Titlebook: Carbon Sequestration for Climate Change Mitigation and Adaptation; David A. N. Ussiri,Rattan Lal Book 2017 Springer International Publishi

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Nonarchimedean and Tropical Geometrye is most acute, food production must increase by more than 100% by 2050 to meet the global food demand. The average annual share of agriculture, forest and land use to the total anthropogenic greenhouse gases (GHGs) has been declining over time from 28.7?±?1.5% in the 1990s and 23.6?±?2.1% in 2000s

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https://doi.org/10.1007/978-3-319-30945-3y sectors and mitigation perspectives as well as from the perspective of developmental goals such as energy security and rural development. It is argued that increasing the contribution of biofuels will reduce the GHG emission by reducing the carbon intensity of the transport sector and addressing e

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imate change. Although the targeted audience is the educators, students, researchers and scientific community, the simplified analysis and synthesis of current and up to date scientific literature makes the volume easier to understand and a tool policy makers can use to make an informed policy decisions.978-3-319-85255-3978-3-319-53845-7

箴言

Introduction: Climate Overview,of the Earth’s climate system is discussed in this chapter. The?processes that Earth retains more electromagnetic radiation energy than it receives?are also explained. In addition, the role of greenhouse gases (GHGs) in regulating the energy balance is discussed with the emphasis on carbon dioxide (

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Introduction to Global Carbon Cycling: An Overview of the Global Carbon Cycle,ion. Fossil fuel and cement production released 410?±?20 Pg C between 1750 and 2015. Similarly, land use change released 190?±?65 Pg C over the same period. The atmospheric C burden increased by 260?±?5 Pg between 1750 and 2015. The consequences of changes in global C cycling extend beyond the globa

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The Global Carbon Inventory,soil inorganic C (SIC) in the top 3?m depth. The terrestrial SOC is dominantly preserved in forest biomass and soils. The ocean C inventory amounts to 39,000?Pg, of which, only 700–900?Pg?C exist in the surface water layer which is in direct contact with the atmosphere. More than 90% of C is present