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Carbon footprint and carbon balance of three long‐term dryland cropping sequences.

Authors :
Sainju, Upendra M.
Allen, Brett L.
Source :
Soil Science Society of America Journal. Jul2024, Vol. 88 Issue 4, p1405-1418. 14p.
Publication Year :
2024

Abstract

Carbon footprints from plants, soil, and the environment are needed to evaluate C balance of an agroecosystem, which indicates if a system is a C source or sink for mitigating climate change. There is scarce information about C footprint and C balance in dryland agroecosystems. We measured C storage of above‐ and belowground crop biomass, CO2 fluxes, soil C sequestration rates, and C balances of three long‐term (34‐year‐old) dryland cropping sequences from 2016 to 2018 in the US northern Great Plains. Cropping sequences were no‐till continuous spring wheat (NTCW; Triticum aestivum L.), no‐till spring wheat–pea (NTWP; Pisum sativum L.), and conventional till spring wheat–fallow (CTWF). Carbon storage in grain, straw, root, and rhizodeposit were 29%–61% greater for NTCW and NTWP than CTWF. The CO2 flux peaked immediately after tillage, planting, fertilization, and intense precipitation (>10 mm) for 3 months in 2016–2017. Cumulative annual CO2 flux was 8%–37% greater for NTCW than NTWP and CTWF in 2016–2017, but was not different among cropping sequences in 2017–2018. Soil C sequestration rate at 0–10 cm measured from 2012 to 2019 was in the order: NTCW (0.27 Mg C ha−1 year−1) > NTWP > CTWF (−0.23 Mg C ha−1 year−1). Carbon balance remained negative and was not significantly different among cropping sequences but varied by year. Carbon loss increased with increased precipitation, regardless of cropping systems. Although a C source, the legume–nonlegume rotation can reduce C loss due to greater grain C output than other cropping sequences in the semiarid region of the northern Great Plains. Core Ideas: Above‐ and belowground C inputs were greater for continuous cropping than crop‐fallow.Cumulative annual CO2 flux was greater for continuous cropping than crop‐fallow in the wet year.Soil C sequestration rate was also greater for continuous cropping than crop‐fallow.All dryland cropping systems were C sources.Legume–nonlegume rotation may reduce C loss and enhance grain C output compared to other cropping sequences. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
03615995
Volume :
88
Issue :
4
Database :
Academic Search Index
Journal :
Soil Science Society of America Journal
Publication Type :
Academic Journal
Accession number :
178355958
Full Text :
https://doi.org/10.1002/saj2.20703