Titlebook: Hydrogeological and Environmental Investigations in Karst Systems; Bartolomé Andreo,Francisco Carrasco,James W. LaMor Textbook 2015 Spring

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Middle Term Evolution of Water Chemistry in a Karst River: Example from the Loue River (Jura Mountaarstification processes in the Jurassic limestones of the Jura Mountains. Indeed, no direct anthropogenic cause may be invoked for such an evolution. An increase of dissolution throughout the system is necessarily correlated to an increase in the carbon dioxide transfer, resulting from an increase in dissolution and/or production rate.

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Comparative Study of the Physicochemical Response of Two Karst Systems During Contrasting Flood Evere characterized by localized and diffuse recharge. Physicochemical monitoring was performed at the karst outlet (springs), as well as in the unsaturated zone (cave and epikarstic spring). During two contrasting flood events, water level, temperature, electrical conductivity, dissolved organic carbo

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進(jìn)取心

Contribution of Hydrogeological Time Series Statistical Analysis to the Study of Karst Unsaturated s study, we use rainfall-discharge cross-correlation analysis to improving the understanding of the hydrodynamic functioning of the karst unsaturated zone. This analysis is based on sparse discharge measurements from five flow points located within the artificial LSBB gallery. Our results are consis

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