Radon flux density at the Earth's surface as a possible indicator of the stress and strain state of the geological environment

V. S. Yakovleva, V. D. Karataev

Результат исследований: Материалы для журналаСтатья

3 Цитирования (Scopus)

Аннотация

Usage of the radon flux density at the Earth's surface as an indicator of seismic activity is proposed in addition to unit-volume radon activity in the soil air that has previously been used for this purpose. Numerical calculations based on the diffusion-convection equation for radon transport in porous media are presented, which confirm that the radon flux density is more sensitive to changes in convection rate than unit-volume radon activity. It has been indicated that the advantage in using radon flux density could be greatest for homogeneous geological media.

Язык оригиналаАнглийский
Страницы (с-по)67-70
Число страниц4
ЖурналJournal of Volcanology and Seismology
Том1
Номер выпуска1
DOI
СостояниеОпубликовано - 1 фев 2007

ASJC Scopus subject areas

  • Geochemistry and Petrology
  • Geology
  • Geophysics

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