Monitoring 222 Rn in soil gas of Garfagnana (Tuscany) aimed at earthquake prediction

222 Rn concentration in soil gas from nineteen stations of Garfagnana valley (Central ltaly) was continuously monitored from December 1990 to May 1993. 222 Rn activity was measured by solid state nuclear track detector (SSNTD). Tracks detected by spark-counter and by optical microscope were proporti...

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Main Authors: A. Pescia, P. Norelli, C. Meletti, M. Leonardi, R. Cioni, G. Bigazzi, O. Balducci, G. Taddeucci
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 1994-06-01
Series:Annals of Geophysics
Subjects:
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/4179
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spelling doaj-fe344cc881c64cfdaf5a7be3c34efba72020-11-25T02:27:45ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X1994-06-0137510.4401/ag-4179Monitoring 222 Rn in soil gas of Garfagnana (Tuscany) aimed at earthquake predictionA. PesciaP. NorelliC. MelettiM. LeonardiR. CioniG. BigazziO. BalducciG. Taddeucci222 Rn concentration in soil gas from nineteen stations of Garfagnana valley (Central ltaly) was continuously monitored from December 1990 to May 1993. 222 Rn activity was measured by solid state nuclear track detector (SSNTD). Tracks detected by spark-counter and by optical microscope were proportionally constant for track densities lower than 2500 tracks/cm2. Since time variations in track density both for the same monitoring station and for different stations are significanfly higher than fluctuations in the experimental conditions, the validity of spark-counter for radon activity measurements is confirmed. Data collected in the period of monitoring indicate significant seasonal variations in radon concentration for every monitoring station. Moreover, the soil characteristics play an important role in determining the observed patterns. No significant correlation could be found between radon emission and seismicity. However, it should be noted that no earthquake with a magnitude higher than 3.5 occurred in Garfagnana during the monitoring period.http://www.annalsofgeophysics.eu/index.php/annals/article/view/4179Radontracksoil gasmonitoringearthquake prediction
collection DOAJ
language English
format Article
sources DOAJ
author A. Pescia
P. Norelli
C. Meletti
M. Leonardi
R. Cioni
G. Bigazzi
O. Balducci
G. Taddeucci
spellingShingle A. Pescia
P. Norelli
C. Meletti
M. Leonardi
R. Cioni
G. Bigazzi
O. Balducci
G. Taddeucci
Monitoring 222 Rn in soil gas of Garfagnana (Tuscany) aimed at earthquake prediction
Annals of Geophysics
Radon
track
soil gas
monitoring
earthquake prediction
author_facet A. Pescia
P. Norelli
C. Meletti
M. Leonardi
R. Cioni
G. Bigazzi
O. Balducci
G. Taddeucci
author_sort A. Pescia
title Monitoring 222 Rn in soil gas of Garfagnana (Tuscany) aimed at earthquake prediction
title_short Monitoring 222 Rn in soil gas of Garfagnana (Tuscany) aimed at earthquake prediction
title_full Monitoring 222 Rn in soil gas of Garfagnana (Tuscany) aimed at earthquake prediction
title_fullStr Monitoring 222 Rn in soil gas of Garfagnana (Tuscany) aimed at earthquake prediction
title_full_unstemmed Monitoring 222 Rn in soil gas of Garfagnana (Tuscany) aimed at earthquake prediction
title_sort monitoring 222 rn in soil gas of garfagnana (tuscany) aimed at earthquake prediction
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
series Annals of Geophysics
issn 1593-5213
2037-416X
publishDate 1994-06-01
description 222 Rn concentration in soil gas from nineteen stations of Garfagnana valley (Central ltaly) was continuously monitored from December 1990 to May 1993. 222 Rn activity was measured by solid state nuclear track detector (SSNTD). Tracks detected by spark-counter and by optical microscope were proportionally constant for track densities lower than 2500 tracks/cm2. Since time variations in track density both for the same monitoring station and for different stations are significanfly higher than fluctuations in the experimental conditions, the validity of spark-counter for radon activity measurements is confirmed. Data collected in the period of monitoring indicate significant seasonal variations in radon concentration for every monitoring station. Moreover, the soil characteristics play an important role in determining the observed patterns. No significant correlation could be found between radon emission and seismicity. However, it should be noted that no earthquake with a magnitude higher than 3.5 occurred in Garfagnana during the monitoring period.
topic Radon
track
soil gas
monitoring
earthquake prediction
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/4179
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