Radon content of groundwater as an earthquake precursor: Evaluation of worldwide data and physical basis

The properties of a worldwide data set of 91 radon (^(222)Rn) anomalies (the frequency of occurrence, the precursor time interval, and the distribution of peak amplitudes) are correlated with earthquake data such as the respective magnitude and epicentral distance. These anomalies were reported as p...

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Published in:Journal of Geophysical Research: Solid Earth
Main Author: Hauksson, Egill
Format: Article in Journal/Newspaper
Language:unknown
Published: American Geophysical Union 1981
Subjects:
Online Access:https://doi.org/10.1029/JB086iB10p09397
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spelling ftcaltechauth:oai:authors.library.caltech.edu:nmxt7-wsz14 2024-10-13T14:08:33+00:00 Radon content of groundwater as an earthquake precursor: Evaluation of worldwide data and physical basis Hauksson, Egill 1981-10 https://doi.org/10.1029/JB086iB10p09397 unknown American Geophysical Union https://doi.org/10.1029/JB086iB10p09397 eprintid:38331 info:eu-repo/semantics/openAccess Other Journal of Geophysical Research B, 86(B10), 9397-9410, (1981-10) info:eu-repo/semantics/article 1981 ftcaltechauth https://doi.org/10.1029/JB086iB10p09397 2024-09-25T18:46:46Z The properties of a worldwide data set of 91 radon (^(222)Rn) anomalies (the frequency of occurrence, the precursor time interval, and the distribution of peak amplitudes) are correlated with earthquake data such as the respective magnitude and epicentral distance. These anomalies were reported as precursors to earthquakes in the United States, USSR, China, Japan, and Iceland. Although the data set is incomplete and limited by experimental deficiencies, several consistent patterns emerge. Radon anomalies from different tectonic regions show similar patterns. The radon anomalies occur at greater epicentral distances for earthquakes of the larger magnitude. Anomalies preceding large earthquakes (M ≥ 6) are frequently observed at a distance of 100 to 500 km. These distances are larger than several times the rupture dimensions of the future earthquakes. The time from the onset of an anomaly to the time of the earthquake (the precursor time) increases with magnitude but decreases with distance between epicenter and radon station. In addition, radon anomalies are observed more frequently prior to large earthquakes than prior to small ones, indicating that the preparation zone increases in size as magnitude increases. The peak amplitude does not scale with magnitude but forms a consistent pattern with epicentral distance in that the larger the earthquake magnitude, the farther away the largest amplitudes tend to occur. The preparation zone of the earthquake where the anomalies occur forms an almost continuous annulus that expands with time away from the future rupture zone. The outer radius of this annulus scales with the earthquake magnitude. Model calculations indicate that strain fields of at most 10^(−6) to 10^(−8) strain caused the radon anomalies. If these strains are divided by the appropriate precursor time, minimum strain rates from 10^(−7) day^(−1) to 10^(−10) day^(−1) are obtained. Such small strains and strain rates suggest that in most cases neither mechanical crack growth induced by ... Article in Journal/Newspaper Iceland Caltech Authors (California Institute of Technology) Journal of Geophysical Research: Solid Earth 86 B10 9397 9410
institution Open Polar
collection Caltech Authors (California Institute of Technology)
op_collection_id ftcaltechauth
language unknown
description The properties of a worldwide data set of 91 radon (^(222)Rn) anomalies (the frequency of occurrence, the precursor time interval, and the distribution of peak amplitudes) are correlated with earthquake data such as the respective magnitude and epicentral distance. These anomalies were reported as precursors to earthquakes in the United States, USSR, China, Japan, and Iceland. Although the data set is incomplete and limited by experimental deficiencies, several consistent patterns emerge. Radon anomalies from different tectonic regions show similar patterns. The radon anomalies occur at greater epicentral distances for earthquakes of the larger magnitude. Anomalies preceding large earthquakes (M ≥ 6) are frequently observed at a distance of 100 to 500 km. These distances are larger than several times the rupture dimensions of the future earthquakes. The time from the onset of an anomaly to the time of the earthquake (the precursor time) increases with magnitude but decreases with distance between epicenter and radon station. In addition, radon anomalies are observed more frequently prior to large earthquakes than prior to small ones, indicating that the preparation zone increases in size as magnitude increases. The peak amplitude does not scale with magnitude but forms a consistent pattern with epicentral distance in that the larger the earthquake magnitude, the farther away the largest amplitudes tend to occur. The preparation zone of the earthquake where the anomalies occur forms an almost continuous annulus that expands with time away from the future rupture zone. The outer radius of this annulus scales with the earthquake magnitude. Model calculations indicate that strain fields of at most 10^(−6) to 10^(−8) strain caused the radon anomalies. If these strains are divided by the appropriate precursor time, minimum strain rates from 10^(−7) day^(−1) to 10^(−10) day^(−1) are obtained. Such small strains and strain rates suggest that in most cases neither mechanical crack growth induced by ...
format Article in Journal/Newspaper
author Hauksson, Egill
spellingShingle Hauksson, Egill
Radon content of groundwater as an earthquake precursor: Evaluation of worldwide data and physical basis
author_facet Hauksson, Egill
author_sort Hauksson, Egill
title Radon content of groundwater as an earthquake precursor: Evaluation of worldwide data and physical basis
title_short Radon content of groundwater as an earthquake precursor: Evaluation of worldwide data and physical basis
title_full Radon content of groundwater as an earthquake precursor: Evaluation of worldwide data and physical basis
title_fullStr Radon content of groundwater as an earthquake precursor: Evaluation of worldwide data and physical basis
title_full_unstemmed Radon content of groundwater as an earthquake precursor: Evaluation of worldwide data and physical basis
title_sort radon content of groundwater as an earthquake precursor: evaluation of worldwide data and physical basis
publisher American Geophysical Union
publishDate 1981
url https://doi.org/10.1029/JB086iB10p09397
genre Iceland
genre_facet Iceland
op_source Journal of Geophysical Research B, 86(B10), 9397-9410, (1981-10)
op_relation https://doi.org/10.1029/JB086iB10p09397
eprintid:38331
op_rights info:eu-repo/semantics/openAccess
Other
op_doi https://doi.org/10.1029/JB086iB10p09397
container_title Journal of Geophysical Research: Solid Earth
container_volume 86
container_issue B10
container_start_page 9397
op_container_end_page 9410
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