Articles | Volume 15, issue 1
https://doi.org/10.5194/se-15-23-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.Modeling liquid transport in the Earth's mantle as two-phase flow: effect of an enforced positive porosity on liquid flow and mass conservation
Related authors
Cited articles
Arbogast, T., Hesse, M. A., and Taicher, A. L.: Mixed Methods for Two-Phase Darcy–Stokes Mixtures of Partially Melted Materials with Regions of Zero Porosity, SIAM J. Sci. Comput., 39, B375–B402, https://doi.org/10.1137/16m1091095, 2017.
Bercovici, D. and Karato, S.-i.: Whole-mantle convection and the transition-zone water filter, Nature, 425, 39–44, https://doi.org/10.1038/nature01918, 2003.
Bie, L., Hicks, S., Rietbrock, A., Goes, S., Collier, J., Rychert, C., Harmon, N., and Maunder, B.: Imaging slab-transported fluids and their deep dehydration from seismic velocity tomography in the Lesser Antilles subduction zone, Earth Planet. Sci. Lett., 586, 117535, https://doi.org/10.1016/j.epsl.2022.117535, 2022.
Butler, S. L.: Shear-induced porosity bands in a compacting porous medium with damage rheology, Phys. Earth Planet. In., 264, 7–17, https://doi.org/10.1016/j.pepi.2016.12.006, 2017.
Cerpa, N. G., Rees Jones, D. W., and Katz, R. F.: Consequences of glacial cycles for magmatism and carbon transport at mid-ocean ridges, Earth Planet. Sci. Lett., 528, 115845, https://doi.org/10.1016/j.epsl.2019.115845, 2019.