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by S. Jordan, S. Velty and J. Zeitz
This article is dedicated to the memory of our very good
friend and colleague,
Dr Silke Velty, 07 April 1973 – 14 October 2007.
Published online: 14.10.2007
Summary
Re-wetting of drained fens can release phosphorus, introducing a
eutrophication risk for associated aquatic
ecosystems. Characterisation of the different forms of organic and
inorganic bound phosphorus in the peat is
an important step towards the development of tools for assessing the
level of risk attached to individual rewetting
projects. In the work reported here, a sequential extraction
(fractionation) method was used to
distinguish the following P binding forms:
1. labile P, detected by NH4Cl extraction;
2. redox-sensitive P, detected by Na2S2O4/NaHCO3
extraction;
3. P adsorbed to metal oxides, detected by HCl extraction;
4. P bound to humic substances, detected by NaOH extraction; and
5. organic and refractory bound P, detected using H2SO4
and H2O2.
Special attention was paid to the degree of decomposition (DPD) of the
peat, and metal concentrations were
measured in selected fractions. Higher P concentrations were found in
completely humified than in little
humified peat for all fractions except the NH4Cl
(labile P) fraction, where P content increased as DPD
decreased. As only 1% of total phosphorus (TP) was present as labile P,
the results indicate that the decisive
horizons for nutrient release after re-wetting are those that are
completely humified due to pedogenetic
changes. The principal metal sorption partner for P was Fe.
Jordan, S., Velty, S. & Zeitz, J. (2007): The influence of degree of peat decomposition on phosphorus binding forms in fens. Mires and Peat 2: Art. 7. (Online: http://www.mires-and-peat.net/map02/map_02_07.htm)
IMCG and IPS acknowledge the work of the reviewers.
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| Key title: Mires and Peat | ISSN 1819-754X | Abbreviated key title: Mires Peat |