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δ15N of soil N and plants in a N‐saturated, subtropical forest of southern China

doi: 10.1002/rcm.4648
pmid: 20740523
AbstractWe investigated the δ15N profile of N (extractable NH, NO, and organic N (EON)) in the soil of a N‐saturated subtropical forest. The order of δ15N in the soil was EON > NH > NO. Although the δ15N of EON had been expected to be similar to that of bulk soil N, it was higher than that of bulk soil N by 5‰. The difference in δ15N between bulk soil N and EON (Δ15Nbulk‐EON) was correlated significantly with the soil C/N ratio. This correlation implies that carbon availability, which determines the balance between N assimilation and dissimilation of soil microbes, is responsible for the high δ15N of EON, as in the case of soil microbial biomass δ15N. A thorough δ15N survey of available N (NH, NO, and EON) in the soil profiles from the organic layer to 100 cm depth revealed that the δ15N of the available N forms did not fully overlap with the δ15N of plants. This mismatch in δ15N between that of available N and that of plants reflects apparent isotopic fractionation during N uptake by plants, emphasizing the high N availability in this N‐saturated forest. Copyright © 2010 John Wiley & Sons, Ltd.
- Tokyo University of Agriculture and Technology Japan
- University of Tokyo Japan
- Chinese Academy of Sciences China (People's Republic of)
- Chinese Academy of Sciences China (People's Republic of)
Analysis of Variance, China, Tropical Climate, Nitrates, Nitrogen Isotopes, Plants, Carbon, Mass Spectrometry, Potassium Chloride, Plant Leaves, Quaternary Ammonium Compounds, Soil, Linear Models, Biomass, Nitrogen Compounds
Analysis of Variance, China, Tropical Climate, Nitrates, Nitrogen Isotopes, Plants, Carbon, Mass Spectrometry, Potassium Chloride, Plant Leaves, Quaternary Ammonium Compounds, Soil, Linear Models, Biomass, Nitrogen Compounds
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