Organic phosphorus fractionation in wetland soil profiles by chemical extraction and phosphorus-31 nuclear magnetic resonance spectroscopy

► Chemical sequential extraction and 31P NMR spectroscopy were used for organic P analysis. ► Organic P includes orthophosphate, monoester and diester phosphate and pyrophosphate. ► Highly resistant organic P and monoester phosphate were the dominant organic P. ► HCl pretreatment can remove most ino...

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Bibliographic Details
Published in:Applied geochemistry 2013-06, Vol.33, p.213-221
Main Authors: Li, Min, Zhang, Jing, Wang, Guangqian, Yang, Haijun, Whelan, Michael J., White, Sue M.
Format: Article
Language:English
Subjects:
acid treatment
chemical analysis
correlation
Earth sciences
Earth, ocean, space
Engineering and environment geology. Geothermics
Exact sciences and technology
fractionation
Geochemistry
hydrochloric acid
nuclear magnetic resonance spectroscopy
organic soils
orthophosphates
phosphorus
plant residues
Pollution, environment geology
soil depth
soil organic matter
soil profiles
wetland plants
wetland soils
wetlands
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Summary:► Chemical sequential extraction and 31P NMR spectroscopy were used for organic P analysis. ► Organic P includes orthophosphate, monoester and diester phosphate and pyrophosphate. ► Highly resistant organic P and monoester phosphate were the dominant organic P. ► HCl pretreatment can remove most inorganic P and increase organic P recovery rate. ► A comprehensive organic P chemical sequential fractionation approach was proposed. Organic P (OP) plays an important role in soil P cycling and is a potential P source for wetland plants. In this study, a modified chemical sequential fractionation method and 31P nuclear magnetic resonance spectroscopy (31P NMR) of NaOH–EDTA extracts were used to examine the distribution of organic P fractions and compounds in soil profiles of the Beijing Yeyahu Wetland, China. The influence of acid treatment prior to NaOH–EDTA extraction on 31P NMR spectra was also investigated. Results show that highly resistant OP was the major class of organic P. The rank order of organic P fractions was highly resistant OP (on average accounting for 68.5% of total OP)>moderately resistant OP (15.8%m of total OP)>moderately labile OP (11.4% of total OP)>labile OP (4.3% of total OP). Most of the organic P fractions decreased with soil depth due to the accumulation of plant residues in surface soils and the deposition and diagenesis of soils. Moderately (r=0.586, p
ISSN:0883-2927
1872-9134
DOI:10.1016/j.apgeochem.2013.02.014