Suitability of calibrated X-ray fluorescence core scanning for environmental geochemical characterisation of heterogeneous sediment cores

Tatiana Goldberg, Rick Hennekam, Laura Wasch, Gert-Jan Reichart, Oliver Rach, Jessica A. Stammeier, Jasper Griffioen

Research output: Contribution to journalArticleAcademicpeer-review

Abstract

Multi-element analysis of discrete samples via X-Ray fluorescence or inductively coupled plasma spectrometry is commonly used to characterise the composition of solid geo-materials for environmental geochemical characterisation. Conventional geochemical analysis of individual samples is time consuming and costly, which often results in low-resolution sampling with the danger of missing crucial information. X-ray fluorescence Core Scanning (XCS) provides an alternative method to obtain elemental information, which can be potentially used quantitatively when combined with the Multivariate Log-ratio Calibration (MLC) approach. The suitability of the XCS-MLC method was tested for environmental geochemical characterisation on four terrestrial Holocene-Pleistocene sediment cores that have a variable lithology (clay, sand, peat, with variable calcareous content), were stored at ambient room conditions and scanned post sampling. Element contents based on XCS-MLC and conventional geochemical analysis proved to be comparable (R2 > 0.5) for Al, Ca, Cr, Fe, K, Sr, Mn, Ni, Pb, Rb, S, Si, Ti, Zn, Zr, and also for Br as proxy for organic matter. For As, Cu and Ba the correlations were less satisfactory (R2 
Original languageEnglish
Article number104824
Pages (from-to)1-13
Number of pages13
JournalApplied Geochemistry
Volume125
DOIs
Publication statusPublished - Feb 2021

Bibliographical note

Funding Information:
This research project was performed within the framework of the legal task assigned by the government to TNO to collect, to process and to make available geo-scientific data as well as information of the Dutch subsurface (funded by Ministry of the Interior and Kingdom Relations, PN 060.43296 ). This work at NIOZ was supported by the SCANALOGUE-project (ALWOP. 2015.113 ) by the Netherlands Organization for Scientific Research (NWO) , The Netherlands. This research was also partially funded by the NESSC Gravitation Grant (024.002.001) from the Dutch Ministry of Education , Culture and Science (OCW). R.H. would like to thank Rineke Gielens and Piet van Gaever for their help during the XRF-core-scan analyses. The authors thank three anonymous reviewers for their useful suggestions to improve the manuscript.

Funding Information:
This research project was performed within the framework of the legal task assigned by the government to TNO to collect, to process and to make available geo-scientific data as well as information of the Dutch subsurface (funded by Ministry of the Interior and Kingdom Relations, PN 060.43296). This work at NIOZ was supported by the SCANALOGUE-project (ALWOP.2015.113) by the Netherlands Organization for Scientific Research (NWO), The Netherlands. This research was also partially funded by the NESSC Gravitation Grant (024.002.001) from the Dutch Ministry of Education, Culture and Science (OCW). R.H. would like to thank Rineke Gielens and Piet van Gaever for their help during the XRF-core-scan analyses. The authors thank three anonymous reviewers for their useful suggestions to improve the manuscript.

Publisher Copyright:
© 2020 Elsevier Ltd

Keywords

  • Core scan
  • Diagenesis
  • Element contents
  • Geochemistry
  • Mineralogy
  • Multivariate log-ratio calibration

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