Výsledky vyhledávání - "Rancourt, D.G."

Akademický článek

dSED: a database tool for modeling sediment early diagenesis

Autor: Katsev, S., Rancourt, D.G. ^*, L’Heureux, I.

Publikováno v: In Computers and Geosciences 2004 30(9):959-967

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Akademický článek

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Akademický článek

Observation of a composition-controlled high-moment/low-moment transition in the face centered cubic Fe–Ni system: Invar effect is an expansion, not a contraction

Autor: Lagarec, K, Rancourt, D.G ^*, Bose, S.K, Sanyal, B, Dunlap, R.A

Publikováno v: In Journal of Magnetism and Magnetic Materials 2001 236(1):107-130

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A Mössbauer spectroscopic study of the iron redox transition in eastern Mediterranean sediments

Autor: Zee, C. van der, Slomp, C.P., Rancourt, D.G., Lange, G.J. de, Raaphorst, W. van

Publikováno v: Geochimica et Cosmochimica Acta, 69(2), 441. Elsevier

Fe cycling at two sites in the Mediterranean Sea (southwest of Rhodes and in the North Aegean) has been studied, combining the pore water determination of nutrients, manganese, and iron, citrate-bicarbonate-dithionite (CDB) and total sediment extract

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::1654fe9939daa8c68a9075e9ce1884d7
https://dspace.library.uu.nl/handle/1874/31398

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Nanogoethite is the dominant reactive oxyhydroxide phase in lake and marine sediments

Autor: Zee, C. van der, Roberts, D.R., Rancourt, D.G., Slomp, C.P.

Publikováno v: Geology, 31(11), 993. Geological Society of America

Iron oxides affect many elemental cycles in aquatic sediments via numerous redox reactions and their large sorption capacities for phosphate and trace elements. The reactive ferric oxides and oxyhydroxides are usually quantified by operationally defi

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::c85866978b8ddcb63a03be7240d5a202
https://dspace.library.uu.nl/handle/1874/31393

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Control of site populations, at synthesis, by inter-sheet differential thermal expansion in a 2:1 layer silicate

Autor: Mercier, P.H.J., Rancourt, D.G., Berman, R.G., Robert, J.-L.

We have measured octahedral Fe3+ and tetrahedral Fe3+ site populations, in annite samples equilibrated at different temperatures under the C-CH4 buffer at 2 kbar, with sufficient accuracy (0.2-1 %total-Fe) to test a lateral constraint model that incl

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od______1674::1084040997519cdcba77805dd8e776e9
https://nrc-publications.canada.ca/eng/view/object/?id=abea1ff3-9127-4a21-97a6-27182bb4d1a4

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