Soil gross nitrogen transformations in forestland and cropland of Regosols

Abstract Soil gross nitrogen (N) transformations could be influenced by land use change, however, the differences in inherent N transformations between different land use soils are still not well understood under subtropical conditions. In this study, an 15N tracing experiment was applied to determi...

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Main Authors: Xiao Ren, Jinbo Zhang, Hamidou Bah, Christoph Müller, Zucong Cai, Bo Zhu
Format: Article
Language:English
Published: Nature Publishing Group 2021-01-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-020-80395-x
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spelling doaj-877ed8a8f9e44beaae583a3259889d8e2021-01-10T12:48:40ZengNature Publishing GroupScientific Reports2045-23222021-01-0111111110.1038/s41598-020-80395-xSoil gross nitrogen transformations in forestland and cropland of RegosolsXiao Ren0Jinbo Zhang1Hamidou Bah2Christoph Müller3Zucong Cai4Bo Zhu5Key Laboratory of Mountain Surface Processes and Ecological Regulation, Institute of Mountain Hazards and Environment, Chinese Academy of SciencesSchool of Geography Sciences, Nanjing Normal UniversityKey Laboratory of Mountain Surface Processes and Ecological Regulation, Institute of Mountain Hazards and Environment, Chinese Academy of SciencesInstitute of Plant Ecology, Justus-Liebig University GiessenSchool of Geography Sciences, Nanjing Normal UniversityKey Laboratory of Mountain Surface Processes and Ecological Regulation, Institute of Mountain Hazards and Environment, Chinese Academy of SciencesAbstract Soil gross nitrogen (N) transformations could be influenced by land use change, however, the differences in inherent N transformations between different land use soils are still not well understood under subtropical conditions. In this study, an 15N tracing experiment was applied to determine the influence of land uses on gross N transformations in Regosols, widely distributed soils in Southwest China. Soil samples were taken from the dominant land use types of forestland and cropland. In the cropland soils, the gross autotrophic nitrification rates (mean 14.54 ± 1.66 mg N kg−1 day−1) were significantly higher, while the gross NH4 + immobilization rates (mean 0.34 ± 0.10 mg N kg−1 day−1) were significantly lower than those in the forestland soils (mean 1.99 ± 0.56 and 6.67 ± 0.74 mg N kg−1 day−1, respectively). The gross NO3 − immobilization and dissimilatory NO3 − reduction to NH4 + (DNRA) rates were not significantly different between the forestland and cropland soils. In comparison to the forestland soils (mean 0.51 ± 0.24), the cropland soils had significantly lower NO3 − retention capacities (mean 0.01 ± 0.01), indicating that the potential N losses in the cropland soils were higher. The correlation analysis demonstrated that soil gross autotrophic nitrification rate was negatively and gross NH4 + immobilization rate was positively related to the SOC content and C/N ratio. Therefore, effective measures should be taken to increase soil SOC content and C/N ratio to enhance soil N immobilization ability and NO3 − retention capacity and thus reduce NO3 − losses from the Regosols.https://doi.org/10.1038/s41598-020-80395-x
collection DOAJ
language English
format Article
sources DOAJ
author Xiao Ren
Jinbo Zhang
Hamidou Bah
Christoph Müller
Zucong Cai
Bo Zhu
spellingShingle Xiao Ren
Jinbo Zhang
Hamidou Bah
Christoph Müller
Zucong Cai
Bo Zhu
Soil gross nitrogen transformations in forestland and cropland of Regosols
Scientific Reports
author_facet Xiao Ren
Jinbo Zhang
Hamidou Bah
Christoph Müller
Zucong Cai
Bo Zhu
author_sort Xiao Ren
title Soil gross nitrogen transformations in forestland and cropland of Regosols
title_short Soil gross nitrogen transformations in forestland and cropland of Regosols
title_full Soil gross nitrogen transformations in forestland and cropland of Regosols
title_fullStr Soil gross nitrogen transformations in forestland and cropland of Regosols
title_full_unstemmed Soil gross nitrogen transformations in forestland and cropland of Regosols
title_sort soil gross nitrogen transformations in forestland and cropland of regosols
publisher Nature Publishing Group
series Scientific Reports
issn 2045-2322
publishDate 2021-01-01
description Abstract Soil gross nitrogen (N) transformations could be influenced by land use change, however, the differences in inherent N transformations between different land use soils are still not well understood under subtropical conditions. In this study, an 15N tracing experiment was applied to determine the influence of land uses on gross N transformations in Regosols, widely distributed soils in Southwest China. Soil samples were taken from the dominant land use types of forestland and cropland. In the cropland soils, the gross autotrophic nitrification rates (mean 14.54 ± 1.66 mg N kg−1 day−1) were significantly higher, while the gross NH4 + immobilization rates (mean 0.34 ± 0.10 mg N kg−1 day−1) were significantly lower than those in the forestland soils (mean 1.99 ± 0.56 and 6.67 ± 0.74 mg N kg−1 day−1, respectively). The gross NO3 − immobilization and dissimilatory NO3 − reduction to NH4 + (DNRA) rates were not significantly different between the forestland and cropland soils. In comparison to the forestland soils (mean 0.51 ± 0.24), the cropland soils had significantly lower NO3 − retention capacities (mean 0.01 ± 0.01), indicating that the potential N losses in the cropland soils were higher. The correlation analysis demonstrated that soil gross autotrophic nitrification rate was negatively and gross NH4 + immobilization rate was positively related to the SOC content and C/N ratio. Therefore, effective measures should be taken to increase soil SOC content and C/N ratio to enhance soil N immobilization ability and NO3 − retention capacity and thus reduce NO3 − losses from the Regosols.
url https://doi.org/10.1038/s41598-020-80395-x
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