Journal
SOIL BIOLOGY & BIOCHEMISTRY
Volume 111, Issue -, Pages 157-165Publisher
PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.soilbio.2017.04.012
Keywords
Biopores; Oxygen isotopes; Phosphate; Subsoil; XANES
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Funding
- Natural Sciences and Engineering Research Council of Canada
- National Research Council Canada
- Canadian Institutes of Health Research
- Province of Saskatchewan, Western Economic Diversification Canada
- University of Saskatchewan
- German Research Foundation (Deutsche Forschungsgemeinschaft, DFG) within the research consortium DFG [DFG AM 134/21-1]
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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 (delta O-18(HCl 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 delta O-18(HCl) (P) values close to equilibrium in biopores even at great depths. When incubating bulk soil samples with O-18-labelled water, however, we observed a significant increase of delta O-18(HCl) (P) values in the topsoil, but only small if any changes of delta O-18(HCl) (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. (C) 2017 Elsevier Ltd. All rights reserved.
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