Matches in SemOpenAlex for { <https://semopenalex.org/work/W3039454493> ?p ?o ?g. }
- W3039454493 endingPage "107896" @default.
- W3039454493 startingPage "107896" @default.
- W3039454493 abstract "Altered drying-rewetting patterns due to climate change may affect soil nitrogen (N) and phosphorus (P) cycling in terrestrial ecosystems. The responses of soil N and P cycling to drying and rewetting cycles can vary with drying-rewetting patterns, experimental methods, ecosystems, and soil types, thus making a synthesis of these studies necessary for understanding mechanisms and predicting future responses to climate change. Here, we compiled data of 1882 observations from 79 studies for a meta-analysis of the responses of soil N and P pools and fluxes to drying and rewetting and how these responses are modified by experimental conditions. Results showed that 1) experimental drying increased NH 4 + , extractable organic nitrogen (EON), and available P in the soil significantly by 22, 27, and 72%, respectively. In contrast, soil NO 3 − , enzymatic activities, microbial biomass, net nitrification, and N 2 O emissions significantly decreased by 37, 13–21, 21–28, 39, and 93%, respectively. 2) Upon rewetting of dried soil, soil EON, extractable organic phosphorus (EOP), net N mineralization, nitrification, phosphatase activity, dissolved organic N leaching, dissolved inorganic P leaching, and N 2 O emissions significantly increased by 59, 27, 19, 15, 12, 60, 116, and 218%, respectively, while soil NO 3 − and NO 3 − leaching significantly decreased by 9 and 74%, respectively. Soil microbial N and P as well as enzymatic activities recovered from drought during the rewetting phase. The mean effect sizes of drying and rewetting generally increased with drying intensity, which was probably also the main reason for greater effect sizes observed in laboratory than in field experiments. Our meta-analysis showed stronger positive responses of available P to drying and rewetting than mineral N, which agreed with greater effect sizes on P than on N leaching. This suggests that drying and rewetting induce an imbalance between N and P, which was more pronounced in soils from forests than from agricultural systems. Overall, these results imply that the expected increase in the frequency and intensity of droughts potentially decouples the cycling of P and N, with consequences for nutrient leaching and the supply of plants and microorganisms with these nutrients. • We compiled data of 1882 observations and conducted a meta-analysis. • Drying and rewetting significantly affected soil N and P pools and fluxes. • Soil microorganisms could recover from drought on rewetting. • There were higher effect sizes of N and P in laboratory than in field. • The responses of soil N and P also depended on soil and land use types." @default.
- W3039454493 created "2020-07-10" @default.
- W3039454493 creator A5020102404 @default.
- W3039454493 creator A5027592742 @default.
- W3039454493 creator A5034782016 @default.
- W3039454493 creator A5063317810 @default.
- W3039454493 creator A5087129072 @default.
- W3039454493 creator A5089042170 @default.
- W3039454493 date "2020-09-01" @default.
- W3039454493 modified "2023-10-17" @default.
- W3039454493 title "Responses of soil nitrogen and phosphorus cycling to drying and rewetting cycles: A meta-analysis" @default.
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