316-7 Combined XANES and Nanosims Analysis to Assess Spatial Patterns of Soil P Speciation from the Nano- to the Pedon Scale.

See more from this Division: SSSA Division: Soil Chemistry
See more from this Session: Advanced Molecular Techniques Characterizing Soil Biogeochemical Processes: I (includes student competition)
Tuesday, November 4, 2014: 3:20 PM
Long Beach Convention Center, Room 104C
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Florian Werner, Technische Universitaet Muenchen, Freising, (Non U.S.), GERMANY, Carsten Mueller, Technische Universitaet Muenchen, Freising, Germany and Joerg Prietzel, Technical University of Munich, Peiting, GERMANY
In recent years, it has become apparent that soil micro- and nano-structures highly determine the availability and allocation of phosphorus (P) in soils. Thus beside traditional wet-chemical methods, novel techniques that allow for the identification and quantification of P in different binding forms are needed to assess the importance of biogeochemical processes such as P transformation and storage in soils. Advanced techniques such as nano-scale Secondary Ion Mass Spectrometry (NanoSIMS) and synchrotron-based X-ray absorption near edge structure (XANES) spectroscopy enable us to examine P in various intact soil structures from the nano- up to the pedon scale.

By comparison with reference compounds it is possible to unveil P speciation, a crucial parameter for P availability in soils, using XANES spectroscopy. Correla­ting the small scale spatial P distribution with the distribution of other elements like Fe, Al, Si or C obtained from NanoSIMS data enables also assumptions about the P speciation. Combination of both methods will allow an even more detailed in­sight into the distribution of P species at different spatial scales in soils.

We present data on the spatial distribution of different P forms in soils and soil aggregates from different forest sites in Germany which represent a gradient in P supply, from the nano- to the pedon scale. Results from cluster- and correlation analysis of NanoSIMS data, as well as results of linear combination fitting performed on XANES spectroscopy data are combined to determine P binding patterns in the investigated soils. Moreover, we discuss the capabilities and limitations of the used methods and the scale-dependency of the observed P distribution patterns.

See more from this Division: SSSA Division: Soil Chemistry
See more from this Session: Advanced Molecular Techniques Characterizing Soil Biogeochemical Processes: I (includes student competition)