Skip to main content

Major Carbon Reservoirs of the Pedosphere; Source - Sink Relations; Potential of D14C and δ13C as Supporting Methodologies

  • Chapter
Terrestrial Biospheric Carbon Fluxes Quantification of Sinks and Sources of CO2

Abstract

I tried to identify and assess the C reservoirs in the pedo-sphere with C-source-sink-relations whereever it seemed possible and pointing to the poorly known rather enigmatic remainder. A special endeavor focussed on the chances and limitations of applying radio-carbon dating and stable isotope δ13 C measuring techniques.

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 39.99
Price excludes VAT (USA)
  • Available as EPUB and PDF
  • Read on any device
  • Instant download
  • Own it forever
Softcover Book
USD 54.99
Price excludes VAT (USA)
  • Compact, lightweight 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

Preview

Unable to display preview. Download preview PDF.

Unable to display preview. Download preview PDF.

References

  • Aselmann, I., Crutzen, P.J.: 1990, A Global inventory of wetland distribution and seasonality, net primary productivity and estimated methane emissions, in:Soils and the Greenhouse Effect,(Ed. A.F. Bouwman), Wiley, pp. 441–449.

    Google Scholar 

  • Armentano, T.V. (Ed.): 1980, The role of organic soils in the world carbon cycle, CONF.7905135, United States Department of Energy, Washington D.C.

    Google Scholar 

  • Batjes, N.H., Bridges, E.M.:1992, World Inventory of Soil Emissions. ISRIC, WISE Report 1, p.132, Wageningen.

    Google Scholar 

  • Becker-Heidmann, P.:1989, Die Tiefenfunktionen der natürlichen Kohlenstoff Isotopengehalte von dünnschichtweise beprobten Parabraunerden und ihre Relation zur Dynamik der organischen Substanz in diesen Böden.(Dissertation), Hamburger Bodenkundliche Arbeiten,Vol 13,1–228.

    Google Scholar 

  • Becker-Heidmann, P.:1990, Carbon fluxes in important soil classes, with emphasis on lessivé soils and on soil of the terrestrial, of the hydromorphic and temporarily submerged environment. Terminal Report to GTZ (contract 72.7866.6–01.400/1420), pp.1–177.

    Google Scholar 

  • Berner, R.A.: Atmospheric carbon dioxide levels over Phanerozoic time, Science 249, pp. 1382–1386.

    Article  Google Scholar 

  • Budyko, M.J., Ronov, A.B., Yanshin, A.L.:1987, History of the Earth Atmosphere,p.80, Springer,Berlin.

    Book  Google Scholar 

  • Driessen, P.M., Dudal, R.:1989 Lecture notes on the geography, formation, properties and use of the major soils of the world. Agricultural University Wageningen & Katholieke Universiteit Leuven, p.1–296.

    Google Scholar 

  • Esser, G.:1990, Modelling global terrestrial sources and sinks of CO2 with special reference to soil organic matter. In: Soils and the Greenhouse Effect, (Ed. A.F. Bouwman),Wiley,pp.247–263.

    Google Scholar 

  • FAO, World Resources Reports: 1991, Vol.66, Food and Agricultural Organization of the United Nations, Rome, p.10.

    Google Scholar 

  • Graßl, H., Klingholz, R.:1990, Wir Klimamacher, p.70, S.Fischer Publ.Frankfurt.

    Google Scholar 

  • Lovelock, J.E.;1979,1978, Gaia, p.39, Oxford University Press.

    Google Scholar 

  • Lovelock, J.E.: 1988, The Ages of Gaia, p. 84, W.W.Norton & Co,London,N.Y.

    Google Scholar 

  • Lovelock, J.E.: 1991, Healing Gaia, p.23, Harmony Books, N.Y.

    Google Scholar 

  • Houtermans, J., Suess, H.E., Munk, W.:1967,Effect of industrial fuel combustion on the carbon-14 level of atmospheric CO2. In: Radioactive Dating and Methods of Low Level Counting, Vienna, TAEA, pp. 57–68.

    Google Scholar 

  • Martin, A., Mariotti, A., Balesdent, B., Lavelle, P., Vuattoux, R.:1990, Estimate of organic matter turnover rate in a savanna soil by 13C natural abundance measurements. Soil Biol.Biochem. Vol. 22, No.4, pp.517–523.

    Article  Google Scholar 

  • Moore III, B.M.P., Gildea, L.J., Vorosmarty plus five other contributors: 1989, Biogeochemical cycles. In: Global Ecology Towards a Science of the Biosphere (Eds. M.B. Rambler, L. Margulis, R. Fester). Academic Press, Boston, pp.113–141.

    Google Scholar 

  • Roeloffzen, J.E., Mook, W.G., Keeling, C.D.: 1990,Trends and variations in stable carbon isotopes of atmospheric carbon dioxide. Proc. IAEA/FAO Intern. Sympos. on the Use of Stable Isotopes in Plant Nutrition, Soil Fertility and Environmental Studies. IAEA-SM-313, pp.1–24.

    Google Scholar 

  • Scharpenseel, H.W., Schiffmann, H., Hintze, B.: 1984, Hamburg University Radiocarbon Dates III, Radiocarbon. (listed C-14 dates of Chinchilla-, Paget-, Gabbinbar-, Beechmont- Profiles, samples by Dr. Hubble, Australia.

    Google Scholar 

  • Scharpenseel, H.W., Becker-Heidmann, P.: 1992, The dilemma of conflicting interests between CO2’s and CH4’s IR trapping capacity and role, in case of CO2 even as Limiting factor for plant growth. Proceedings of “Global Warming, A Call for International Coordination”, in World Resource Review,Chicago, April 1992.

    Google Scholar 

  • Scharpenseel, H.W., Becker-Heidmann, P.:1993, Carbon storage by grassland soils in different climate zones as revealed by carbon-14 dating. Paper 81+1, Proceedings of International Grassland Congress, February 1993, Palmerston North, N.Z. and Rockhampton, Australia.

    Google Scholar 

  • Schlesinger, W.H.: 1985, The formation of caliche is soils of the Mojave desert, California. Geochim. Cosmochim. Acta,Vol 49, pp 57–66.

    CAS  Google Scholar 

  • Schlesinger, W.H., Melack, J.M.:1981, Transport of organic carbon in the world rivers. Tellus, Vol 33, pp.172–187.

    Article  CAS  Google Scholar 

  • Tamers, M.A., Balke, K.D., Scharpenseel, H.W.: 1968, Untersuchungen zur Fließgeschwindigkeit des Grundwassers durch Bestimmung der Radiokohlenstoff-und Tritiumaktivität. Zeitschr. Kulturtechnik, Flurbereinigung, Vol 9, p.364. (Curve in later years extended).

    CAS  Google Scholar 

  • Whittaker, R.H., Likens, G.E.: 1973, The primary production of the biosphere. Human Ecology Vol 1, pp.299–369.

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Editor information

Editors and Affiliations

Rights and permissions

Reprints and permissions

Copyright information

© 1993 Springer Science+Business Media Dordrecht

About this chapter

Cite this chapter

Scharpenseel, H.W. (1993). Major Carbon Reservoirs of the Pedosphere; Source - Sink Relations; Potential of D14C and δ13C as Supporting Methodologies. In: Wisniewski, J., Sampson, R.N. (eds) Terrestrial Biospheric Carbon Fluxes Quantification of Sinks and Sources of CO2 . Springer, Dordrecht. https://doi.org/10.1007/978-94-011-1982-5_30

Download citation

  • DOI: https://doi.org/10.1007/978-94-011-1982-5_30

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-94-010-4875-0

  • Online ISBN: 978-94-011-1982-5

  • eBook Packages: Springer Book Archive

Publish with us

Policies and ethics