nerc.ac.uk

Significance of phosphorus inclusions and discrete micron‐sized grains of apatite in postglacial forest soils

Adediran, Gbotemi A. ORCID: https://orcid.org/0000-0001-6657-3336; Kielman‐Schmitt, Melanie; Kooijman, Ellen; Gustafsson, Jon‐Petter. 2022 Significance of phosphorus inclusions and discrete micron‐sized grains of apatite in postglacial forest soils. European Journal of Soil Science, 73 (5), e13310. 14, pp. https://doi.org/10.1111/ejss.13310

Before downloading, please read NORA policies.
[img]
Preview
Text
N533386JA.pdf - Published Version
Available under License Creative Commons Attribution 4.0.

Download (3MB) | Preview

Abstract/Summary

Recent advances in soil phosphorus (P) studies have revealed unique P hot spots and discrete micron-sized grains at soil microsites, but the significance of these so-called ‘hot spots’ and grains in P cycling and long-term supply is yet to be determined. We examined soil particles and pore space distribution at a micro-scale in two postglacial forest soils by laser ablation ICP-MS imaging. This allowed us to semi-quantitatively reveal both axial and lateral abundance, distribution, and co-localization of P with elements known to influence its chemical speciation (e.g., Si, Al, Mn, Ca, and Fe). The results show topsoil P to be co-localised predominantly with Si, Al, and Fe. However, in the subsoils, P was co-localised mainly with Ca, Si, Al, and Mg in spots within Si and Al-bearing minerals and with only Ca in discrete micron-sized grains. While the spots of P-Ca inclusions were ~ 1000 μm apart and present at 40–100 cm depth in Tärnsjö, the discrete grains of P-Ca were ~ 700–1200 μm apart and present at 90–100 cm depth in Tönnersjöheden. The P concentrations in these ‘hot spots’ and grains were 7 to 600 times greater than the average soil P concentrations, with the highest values (3434–8716 mmol P kg−1) occurring in the C horizons of the two soils. When combined with previous P speciation results obtained by synchrotron P K-edge XANES in the same soils, our work confirms geogenic apatite to have been dissolved in the topsoil and its P transformed to P adsorbed by Al-Si and Fe phases, and to organic P. Most importantly, our work shows subsoil spots of P-Ca inclusions and micron-sized grains to be a long-term source of P and Ca.

Item Type: Publication - Article
Digital Object Identifier (DOI): https://doi.org/10.1111/ejss.13310
UKCEH and CEH Sections/Science Areas: Pollution (Science Area 2017-)
ISSN: 1351-0754
Additional Information. Not used in RCUK Gateway to Research.: Open Access paper - full text available via Official URL link.
Additional Keywords: apatite inclusions, chemical speciation, discrete particles, elemental co-localizations, LAICP-MS imaging, phosphorus cycling
NORA Subject Terms: Agriculture and Soil Science
Date made live: 20 Oct 2022 09:30 +0 (UTC)
URI: https://nora.nerc.ac.uk/id/eprint/533386

Actions (login required)

View Item View Item

Document Downloads

Downloads for past 30 days

Downloads per month over past year

More statistics for this item...