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δ 15 N of soil N and plants in a N‐saturated, subtropical forest of southern China
Author(s) -
Koba K.,
Isobe K.,
Takebayashi Y.,
Fang Y.T.,
Sasaki Y.,
Saito W.,
Yoh M.,
Mo J.,
Liu L.,
Lu X.,
Zhang T.,
Zhang W.,
Senoo K.
Publication year - 2010
Publication title -
rapid communications in mass spectrometry
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.528
H-Index - 136
eISSN - 1097-0231
pISSN - 0951-4198
DOI - 10.1002/rcm.4648
Subject(s) - delta , chemistry , soil carbon , soil ph , environmental chemistry , soil water , soil science , environmental science , physics , astronomy
We investigated the δ 15 N profile of N (extractable NH 4 + , NO 3 − , and organic N (EON)) in the soil of a N‐saturated subtropical forest. The order of δ 15 N in the soil was EON > NH 4 + > NO 3 − . Although the δ 15 N 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 δ 15 N between bulk soil N and EON (Δ 15 N bulk‐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 δ 15 N of EON, as in the case of soil microbial biomass δ 15 N. A thorough δ 15 N survey of available N (NH 4 + , NO 3 − , and EON) in the soil profiles from the organic layer to 100 cm depth revealed that the δ 15 N of the available N forms did not fully overlap with the δ 15 N of plants. This mismatch in δ 15 N 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.