Radon groundwater anomalies related to the Umbria-Marche, September 26, 1997, earthquakes

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1. Verfasser: F. Bella
Format: Artículo científico
Sprache:en
Veröffentlicht: Universidad Nacional Autónoma de México 2002
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author F. Bella
author_facet F. Bella
contents Radon groundwater anomalies related to the Umbria-Marche, September 26, 1997, earthquakes F. Bella P. G. Catalano R. Di Giovambattista W. Plastino Ciencias de la Tierra Radon earthquake radon and hydrogeochemical anomalies From May 1996, measurements of the radon content in groundwater and other parameters (pH, electrical conductivity,pressure of dissolved gases and groundwater temperature) were conducted at the Gran Sasso underground laboratory of theNational Institute for Nuclear Physics, Italy, using multiparametric equipment. We have analyzed the correlations between radonvariations and the stress-strain processes in the rock, and the radon diffusion processes related to groundwater geochemistry. Timeseries analysis showed strong anomalies in pH, radon concentrations and pressure of dissolved gases, which highly correlate withthe Umbria-Marche seismic sequence of 1997-1998. This may be caused by a transient compression phase producing a change ofcarbon dioxide content in groundwater. Spike-like anomalies of electrical conductivity correlate with local seismic events thussuggesting variations in groundwater dynamics. 2002 artículo científico 0016-7169 https://www.redalyc.org/articulo.oa?id=56841403 en http://www.redalyc.org/revista.oa?id=568 Geofísica Internacional application/pdf Universidad Nacional Autónoma de México Geofísica Internacional (México) Num.4 Vol.41
format Artículo científico
id redalyc_56841403
institution Redalyc
language en
publishDate 2002
publisher Universidad Nacional Autónoma de México
spellingShingle Radon groundwater anomalies related to the Umbria-Marche, September 26, 1997, earthquakes
F. Bella
Ciencias de la Tierra
Radon
earthquake
radon and hydrogeochemical anomalies
Radon groundwater anomalies related to the Umbria-Marche, September 26, 1997, earthquakes F. Bella P. G. Catalano R. Di Giovambattista W. Plastino Ciencias de la Tierra Radon earthquake radon and hydrogeochemical anomalies From May 1996, measurements of the radon content in groundwater and other parameters (pH, electrical conductivity,pressure of dissolved gases and groundwater temperature) were conducted at the Gran Sasso underground laboratory of theNational Institute for Nuclear Physics, Italy, using multiparametric equipment. We have analyzed the correlations between radonvariations and the stress-strain processes in the rock, and the radon diffusion processes related to groundwater geochemistry. Timeseries analysis showed strong anomalies in pH, radon concentrations and pressure of dissolved gases, which highly correlate withthe Umbria-Marche seismic sequence of 1997-1998. This may be caused by a transient compression phase producing a change ofcarbon dioxide content in groundwater. Spike-like anomalies of electrical conductivity correlate with local seismic events thussuggesting variations in groundwater dynamics. 2002 artículo científico 0016-7169 https://www.redalyc.org/articulo.oa?id=56841403 en http://www.redalyc.org/revista.oa?id=568 Geofísica Internacional application/pdf Universidad Nacional Autónoma de México Geofísica Internacional (México) Num.4 Vol.41
title Radon groundwater anomalies related to the Umbria-Marche, September 26, 1997, earthquakes
topic Ciencias de la Tierra
Radon
earthquake
radon and hydrogeochemical anomalies
url https://www.redalyc.org/articulo.oa?id=56841403