tailieunhanh - Soil organic carbon responses under different forest cover of manipur: A review

The relentlessly increase of atmospheric carbon dioxide (CO2) concentration due to release from different sources leads to global warming and climate change which are a cause for great concern demanding in-depth research on CO2 emission from soil under different forest cover. Forest cover can reverse the increasing CO2 in the atmosphere, thus, contributes to mitigate climate change. Forest stored about half of the organic carbon (C) contained in terrestrial ecosystems. The role of forests has a great impact on the global biogeochemical cycles and in particular, the carbon cycle. Larger parts of the global C stock are stored in forest ecosystems. So, identifying the tree species in a forest with high SOC, soil organic carbon stocks (SOCS) and high C sequestration with low CO2 emission is a priority for mitigating the global climate change. Carbon sequestration in forest occurs in both aboveground and below ground biomass. But, the below ground C sequestration was quite low in comparison to the above ground. The rate of C sequestration in Schizostachyum pergracile dominant forest was Mg ha–1 year–1 whereas for Dipterocarpus tuberculatus dominant forest was Mg ha-1 year-1 . The annual organic C input (gCm-2 year-1 ) as litter fall of forest dominated by Quercus serrata + Schima wallichii and Ficus virens + Cinnamomum zeylanicum, were and respectively. | Soil organic carbon responses under different forest cover of manipur: A review

• Hoá học
• Carbon sequestration
• Soil organic carbon stock
• Oak forest
• Different forest cover
• Soil organic carbon responses
• Soil carbon
• Carbon sequestration potential
• Natural forest or soil erosion
• Carbon storage potential
• Soil quality
• Climate change
• Soil organic carbon
• Carbon sequestration in climate change
• Tree biomass
• Medicinal tree species
• Kafal (Myrica esculenta)
• Carbon sequestration potential of Kafal
• Soil microbial carbon and nitrogen
• Enzymatic activity
• Soybean intercropping system
• Agroforestry systems
• CH4 sinks
• Crop residue
• Cover crop
• Carbon sequestration in soils
• Climate change scenario
• Clay fraction
• Green house
• Different land uses
• Soil carbon sequestration
• Quantifying the stock
• Conservation tillage
• Soil physical properties
• Soil organic carbon sequestration
• RWCS in an inceptisol
• Oil palm
• Irrigated conditions
• Smart agriculture
• Climate resilient agriculture
• Precision agriculture
• Carbon stocks
• Populus deltoides plantations
• Aboveground biomass
• Carbon mitigation
• Carbon mineralization
• Irrigated rice wheat rotation
• Green house gas
• Carbon rich charcoal like substance created
• SOC sequestration
• Nutrient balances
• Nutrient balances in vertisols
• Native vegetation
• Biomass carbon
• Carbon fixation
• Increasing ecosystem service
• Above ground biomass
• Below ground biomass
• Moisture content
• Fixed carbon
• Agricultural residues
• Slow pyrolysis
• Total carbon content
• Green house gas mitigation
• Impact of clay mineralogy
• Clay mineralogy
• Clay mineralogy on stabilization
• Long term carbon sequestration
• Land use
• Soil series
• Organic carbon stock
• Dominant soil series
• Tree biomass etc
• Rhododendron arboretum
• State flower of Uttarakhand
• Carbon stock
• Cocoa and biomass
• Oil palm cocoa cropping system grown
• Agrisilvicultural system
• Dalbergia sissoo
• Agronomic practices
• Based agri silviculture system
• Agro forestry system
• Reduced tillage and mulching
• Different cultivation practices
• Mulberry vis à vis soils
• Cereal crops
• Vegetable crops
• Fruit crops
• Soil properties
• Agroforestry system
• Agrisilvicultural systems
• Agri silvihorticultural systems
• BC ratio
• Biomass and economic yield