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Alain C.M. Bourg

Researcher at University of Pau and Pays de l'Adour

Publications -  56
Citations -  3340

Alain C.M. Bourg is an academic researcher from University of Pau and Pays de l'Adour. The author has contributed to research in topics: Aquifer & Adsorption. The author has an hindex of 25, co-authored 56 publications receiving 3136 citations. Previous affiliations of Alain C.M. Bourg include University of Limoges & University of Bern.

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Aqueous geochemistry of chromium: A review

TL;DR: In this paper, the authors reviewed the aqueous geochemistry of chromium, especially with reference to the recent work of Rai et al. (report EPRI EA-4544, 1986, Report EPRi EA-5741, 1988), and showed that the chromium content of natural waters is generally low whereas rocks exhibit a wide range of Cr concentrations.
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Speciation of Fe(II) and Fe(III) in Contaminated Aquifer Sediments Using Chemical Extraction Techniques.

TL;DR: The iron mineralogy of aquifer sediments was described by chemical extraction techniques and a rapid indication of the redox status of a sediment sample can be achieved by a 0.5 M HCl extraction.
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Biogeochemical processes during the infiltration of river water into an alluvial aquifer

TL;DR: In this article, the chemical changes in the infiltration flow path from the Lot River to an adjacent aquifer were followed using chloride as an indicator of physical mixing of the river water with groundwater.
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Modeling the acid-base surface chemistry of montmorillonite.

TL;DR: This study finds that montmorillonite edge surface chemistry models that account for the "spillover" of electrostatic potential from basal onto edge surfaces and for the stabilization of deprotonated Al-Si bridging sites through bond-length relaxation at the edge surface can reproduce key features of the best available experimental titration data.
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Tracer diffusion in compacted, water-saturated bentonite

TL;DR: In this article, the pore space of water-saturated bentonite is divided into macropore and interlayer nanopore compartments, and the relative contributions of pore-network geometry and diffusive behavior of water molecules near montmorillonite basal surfaces are determined quantitatively.