Bj. Wienhold et Ad. Halvorson, Nitrogen mineralization responses to cropping, tillage, and nitrogen rate in the Northern Great Plains, SOIL SCI SO, 63(1), 1999, pp. 192-196
Nitrogen-mineralization rates are needed to accurately determine N fertiliz
ation requirements to meet plant needs while minimizing environmental conta
mination. A spring wheat (Triticum aestivum L.)-fallow (SW-F) system was co
mpared with a spring wheat-winter wheat-sunflower (Helianthus annuus L.) (S
W-WW-SF) system on a Temvik-Wilton silt loam (fine-silty, mixed Typic and P
achie Haploborolls) at three N rates (0, 22, and 45 kg ha(-1) for SW-F and
34, 67, and 101 kg ha(-1) for SW-WW-SF) under conventional, minimum, and no
-tillage. After 10 Sr, soil samples were incubated to determine N-mineraliz
ation rates. Cropping intensity, N rate, and tillage intensity interacted t
o affect N-mineralization rates. Within the SW-F system N-mineralization ra
tes in 0- to 0.05-m depth were 8.2 +/- 0.8 kg ha(-1) wk(-1) in the fallow p
hase vs. 5.0 +/- 0.7 kg ha(-1) wk(-1) in the crop phase under conventional
tillage and were 6.2 +/-. 0.3 kg ha(-1) wk(-1) under minimum and no-tillage
in both phases. The N-mineralization rates were 2.3 +/- 0.4 kg ha(-1) wk(-
1) in 0.05- to 0.15-m depth soils of the SW-F system. In spring wheat, N-mi
neralization rates in 0- to 0.05-m depth soil were 9.9 +/- 0.8 kg ha(-1) wk
(-1) in the SW-WW-SF system vs. 5.6 +/- 0.4 kg ha(-1) wk(-1) in the SW-F sy
stem and in the 0.05 to 0.15-m depth were 3.6 +/- 0.1 kg ha(-1) wk(-1) in t
he SW-WW-SF system vs. 2.4 +/- 0.2 kg ha(-1) wk(-1) in the SW-F system With
in the SW-WW-SF system, N mineralization rates in the 0- to 0.05-m soil lay
er were 6.8 +/- 0.5 kg ha(-1) wk(-1) under winter wheat vs. 9.9 +/- 0.8 kg
ha(-1) wk(-1) under spring wheat and 9.2 +/- 0.6 kg ha(-1) wk(-1) under sun
flower. In the 0.05- to 0.15-m soil layer, N-mineralization rates were 3.3
+/- 1.0 kg ha(-1) wk(-1). More intensive cropping and conservation tillage
increased N-mineralization rates in this soil and may ameliorate the declin
e in N fertility associated with crop-fallow systems.