38 research outputs found
Forecasting Bond Risk Premia Using Technical Analysis
This paper is selected as one of the Top Ten Paper in Forecasting in SSRN
Eshelby tensor for a penny-shaped inclusion with limited thickness in transversely isotropic elastic medium
Efficient Access to Isoquinolines via Rhodium-Catalyzed Oxidative Annulation of Pyridyl C–H Bonds Directed by Carbonyl with Internal Alkynes
Actions, progress and prospects in implementation of the Convention on Biological Diversity during the past 20 years in China
Reusable N-Heterocyclic Carbene Complex Catalysts and Beyond: A Perspective on Recycling Strategies
Preparative Separation and Purification of Sesamin and Sesamolin from Sesame Seeds by High-Speed Counter-Current Chromatography
Interactive global change factors mitigate soil aggregation and carbon change in a semi-arid grassland
The ongoing global change is multi-faceted, but the interactive effects of multiple drivers on the persistence of soil carbon (C) are poorly understood. We examined the effects of warming, reactive nitrogen (N) inputs (12 g N m(-2) year(-1)) and altered precipitation (+ or - 30% ambient) on soil aggregates and mineral-associated C in a 4 year manipulation experiment with a semi-arid grassland on China's Loess Plateau. Our results showed that in the absence of N inputs, precipitation additions significantly enhanced soil aggregation and promoted the coupling between aggregation and both soil fungal biomass and exchangeable Mg2+. However, N inputs negated the promotional effects of increased precipitation, mainly through suppressing fungal growth and altering soil pH and clay-Mg2+-OC bridging. Warming increased C content in the mineral-associated fraction, likely by increasing inputs of root-derived C, and reducing turnover of existing mineral-associated C due to suppression of fungal growth and soil respiration. Together, our results provide new insights into the potential mechanisms through which multiple global change factors control soil C persistence in arid and semi-arid grasslands. These findings suggest that the interactive effects among global change factors should be incorporated to predict the soil C dynamics under future global change scenarios
