BaukeSperberSiebersEtAl2017

Référence

Bauke, S.L., von Sperber, C., Siebers, N., Tamburini, F., Amelung, W. (2017) Biopore effects on phosphorus biogeochemistry in subsoils. Soil Biology and Biochemistry, 111:157-165. (Scopus )

Résumé

Biopores are characterised by high concentrations of plant available nutrients and provide preferential pathways for root growth into the subsoil, thereby potentially enabling plants to access phosphorus (P) resources located in the subsoil. Here, we sampled biopores from a replicated agricultural field trial in Klein-Altendorf, Germany, to analyse their nutrient composition and P speciation as determined by Hedley sequential extraction and X-ray absorption near edge structure (XANES) spectroscopy. In addition, we analysed the oxygen isotopic composition of HCl P (δ18OHCl P) as an indicator of long-term effects of biological P turnover. We found that biopore effects were most pronounced in the subsoil, where the concentration of easily extractable (labile) P tended to be greater in biopores than in bulk soil, as evident in both Hedley sequential extraction and XANES spectroscopy. We assume that these findings result from inputs of organic matter from the topsoil as well as an input of Ca-particles into subsoil biopores by earthworm activity. Biologically cycled P was subsequently precipitated as Ca-P as evident by δ18OHCl P values close to equilibrium in biopores even at great depths. When incubating bulk soil samples with 18O-labelled water, however, we observed a significant increase of δ18OHCl P values in the topsoil, but only small if any changes of δ18OHCl P values in the subsoil. Thus, biopores present hotspots of P cycling in the subsoil, but the effect of biopores on overall P turnover in the bulk subsoil is limited. © 2017 Elsevier Ltd

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@ARTICLE { BaukeSperberSiebersEtAl2017,
    AUTHOR = { Bauke, S.L. and von Sperber, C. and Siebers, N. and Tamburini, F. and Amelung, W. },
    TITLE = { Biopore effects on phosphorus biogeochemistry in subsoils },
    JOURNAL = { Soil Biology and Biochemistry },
    YEAR = { 2017 },
    VOLUME = { 111 },
    PAGES = { 157-165 },
    NOTE = { cited By 7 },
    ABSTRACT = { Biopores are characterised by high concentrations of plant available nutrients and provide preferential pathways for root growth into the subsoil, thereby potentially enabling plants to access phosphorus (P) resources located in the subsoil. Here, we sampled biopores from a replicated agricultural field trial in Klein-Altendorf, Germany, to analyse their nutrient composition and P speciation as determined by Hedley sequential extraction and X-ray absorption near edge structure (XANES) spectroscopy. In addition, we analysed the oxygen isotopic composition of HCl P (δ18OHCl P) as an indicator of long-term effects of biological P turnover. We found that biopore effects were most pronounced in the subsoil, where the concentration of easily extractable (labile) P tended to be greater in biopores than in bulk soil, as evident in both Hedley sequential extraction and XANES spectroscopy. We assume that these findings result from inputs of organic matter from the topsoil as well as an input of Ca-particles into subsoil biopores by earthworm activity. Biologically cycled P was subsequently precipitated as Ca-P as evident by δ18OHCl P values close to equilibrium in biopores even at great depths. When incubating bulk soil samples with 18O-labelled water, however, we observed a significant increase of δ18OHCl P values in the topsoil, but only small if any changes of δ18OHCl P values in the subsoil. Thus, biopores present hotspots of P cycling in the subsoil, but the effect of biopores on overall P turnover in the bulk subsoil is limited. © 2017 Elsevier Ltd },
    AFFILIATION = { Institute for Crop Science and Resource Conservation (INRES) – Soil Science and Soil Ecology, University of Bonn, Nussallee 13, Bonn, 53115, Germany; Institute for Bio- and Geosciences – IBG-3: Agrosphere, Forschungszentrum Jülich GmbH, Jülich, 52425, Germany; Institute of Agricultural Sciences, ETH Zürich, Lindau, 8315, Switzerland },
    AUTHOR_KEYWORDS = { Biopores; Oxygen isotopes; Phosphate; Subsoil; XANES },
    DOCUMENT_TYPE = { Article },
    DOI = { 10.1016/j.soilbio.2017.04.012 },
    SOURCE = { Scopus },
    URL = { https://www.scopus.com/inward/record.uri?eid=2-s2.0-85018662270&doi=10.1016%2fj.soilbio.2017.04.012&partnerID=40&md5=14a2bdbdffab5616f5b61efa69f4418b },
}

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