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Stable Nitrogen and Carbon Isotope Compositions in Plant-soil Systems Under Different Land-use Types in a Red Soil Region, Southeast China

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Journal PeerJ
Date 2022 Jun 13
PMID 35694377
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Abstract

Background: Stable N isotope compositions in plant-soil systems have been widely used to indicate soil N transformation and translocation processes in ecosystems. However, soil N processes and nitrate ( ) loss potential under different land-use types are short of systematic comparison in the red soil region of Southeast China.

Methods: In the present study, the stable N and C isotope compositions ( N and C) of soil and leaf were analyzed to indicate soil N transformation processes, and the soil to plant N enrichment factor () was used to compare soil loss potential under different land-use types, including an abandoned agricultural land, a natural pure forest without understory, and a natural pure forest with a simple understory.

Results: The foliar N value (-0.8‰) in the abandoned agricultural land was greater than those of the forest lands (ranged from -2.2‰ to -10.8‰). In the abandoned agricultural land, N values of soil organic nitrogen (SON) increased from 0.8‰ to 5.7‰ and C values of soil organic carbon (SOC) decreased from -22.7‰ to -25.9‰ with increasing soil depth from 0-70 cm, mainly resulting from SON mineralization, soil organic matter (SOM) decomposition, and C plant input. In the soils below 70 cm depth, N values of SON (mean 4.9‰) were likely affected by microbial assimilation of N-depleted . The variations in N values of soil profiles under the two forests were similar, but the values were significant different between the pure forest with a simple understory (-10.0‰) and the forest without understory (-5.5‰).

Conclusions: These results suggest that soil to plant N enrichment factor have a great promise to compare soil loss potential among different ecosystems.

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