Poster's note : relevant to soil carbon CDR, and BECCS. Also has impacts on
SRM, as the crop residue albedo is a significant factor. I'd recommend
reading the non-technical version at
https://dl.sciencesocieties.org/node/209/view which more clearly explains
both the work and the CE impacts.

https://dl.sciencesocieties.org/publications/sssaj/abstracts/79/2/612

doi:10.2136/sssaj2014.07.0298

Greenhouse Gas Emissions Dynamics as Influenced by Corn Residue Removal in
Continuous Corn System

Jose Guzman *a,
Mahdi Al-Kaisib and
Timothy Parkinc

Abstract

The removal of corn residue for bioethanol may require changes in current
tillage and fertilization practices to minimize potential alterations to
the soil environment that may lead to increase in greenhouse gas (GHG)
emission. The objectives of this study were to examine how tillage, N
fertilization rates, residue removal, and their interactions affect CO2,
and N2O soil surface emissions. Greater CO2 emission coincided with higher
soil temperatures typically observed with conventional tillage (CT)
compared with no-tillage (NT), resulting in greater annual cumulative CO2
emission in CT (18.1 CO2 Mg ha−1 yr−1) compared with NT (16.2 CO2 Mg ha−1
yr−1) in 2009 and 2010 across sites. However, drier soil conditions during
the growing season in 2011 lead to higher soil temperatures compared with
2009 and 2010. Consequently, annual cumulative CO2 emission from NT with 50
and 100% residue removal was (19.5 CO2 Mg ha−1 yr−1) greater than that from
CT (17.8 CO2 Mg ha−1 yr−1) across all residue removal rates and from NT
(17.5 CO2 Mg ha−1 yr−1) with no residue removal, respectively across all N
rates in the Ames central site (AC) in 2011. In the Armstrong southwest
site (ASW) site, there were no significant differences between tillage or
residue removal rates for annual cumulative CO2 emission (19.9 CO2 Mg ha−1
yr−1) in 2011. Although N2O emission was considerably lower than CO2
emission, differences in N fertilization rates did have a significant
impact on global warming potential once these gases were converted on the
basis of their radiative forcing of the atmosphere.

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