (N 0 estimated with a fixed k equal to 0.054 wk −1 ). Out of 13 indices, five [total C (TC), total N (TN), N mineralized by hot KCl (Hot_N), anaerobic N (Ana_N), and N mineralized in 24 d (Nmin_24)] were strongly correlated to N 0 ( r > 0.85) and had linear regressions with r 2 > 0.60. None of the indices were good predictors of k Correlations between indices and N 0 * improved compared with N 0 , ranging from r = 0.90 to 0.95. Total N and flush of CO 2 determined after 3 d (Fl_CO2) produced the best multiple regression for predicting N 0 ( R 2 = 0.85) while the best combination for predicting N 0 * ( R 2 = 0.94) included TN, Fl_CO2 , Cold_N, and NaOH_N. Combining indices appears promising for predicting potentially mineralizable N, and because TN and Fl_CO2 are rapid and simple, this approach could be easily adopted by soil testing laboratories.

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