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• W2034004833 abstract "Abstract The dominant pools of C and N in the terrestrial biosphere are in soils, and understanding what factors control the rates at which these pools cycle is essential in understanding soil CO 2 production and N availability. Many previous studies have examined large scale patterns in decomposition of C and N in plant litter and organic soils, but few have done so in mineral soils, and fewer have looked beyond ecosystem specific, regional, or gradient-specific drivers. In this study, we examined the rates of microbial respiration and net N mineralization in 84 distinct mineral soils in static laboratory incubations. We examined patterns in C and N pool sizes, microbial biomass, and process rates by vegetation type (grassland, shrubland, coniferous forest, and deciduous/broadleaf forest). We also modeled microbial respiration and net N mineralization in relation to soil and site characteristics using structural equation modeling to identify potential process drivers across soils. While we did not explicitly investigate the influence of soil organic matter quality, microbial community composition, or clay mineralogy on microbial process rates in this study, our models allow us to put boundaries on the unique explanatory power these characteristics could potentially provide in predicting respiration and net N mineralization. Mean annual temperature and precipitation, soil C concentration, microbial biomass, and clay content predicted 78% of the variance in microbial respiration, with 61% explained by microbial biomass alone. For net N mineralization, only 33% of the variance was explained, with mean annual precipitation, soil C and N concentration, and clay content as the potential drivers. We suggest that the high R 2 for respiration suggests that soil organic matter quality, microbial community composition, and clay mineralogy explain at most 22% of the variance in respiration, while they could explain up to 67% of the variance in net N mineralization." @default.
• W2034004833 created "2016-06-24" @default.
• W2034004833 creator A5020677883 @default.
• W2034004833 creator A5049200035 @default.
• W2034004833 date "2013-05-01" @default.
• W2034004833 modified "2023-10-17" @default.
• W2034004833 title "Drivers of microbial respiration and net N mineralization at the continental scale" @default.
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• W2034004833 cites W1964994969 @default.
• W2034004833 cites W1968092043 @default.
• W2034004833 cites W1974180425 @default.
• W2034004833 cites W1981481141 @default.
• W2034004833 cites W1983818948 @default.
• W2034004833 cites W1989937096 @default.
• W2034004833 cites W1989998931 @default.
• W2034004833 cites W1990385015 @default.
• W2034004833 cites W1993778218 @default.
• W2034004833 cites W1996440470 @default.
• W2034004833 cites W1999167246 @default.
• W2034004833 cites W2000766108 @default.
• W2034004833 cites W2007903517 @default.
• W2034004833 cites W2008962657 @default.
• W2034004833 cites W2010676906 @default.
• W2034004833 cites W2016071773 @default.
• W2034004833 cites W2020971327 @default.
• W2034004833 cites W2023172395 @default.
• W2034004833 cites W2027407472 @default.
• W2034004833 cites W2027770048 @default.
• W2034004833 cites W2027815129 @default.
• W2034004833 cites W2028960858 @default.
• W2034004833 cites W2032604387 @default.
• W2034004833 cites W2035177583 @default.
• W2034004833 cites W2038714217 @default.
• W2034004833 cites W2040682725 @default.
• W2034004833 cites W2053621112 @default.
• W2034004833 cites W2060565559 @default.
• W2034004833 cites W2066202928 @default.
• W2034004833 cites W2066232493 @default.
• W2034004833 cites W2069222203 @default.
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• W2034004833 cites W2098838415 @default.
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• W2034004833 doi "https://doi.org/10.1016/j.soilbio.2013.01.003" @default.
• W2034004833 hasPublicationYear "2013" @default.
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