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Boreskov Institute of Catalysis of the Siberian Branch of Russian ...

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PP-III-38orders <strong>of</strong> magnitude larger than predicted by classical Arrhenius factors. This energytransformation is a result <strong>of</strong> self-sustained brittle disruption (fracture in form <strong>of</strong> dispersedsolid substance) <strong>of</strong> solid matrix and this phenomenon may be named «autowave self-sustainedtribo-chemical mechanism».The first simple <strong>the</strong>oretical model <strong>of</strong> autowave processes in solid-phase cryochemicalreactions was proposed in [1,2]. The model considered was constructed on <strong>the</strong> physicalscheme that brittle fracture is induced by <strong>the</strong>rmal strain from reaction heat generation. The<strong>the</strong>ory is being developed by <strong>the</strong> work [3] which are investigating different bifurcationphenomena concerning <strong>of</strong> critical conditions with parameters <strong>of</strong> heat-transfer, sample sizes,and also with thresholds <strong>of</strong> «cold» ignition <strong>of</strong> autowave transformation in frozen reagents bylocal disruption etc.We suppose <strong>the</strong> autowave hypo<strong>the</strong>sis may give an ideological base <strong>of</strong> fast cryochemicalevolution <strong>of</strong> <strong>the</strong> cosmic substances. In particular, one can imagine <strong>the</strong> formation, from <strong>the</strong>frozen mixture <strong>of</strong> elements, <strong>of</strong> compounds such as ammonia and methane that are found inappreciable amounts in crusts <strong>of</strong> <strong>the</strong> cold planets <strong>of</strong> <strong>the</strong> Solar system.APPLICATION: autowaves <strong>of</strong> fracture <strong>of</strong> metastable phase states in solids as a newapproach for explanation <strong>of</strong> mechanisms <strong>of</strong> geotectonics phenomena and earthquakes.By using above presented mechanism <strong>of</strong> solid phase chemical transformations we formeda nonlinear <strong>the</strong>oretical model for describing <strong>of</strong> mechanisms <strong>of</strong> initiating and dynamics <strong>of</strong>moving in time and space <strong>of</strong> geotectonic phenomena and earthquakes. A base <strong>of</strong> <strong>the</strong> model is<strong>the</strong> «gasless detonation» in fracture <strong>of</strong> solids, supersonic wave <strong>the</strong>ory created in [4,5] forexplanation <strong>of</strong> catastrophically fast decays <strong>of</strong> metastable phase states in solid matter. Theuntraditional fracture notions was developed for different solid transformations in physics <strong>of</strong>semiconductors, in physics <strong>of</strong> explosives sensibility to friction and shock. Possibility <strong>of</strong>application <strong>of</strong> <strong>the</strong> <strong>the</strong>ory to geophysical processes is based on a hypo<strong>the</strong>sis that geotectonicphenomena and earthquakes are a result <strong>of</strong> catastrophic phase transitions in rocks <strong>of</strong> EarthCrust. Classical <strong>the</strong>ory <strong>of</strong> polymorphism describes a lot <strong>of</strong> metastable phases in earth rocksbut never investigated dynamics <strong>of</strong> <strong>the</strong> transitions between <strong>the</strong>m. A bifurcation approach tomodeling <strong>of</strong> <strong>the</strong> geological phenomena is proposed in <strong>the</strong> present work.The phenomenon is modeled by coupling <strong>the</strong> reaction diffusion equation, describingchemical or phase transformations, and <strong>the</strong> wave equation, describing elastic perturbations.The feedback coupling considered in this work involves (i) a dependence <strong>of</strong> <strong>the</strong> soundvelocity on <strong>the</strong> phase (chemical) field, and (ii) <strong>the</strong> destruction (fracture) <strong>of</strong> initial phaseequilibrium when <strong>the</strong> strain exceeds a critical value: such critical strain destroys <strong>the</strong> matrix376

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