Abstract

In the Universe, chemical reactions occur at very low temperature, very close to 0K. According to the standard Arrhenius mechanism, these reactions should occur with vanishingly small efficiency. However, cold planets of the solar system, such as Pluto, are covered by a crust composed of ammonia and methane, produced on earth only at very high temperature and pressure, in the presence of catalysts. This observation is incompatible with the predictions of Arrhenius kinetics. Here, we propose a general mechanism to explain the abundance of chemical reactions at very low temperature in the Universe. We postulate that the feedback between mechanical stress and chemical reaction provides, through fracture propagation, the energy necessary to overcome the activation barrier in the absence of thermal fluctuations. The notion described in this work can also be applied to other fields such as explosive-like solid phase transformations and catastrophical geotectonics phenomena (earthquakes).

Highlights

  • In the Universe, chemical reactions occur at very low temperature, very close to 0 K

  • Chemical evolution in solid phase occurs in the Universe, whose temperature is very close to 0 K, at rates much faster than expected based on standard Arrhenius considerations

  • This fact has remained difficult to explain for many years: how to reconcile the abundance of certain chemical species, whose synthesis on earth cannot proceed without very high temperature and pressure conditions, with the classical picture of chemical reactions occurring as a result of thermal fluctuations overcoming an activation barrier?

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Summary

Natural Science

Nonlinear wave mechanisms of very fast chemical and phase transformations in solids. applications to cosmic chemistry processes near to 0 K, to explosive-like decays of metastable solid phases and to catastrophic geotectonic phenomena. Nonlinear wave mechanisms of very fast chemical and phase transformations in solids. Applications to cosmic chemistry processes near to 0 K, to explosive-like decays of metastable solid phases and to catastrophic geotectonic phenomena. Viktor Barelko1*, Dmitryi Kiryukhin, Igor Barkalov, Galina Kichigina, Alain Pumir. Received 28 August 2010; revised 30 September 2010; accepted 3 October 2010

SOLID PHASE STATES
GEOTECTONIC PHENOMENA AND
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