Not all soil carbon is created equal : Labile and stable pools under nitrogen input

© 2024 The Author(s). Global Change Biology published by John Wiley & Sons Ltd.

Bibliographische Detailangaben
Veröffentlicht in:Global change biology. - 1999. - 30(2024), 7 vom: 01. Juli, Seite e17405
1. Verfasser: Zang, Huadong (VerfasserIn)
Weitere Verfasser: Mehmood, Imran, Kuzyakov, Yakov, Jia, Rong, Gui, Heng, Blagodatskaya, Evgenia, Xu, Xingliang, Smith, Pete, Chen, Haiqing, Zeng, Zhaohai, Fan, Mingsheng
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2024
Zugriff auf das übergeordnete Werk:Global change biology
Schlagworte:Journal Article 13C natural abundance SOM decomposition labile C pools microbial biomass microbial community nutrient availability stable C pools Soil Nitrogen mehr... N762921K75 Carbon 7440-44-0 Carbon Dioxide 142M471B3J Carbon Isotopes
Beschreibung
Zusammenfassung:© 2024 The Author(s). Global Change Biology published by John Wiley & Sons Ltd.
Anthropogenic activities have raised nitrogen (N) input worldwide with profound implications for soil carbon (C) cycling in ecosystems. The specific impacts of N input on soil organic matter (SOM) pools differing in microbial availability remain debatable. For the first time, we used a much-improved approach by effectively combining the 13C natural abundance in SOM with 21 years of C3-C4 vegetation conversion and long-term incubation. This allows to distinguish the impact of N input on SOM pools with various turnover times. We found that N input reduced the mineralization of all SOM pools, with labile pools having greater sensitivity to N than stable ones. The suppression in SOM mineralization was notably higher in the very labile pool (18%-52%) than the labile and stable (11%-47%) and the very stable pool (3%-21%) compared to that in the unfertilized control soil. The very labile C pool made a strong contribution (up to 60%) to total CO2 release and also contributed to 74%-96% of suppressed CO2 with N input. This suppression of SOM mineralization by N was initially attributed to the decreased microbial biomass and soil functions. Over the long-term, the shift in bacterial community toward Proteobacteria and reduction in functional genes for labile C degradation were the primary drivers. In conclusion, the higher the availability of the SOM pools, the stronger the suppression of their mineralization by N input. Labile SOM pools are highly sensitive to N availability and may hold a greater potential for C sequestration under N input at global scale
Beschreibung:Date Completed 08.07.2024
Date Revised 08.07.2024
published: Print
Citation Status MEDLINE
ISSN:1365-2486
DOI:10.1111/gcb.17405