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Featured researches published by R.B. Georg.


Scopus | 2007

An inter-laboratory comparison of Si isotope reference materials

Ben C. Reynolds; R.B. Georg; Jugdeep Aggarwal; Luc André; Sophie Opfergelt; Damien Cardinal; Douglas C. Baxter; Emma Engström; Ilia Rodushkin; Charlotte P. Beucher; Mark A. Brzezinski; Magnus Land; Melanie J. Leng; Hilary J. Sloane; Van Den Boorn Shjm; P.Z. Vroon

Three Si isotope materials have been used for an inter-laboratory comparison exercise to ensure reproducibility between international laboratories investigating natural Si isotope variations using a variety of chemical preparation methods and mass spectrometric techniques. These proposed standard reference materials are (i) IRMM-018 (a SiO2 standard), (ii) Big-Batch (a fractionated SiO2 material prepared at the University of California Santa Barbara), and (iii) Diatomite (a natural diatomite sample originally deposited as marine biogenic opal). All analyses are compared with the international Si standard NBS28 (RM8546) and are in reasonable agreement (<+/- 0.22 parts per thousand. 1 sigma(SD) delta Si-30) given the different measurement techniques involved. These methods include both acid and alkaline dissolution/fusion, Si separation using cation exchange, selective co-precipitation, and gas-source versus plasma-ionization (high and low resolution) mass-spectrometric techniques. The average delta Si-30 for Diatomite, IRMM-018, and Big-Batch are + 1.26 parts per thousand, -1.65 parts per thousand and -10.48 parts per thousand, respectively, with corresponding delta Si-9 values of + 0.64 parts per thousand, -0.85 parts per thousand and -5.35 parts per thousand for the same standards, respectively. For the most fractionated standard (Big-Batch), results demonstrate a kinetic mass-dependent fractionation effect for atomic Si (i.e., delta Si-29 similar to 0.51 x delta Si-30). There is almost no statistical difference between the mean values obtained by each participating laboratory, with the notable exception of the IRMM-018 standard. This effect could be caused by heterogeneity or contamination of this standard. The results for the other two standards indicate that data sets produced using any of the methods employed in this study will have similar precision and differences are limited to 0.2 parts per thousand in mean delta Si-30 values for a given sample between laboratories, or differences of 0.13 parts per thousand. in mean delta Si-29 values.


Geochimica et Cosmochimica Acta | 2006

An inter-laboratory calibration of Si isotope reference materials

Ben C. Reynolds; Jugdeep Aggarwal; Brzezinski; Damien Cardinal; Emma Engström; R.B. Georg; Magnus Land; Melanie J. Leng; Sophie Opfergelt; P.Z. Vroon


EOS Trans. AGU, Fall Meet. Suppl. | 2010

Magnesium isotope fractionation in volcanic soils controlled by clay mineralogy and exchangeable Mg

Sophie Opfergelt; R.B. Georg; Kevin W. Burton; Bruno Delvaux; Christopher Siebert; R. Guicharnaud; Y.M Cadiboche; Alex N. Halliday


Mineralogical Magazine | 2011

Seasonal magnesium isotope variations in soil solutions reflecting physico-chemical processes controlling soil weathering fluxes

Sophie Opfergelt; R.B. Georg; Kevin W. Burton; R. Guicharnaud; Christopher Siebert; Sigurður R. Gislason; Alex N. Halliday


AGU Fall Meeting 2016 | 2016

Seasonal freeze-thaw cycles and iron mobilization from peat soils: role of organo-metallic complexes

Sophie Opfergelt; H. M. Williams; Jean-Thomas Cornélis; Rannveig Guicharnaud; R.B. Georg; Chris Siebert; Sigurður R. Gislason; Alexander N. Halliday; Kevin W. Burton


Goldschmidt 2014 | 2014

Impact of the soil weathering degree on the fate of soil organic carbon, Fe and Si: insights from Si and Fe isotopes in Icelandic soils.

Sophie Opfergelt; H. M. Williams; Jean-Thomas Cornélis; Florence Van Hoye; R. Guicharnaud; Bergur Sigfússon; R.B. Georg; Christopher Siebert; Sigurður R. Gislason; Alex N. Halliday; Kevin W. Burton


EnvironMetal Isotopes | 2013

Controls on magnesium fluxes from basalt weathering and the role of plant cycling: evidence from Mg isotopes in Icelandic soils

Sophie Opfergelt; Kevin W. Burton; R.B. Georg; A.J. West; R. Guicharnaud; Bergur Sigfússon; Christopher Siebert; Sigurður R. Gislason; Alex N. Halliday


Young Soil Scientists Day, 2011 | 2011

Magnesium isotopes as a proxy of physico-chemical processes controlling soil weathering fluxes

Sophie Opfergelt; R.B. Georg; Kevin W. Burton; R. Guicharnaud; Christopher Siebert; Sigurður R. Gislason; Alex N. Halliday


Mineralogical Magazine | 2011

Contrasting silicon and magnesium isotope fractionation with clay mineralogy in volcanic soil weathering sequences, Guadeloupe

Sophie Opfergelt; Bruno Delvaux; R.B. Georg; Y.M. Cabidoche; Kevin W. Burton; Alex N. Halliday


Proceedings of the 19th World Congress of Soil Science: Soil solutions for a changing world, Brisbane, Australia, 1-6 August 2010. Symposium 2.2.1 Biogeochemical interfaces in soils | 2010

Tracing impact of pedogenic processes on soil solutions with Si and Mg isotopes

Sophie Opfergelt; R.B. Georg; Kevin W. Burton; R. Guicharnaud; Sigurður R. Gislason; Alex N. Halliday

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Sophie Opfergelt

Université catholique de Louvain

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R. Guicharnaud

Agricultural University of Iceland

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Bruno Delvaux

Université catholique de Louvain

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Damien Cardinal

Royal Museum for Central Africa

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