L'alteration naturelle des scories de la metallurgie ancienne : un analogue de déchets vitrifiés
C. Le Carlier Mahe and Christian Le Carlier de Veslud and A. Ploquin and Jean-Jacques Royer. ( 2000 )
in: Comptes Rendus de l'Academie des Sciences de Paris, 330 (179--184)
Abstract
The study of the natural alteration of ancient vitreous slags (100 to 4 000 years) suggests a single global mechanism. In a first stage, weathering consists of a selective extraction of the modifier cations of glass (including Pb and Ba). This phenomenon is associated with an increase of the solution pH, inducing the glass dissolution. The elements with a weak limit of solubility remain in place and can form hydroxides (Al, Fe). Pb and Ba are extracted from weathered glass. Pb is located in Fe-hydroxides, Ba may form sulfides. The rate of alteration varies from 20 to 180 μm per 1 000 years.
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@ARTICLE{, author = { Le Carlier Mahe, C. and Le Carlier de Veslud, Christian and Ploquin, A. and Royer, Jean-Jacques }, title = { L'alteration naturelle des scories de la metallurgie ancienne : un analogue de déchets vitrifiés }, journal = { Comptes Rendus de l'Academie des Sciences de Paris }, volume = { 330 }, chapter = { 0 }, year = { 2000 }, pages = { 179--184 }, abstract = { The study of the natural alteration of ancient vitreous slags (100 to 4 000 years) suggests a single global mechanism. In a first stage, weathering consists of a selective extraction of the modifier cations of glass (including Pb and Ba). This phenomenon is associated with an increase of the solution pH, inducing the glass dissolution. The elements with a weak limit of solubility remain in place and can form hydroxides (Al, Fe). Pb and Ba are extracted from weathered glass. Pb is located in Fe-hydroxides, Ba may form sulfides. The rate of alteration varies from 20 to 180 μm per 1 000 years. } }