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Fluxes of carbon dioxide, nitrous oxide, and methane in grass sod and winter wheat-fallow tillage management

Journal Article · · Journal of Environmental Quality
;  [1];  [2];  [3];  [4];  [5]
  1. Univ. of Nebraska, Lincoln, NE (United States). Dept. of Agronomy
  2. Dept. of Agriculture, Fort Collins, CO (United States)
  3. Dept. of Agriculture, Lincoln, NE (United States)
  4. Panhandle Research and Extension Center, Scottsbluff, NE (United States)
  5. FAL, Braunschweig (Germany)

Cropping and tillage management can increase atmospheric CO{sub 2}, N{sub 2}O, and CH{sub 4} concentrations, and contribute to global warming and destruction of the ozone layer. Fluxes of these gases in vented surface chambers, and water-filled pore space (WFPS) and temperature of surface soil were measured weekly from a long-term winter wheat (Triticum aestivum L.)-fallow rotation system under chemical and mechanical tillage follow management and compared with those from native grass sod at Sidney, NE, from March 1993 to July 1995. Cropping, tillage, within-field location, time of year, soil temperature, and WFPS influenced net greenhouse gas fluxes. Mean annual interrow CO{sub 2} emissions from wheat-fallow ranged from 6.0 to 20.1 kg C ha{sup {minus}1} d{sup {minus}1} and generally increased with intensity and degree of tillage. Nitrous oxide flux averaged < 1.2 g N ha{sup {minus}1} d{sup {minus}1} for sod and 1 to 2 g N ha{sup {minus}1} d{sup {minus}1} for wheat-fallow. Tillage during fallow increased N{sub 2}O flux by almost 100%. Nitrous oxide emissions were 1.5 to 3.7 times greater from crop row than interrow locations with greatest differences occurring during periods of highest N{sub 2}O emission. Mean annual N{sub 2}O flux over the 3 yr of study were 1.54 and 0.76 g N ha{sup {minus}1} d{sup {minus}1} for row and interrow locations. Methane uptake ranged from 5.9 to 9.9 g C ha{sup {minus}1} d{sup {minus}1} and was not influenced by row location. Seasonal CO{sub 2} and N{sub 2}O flux, and CH{sub 4} uptake ranked as spring {ge} summer > autumn > winter. Winter periods accounted for 4 to 10% and 3 to 47% of the annual CO{sub 2} and N{sub 2}O flux, respectively, and 12 to 21% of the annual CH{sub 4} uptake. Fluxes of CO{sub 2} and N{sub 2}O, and CH{sub 4} uptake increased linearly with soil temperature. No-till fallow exhibited the least threat to deterioration of atmospheric or soil quality as reflected by greater CH{sub 4} uptake, decreased N{sub 2}O and CO{sub w} emissions, and less loss of soil organic C than tilled soils. However, potential for increased C sequestration in this wheat-fallow system is limited due to reduced C input from intermittent cropping.

Sponsoring Organization:
USDOE
OSTI ID:
290129
Journal Information:
Journal of Environmental Quality, Journal Name: Journal of Environmental Quality Journal Issue: 5 Vol. 27; ISSN JEVQAA; ISSN 0047-2425
Country of Publication:
United States
Language:
English

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