TamburiniPfahlerVonSperberEtAl2014

Référence

Tamburini, F., Pfahler, V., von Sperber, C., Frossard, E., Bernasconi, S.M. (2014) Oxygen isotopes for unraveling phosphorus transformations in the soil-plant system: A review. Soil Science Society of America Journal, 78(1):38-46. (Scopus )

Résumé

Phosphorus is a major nutrient for all living organisms. In the terrestrial environment, P is considered a double-edged sword. In some areas, agricultural production is strongly limited by the low soil P availability, while in others, P inputs in excess of plant needs have resulted in pollution of water bodies. A better understanding of soil-plant P cycling is needed to provide agricultural and environmental managers with better concepts for P use. Together with the routine analysis of soil available P, the determination of P chemical forms, and the use of P radioisotopes, researchers have recently started using the ratio of stable oxygen isotopes in phosphate (d18O-P). The scientific community interested in using this isotopic tracer is slowly but steadily expanding because δ18O-P has proven to provide important information on biological processes influencing the P cycle and it could be used to trace the origin and fate of P in soil-plant systems. This review examines the published results and compiles the available data relevant for soil-plant systems, pinpoints gaps in analytical techniques and knowledge, and suggests key questions and topics to be investigated. © Soil Science Society of America.

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@ARTICLE { TamburiniPfahlerVonSperberEtAl2014,
    AUTHOR = { Tamburini, F. and Pfahler, V. and von Sperber, C. and Frossard, E. and Bernasconi, S.M. },
    TITLE = { Oxygen isotopes for unraveling phosphorus transformations in the soil-plant system: A review },
    JOURNAL = { Soil Science Society of America Journal },
    YEAR = { 2014 },
    VOLUME = { 78 },
    NUMBER = { 1 },
    PAGES = { 38-46 },
    NOTE = { cited By 42 },
    ABSTRACT = { Phosphorus is a major nutrient for all living organisms. In the terrestrial environment, P is considered a double-edged sword. In some areas, agricultural production is strongly limited by the low soil P availability, while in others, P inputs in excess of plant needs have resulted in pollution of water bodies. A better understanding of soil-plant P cycling is needed to provide agricultural and environmental managers with better concepts for P use. Together with the routine analysis of soil available P, the determination of P chemical forms, and the use of P radioisotopes, researchers have recently started using the ratio of stable oxygen isotopes in phosphate (d18O-P). The scientific community interested in using this isotopic tracer is slowly but steadily expanding because δ18O-P has proven to provide important information on biological processes influencing the P cycle and it could be used to trace the origin and fate of P in soil-plant systems. This review examines the published results and compiles the available data relevant for soil-plant systems, pinpoints gaps in analytical techniques and knowledge, and suggests key questions and topics to be investigated. © Soil Science Society of America. },
    AFFILIATION = { Institute of Agricultural Sciences, ETH Zurich, Research Station Eschikon 33, 8315 Lindau, Switzerland; Geological Institute, ETH Zurich, Sonneggstrasse 5, 8092 Zurich, Switzerland },
    DOCUMENT_TYPE = { Conference Paper },
    DOI = { 10.2136/sssaj2013.05.0186dgs },
    SOURCE = { Scopus },
    URL = { https://www.scopus.com/inward/record.uri?eid=2-s2.0-84893254107&doi=10.2136%2fsssaj2013.05.0186dgs&partnerID=40&md5=922bf709e18bb9b3eed88e851cf9f1ff },
}

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