Effect of Soil Drying Intensity During an Experimental Drying-Rewetting Event on Nutrient Transformation and Microbial Community Composition
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Siltation of check dams alters microbial communities and thus limits organic carbon mineralization
2024, Soil and Tillage ResearchEffects of drying-rewetting cycles on colloidal phosphorus composition in paddy and vegetable soils
2024, Science of the Total EnvironmentDry–wet cycles induce the decoupling of carbon and nitrogen mineralization at high temperatures in semi-arid grassland soil
2024, Soil Biology and BiochemistryResponses of soil microbial biomass carbon and dissolved organic carbon to drying-rewetting cycles: A meta-analysis
2021, CatenaCitation Excerpt :By contrast, the DWC stress significantly reduced MBC and DOC in a 60-day laboratory experiment of rice paddy soil (Novair et al., 2020). These distinct results may be caused by multiple factors, including soil fertility, drought intensity, oxygen and soluble substrates (e.g., nitrate) diffusion under different water conditions (Shi and Marschner, 2017; Sun et al., 2018; Ye et al., 2019; Dogan et al., 2020). The factors driving the variable effects of DWC on soil MBC and DOC among different studies remain unclear.
Impact of multiple drying and rewetting events on biochar amendments for Hg stabilization in floodplain soil from South River, VA
2021, ChemosphereCitation Excerpt :For example, bacteria that are more resistant to arid/semi-arid environments (e.g., Gemmatimonas and Ramlibacter) became more abundant in the biochar-amended systems. These shifts in taxonomic structure in soils are consistent with other observations after drying and rewetting events (Sun et al., 2018). As wetting and drying cycles increased, the microbial communities in HCSed and HCDIG were similar, while more distinct changes were observed in HCMOAK.
Effects of drought-flood abrupt alternation on phosphorus in summer maize farmland systems
2020, GeodermaCitation Excerpt :The soil P cycle has also been studied during the drying-rewetting process. The regular drying and rewetting events affect microbial survival and activity, alter soil aggregation, accelerate organic matter decomposition, and enhance soil P mineralization, which result in short-lived pulses of available P (Harrison-Kirk et al., 2014; Li et al., 2018; Sun et al., 2017a, b, 2018). Previous studies have mainly addressed the effects of individual drought events, individual flood events, the drying-rewetting process, or dry-wet cycling on the migration and transformation of P in soil and plants.