Denis Rancourt
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Environmental Science
2016-05-22 ::: Anatomy of the false link between forest fires and anthropogenic CO2
2021-07-16 ::: REPORT ::: Glyphosate should be banned, not increased
2011 ::: Iron solid-phase differentiation along a redox gradient in basaltic soils
2009 ::: Mineralogical confirmation of a near-P:Fe = 1:2 limiting stoichiometric ratio in colloidal P-bearing ferrihydrite-like hydrous ferric oxide
2009 ::: General model for the aqueous precipitation of rough-surface nanocrystals and application to ferrihydrite genesis
2008 ::: Constraints on structural models of ferrihydrite as a nanocrystalline material
2007 ::: Reversible surface-sorption-induced electron-transfer oxidation of Fe(II) at reactive sites on a synthetic clay mineral
2006 ::: The role of smelter emissions and element remobilization in the sediment chemistry of 99 lakes around the Horne smelter, Québec
2006 ::: Iron-oxide crystallinity increases during soil redox oscillations
2006 ::: Factors controlling long-term phosphorus efflux from lake sediments: Exploratory reactive-transport modeling
2005 ::: Hydrous ferric oxide precipitation in the presence of nonmetabolizing bacteria: Constraints on the mechanism of a biotic effect
2005 ::: Absolute quantification by powder X-ray diffraction of complex mixtures of crystalline and amorphous phases for applications in the Earth sciences
2005 ::: A Mössbauer spectroscopic study of the iron redox transition in eastern Mediterranean sediments
2004 ::: dSED: a database tool for modeling sediment early diagenesis
2003 ::: Nanogoethite is the dominant reactive oxyhydroxide phase in lake and marine sediments
2001 ::: Mineralogy of a natural As-rich hydrous ferric oxide coprecipitate formed by mixing of hydrothermal fluid and seawater: Implications regarding surface complexation and color banding in ferrihydrite deposits
2001 ::: Magnetism of Earth, Planetary, and Environmental Nanomaterials
1999 ::: Mineralogical analysis of a loess/paleosol couplet from the Chinese loess plateau
1985 ::: The discrimination of pyroclastic deposits on the basis of the Mössbauer spectra of their magnetites: a preliminary test