Effects on the groundwater levels of the May-June 2012 Emilia seismic sequence

<p>A variety of phenomena were observed in the groundwaters in concomitance with the May-June 2012 seismic sequence that occurred in the Emilia Romagna area. In particular, phreatic wells close to the epicentral area were affected by a sudden increase in water level of up to 4 m. In some cases...

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Main Authors: Marco Marcaccio, Giovanni Martinelli
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 2012-10-01
Series:Annals of Geophysics
Subjects:
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/6139
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spelling doaj-a6252a440d564695b8ae70e0a5f1f5a02020-11-24T23:31:58ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X2012-10-0155410.4401/ag-61395799Effects on the groundwater levels of the May-June 2012 Emilia seismic sequenceMarco Marcaccio0Giovanni Martinelli1Agenzia Regionale Prevenzione e Ambiente (ARPA) dell'Emilia-Romagna, Direzione Tecnica, BolognaAgenzia Regionale Prevenzione e Ambiente (ARPA) dell'Emilia-Romagna, Sezione di Reggio Emilia, Reggio Emilia<p>A variety of phenomena were observed in the groundwaters in concomitance with the May-June 2012 seismic sequence that occurred in the Emilia Romagna area. In particular, phreatic wells close to the epicentral area were affected by a sudden increase in water level of up to 4 m. In some cases, the sands of aquifers were ejected outside wells, and &gt;700 liquefaction phenomena were recorded [Bertolini and Fioroni 2012, this volume]. Some automatic stations of the regional well network recorded variations in well levels. These data can be considered useful to understand the relationships between seismic events and the local groundwaters [see also Italiano et al. 2012, this volume]. […] In 1976, a regional network composed of 330 wells was set up with the purpose of monitoring the groundwater levels using manual techniques. These data have been used for environmental purposes and for water management. In recent years, the monitoring network managed by Agenzia Regionale Prevenzione e Ambiente (ARPA) has increased the number of wells (to about 600), and chemical analyses are also periodically carried out for environmental monitoring activities. In the past three years, an automatic monitoring network composed of 40 stations was set up and this has allowed the monitoring of the water levels and the temperatures, at a rate of one measure per hour, and to broadcast the data to the host center located in Bologna. […]</p>http://www.annalsofgeophysics.eu/index.php/annals/article/view/6139Groundwater processesGroundwatersSeismic effectsWater levelHydrology
collection DOAJ
language English
format Article
sources DOAJ
author Marco Marcaccio
Giovanni Martinelli
spellingShingle Marco Marcaccio
Giovanni Martinelli
Effects on the groundwater levels of the May-June 2012 Emilia seismic sequence
Annals of Geophysics
Groundwater processes
Groundwaters
Seismic effects
Water level
Hydrology
author_facet Marco Marcaccio
Giovanni Martinelli
author_sort Marco Marcaccio
title Effects on the groundwater levels of the May-June 2012 Emilia seismic sequence
title_short Effects on the groundwater levels of the May-June 2012 Emilia seismic sequence
title_full Effects on the groundwater levels of the May-June 2012 Emilia seismic sequence
title_fullStr Effects on the groundwater levels of the May-June 2012 Emilia seismic sequence
title_full_unstemmed Effects on the groundwater levels of the May-June 2012 Emilia seismic sequence
title_sort effects on the groundwater levels of the may-june 2012 emilia seismic sequence
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
series Annals of Geophysics
issn 1593-5213
2037-416X
publishDate 2012-10-01
description <p>A variety of phenomena were observed in the groundwaters in concomitance with the May-June 2012 seismic sequence that occurred in the Emilia Romagna area. In particular, phreatic wells close to the epicentral area were affected by a sudden increase in water level of up to 4 m. In some cases, the sands of aquifers were ejected outside wells, and &gt;700 liquefaction phenomena were recorded [Bertolini and Fioroni 2012, this volume]. Some automatic stations of the regional well network recorded variations in well levels. These data can be considered useful to understand the relationships between seismic events and the local groundwaters [see also Italiano et al. 2012, this volume]. […] In 1976, a regional network composed of 330 wells was set up with the purpose of monitoring the groundwater levels using manual techniques. These data have been used for environmental purposes and for water management. In recent years, the monitoring network managed by Agenzia Regionale Prevenzione e Ambiente (ARPA) has increased the number of wells (to about 600), and chemical analyses are also periodically carried out for environmental monitoring activities. In the past three years, an automatic monitoring network composed of 40 stations was set up and this has allowed the monitoring of the water levels and the temperatures, at a rate of one measure per hour, and to broadcast the data to the host center located in Bologna. […]</p>
topic Groundwater processes
Groundwaters
Seismic effects
Water level
Hydrology
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/6139
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AT giovannimartinelli effectsonthegroundwaterlevelsofthemayjune2012emiliaseismicsequence
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