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Soil organic carbon sequestration and climate change
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Anthropogenic activities, in particular the burning of fossil fuels and land use changes, have resulted in a substantial increase in greenhouse gases (GHGs) in the atmosphere, which are causing mea...
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07 November 2022

Anthropogenic activities, in particular the burning of fossil fuels and land use changes, have resulted in a substantial increase in greenhouse gases (GHGs) in the atmosphere, which are causing measurable climate change. Climate change directly affects agricultural production and food security through changes in precipitation patterns, elevated temperature, and occurrence of extreme events. It warrants strategies to draw down anthropogenic GHGs from the atmosphere and their long-term storage in soil as soil organic matter, known as soil organic carbon (SOC) sequestration. Terrestrial ecosystems, comprising of forests, grasslands, croplands, drylands, and peatlands, significantly impact the global C cycle. This chapter presents a comprehensive overview of the factors causing climate change with special reference to the terrestrial ecosystem. Moreover, the impacts of various climate changes (i.e. elevated carbon dioxide (CO2), elevated temperature, altered precipitation) and other extreme climatic events on SOC storage and C sequestrations in the terrestrial ecosystem are described in detail.
Price: £25.00
Publisher: Burleigh Dodds Science Publishing
Imprint: Burleigh Dodds Science Publishing
Series: Burleigh Dodds Series in Agricultural Science
Publication Date:
07 November 2022
ISBN: 9781801467049
Format: eBook
BISACs:
TECHNOLOGY & ENGINEERING / Agriculture / Agronomy / Soil Science, Soil science and management, TECHNOLOGY & ENGINEERING / Agriculture / Agronomy / Crop Science, TECHNOLOGY & ENGINEERING / Agriculture / Sustainable Agriculture, SCIENCE / Global Warming & Climate Change, Sustainable agriculture, Agronomy and crop production, Climate change, Plains and grasslands
1 Introduction 2 Causes of climate change 3 Carbon sequestration and climate change in terrestrial ecosystems 4 Conclusion 5 References