Computed tomography scanning revealed macropore-controlled N 2 O emissions under long-term tillage and cover cropping practices.

Autor: Dhaliwal JK; Biosystems Engineering and Soil Science, University of Tennessee, Knoxville, TN, USA., Anderson SH; College of Agriculture, Food and Natural Resources, University of Missouri, Columbia, MO, USA., Lee J; Biosystems Engineering and Soil Science, University of Tennessee, Knoxville, TN, USA., Jagadamma S; Biosystems Engineering and Soil Science, University of Tennessee, Knoxville, TN, USA., Saha D; Biosystems Engineering and Soil Science, University of Tennessee, Knoxville, TN, USA. Electronic address: dsaha3@utk.edu.
Jazyk: angličtina
Zdroj: The Science of the total environment [Sci Total Environ] 2024 May 20; Vol. 926, pp. 171782. Date of Electronic Publication: 2024 Mar 22.
DOI: 10.1016/j.scitotenv.2024.171782
Abstrakt: Microscale alterations in soil physical characteristics resulting from long-term soil health practices can contribute to changes in soil nitrous oxide (N 2 O) emissions. In this study, we investigated soil N 2 O emissions in relation to pore characteristics influencing soil gas diffusivity under long-term tillage and cover cropping practices. Intact soil cores from tillage (conventional tillage, Conv. T versus no tillage, NT) and cover crop (hairy vetch, HV versus no cover crop, NC) treatments were used for N 2 O measurements and computed tomography (CT) scanning. Using X-ray CT technique with a resolution of 59 μm, pore structure parameters including macroporosity, number of macropores, anisotropy, fractal dimension, tortuosity, and connectivity were determined. The results showed that Conv. T and HV emitted significantly higher N 2 O than NT and NC, respectively. A similar trend was observed for macroporosity, Conv. T soils had 27.4 % higher CT-derived macroporosity than the NT soils and HV increased macroporosity by 31.1 % over the NC treatment. The number of macropores and fractal dimension were significantly higher whereas degree of anisotropy was significantly lower under HV compared to NC. In the upper 3 cm of soil, HV had a connected porosity, whereas the pores were disconnected and isolated in NC. These CT-derived properties; however, were not impacted by tillage treatments. N 2 O emissions were positively and significantly correlated to relative soil gas diffusivity, CT-derived macroporosity, number of macropores, and fractal dimension. Our results demonstrated that soil macroporosity and relative gas diffusivity could lead to improved understanding and predictability of N 2 O emissions under high soil moisture conditions.
Competing Interests: Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.
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Databáze: MEDLINE