Titlebook: Water Circulation in Rocks; Laura Scesi,Paola Gattinoni Book 2010 Springer Science+Business Media B.V. 2010 Fractures.Hydrogeological risk

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Case Histories,orthern Italy; Fig. 6.1). Here groundwater flow was analyzed in order to find possible correlations with the slope mass movements of this area, situated at the border of the large and deep gravitational deformation affecting Berceto.

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Book 2010ing engineering. This book offers a synthesis of the actual knowledge about the fluid flow in rocks:..- from the medium characterization and the structural geological survey to the generation of stereonets;..- the evaluation of the hydrogeological parameters using either deterministic or probabilist

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Methods and Models to Simulate the Groundwater Flow in Rock Masses, to its application. Actually, that approach is quite difficult due to the need to recreate a complex system such as that of the rock mass, where the availability of data in depth is often almost scarce, in particular if quite large areas are taken into consideration.

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Methods and Models to Simulate the Groundwater Flow in Rock Masses, to its application. Actually, that approach is quite difficult due to the need to recreate a complex system such as that of the rock mass, where the availability of data in depth is often almost scarce, in particular if quite large areas are taken into consideration.

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Influence of Joint Features on Rock Mass Hydraulic Conductivity,the frequency and persistence of joints. Those features are extremely variable in space due to the heterogeneity of the rock mass system. The definition of those relations apt to describe the variability of the parameters involved, both in a deterministic way and through a statistical approach, is therefore very important.

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