Interactive global change factors mitigate soil aggregation and carbon change in a semi-arid grassland

© 2020 John Wiley & Sons Ltd.

Bibliographische Detailangaben
Veröffentlicht in:Global change biology. - 1999. - 26(2020), 9 vom: 13. Sept., Seite 5320-5332
1. Verfasser: Bai, Tongshuo (VerfasserIn)
Weitere Verfasser: Wang, Peng, Hall, Steven J, Wang, Fuwei, Ye, Chenglong, Li, Zhen, Li, Shijie, Zhou, Luyao, Qiu, Yunpeng, Guo, Jiuxin, Guo, Hui, Wang, Yi, Hu, Shuijin
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2020
Zugriff auf das übergeordnete Werk:Global change biology
Schlagworte:Journal Article N-induced acidification aggregate stability carbonate global change mineral-associated C soil respiration Soil Carbon 7440-44-0 mehr... Nitrogen N762921K75
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520 |a The ongoing global change is multi-faceted, but the interactive effects of multiple drivers on the persistence of soil carbon (C) are poorly understood. We examined the effects of warming, reactive nitrogen (N) inputs (12 g N m-2  year-1 ) and altered precipitation (+ or - 30% ambient) on soil aggregates and mineral-associated C in a 4 year manipulation experiment with a semi-arid grassland on China's Loess Plateau. Our results showed that in the absence of N inputs, precipitation additions significantly enhanced soil aggregation and promoted the coupling between aggregation and both soil fungal biomass and exchangeable Mg2+ . However, N inputs negated the promotional effects of increased precipitation, mainly through suppressing fungal growth and altering soil pH and clay-Mg2+ -OC bridging. Warming increased C content in the mineral-associated fraction, likely by increasing inputs of root-derived C, and reducing turnover of existing mineral-associated C due to suppression of fungal growth and soil respiration. Together, our results provide new insights into the potential mechanisms through which multiple global change factors control soil C persistence in arid and semi-arid grasslands. These findings suggest that the interactive effects among global change factors should be incorporated to predict the soil C dynamics under future global change scenarios 
650 4 |a Journal Article 
650 4 |a N-induced acidification 
650 4 |a aggregate stability 
650 4 |a carbonate 
650 4 |a global change 
650 4 |a mineral-associated C 
650 4 |a soil respiration 
650 7 |a Soil  |2 NLM 
650 7 |a Carbon  |2 NLM 
650 7 |a 7440-44-0  |2 NLM 
650 7 |a Nitrogen  |2 NLM 
650 7 |a N762921K75  |2 NLM 
700 1 |a Wang, Peng  |e verfasserin  |4 aut 
700 1 |a Hall, Steven J  |e verfasserin  |4 aut 
700 1 |a Wang, Fuwei  |e verfasserin  |4 aut 
700 1 |a Ye, Chenglong  |e verfasserin  |4 aut 
700 1 |a Li, Zhen  |e verfasserin  |4 aut 
700 1 |a Li, Shijie  |e verfasserin  |4 aut 
700 1 |a Zhou, Luyao  |e verfasserin  |4 aut 
700 1 |a Qiu, Yunpeng  |e verfasserin  |4 aut 
700 1 |a Guo, Jiuxin  |e verfasserin  |4 aut 
700 1 |a Guo, Hui  |e verfasserin  |4 aut 
700 1 |a Wang, Yi  |e verfasserin  |4 aut 
700 1 |a Hu, Shuijin  |e verfasserin  |4 aut 
773 0 8 |i Enthalten in  |t Global change biology  |d 1999  |g 26(2020), 9 vom: 13. Sept., Seite 5320-5332  |w (DE-627)NLM098239996  |x 1365-2486  |7 nnns 
773 1 8 |g volume:26  |g year:2020  |g number:9  |g day:13  |g month:09  |g pages:5320-5332 
856 4 0 |u http://dx.doi.org/10.1111/gcb.15220  |3 Volltext 
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