Thermodynamically consistent model for poroelastic rocks towards tectonic and volcanic processes and earthquakes

0548828 - ÚT 2022 RIV GB eng J - Článek v odborném periodiku
Roubíček, Tomáš
Thermodynamically consistent model for poroelastic rocks towards tectonic and volcanic processes and earthquakes.
Geophysical Journal International. Roč. 227, č. 3 (2021), s. 1893-1904. ISSN 0956-540X. E-ISSN 1365-246X
Grant CEP: GA ČR(CZ) GA19-04956S; GA MŠMT(CZ) EF15_003/0000493
Institucionální podpora: RVO:61388998
Klíčová slova: fracture and flow * plasticity, diffusion, and creep * geomechanics * non-linear differential equations * dynamics of lithosphere and mantle * magma genesis and partial melting
Obor OECD: Thermodynamics
Impakt faktor: 3.352, rok: 2021
Způsob publikování: Omezený přístup
https://academic.oup.com/gji/article/227/3/1893/6346570

A general-purpose model combining concepts from rational continuum mechanics, fracture and damage mechanics, plasticity and poromechanics is devised in Eulerian coordinates, involving objective time derivatives. The model complies with mass, momentum and energy conservation as well as entropy inequality and objectivity. It is devised to cover many diverse phenomena, specifically rupture of existing lithospheric faults, tectonic earthquakes, generation and propagation of seismic waves, birth of new tectonic faults, or volcanic activity, aseismic creep, folding of rocks, aging of rocks, long-distance saturated water transport and flow in poroelastic rocks, melting of rocks and formation of magma chambers, or solidification of magma.
Trvalý link: http://hdl.handle.net/11104/0327480