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  1. Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur
  2. Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur : Volume 65
  3. Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur : Volume 65, Issue 4, December 2006
  4. Investigating epikarst using low-frequency GPR: example from the Gran Sasso range (Central Italy)
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Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur : Volume 76
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur : Volume 75
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur : Volume 74
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur : Volume 73
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur : Volume 72
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur : Volume 71
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur : Volume 70
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur : Volume 69
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur : Volume 68
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur : Volume 67
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur : Volume 66
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur : Volume 65
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur : Volume 65, Issue 4, December 2006
Engineering geology maps: landslides and geographical information systems
Discontinuity networks in mudstones: a geological approach : Implications for radioactive wastes isolation in deep geological formations in Belgium, France, Switzerland
BDMPL: a data bank of the local raw materials in Tunisia
Investigating epikarst using low-frequency GPR: example from the Gran Sasso range (Central Italy)
The behaviour of organic matter in the process of soft soil stabilization using cement
Cohesion of unsaturated residual soils as a function of volumetric water content
Highway failure over talc–tremolite schist terrain: a case study of the Ife to Ilesha highway, South Western Nigeria
Assessing groundwater contamination risk using the DASTI/IDRISI GIS method: coastal system of western Mamora, Morocco
Common ground in engineering geology, soil mechanics and rock mechanics: past, present and future
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur : Volume 65, Issue 3, August 2006
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur : Volume 65, Issue 2, May 2006
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur : Volume 65, Issue 1, March 2006
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur : Volume 64
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur : Volume 63
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur : Volume 62
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur : Volume 61
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur : Volume 60
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur : Volume 59
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur : Volume 58
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur : Volume 57
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur : Volume 55

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Investigating epikarst using low-frequency GPR: example from the Gran Sasso range (Central Italy)

Content Provider Springer Nature Link
Author Tallini, Marco Gasbarri, Diego Ranalli, Danilo Scozzafava, Marco
Copyright Year 2005
Abstract A realistic 3D view of the epikarst is key to understanding karst groundwater phenomena. Ground penetrating radar proved to be highly effective for investigating the epikarst of a sinkhole located in the Gran Sasso karst range (central Italy). Two different low-frequency antennae (100 MHz bistatic shielded and 40 MHz bistatic unshielded) were used. The radar signal interpretation was correlated with field observations of the epikarst and borehole data. Two radar anomaly surfaces were identified, which were correlated with the top and bottom of the epikarst surface. The shape of the two surfaces correlates well with the surface topography of the study sinkhole and with the orientation of its main joints and karren. The work indicated that such a 3D reconstruction could be usefully applied to karst aquifer vulnerability studies.Une vue 3D de l’épikarst constitue un progrès notable pour la compréhension des écoulements karstiques. Le radar géologique s’est révélé très efficace pour reconnaître l’épikarst d’une dépression karstique située dans la chaîne du Gran Sasso (Italie centrale). Deux antennes basse fréquence (100 et 40 MHz) ont été utilisées. L’interprétation du signal radar a été corrélée avec des observations de terrain relatives à l’épikarst et des données de sondage. Deux discontinuités radar ont été identifiées et reconnues comme les surfaces supérieures et inférieures de l’épikarst. La forme des deux surfaces est contrôlée par la surface topographique de la dépression karstique étudiée et par l’orientation des discontinuités principales et des lapiaz. Le travail réalisé a montré qu’une telle reconstitution 3D pouvait être utile pour des études de vulnérabilité à la pollution d’aquifères karstiques.
Starting Page 435
Ending Page 443
Page Count 9
File Format PDF
ISSN 14359529
Journal Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur
Volume Number 65
Issue Number 4
e-ISSN 14359537
Language English
Publisher Springer-Verlag
Publisher Date 2006-01-04
Publisher Place Berlin, Heidelberg
Access Restriction One Nation One Subscription (ONOS)
Subject Keyword Radar géologique Epikarst Ecoulement souterrain Vulnérabilité d’aquifère karstique Italie centrale. Nature Conservation Geoecology/Natural Processes Structural Foundations, Hydraulic Engineering Applied Geosciences
Content Type Text
Resource Type Article
Subject Geology Geotechnical Engineering and Engineering Geology
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