Experimental Study of Pyrite Oxidation at 100 °C: Implications for Deep Geological Radwaste Repository in Claystone

Experimental Study of Pyrite Oxidation at 100 °C: Implications for Deep Geological Radwaste Repository in Claystone

The oxidation of pyrite is one of the near field processes of the chemical evolution of clay rock planned to host a deep geological radioactive waste repository during operation. Indeed, this process can lead to transitory acidic conditions in the medium (i.e., production of sulphuric acid, carbonic...

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Bibliographic Details
Main Authors: Héloïse Verron, Jérôme Sterpenich, Julien Bonnet, Franck Bourdelle, Régine Mosser-Ruck, Catherine Lorgeoux, Aurélien Randi, Nicolas Michau
Format: Article
Language:English
Published: MDPI AG 2019-07-01
Series:Minerals
Subjects:
pyrite
oxidation
claystone
gas analysis
radwaste geological repository
Online Access:https://www.mdpi.com/2075-163X/9/7/427

Internet

https://www.mdpi.com/2075-163X/9/7/427

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