IJEGE 11 - Volume 01
Up one level
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by
Alberto
Prestininzi - Scientific Editor-in-Chief
DOI:
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by
Luca
Lenti - IFSTTAR - University Paris Est - Paris, France
Salvatore
Martino - CERI - Sapienza University of Rome - Rome, Italy
Antonella
Paciello - ENEA - R.C. Casaccia - Rome, Italy
Alberto
Prestininzi - CERI - Sapienza University of Rome - Rome, Italy
Roberto W.
Romeo - University of Urbino “Carlo Bo” - Urbino, Italy
DOI: 10.4408/IJEGE.2011-01.O-01
This paper is a follow-up of a preliminary report on the same subject, which was posted on the website of this Journal on 25 March 2011. The report investigated the ground motion records of the Honshu earthquake of 11 March 2011, made available by the Japanese accelerometric networks KIK-NET and K-NET and by an Italian seismometric network, operated by the CERI Research Centre (Sapienza University of Rome) and located in the central
Apennines.
The paper highlights some kinematic and spectral features iden
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by
Massimo
Rinaldi - Università degli Studi di Firenze - Dipartimento di Ingegneria Civile e Ambientale
Nicola
Surian - Università degli Studi di Padova - Dipartimento di Geografia
Francesco
Comiti - Libera Università di Bolzano - Facoltà di Scienze e Tecnologie
Martina
Bussettini - Istituto Superiore per la Protezione e la Ricerca Ambientale (IS PRA ), Roma
DOI: 10.4408/IJEGE.2011-01.O-02
The general structure of a new methodology, named IDRAIM
(sistema IDRomorfologico di valutazione, AnalisI e Monitoraggio
dei corsi d’acqua), aimed at a hydromorphological assessment and
analysis of streams is presented. In particular, a stream Morphological
Quality Index (IQM) developed for the hydromorphological
classification required by the European Water Framework Directive
2000/60/EC (WFD) is illustrated.
The methodological approach is based on integration of field
surveys with remote sensing
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by
Marco
Amanti - ISPRA Istituto Superiore per la Protezione e la Ricerca Ambientale - Dipartimento Difesa del Suolo/Servizio Geologico d’Italia
Giovanni
Conte - ISPRA Istituto Superiore per la Protezione e la Ricerca Ambientale - Dipartimento Difesa del Suolo/Servizio Geologico d’Italia
Maurizio
Marino - ISPRA Istituto Superiore per la Protezione e la Ricerca Ambientale - Dipartimento Difesa del Suolo/Servizio Geologico d’Italia
Gennaro Maria
Monti - ISPRA Istituto Superiore per la Protezione e la Ricerca Ambientale - Dipartimento Difesa del Suolo/Servizio Geologico d’Italia
Guido
Motteran - ISPRA Istituto Superiore per la Protezione e la Ricerca Ambientale - Dipartimento Difesa del Suolo/Servizio Geologico d’Italia
Paolo
Perini - ISPRA Istituto Superiore per la Protezione e la Ricerca Ambientale - Dipartimento Difesa del Suolo/Servizio Geologico d’Italia
Angelantonio
Silvi - ISPRA Istituto Superiore per la Protezione e la Ricerca Ambientale - Dipartimento Difesa del Suolo/Servizio Geologico d’Italia
DOI: 10.4408/IJEGE.2011-01.O-03
This work is aimed to the hydrostructural characterisation of a portion of the Mt. Cambio aquifer system (eastern Reatini Mountains) and the hydrodynamic study of perennial suspended springs for which time series data on discharge are available.
The outcropping lithotypes belong to the Umbro-Marchigiano-Sabina Succession (pelagic basin sediments, mainly fine-grained and well-stratified), interfingered with detritic flows. A synform structure was identified, including associated undulations, minor folds and
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by
Giuseppe Cesareo
Calò - Politecnico di Bari - Dipartimento di Ingegneria delle Acque e di Chimica
Fabio
Macrì - Studio Geologico Macrì
Ferruccio
Piccinni - Politecnico di Bari - Dipartimento di Ingegneria delle Acque e di Chimica
Roccaldo
Tinelli - Politecnico di Bari - Dipartimento di Ingegneria delle Acque e di Chimica
DOI: 10.4408/IJEGE.2011-01.O-04
Casalabate is an outlying ward of Lecce located on the Adriatic Sea shore, over the time this small village has undergone remarkable hydrogeologic disturbance resulting in the collapse of some dwellings and the condemn of many others. In order to find out the causes, an accurate multidisciplinary investigation planning has been implemented. This includes a geological survey with 23 boreholes, a georadar investigation, as well as chemical-physical
analyses, thermo-saline logging and groundwater flow velocit
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by
Scott W.
McCoy - University of Colorado - CIRES & Department of Geological Sciences - Boulder, Colorado 80309, USA
Jeffrey A.
Coe - U.S. Geological Survey - Denver Federal Center - MS 966, Denver, Colorado 80225, USA
Jason W.
Kean - U.S. Geological Survey - Denver Federal Center - MS 966, Denver, Colorado 80225, USA
Greg E.
Tucker - University of Colorado - CIRES & Department of Geological Sciences - Boulder, Colorado 80309, USA
Dennis M.
Staley - U.S. Geological Survey - Denver Federal Center - MS 966, Denver, Colorado 80225, USA
Thad A.
Wasklewicz - East Carolina University - Department of Geography - Greenville, North Carolina 27858, USA
DOI: 10.4408/IJEGE.2011-03.B-078
Debris flows initiated by surface-water runoff during short duration, moderate- to high-intensity rainfall are common in steep, rocky, and sparsely vegetated terrain. Yet large uncertainties remain about the
potential for a flow to grow through entrainment of loose debris, which make formulation of accurate mechanical models of debris-flow routing difficult. Using a combination of in situ measurements of debris flow dynamics, video imagery, tracer rocks implanted with passive integrated transponders (PIT)
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