Soil Surface Fluxes of Greenhouse Gases in an Irrigated Maize-Based Agroecosystem

Authors

Brigid Amos, University of Nebraska-LincolnFollow
Timothy J. Arkebauer, University of Nebraska-LincolnFollow
John W. Doran, University of Nebraska-LincolnFollow

Date of this Version

2005

Comments

Published in Published in Soil Sci. Soc. Am. J. 69:387–395 (2005). Copyright © Soil Science Society of America. Used by permission.

Abstract

An understanding of the effect of fertility management on soil surface fluxes of CO₂, N₂O, and CH₄ is essential in evaluating C sequestration measures that attempt to increase the amount of crop residue returned to the soil through increased fertilizer inputs. In this, soil surface CO₂ flux was measured over a 27-mo sampling period in continuous maize (Zea mays L.) plots managed under either an intensive fertility regime (M2) or recommended best management (M1). Flux was significantly higher in the M2 treatment on only 2 d during the first growing season. Annual estimates of soil surface CO₂ flux, based on a modified exponential equation that incorporates leaf area index (LAI) to predict temporal changes in soil respiration, averaged 11 550 kg C ha^-1 yr^-1 for both treatments (approximately 31.64 kg C ha^-1 d^-1 on average). Within row soil surface CO₂ flux was, on average, 64% higher than between row flux. Plant population did not significantly affect measured soil surface CO2 flux. While fertility management had no significant effect on CH₄ flux, N₂O flux as measured on 3 d during the 2000 growing season was significantly higher in the M2 treatment. In 2001, no significant differences in N₂O flux were observed, possibly due to changes in N management and irrigation method. Electrical conductivity measured during the 2000 and 2001 growing seasons was significantly higher in the M2 treatment while pH measured during the 2001 season was significantly lower for M2.