2012
DOI: 10.4236/ijg.2012.31015
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Test of Strain Behavior Model with Radon Anomaly in Seismogenic Area: A Bayesian Melding Approach

Abstract: Mathematical models in seismo-geochemical monitoring offer powerful tools for the study and exploration of complex dynamics associated with discharge of radon as the indicator of change of intense-deformed conditions of seismogenic layers or blocks within the lithosphere. Seismic precursory model of radon gas emanation in the process of earthquake prediction research aims to find out the distinct anomaly variation necessary to correlate radon gas with processes of preparation and realization of tectonic earthq… Show more

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Cited by 9 publications
(6 citation statements)
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References 25 publications
(21 reference statements)
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“…The DD model describes earthquake nucleation as being caused by strain cracking (dilation), and then fluid motion (diffusion) into the new pore space. The DD model does account for some results, for example, increased radon gas emission (Dutta et al, 2012) and an increase in seismic wave velocity immediately prior to rock failure. It also accounts for the positive correlation between variance in high frequency seismic noise and diurnal ground temperature, as described in Gordeev et al (1992) since variation in surface heating causes diurnal fluctuations in groundwater pressure.…”
Section: Streaming-potential Mechanismmentioning
confidence: 99%
“…The DD model describes earthquake nucleation as being caused by strain cracking (dilation), and then fluid motion (diffusion) into the new pore space. The DD model does account for some results, for example, increased radon gas emission (Dutta et al, 2012) and an increase in seismic wave velocity immediately prior to rock failure. It also accounts for the positive correlation between variance in high frequency seismic noise and diurnal ground temperature, as described in Gordeev et al (1992) since variation in surface heating causes diurnal fluctuations in groundwater pressure.…”
Section: Streaming-potential Mechanismmentioning
confidence: 99%
“…It describes earthquake nucleation as a process of strain cracking (dilation), and then fluid motion (diffusion) into the new pore space. The dilatancy-diffusion model does perhaps account for some results, for example, increased radon gas emission (Dutta et al, 2012) and an increase in seismic wave velocity immediately prior to rock failure. It also accounts for the positive correlation between variance in high frequency seismic noise and diurnal ground temperature, as described in Gordeev et al (1992), since surface heating causes diurnal fluctuations in groundwater pressure.…”
Section: Data Relating To the Mechanisms Of Ses Generationmentioning
confidence: 99%
“…which A i j denote the size of j -covered area after i sensor nodes have been placed in j Y i denote the extra area to the sensor region of i th placed sensor node to the size of j -covered region, P i j is the proportion of Y i j to A i . According to (5) and 6…”
Section: Figure5 Sensing Range Identification Based On Inner and Outmentioning
confidence: 99%