Re. Martin et al., CONTROLS ON ANNUAL EMISSIONS OF NITRIC-OX IDE FROM SOILS OF THE COLORADO SHORTGRASS STEPPE - ENGLISH, FINNISH, Global biogeochemical cycles, 12(1), 1998, pp. 81-91
Estimates of NOx (NO+NO2) emissions from temperate grasslands range fr
om 0.003 to 101 ng NO-N m(-2)s(-1) (average 4.17 ng NO-N m(-2)s(-1)).
As a result of this uncertainty, the potential contribution of soil NO
x emissions to the global budget and to nitrogen loss for this ecosyst
em is unclear. The few existing measurements are short-term observatio
ns of growing-season fluxes. We measured soil NOx emissions from six s
ites within the shortgrass steppe at the Central Plains Experimental R
ange in Colorado from June 1994 through October 1995. The soils at the
se sites provided a range of texture (from a sandy loam to a clay loam
) and soil moisture. Mean NOx emissions over the sampling period range
d from 2.6 to 5.7 ng NO-N m(-2)s(-1) from the four unfertilized sites.
Temperature was the dominant control on seasonal variations in NOx fl
uxes. Seasonal fluxes were highest in the summers (5.4 to 10.5 ng NO-N
m(-2)s(-1)) and lowest in the winter (0.2 to 1.5 ng NO-N m(-2)s(-1)).
The winter NOx emissions contribute up to 25% to the mean annual flux
. Water-filled pore space (WFPS) alone was a poor predictor of NOx emi
ssions; however, peak NOx emissions were found near the field capaciti
es for these soils (32-35% WFPS for coarse soils and 66% WFPS for fine
-textured soils). Water additions produced large (22-51 ng NO-N m(-2)s
(-1)) but short-lived (24 hour) pulses of NOx emissions that were inde
pendent of both the amount of water added and the number of antecedent
dry days. Short-term increases in NOx flux stimulated by wetting are
significant, and increase the summer estimate of NOx emissions 8 times
estimates calculated from periodic sampling. Nitrogen applied in prev
ious studies, 5 to 12 years earlier, increased the average annual NOx
emissions approximately 1.5 times. Extrapolating our estimate to simil
ar systems around the world, we estimate that grassland ecosystems, gl
obally, emit 1.0 Tg N yr(-1) as NOx. A current estimate of NOx emissio
ns from grassland soils is 0.6 Tg N yr(-1) [Davidson, 1991].