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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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 >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 >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 |
work_keys_str_mv |
AT marcomarcaccio effectsonthegroundwaterlevelsofthemayjune2012emiliaseismicsequence AT giovannimartinelli effectsonthegroundwaterlevelsofthemayjune2012emiliaseismicsequence |
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1725535792686694400 |