Patterns and drivers of global gross nitrogen mineralization in soils

© 2021 John Wiley & Sons Ltd.

Bibliographische Detailangaben
Veröffentlicht in:Global change biology. - 1999. - 27(2021), 22 vom: 13. Nov., Seite 5950-5962
1. Verfasser: Elrys, Ahmed S (VerfasserIn)
Weitere Verfasser: Ali, Ahmad, Zhang, Huimin, Cheng, Yi, Zhang, Jinbo, Cai, Zu-Cong, Müller, Christoph, Chang, Scott X
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2021
Zugriff auf das übergeordnete Werk:Global change biology
Schlagworte:Journal Article Meta-Analysis 15N isotope dilution technique climate ecosystems gross nitrogen mineralization microbial biomass soil properties Soil Carbon mehr... 7440-44-0 Nitrogen N762921K75
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520 |a Soil gross nitrogen (N) mineralization (GNM), a key microbial process in the global N cycle, is mainly controlled by climate and soil properties. This study provides for the first time a comprehensive analysis of the role of soil physicochemical properties and climate and their interactions with soil microbial biomass (MB) in controlling GNM globally. Through a meta-analysis of 970 observations from 337 published papers from various ecosystems, we found that GNM was positively correlated with MB, total carbon, total N and precipitation, and negatively correlated with bulk density (BD) and soil pH. Our multivariate analysis and structural equation modeling revealed that GNM is driven by MB and dominantly influenced by BD and precipitation. The higher total N accelerates GNM via increasing MB. The decrease in BD stimulates GNM via increasing total N and MB, whereas higher precipitation stimulates GNM via increasing total N. Moreover, the GNM varies with ecosystem type, being greater in forests and grasslands with high total carbon and MB contents and low BD and pH compared to croplands. The highest GNM was observed in tropical wet soils that receive high precipitation, which increases the supply of soil substrate (total N) to microbes. Our findings suggest that anthropogenic activities that affect soil microbial population size, BD, soil substrate availability, or soil pH may interact with changes in precipitation regime and land use to influence GNM, which may ultimately affect ecosystem productivity and N loss to the environment 
650 4 |a Journal Article 
650 4 |a Meta-Analysis 
650 4 |a 15N isotope dilution technique 
650 4 |a climate 
650 4 |a ecosystems 
650 4 |a gross nitrogen mineralization 
650 4 |a microbial biomass 
650 4 |a soil properties 
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 Ali, Ahmad  |e verfasserin  |4 aut 
700 1 |a Zhang, Huimin  |e verfasserin  |4 aut 
700 1 |a Cheng, Yi  |e verfasserin  |4 aut 
700 1 |a Zhang, Jinbo  |e verfasserin  |4 aut 
700 1 |a Cai, Zu-Cong  |e verfasserin  |4 aut 
700 1 |a Müller, Christoph  |e verfasserin  |4 aut 
700 1 |a Chang, Scott X  |e verfasserin  |4 aut 
773 0 8 |i Enthalten in  |t Global change biology  |d 1999  |g 27(2021), 22 vom: 13. Nov., Seite 5950-5962  |w (DE-627)NLM098239996  |x 1365-2486  |7 nnns 
773 1 8 |g volume:27  |g year:2021  |g number:22  |g day:13  |g month:11  |g pages:5950-5962 
856 4 0 |u http://dx.doi.org/10.1111/gcb.15851  |3 Volltext 
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