Controls on annual emissions of nitric oxide from soils of the Colorado shortgrass steppe

R. E. Martin, M. C. Scholes, A. R. Mosier, D. S. Ojima, E. A. Holland, W. J. Parton

Research output: Contribution to journalArticle

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Abstract

Estimates of NOx (NO+NO2) emissions from temperate grasslands range from 0.003 to 101 ng NO-N m-2s- (average 4.17 ng NO-N m-2s-1). As a result of this uncertainty, the potential contribution of soil NOx emissions to the global budget and to nitrogen loss for this ecosystem is unclear. The few existing measurements are short-term observations of growing-season fluxes. We measured soil NOx emissions from six sites within the shortgrass steppe at the Central Plains Experimental Range in Colorado from June 1994 through October 1995. The soils at these sites provided a range of texture (from a sandy loam to a clay loam) and soil moisture. Mean NOx emissions over the sampling period ranged 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 fluxes. 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 emissions; however, peak NOx emissions were found near the field capacities 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 independent 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 previous studies, 5 to 12 years earlier, increased the average annual NOx emissions approximately 1.5 times. Extrapolating our estimate to similar systems around the world, we estimate that grassland ecosystems, globally, emit 1.0 Tg N yr-1 as NOx. A current estimate of NOx emissions from grassland soils is 0.6 Tg N yr1 [Davidson, 1991].

Original languageEnglish (US)
Pages (from-to)81-91
Number of pages11
JournalGlobal Biogeochemical Cycles
Volume12
Issue number1
DOIs
StatePublished - Mar 1 1998
Externally publishedYes

Fingerprint

nitric oxide
steppe
Nitric Oxide
Soils
Fluxes
Water
soil
pore space
Ecosystems
soil emission
Nitrogen
Sampling
water
Soil moisture
grassland soil
clay loam
nitrogen
Wetting
field capacity
winter

ASJC Scopus subject areas

  • Global and Planetary Change
  • Environmental Chemistry
  • Environmental Science(all)
  • Atmospheric Science

Cite this

Controls on annual emissions of nitric oxide from soils of the Colorado shortgrass steppe. / Martin, R. E.; Scholes, M. C.; Mosier, A. R.; Ojima, D. S.; Holland, E. A.; Parton, W. J.

In: Global Biogeochemical Cycles, Vol. 12, No. 1, 01.03.1998, p. 81-91.

Research output: Contribution to journalArticle

Martin, R. E. ; Scholes, M. C. ; Mosier, A. R. ; Ojima, D. S. ; Holland, E. A. ; Parton, W. J. / Controls on annual emissions of nitric oxide from soils of the Colorado shortgrass steppe. In: Global Biogeochemical Cycles. 1998 ; Vol. 12, No. 1. pp. 81-91.
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