2022
DOI: 10.1016/j.envpol.2022.118876
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Soil N2O emission in Cinnamomum camphora plantations along an urbanization gradient altered by changes in litter input and microbial community composition

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Cited by 13 publications
(3 citation statements)
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“…In addition to climate conditions, greater atmospheric N deposition (due to fossil fuel combustion and industrial processes) as well as anthropogenic management (e.g., N fertilization and irrigation) in urban greenspaces can result in increased abundances and activity of ammonia oxidizer and denitrifier populations, and higher soil inorganic N concentrations and soil TN content [as shown in this and previous (Dutt & Tanwar, 2020) studies]. These changes in soil nutrient concentrations and the soil microbiome in urban soils support greater rates of nitrification and denitrification and subsequent N 2 O emissions (Rao et al, 2014; Xu et al, 2022; Zhang, Zhang, et al, 2022). Higher rates of N cycling in urban soils usually leads to a reduction in CH 4 uptake by suppressing methanotroph populations and activities (Bodelier, 2011; Costa & Groffman, 2013; Kravchenko et al, 2002; Tate, 2015; Wu et al, 2022).…”
Section: Discussionsupporting
confidence: 61%
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“…In addition to climate conditions, greater atmospheric N deposition (due to fossil fuel combustion and industrial processes) as well as anthropogenic management (e.g., N fertilization and irrigation) in urban greenspaces can result in increased abundances and activity of ammonia oxidizer and denitrifier populations, and higher soil inorganic N concentrations and soil TN content [as shown in this and previous (Dutt & Tanwar, 2020) studies]. These changes in soil nutrient concentrations and the soil microbiome in urban soils support greater rates of nitrification and denitrification and subsequent N 2 O emissions (Rao et al, 2014; Xu et al, 2022; Zhang, Zhang, et al, 2022). Higher rates of N cycling in urban soils usually leads to a reduction in CH 4 uptake by suppressing methanotroph populations and activities (Bodelier, 2011; Costa & Groffman, 2013; Kravchenko et al, 2002; Tate, 2015; Wu et al, 2022).…”
Section: Discussionsupporting
confidence: 61%
“…Urbanization significantly alters these factors due to heat island effects, increased atmospheric N deposition as a result of industrial and traffic emissions, and soil compaction and redistribution in the course of urban landscaping. This alteration affects C and N biogeochemical cycles in urban soils and associated production and consumption of CH 4 and N 2 O (Groffman et al, 2009; Kaye et al, 2006; Ni & Groffman, 2018; Xu et al, 2022). Previous studies have reported low or full inhibition of soil atmospheric CH 4 uptake in urban forests and lawns in China and the United States due to increases in soil bulk density (BD), which constrains diffusion of atmospheric CH 4 to sites of microbial CH 4 uptake by methanotrophs, or increases in soil N availability, which may directly inhibit CH 4 uptake (Groffman & Pouyat, 2009; Kaye et al, 2004; Zhang et al, 2014).…”
Section: Introductionmentioning
confidence: 99%
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