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Can conservation tillage reduce N 2 O emissions on cropland transitioning to organic vegetable production?

Nitrous oxide (N O) is an important greenhouse gas and a catalyst of stratospheric ozone decay. Agricultural soils are the source of 75% of anthropogenic N O emissions globally. Recently, significant attention has been directed at examining effects of conservation tillage on carbon sequestration in...

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Bibliographic Details
Published in:The Science of the total environment 2018-03, Vol.618, p.927
Main Authors: Chen, Guihua, Kolb, Lauren, Cavigelli, Michel A, Weil, Ray R, Hooks, Cerruti R R
Format: Article
Language:English
Online Access:Get full text
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Summary:Nitrous oxide (N O) is an important greenhouse gas and a catalyst of stratospheric ozone decay. Agricultural soils are the source of 75% of anthropogenic N O emissions globally. Recently, significant attention has been directed at examining effects of conservation tillage on carbon sequestration in agricultural systems. However, limited knowledge is available regarding how these practices impact N O emissions, especially for organic vegetable production systems. In this context, a three-year study was conducted in a well-drained sandy loam field transitioning to organic vegetable production in the Mid-Atlantic coastal plain of USA to investigate impacts of conservation tillage [strip till (ST) and no-till (NT)] and conventional tillage (CT) [with black plastic mulch (CT-BP) and bare-ground (CT-BG)] on N O emissions. Each year, a winter cover crop mixture (forage radish: Raphanus sativus var. longipinnatus, crimson clover: Trifolium incarnatum L., and rye: Secale cereale L.) was grown and flail-mowed in the spring. Nearly 80% of annual N O-nitrogen (N) emissions occurred during the vegetable growing season for all treatments. Annual N O-N emissions were greater in CT-BP than in ST and NT, and greater in CT-BG than in NT, but not different between CT-BG and CT-BP, ST and NT, or CT-BG and ST. Conventional tillage promoted N mineralization and plastic mulch increased soil temperature, which contributed to greater N O-N fluxes. Though water filled porosity in NT was higher and correlated well with N O-N fluxes, annual N O-N emissions were lowest in NT suggesting a lack of substrates for nitrification and denitrification processes. Crop yield was lowest in NT in Year 1 and CT-BP in Year 3 but yield-scaled N O-N emissions were consistently greatest in CT-BP and lowest in NT each year. Our results suggest that for coarse-textured soils in the coastal plain with winter cover crops, conservation tillage practices may reduce N O emissions in organic vegetable production systems.
ISSN:1879-1026