Management of fertilizer N in dryland cropping systems in the semi-ari
d Great Plains is important to the economic and environmental sustaina
bility of these systems. As producers shift from the traditional tille
d winter wheat (Triticum aestivium L.)-fallow (WF) cropping systems to
those that include summer crops in the rotation, N management becomes
more important because yield losses as a result of underfertilization
become greater. Fertilizer N rate is more important in obtaining opti
mum yields of dryland crops than N placement in drier environments, wh
ile placement becomes more important as rainfall increases. Soil testi
ng is an accurate method of quantifying the residual soil nitrate-N le
vel in the root zone. However, a combination of soil testing, fertiliz
er N experiences of the producer, and projected N requirement (expecte
d yield) are the best factors producers can use in determining fertili
zer N rates. If soil testing occurs early in the spring/summer fallow
period preceding planting, a correction to the fertilizer N recommenda
tion should be made to account for N mineralization that occurs betwee
n soil sampling and planting. This can prevent overfertilization. Dryl
and systems appear to have a soil-plant N buffer capacity that prevent
s inorganic N accumulation at fertilizer N rates that exceed optimal N
requirements to meet crop needs. Recent research has reported N buffe
ring in the range of 21 to 76 lb N/acre per yr for annually cropped dr
yland wheat production systems. This means that the application of fro
m 21 to 76 lb N/acre per yr did not result in an accumulation of inorg
anic N in the soil. This concept should be evaluated on additional dat
asets, and, if found to be applicable to a range of conditions, it cou
ld have an effect on establishing environmentally safe fertilizer N ra
tes for dryland cropping systems.