2010
DOI: 10.1007/978-3-642-15271-9_1
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Soil Organic Phosphorus Speciation Using Spectroscopic Techniques

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Cited by 38 publications
(25 citation statements)
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“…4 and 5). This can be attributed to the greater density of P in the NMR tube at the 1:4 ratio than at the 1:10 ratio (Doolette and Smernik, 2011). Furthermore, the signal resolution (peak width) appears identical for corresponding 1:4 and 1:10 extracts, clearly indicating that the higher paramagnetic metal concentrations in the 1:4 extracts are not causing additional line broadening for these soils (Figs.…”
Section: Solution Phosphorus-31 Nuclear Magnetic Resonance Spectramentioning
confidence: 89%
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“…4 and 5). This can be attributed to the greater density of P in the NMR tube at the 1:4 ratio than at the 1:10 ratio (Doolette and Smernik, 2011). Furthermore, the signal resolution (peak width) appears identical for corresponding 1:4 and 1:10 extracts, clearly indicating that the higher paramagnetic metal concentrations in the 1:4 extracts are not causing additional line broadening for these soils (Figs.…”
Section: Solution Phosphorus-31 Nuclear Magnetic Resonance Spectramentioning
confidence: 89%
“…NMR probes that accommodate 10 mm rather 5 mm diameter tubes) (Preston, 1996); and/or 4) optimising relaxation delays between pulses for maximum sensitivity (Cade-Menun and Liu, 2014). These strategies have been discussed in several reviews (Cade-Menun, 2005;Cade-Menun and Liu, 2014;Cade-Menun and Preston, 1996;Doolette and Smernik, 2011;Preston, 1996) and most studies employ a combination of these strategies in an effort to increase sensitivity.…”
Section: Introductionmentioning
confidence: 98%
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“…Full chemical speciation to identify specific P forms requires either extraction for individual forms (e.g., for phospholipids or RNA) or advanced spectroscopic techniques such as 31 P NMR spectroscopy or x-ray adsorption near-edge structure (XANES) spectroscopy (e.g., Kizewski et al, 2011;Doolette and Smernik, 2011). The XANES spectroscopy (P K-edge or P L 2,3 -edge) has been most successfully used to characterize inorganic P forms and has been used to identify Ca-bound P (e.g., hydroxyapatite and octocalcium phosphate), Fe-bound P (e.g., strengite), and Al-bound P (e.g., variscite) in soil samples (e.g., Kizewski et al, 2011, and references therein).…”
mentioning
confidence: 99%