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A rapid ammonium fluoride method to determine the oxygen isotope ratio of available phosphorus in tropical soils.
Pfahler, Verena; Bielnicka, Aleksandra; Smith, Andrew C; Granger, Steven J; Blackwell, Martin S A; Turner, Benjamin L.
Afiliación
  • Pfahler V; Sustainable Agriculture Sciences, Rothamsted Research, North Wyke, Okehampton, EX20 2SB, UK.
  • Bielnicka A; Smithsonian Tropical Research Institute, Apartado 0843-03092, Balboa, Ancon, Republic of Panama.
  • Smith AC; Smithsonian Tropical Research Institute, Apartado 0843-03092, Balboa, Ancon, Republic of Panama.
  • Granger SJ; NERC Isotope Geoscience Laboratory, British Geological Survey, Nottingham, NG12 5GG, UK.
  • Blackwell MSA; Sustainable Agriculture Sciences, Rothamsted Research, North Wyke, Okehampton, EX20 2SB, UK.
  • Turner BL; Sustainable Agriculture Sciences, Rothamsted Research, North Wyke, Okehampton, EX20 2SB, UK.
Rapid Commun Mass Spectrom ; 34(7): e8647, 2020 Apr 15.
Article en En | MEDLINE | ID: mdl-31671472
RATIONALE: The isotopic composition of oxygen bound to phosphorus (δ18 OP value) offers an opportunity to gain insight into P cycling mechanisms. However, there is little information for tropical forest soils, which presents a challenge for δ18 OP measurements due to low available P concentrations. Here we report the use of a rapid ammonium fluoride extraction method (Bray-1) as an alternative to the widely used anion-exchange membrane (AEM) method for quantification of δ18 OP values of available P in tropical forest soils. METHODS: We compared P concentrations and δ18 OP values of available and microbial P determined by AEM and Bray-1 extraction for a series of tropical forest soils from Panama spanning a steep P gradient. This involved an assessment of the influence of extraction conditions, including temperature, extraction time, fumigation time and solution-to-soil ratio, on P concentrations and isotope ratios. RESULTS: Depending on the extraction conditions, Bray-1 P concentrations ranged from 0.2 to 66.3 mg P kg-1 across the soils. Extraction time and temperature had only minor effects on Bray-1 P, but concentrations increased markedly as the solution-to-soil ratio increased. In contrast, extraction conditions did not affect Bray-1 δ18 OP values, indicating that Bray-1 provides a robust measure of the isotopic composition of available soil P. For a relatively high P soil, available and fumigation-released (microbial) δ18 OP values determined by Bray-1 extraction (20‰ and 16‰, respectively) were higher than those determined by the AEM method (18‰ and 12‰, respectively), which we attribute to slightly different P pools extracted by the two methods and/or differences resulting from the longer extraction time needed for the AEM method. CONCLUSIONS: The short extraction time, insensitivity to extraction conditions and smaller mass of soil required to extract sufficient P for isotopic analysis make Bray-1extraction a suitable alternative to the AEM method for the determination of δ18 OP values of available P in tropical soils.
Asunto(s)

Texto completo: 1 Banco de datos: MEDLINE Asunto principal: Isótopos de Oxígeno / Fósforo / Suelo / Compuestos de Amonio / Fluoruros Idioma: En Revista: Rapid Commun Mass Spectrom Año: 2020 Tipo del documento: Article

Texto completo: 1 Banco de datos: MEDLINE Asunto principal: Isótopos de Oxígeno / Fósforo / Suelo / Compuestos de Amonio / Fluoruros Idioma: En Revista: Rapid Commun Mass Spectrom Año: 2020 Tipo del documento: Article