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CO2 Leakage Scenarios in Shale Overburden
This is an early access version, the complete PDF, HTML, and XML versions will be available soon. Open AccessArticle by Gilda Currenti 1,*, Barbara Cantucci 1, Giordano Montegrossi 2,3, Rosalba Napoli 1, M. Shahir Misnan 4, M.
Multidisciplinary Study of Mud Emissions Following the 2016 Norcia Earthquake
1. Introduction On 24 August 2016, an earthquake (Mw = 6.2) hit central Italy; its epicenter was close to the village of Accumoli, affecting a very large area, involving four Italian regions: Lazio, Abruzzo, Marche, and Umbria. The earthquake was the first of a strong seismic sequence (Mw max = 6.5), the Amatrice–Norcia–Visso sequence [1,2,3,4,5,6,7].
CO2 Reaction-Diffusion Experiments in Shales and Carbonates
2.3. Experimental Settings The diffusion experiments allow to define the velocity of reactive reaction front in a rock by placing a solution with high concentration of CO2 in contact with an intact rock for a certain period of time; in this study, for 2–5 days.
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