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Published online 7 May 2007
Published in J Environ Qual 36:892-898 (2007)
DOI: 10.2134/jeq2006.0235
© 2007 American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Right arrow Phosphorus
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Sediment Phosphorus Extractants for Phosphorus-31 Nuclear Magnetic Resonance Analysis

A Quantitative Evaluation

Joakim Ahlgrena, Heidi De Brabanderea, Kasper Reitzelb, Emil Rydind, Adolf Gogollc and Monica Waldebäcka,*

a Dep. of Physical and Analytical Chemistry, Analytical Chemistry, Uppsala Univ., Box 599, 751 24 Uppsala, Sweden
b Inst. of Biology, Univ. of Southern Denmark, Campusvej 55, DK-5230 Odense M, Denmark
c Dep. of Biochemistry and Organic Chemistry, Organic Chemistry, Uppsala Univ., Box 599, 751 24 Uppsala, Sweden
d Dep. of Ecology and Evolution, Limnology, Uppsala Univ., Box 573, 751 23 Uppsala, Sweden


Figure 1
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Fig. 1. Typical spectra from the various extractants of the 0- to 2-cm layer of Lake Erken sediments.

 

Figure 2
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Fig. 2. Interaction plot, with standard deviations, of the main extractants and their dependence on pre-extraction procedures (from the top to the bottom, EDTA, BD, and none) for the total extracted amount of P. BD, bicarbonate buffered dithionite.

 

Figure 3
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Fig. 3. Principal components analysis (PCA) of the individual organic P groups extracted by the various extractants. In the PCA, the triplicate pre-extraction procedures are labeled: A = None, B = BD, C = EDTA, and the triplicates of the main extraction procedures: 1 = NaOH, 2 = NaOH-EDTA. The scoreplot (to the left) indicates how the main extractants vary from each other, and the loading plot (to the right) indicates on which organic P compounds this depends. BD, bicarbonate buffered dithionite.

 





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