Forms of nitrogen inputs regulate the intensity of soil acidification

© 2023 John Wiley & Sons Ltd.

Bibliographische Detailangaben
Veröffentlicht in:Global change biology. - 1999. - 29(2023), 14 vom: 11. Juli, Seite 4044-4055
1. Verfasser: Wang, Ze (VerfasserIn)
Weitere Verfasser: Tao, Tingting, Wang, Hu, Chen, Ji, Small, Gaston E, Johnson, David, Chen, Jihui, Zhang, Yingjun, Zhu, Qichao, Zhang, Shengmin, Song, Yantao, Kattge, Jens, Guo, Peng, Sun, Xiao
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2023
Zugriff auf das übergeordnete Werk:Global change biology
Schlagworte:Meta-Analysis Journal Article exchangeable cations nitrogen addition rate nitrogen composition plant community soil buffering system soil pH Soil Nitrogen N762921K75
Beschreibung
Zusammenfassung:© 2023 John Wiley & Sons Ltd.
Soil acidification induced by reactive nitrogen (N) inputs can alter the structure and function of terrestrial ecosystems. Because different N-transformation processes contribute to the production and consumption of H+ , the magnitude of acidification likely depends on the relative amounts of organic N (ON) and inorganic N (IN) inputs. However, few studies have explicitly measured the effects of N composition on soil acidification. In this study, we first conducted a meta-analysis to test the effects of ON or IN inputs on soil acidification across 53 studies in grasslands. We then compared soil acidification across five different ON:IN ratios and two input rates based on long-term field N addition experiments. The meta-analysis showed that ON had weaker effects on soil acidification than IN when the N addition rate was above 20 g N m-2  year-1 . The field experiment confirmed the findings from meta-analysis: N addition with proportions of ON ≥ 20% caused less soil acidification, especially at a high input rate (30 g N m-2  year-1 ). Structural equation model analysis showed that this result was largely due to a relatively low rate of H+ production from ON as NH3 volatilization and uptake of ON and NH4 + by the dominant grass species Leymus chinensis (which are both lower net contributors to H+ production) result in less NH4 + available for nitrification (which is a higher net contributor to H+ production). These results indicate that the evaluation of soil acidification induced by N inputs should consider N forms and manipulations of relative composition of N inputs may provide an effective approach to alleviate the N-induced soil acidification
Beschreibung:Date Completed 15.06.2023
Date Revised 31.08.2023
published: Print-Electronic
Citation Status MEDLINE
ISSN:1365-2486
DOI:10.1111/gcb.16746