The episodic movement of deep-seated landslides is often governed by the presence of
high pore pressures and reduced effective stresses along active shear surfaces. Pore …

Hydraulic stimulation of deep reservoirs is an essential procedure for developing
engineered/enhanced geothermal systems (EGS), but also in other Geo-energy contexts …

Six hydraulic fracturing (HF) experiments were conducted in situ at the Grimsel Test Site
(GTS), Switzerland, using two boreholes drilled in sparsely fractured crystalline rock. High …

Subglacial water pressures influence groundwater conditions in proximal alpine valley rock
slopes, varying with glacier advance and retreat in parallel with changing ice thickness …

The episodic movement of deep-seated rockslides is often associated with seasonal
variations in precipitation and groundwater recharge. Acceleration and deceleration phases …

Porosity waves correspond to a steady‐state solution to the coupled hydraulic and rheologic
equations that govern the flow of the fluid through the matrix and matrix deformation. This …

The ability to generate deep flow in massive crystalline rocks is governed by the
interconnectivity of the fracture network and its permeability, which in turn is largely …

In this work, we propose a hydro-mechanical simulation model to study the strong interaction
of fluid flow and fracture deformation under in situ stress conditions. The general model is …

Interception of aquifers by tunnel excavation results in water inflow and leads to drawdown
of the water table which may induce ground settlement. In this work, analytical and …

Underground flow processes in fractured porous media possess a great significance
regarding the optimization of energy production based on natural resources. Energy is …