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Quantifying Uncertainties in Sequential Chemical Extraction of Soil Phosphorus Using XANES Spectroscopy.
Gu, Chunhao; Dam, Than; Hart, Stephen C; Turner, Benjamin L; Chadwick, Oliver A; Berhe, Asmeret Asefaw; Hu, Yongfeng; Zhu, Mengqiang.
Afiliação
  • Gu C; Department of Ecosystem Science and Management , University of Wyoming , Laramie , Wyoming 82071 , United States.
  • Dam T; Department of Ecosystem Science and Management , University of Wyoming , Laramie , Wyoming 82071 , United States.
  • Hart SC; Department of Life & Environmental Sciences and Sierra Nevada Research Institute , University of California , Merced , California 95343 , United States.
  • Turner BL; Smithsonian Tropical Research Institute , Apartado 0843-03092 Balboa , Ancon , Panama.
  • Chadwick OA; Department of Geography , University of California , Santa Barbara , California 93106 , United States.
  • Berhe AA; Department of Life & Environmental Sciences and Sierra Nevada Research Institute , University of California , Merced , California 95343 , United States.
  • Hu Y; Canadian Light Source , University of Saskatchewan , Saskatoon , Canada S7N 0X4.
  • Zhu M; Department of Ecosystem Science and Management , University of Wyoming , Laramie , Wyoming 82071 , United States.
Environ Sci Technol ; 54(4): 2257-2267, 2020 02 18.
Article em En | MEDLINE | ID: mdl-31922406
Sequential chemical extraction has been widely used to study soil phosphorus (P) dynamics and inform nutrient management, but its efficacy for assigning P into biologically meaningful pools remains unknown. Here, we evaluated the accuracy of the modified Hedley extraction scheme using P K-edge X-ray absorption near-edge structure (XANES) spectroscopy for nine carbonate-free soil samples with diverse chemical and mineralogical properties resulting from different degrees of soil development. For most samples, the extraction markedly overestimated the pool size of calcium-bound P (Ca-P, extracted by 1 M HCl) due to (1) P redistribution during the alkaline extractions (0.5 M NaHCO3 and then 0.1 M NaOH), creating new Ca-P via formation of Ca phosphates between NaOH-desorbed phosphate and exchangeable Ca2+ and/or (2) dissolution of poorly crystalline Fe and Al oxides by 1 M HCl, releasing P occluded by these oxides into solution. The first mechanism may occur in soils rich in well-crystallized minerals and exchangeable Ca2+ regardless of the presence or absence of CaCO3, whereas the second mechanism likely operates in soils rich in poorly crystalline Fe and Al minerals. The overestimation of Ca-P simultaneously caused underestimation of the pools extracted by the alkaline solutions. Our findings identify key edaphic parameters that remarkably influenced the extractions, which will strengthen our understanding of soil P dynamics using this widely accepted procedure.
Assuntos

Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Assunto principal: Solo / Poluentes do Solo Tipo de estudo: Prognostic_studies Idioma: En Ano de publicação: 2020 Tipo de documento: Article

Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Assunto principal: Solo / Poluentes do Solo Tipo de estudo: Prognostic_studies Idioma: En Ano de publicação: 2020 Tipo de documento: Article