Skip to main content

Carbon Cycling and Formation of Soil Organic Matter

  • Reference work entry
  • First Online:
Encyclopedia of Soil Science

Carbon (C) can form potentially endless hybridized atomic orbitals resulting in the potential to create a vast array of complex organic compounds. The diversity of C compounds no doubt influenced the evolution of life and the diversity of organisms. Carbon was not found on the primordial earth and only after the continuous bombardment by carbonaceous comets and asteroids did appreciable amounts of C accumulate (Anders, 1989). The extraterrestrial C was complex containing a vast array of hydrocarbons and important biological compounds such as amino acids and carboxylic acids, constituents required to assemble primitive life. Early Earth's atmosphere was thought to contain primarily simple hydrocarbons that were continuously altered through ultraviolet photolysis. In addition, the atmosphere contained appreciable amounts of carbon dioxide (CO 2) as a result of meteor and asteroid impacts and volcanic activity. The CO 2dissolved in water to form carbonic acid and may have been...

This is a preview of subscription content, log in via an institution to check access.

Access this chapter

Chapter
USD 29.95
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
eBook
USD 499.99
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
Hardcover Book
USD 599.99
Price excludes VAT (USA)
  • Durable hardcover edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info

Tax calculation will be finalised at checkout

Purchases are for personal use only

Institutional subscriptions

Bibliography

  • Aiken, G.R., 1985. Isolation and concentration techniques for aquatic humic substance. In: Aiken, G.R., McKnight, D.M., Wershaw R.L., and McCarthy, P., eds., Humic Substances in the Soil, sediment and water. New York: Wiley, pp. 363–385.

    Google Scholar 

  • Anders, E., 1989. Prebiotic organic matter from comets and asteroids. Nature, 342: 255–257.

    Article  CAS  Google Scholar 

  • Haider, K., 1992. Problems related to the humification processin soils of temperate climates. In Stotsky G., and Bollag, J.‐M., eds., Soil Biochemistry, Vol.7. New York., Marcel Dekker, pp. 55–94.

    Google Scholar 

  • Horwath, W.R., 2002. Soil Microbial Biomass. In: Encyclopedia of Environmental Microbiology. New York: Academic Press, pp. 663–670.

    Google Scholar 

  • Houghton, J.T., Ding, Y., Griggs, D.J., Noguer, M., van der Linden, P.J., Dai, X., Maskell, K., and Johnson, C.A., (eds.), 2001. Climate Change 2001: The Scientific Basis. New York: Cambridge University Press.Intergovernmental Panel on Climate Change,

    Google Scholar 

  • Kraus, T.E.C., Dahlgren, R.A., and Zasoski, R.J., 2003. Tannins in nutrient dynamics of forest ecosystems – a review. Plant Soil 25: 41–66.

    Article  Google Scholar 

  • Paul, E.A., and Clark, F.E., 1996. Soil microbiology and biochemistry, 2nd edn. New York: Wiley.

    Google Scholar 

  • Piccolo, A., 1996. Humic Substances in Terrestrial Environments. New York: Elsevier.

    Google Scholar 

  • Raich, J.W., and Scheslinger, W.H., 1992. The global carbon dioxide in soil respirationand its relationship to vegetation and climate. Tellus, 44B: 81–99.

    Article  CAS  Google Scholar 

  • Stevenson, F.J., 1994. Humus Chemistry: Genesis, Composition, Reactions. New York: Wiley.

    Google Scholar 

Download references

Authors

Editor information

Editors and Affiliations

Rights and permissions

Reprints and permissions

Copyright information

© 2008 Springer

About this entry

Cite this entry

Chesworth, W. et al. (2008). Carbon Cycling and Formation of Soil Organic Matter. In: Chesworth, W. (eds) Encyclopedia of Soil Science. Encyclopedia of Earth Sciences Series. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-3995-9_88

Download citation

Publish with us

Policies and ethics