2020
DOI: 10.1007/s42832-020-0056-0
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Nitrogen addition inhibits total monoterpene emissions in subtropical forest floor of South China

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Cited by 9 publications
(8 citation statements)
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“…The surface litter layer served as a source of monoterpenes, with emissions (109.09 ± 41.75 ng g −1 h −1 ; Figure 3A) around one-tenth of the emission factor (1.02 ± 0.65 μg g −1 h −1 ; Zeng et al, 2022a) of E. urophylla reported in subtropical China. This contrasts with previous results from tropical and subtropical soils, where the presence of surface litter did not affect soil monoterpene exchanges (Huang et al, 2021;Llusià et al, 2022), although the emitted monoterpenes may hardly escape from the litter-soil layer due to higher soil uptakes of monoterpenes in this study. However, upward fluxes may occur when a large amount of litter (especially leaf litter, see below) covers the soil surface, leading to monoterpene production in the surface litter layer that exceeds soil uptakes of monoterpenes.…”
Section: Eucalyptus Urophylla Plantation Forestcontrasting
confidence: 99%
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“…The surface litter layer served as a source of monoterpenes, with emissions (109.09 ± 41.75 ng g −1 h −1 ; Figure 3A) around one-tenth of the emission factor (1.02 ± 0.65 μg g −1 h −1 ; Zeng et al, 2022a) of E. urophylla reported in subtropical China. This contrasts with previous results from tropical and subtropical soils, where the presence of surface litter did not affect soil monoterpene exchanges (Huang et al, 2021;Llusià et al, 2022), although the emitted monoterpenes may hardly escape from the litter-soil layer due to higher soil uptakes of monoterpenes in this study. However, upward fluxes may occur when a large amount of litter (especially leaf litter, see below) covers the soil surface, leading to monoterpene production in the surface litter layer that exceeds soil uptakes of monoterpenes.…”
Section: Eucalyptus Urophylla Plantation Forestcontrasting
confidence: 99%
“…This contrasts with the decrease in the observed rate of isoprene uptake from temperate forest soils at high temperature (>30°C, Cleveland and Yavitt, 1998). The significant negative linear correlation between monoterpene fluxes and soil temperature was consistent with results found in subtropical pine and broad-leaved forest soils (Huang et al, 2021) and temperate forest soils (Trowbridge et al, 2020). However, significant correlations of soil temperature with monoterpenes and sesquiterpenes contrast with the finding that neither terpene group correlated with soil temperature in tropical forest soils (Llusià et al, 2022).…”
Section: Abiotic and Biotic Controls Of Soil Isoprenoid Fluxes In The...supporting
confidence: 79%
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“…Across major terrestrial ecosystems worldwide, high N inputs may lead to variation in soil nutrient availability and soil acidification, which then can drive changes in plant species diversity and community composition (Bobbink et al, 2010; Payne et al, 2017). In China, high N deposition rates to forest ecosystems have resulted in soil acidification (Liu et al, 2011), plant biodiversity loss (Liu et al, 2013), carbon storage changes (Gu et al, 2015), changes in fluxes of greenhouse gases and increased susceptibility to environmental stresses (Huang et al, 2021; Liu et al, 2011). In contrast, the effects of N deposition on soil fauna have been less explored, especially ground‐dwelling fauna (Gan et al, 2014).…”
Section: Introductionmentioning
confidence: 99%