Articles | Volume 6, issue 4
Solid Earth, 6, 1207–1229, 2015
https://doi.org/10.5194/se-6-1207-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Solid Earth, 6, 1207–1229, 2015
https://doi.org/10.5194/se-6-1207-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article 10 Nov 2015
Research article | 10 Nov 2015
Poroelastic responses of confined aquifers to subsurface strain and their use for volcano monitoring
K. Strehlow et al.
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Cited
11 citations as recorded by crossref.
- Electrokinetic Contributions to Self‐Potential Signals From Magmatic Stressing F. Arens et al. 10.1029/2020GC009388
- The influence of long- and short-term volcanic strain on aquifer pressure: a case study from Soufrière Hills Volcano, Montserrat (W.I.) K. Strehlow et al. 10.1093/gji/ggaa354
- Microgravity changes at the Laguna del Maule volcanic field: Magma-induced stress changes facilitate mass addition C. Miller et al. 10.1002/2017JB014048
- A splitting-based finite element method for the Biot poroelasticity system N. Chaabane & B. Rivière 10.1016/j.camwa.2017.12.009
- Combining Multiphase Groundwater Flow and Slope Stability Models to Assess Stratovolcano Flank Collapse in the Cascade Range J. Ball et al. 10.1002/2017JB015156
- Improving fluid flow in geothermal reservoirs by thermal and mechanical stimulation: The case of Krafla volcano, Iceland G. Eggertsson et al. 10.1016/j.jvolgeores.2018.04.008
- A high-order HDG method for the Biot’s consolidation model G. Fu 10.1016/j.camwa.2018.09.029
- Locking-Free Finite Element Methods for Poroelasticity R. Oyarzúa & R. Ruiz-Baier 10.1137/15M1050082
- A Sequential Discontinuous Galerkin Method for the Coupling of Flow and Geomechanics N. Chaabane & B. Rivière 10.1007/s10915-017-0443-6
- The Role of Pore Fluid Pressure on the Failure of Magma Reservoirs: Insights From Indonesian and Aleutian Arc Volcanoes F. Albino et al. 10.1002/2017JB014523
- Pore pressure embrittlement in a volcanic edifice J. Farquharson et al. 10.1007/s00445-015-0997-9
10 citations as recorded by crossref.
- Electrokinetic Contributions to Self‐Potential Signals From Magmatic Stressing F. Arens et al. 10.1029/2020GC009388
- The influence of long- and short-term volcanic strain on aquifer pressure: a case study from Soufrière Hills Volcano, Montserrat (W.I.) K. Strehlow et al. 10.1093/gji/ggaa354
- Microgravity changes at the Laguna del Maule volcanic field: Magma-induced stress changes facilitate mass addition C. Miller et al. 10.1002/2017JB014048
- A splitting-based finite element method for the Biot poroelasticity system N. Chaabane & B. Rivière 10.1016/j.camwa.2017.12.009
- Combining Multiphase Groundwater Flow and Slope Stability Models to Assess Stratovolcano Flank Collapse in the Cascade Range J. Ball et al. 10.1002/2017JB015156
- Improving fluid flow in geothermal reservoirs by thermal and mechanical stimulation: The case of Krafla volcano, Iceland G. Eggertsson et al. 10.1016/j.jvolgeores.2018.04.008
- A high-order HDG method for the Biot’s consolidation model G. Fu 10.1016/j.camwa.2018.09.029
- Locking-Free Finite Element Methods for Poroelasticity R. Oyarzúa & R. Ruiz-Baier 10.1137/15M1050082
- A Sequential Discontinuous Galerkin Method for the Coupling of Flow and Geomechanics N. Chaabane & B. Rivière 10.1007/s10915-017-0443-6
- The Role of Pore Fluid Pressure on the Failure of Magma Reservoirs: Insights From Indonesian and Aleutian Arc Volcanoes F. Albino et al. 10.1002/2017JB014523
1 citations as recorded by crossref.
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Latest update: 08 Dec 2021
Short summary
When magma chambers inflate, they deform the surrounding Earth’s crust. This deformation affects the pore space available for the water in local aquifers, which in turn leads to pressure variations and water table changes. We can observe these changes in wells, and this study investigates if and how we can utilize them for volcano monitoring. Results show that the hydrological response to deformation helps unravelling subsurface magmatic processes, valuable information for eruption forecasting.
When magma chambers inflate, they deform the surrounding Earth’s crust. This deformation...
