Nitrogen mineralization responses to cropping, tillage, and nitrogen rate in the Northern Great Plains

Citation
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
Citations number
26
Categorie Soggetti
Environment/Ecology
Journal title
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL
ISSN journal
03615995 → ACNP
Volume
63
Issue
1
Year of publication
1999
Pages
192 - 196
Database
ISI
SICI code
0361-5995(199901/02)63:1<192:NMRTCT>2.0.ZU;2-P
Abstract
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.