Skip to product information
1 of 1

Advances in digital soil mapping to assess baseline levels and carbon sequestration at the landscape scale

Regular price £25.00
Sale price £25.00 Regular price £0.00
Sale Sold out
Mapping soil carbon, both organic and inorganic carbon, is gaining a lot of attention and interest, as it can be a substantial source and sink for climate change mitigation, food security and ecosy...
Read More
  • Format:
  • 07 November 2022
View Product Details
Mapping soil carbon, both organic and inorganic carbon, is gaining a lot of attention and interest, as it can be a substantial source and sink for climate change mitigation, food security and ecosystem services. Digital soil mapping and modeling spatiotemporal variations or changes are helpful tools for understanding, planning, and managing soil carbon and its sequestration and greenhouse gas emission. This review discusses factors influencing soil organic carbon distribution over a range of scales, methods for mapping soil carbon variation with depth, and mapping soil carbon change with space and time. Finally, we discuss the need to map soil carbon contribution to soil functions.
files/i.png Icon
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: 9781801467070
Format: eBook
BISACs:

TECHNOLOGY & ENGINEERING / Agriculture / Agronomy / Soil Science, Soil science and management, TECHNOLOGY & ENGINEERING / Agriculture / Sustainable Agriculture, TECHNOLOGY & ENGINEERING / Agriculture / Agronomy / Crop Science, Agronomy and crop production, Sustainable agriculture

REVIEWS Icon

1 Introduction 2 Digital mapping of soil carbon 3 Soil carbon spatial distribution and influencing factors 4 Field-scale spatial variation of soil organic carbon 5 Soil carbon variation with depth 6 2.5D and 3D mapping 7 Soil carbon change and its mapping 8 Mapping soil functions 9 Uncertainty quantification of soil carbon maps 10 Conclusion 11 Where to look for further information 12 References