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The Organic P Composition of Vertisols as Determined by 31 P NMR Spectroscopy
Author(s) -
McLaren Timothy I.,
Smernik Ronald J.,
Guppy Christopher N.,
Bell Mike J.,
Tighe Matthew K.
Publication year - 2014
Publication title -
soil science society of america journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.836
H-Index - 168
eISSN - 1435-0661
pISSN - 0361-5995
DOI - 10.2136/sssaj2014.04.0139
Subject(s) - vertisol , chemistry , sodium hydroxide , nuclear magnetic resonance spectroscopy , topsoil , extraction (chemistry) , hydroxide , subsoil , organic matter , ethylenediaminetetraacetic acid , nuclear chemistry , soil water , inorganic chemistry , organic chemistry , geology , soil science , chelation
Solution 31 P nuclear magnetic resonance (NMR) spectroscopy on sodium hydroxide–ethylenediaminetetraacetic acid (NaOH–EDTA) extracts can provide detailed characterization of soil organic P, but has not been previously applied widely to Vertisols. Vertisol soils were collected at two depths (0–10 cm and 10–30 cm) for chemical and spectroscopic analysis. Sodium hydroxide–EDTA extracted a relatively consistent proportion (17 to 37%; average 25%) of the total organic P content determined by the ignition–H 2 SO 4 extraction technique. Orthophosphate monoesters were the dominant form of organic P detected by solution 31 P NMR spectroscopy of the NaOH–EDTA extracts, the majority of which appeared to be present in large ‘humic’ molecules, based on the predominance of a broad peak in the NMR spectra; some smaller signals due to glycerophosphate, inositol phosphates, and RNA‐derived mononucleotides were also evident. The composition of organic P in the topsoil layer was very similar to that in the subsoil layer. Strong correlations were found between soil organic carbon (C) and nitrogen (N) and extractable organic P, which suggests that processes regulating the cycling of organic C and N are closely related to that for organic P in these Vertisols.