Sediment phosphorus extractants for phosphorus-31 nuclear magnetic resonance analysis: a quantitative evaluation.

The influence of pre-extractant, extractant, and post-extractant on total extracted amounts of P and organic P compound groups measured with 31P nuclear magnetic resonance (31P-NMR) in lacustrine sediment was examined. The main extractants investigated were sodium hydroxide (NaOH) and sodium hydroxide ethylenediaminetetraacetic acid (NaOH-EDTA) with bicarbonate buffered dithionite (BD) or EDTA as pre-extractants. Post extractions were conducted using either NaOH or NaOH-EDTA, depending on the main extractant. Results showed that the most efficient combination of extractants for total P yield was NaOH with EDTA as pre-extractant, yielding almost 50% more than the second best procedure. The P compound groups varying the most between the different extraction procedures were polyphosphates and pyrophosphates. NaOH with BD as pre-extractant was the most efficient combination for these compound groups.

[1]  W. Zech,et al.  Nature of soil organic phosphorus: an assessment of peak assignments in the diester region of 31P NMR spectra , 2002 .

[2]  Benjamin L. Turner,et al.  Phosphorus-31 nuclear magnetic resonance spectral assignments of phosphorus compounds in soil NaOH–EDTA extracts , 2003 .

[3]  J. Moir,et al.  Basic Edta as an Extractant for Soil Organic Phosphorus , 1993 .

[4]  B. Cade-Menun,et al.  Soil and litter phosphorus-31 nuclear magnetic resonance spectroscopy: extractants, metals, and phosphorus relaxation times. , 2002, Journal of environmental quality.

[5]  Benjamin L Turner,et al.  Abiotic stabilization of organic phosphorus in the environment. , 2005 .

[6]  E. Rydin,et al.  Effects of aluminum treatment on phosphorus, carbon, and nitrogen distribution in lake sediment: a 31P NMR study. , 2006, Water research.

[7]  Michael Hupfer,et al.  Polyphosphate in lake sediments: 31P NMR spectroscopy as a tool for its identification , 1995 .

[8]  V. Farmer,et al.  Confirmation of the surface structures of goethite (α-FeOOH) and phosphated goethite by infrared spectroscopy , 1976 .

[9]  L. Tranvik,et al.  Degradation of organic phosphorus compounds in anoxic Baltic Sea sediments: A 31P nuclear magnetic resonance study , 2006 .

[10]  Joanne N. Halls A Spatial Sensitivity Analysis of Land Use Characteristics and Phosphorus Levels in Small Tidal Creek Estuaries of North Carolina, USA , 2002, Journal of Coastal Research.

[11]  K. Markides,et al.  Sediment depth attenuation of biogenic phosphorus compounds measured by 31P NMR. , 2005, Environmental science & technology.

[12]  Richard W. McDowell,et al.  An improved technique for the determination of organic phosphorus in sediments and soils by 31P nuclear magnetic resonance spectroscopy , 2005 .

[13]  R. Carman,et al.  Distribution of organic and inorganic phosphorus compounds in mrine and lacustrine sediments: a31NMR study , 2000 .

[14]  G. Anderson,et al.  THE ADSORPTION OF INOSITOL PHOSPHATES AND GLYCEROPHOSPHATE BY SOIL CLAYS, CLAY MINERALS, AND HYDRATED SESQUIOXIDES IN ACID MEDIA , 1962 .

[15]  R. Newman,et al.  Influence of conifers on the forms of phosphorus in selected New Zealand grassland soils , 1996, Biology and Fertility of Soils.

[16]  B. Cade-Menun,et al.  A comparison of soil extraction procedures for 31P NMR spectroscopy , 1996 .

[17]  A. Paytan,et al.  Selective phosphorus regeneration of sinking marine particles: evidence from 31P-NMR , 2003 .

[18]  D. Powlson,et al.  A 31P nuclear magnetic resonance study of the phosphorus species in alkali extracts of soils from long‐term field experiments , 1984 .

[19]  Michael A. Wilson,et al.  Structural analysis of geochemical samples by solid-state nuclear magnetic resonance spectrometry. Role of paramagnetic material , 1987 .

[20]  R. Newman,et al.  Linkages between phosphorus transformations and carbon decomposition in a forest soil , 1996 .

[21]  W. Amelung,et al.  Climatic effects on soil organic phosphorus in the North American Great Plains identified by phosphorus-31 nuclear magnetic resonance , 1998 .

[22]  R. H. Newman,et al.  Soil phosphorus characterisation by 31p nuclear magnetic resonance , 1980 .

[23]  J. Emsley,et al.  THE ANALYSIS OF SOIL PHOSPHORUS BY ICP AND 31P NMR SPECTROSCOPY , 1983 .

[24]  R. Danielsson,et al.  Biogenic phosphorus in oligotrophic mountain lake sediments: differences in composition measured with NMR spectroscopy. , 2006, Water research.

[25]  Kasper Reitzel,et al.  Degradation rates of organic phosphorus in lake sediment , 2007 .

[26]  E. Rydin Potentially mobile phosphorus in Lake Erken sediment , 2000 .

[27]  G. Sposito,et al.  On the mechanism of specific phosphate adsorption by hydroxylated mineral surfaces: A review , 1985 .

[28]  Susan Newman,et al.  Extraction of soil organic phosphorus. , 2005, Talanta.

[29]  J. Lewandowski,et al.  Retention and early diagenetic transformation of phosphorus in Lake arendsee (Germany) : consequences for management strategies , 2005 .

[30]  P. Schroeder,et al.  The nature of organic phosphorus in marine sediments: New insights from 31P NMR , 1990 .

[31]  P. Schmieder,et al.  Origin and diagenesis of polyphosphate in lake sediments: A 31PߚNMR study , 2004 .

[32]  Clifford H. Mortimer,et al.  THE EXCHANGE OF DISSOLVED SUBSTANCES BETWEEN MUD AND WATER IN LAKES, II , 1941 .

[33]  M. Adams,et al.  31P-NMR analysis of phosphorus compounds in extracts of surface soils from selected karri (Eucalyptus diversicolor F. Muell.) forests , 1989 .

[34]  P. V. Sundareshwar,et al.  Occurrence and ecological implications of pyrophosphate in estuaries , 2001 .

[35]  F. Marsan,et al.  Interaction Of Inositol Hexaphosphate On Clays: Adsorption And Charging Phenomena , 1999 .