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20242026
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physics.geo-ph2026

Poroelastic aquifer response drives seasonal vertical land motion in southern Louisiana

Pritom Sarma, Eduardo Arzabala, Carolina Hurtado-Pulido +4

Coastal Louisiana is sinking, amplifying flooding and land loss, yet the seasonal component of this motion remains difficult to attribute. Satellite geodetic records from Baton Rou…

physics.geo-ph2026

How effective normal stress oscillations advance failure in fault gouge: frequency dependence, non-failure window, and the role of dilation

Pritom Sarma, Einat Aharonov, Renaud Toussaint +1

Cyclic pore-pressure or normal stress variations arise both in relation to natural earthquakes and in engineered subsurface systems, yet their effect on fault stability remains poo…

physics.geo-ph2026

Injection-rate effects on failure in a fluid-saturated granular fault gouge

Pritom Sarma, Stanislav Parez, Renaud Toussaint +1

Fluid injection into the Earth's subsurface, performed for energy extraction, waste disposal, and resource development, is known to reactivate gouge-filled faults and induce seismi…

physics.geo-ph2025

Unveiling the role of seepage forces in the acceleration of landslides creep

Fabian Barras, Andreas Aspaas, Einat Aharonov +1

In the context of global climate change, geological materials are increasingly destabilized by water flow and infiltration. We study the creeping dynamics of a densely monitored la…

physics.geo-ph2024

Fault gouge failure induced by fluid injection: Hysteresis, delay and shear-strengthening

Pritom Sarma, Einat Aharonov, Renaud Toussaint +1

Natural faults often contain a fluid-saturated, granular fault-gouge layer, whose failure and sliding processes play a central role in earthquake dynamics. Using a two-dimensional…