Afforestation of loess soils: Old and new organic carbon in aggregates and density fractionsAfforestation is an important strategy to increase
soil organic carbon (SOC) stocks and stabilize
Fate of Organic and Inorganic Nitrogen in Crusted and Non-Crusted Kobresia Grasslands by overgrazing. However, the fate of inorganic and
organic N in non-crusted and crusted patches in Kobresia
The effect of microorganisms on soil carbonate recrystallization and abiotic CO2 uptake of soil and alkaline
soil, microorganisms may affect the exchange of inorganic
carbon between the
soil solution
Temperature sensitivity of SOM decomposition is linked with a K-selected microbial communityLi H.,
Yang S.,
Semenov M.V.,
Yao F.,
Ye J.,
Bu R.,
Ma R.,
Lin J.,
Kurganova I.,
Wang X.,
Deng Y.,
Kravchenko I.,
Jiang Y.,
Kuzyakov Y. Temperature sensitivity (Q10) of
soil organic matter (SOM) decomposition is a crucial parameter
Root exudate chemistry affects soil carbon mobilization via microbial community reassembly of dissolved
organic carbon (DOC) and bioavailable Fe in an Ultisol through the disruption of organo
Loss of labile organic carbon from subsoil due to land-use changes insubtropical China evaluated
soil labile
organic C fractions, including particulate
organic carbon (POC) and its components
Effect of CO2 increase on ecological parameters of plant ecosystems of Central and South America countries,5%). This analysis is useful for planning environmental practices in order to increase
carbon storage. © The Authors