Abstract
AbstractThis paper reports a review on the relationship between seismic activity and the emissions of CO2 and radon. Direct, indirect and sampling methods are mainly employed to measure CO2 flux and concentration in seismic areas. The accumulation chamber technique is the mostly used in the literature. Radon gas emission in seismic areas can be considered as a short-term pre-seismic precursor. The study and the measurement of radon gas activity prior to earthquakes can be performed through active techniques, with the use of high-precision active monitors and through passive techniques with the use of passive detectors. Several investigators report models to explain the anomalous behavior of in-earth fluid gasses prior to earthquakes. Models are described and discussed.
Funder
Università degli Studi G. D'Annunzio Chieti Pescara
Publisher
Springer Science and Business Media LLC
Subject
Computers in Earth Sciences,Economic Geology,Geology,Environmental Science (miscellaneous),Global and Planetary Change
Cited by
13 articles.
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