2008 Joint Annual Meeting (5-9 Oct. 2008): X-ray Microspectroscopy Analysis of Phosphorus Speciation in an Acidic Organic Soil.

742-10 X-ray Microspectroscopy Analysis of Phosphorus Speciation in an Acidic Organic Soil.



Wednesday, 8 October 2008: 4:00 PM
George R. Brown Convention Center, 360C
Dean Hesterberg, Soil Science, North Carolina State University, Box 7619, Raleigh, NC 27695-7619, Ian McNulty, Advanced Photon Source, Argonne National Laboratory, 401-B3157, 9700 S. Cass Ave., Argonne, IL 60439 and Kimberly Hutchison, Soil Science, North Carolina State University, Box 7619, Raleigh, NC 27606
Because organic soils are often located near surface water bodies, they have a vital role in protecting water quality. To determine how phosphate mobility is affected by reduction and oxidation processes in poorly-drained organic soils, our goal is to quantify proportions of phosphate bound with redox-active soil Fe(III) vs redox-inactive Al(III). We studied an acid soil (pH 4.8) containing total P, Fe, and Al concentrations of 23, 43, and 380 mmol/kg. Micro-XANES analyses at both the phosphorus and aluminum K-edges were performed on the sample to try to identify Fe(III)-bonded PO4 based on a pre-white-line peak, and PO4 bonded with Al by comparison with mineral standards.  Micro-XANES helps overcome limitations of bulk XANES analysis for soil samples with low P concentrations.  Based on micro-x-ray fluorescence analysis using an ~50 x 50 nm synchrotron x-ray beam; P, Al, and Si were heterogeneously distributed within the sample as expected. Phosphorus K-edge micro-XANES spectra collected at various locations on the sample showed little or no evidence for Fe(III)-bonded PO4. Aluminum K-edge micro-XANES spectra were usually characteristic of Al-hydroxide mineral, likely because of the 16-fold greater concentration of Al vs P.  Detailed and quantitative speciation of soil P remains a challenge, but will be important for determining mechanisms and predicting the extent of reductive P dissolution in a given soil.