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by M. Klavins, J. Sire, O. Purmalis and V. Melecis
Published online: 04.10.2008
Summary
Degree of decomposition is an important property of the organic matter
in soils and other deposits which contain fossil carbon. It describes
the intensity of transformation, or the humification degree (HD), of the
original living organic matter. In this article, approaches to the
determination of HD
are thoroughly described and 14C
dated peat columns extracted from several bogs in Latvia are
investigated and compared. A new humification indicator is suggested,
namely the quantity of humic substances as a fraction of the total
amount of organic matter in the peat.
Klavins, M., Sire, J., Purmalis, O. & Melecis, V. (2008): Approaches to estimating humification indicators for peat. Mires and Peat 3: Art. 7. (Online: http://www.mires-and-peat.net/map03/map_03_07.htm)
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| Last update: 23.12.2008 | ![]() |
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| Key title: Mires and Peat | ISSN 1819-754X | Abbreviated key title: Mires Peat |