ANTRONICO L., GULLA' G., TERRANOVA O., 2001, Condizioni di dissesto sui versanti e processi in alveo conseguenti alle piogge dell’8-10 Settembre 2000 nel bacino del T. Beltrame e nelle aree circostanti (Basso Ionio della Calabria),
2001,
GULLA' G., ACETO L., GRECO R., NICEFORO D., DODARO F., 2001, Definizione preliminare del Modello Geotecnico della Frana di Serra di Buda (Acri – Calabria),
2001,
GULLA' G., 2001, Procedura per la valutazione della pericolosità e del rischio da frana,
2001,
Lorenzo M. (1), Schiattarella M. (1), Sdao F. (1), Tansi C. (2), 2001, Inquadramento geologico e condizioni di stabilità dei versanti dell’area interessata dal sisma del 9 settembre 1998,
Dissesti prodotti o aggravati dal sisma del 9 settembre 1998 nei territori del Confine calabro-lucano, edited by Gullà G., Sdao F., pp. 9–35. Soveria Mannelli_ Rubbettino, 2001,
D. Casarano, G. De Carolis, F. Mattia, C. Notarnicola, F. Posa, A. Refice, V.D. Schena, R. Sergi, P. Smacchia, 2001, SIR-C,
Il Nuovo cimento C (Online) 24 (2001): 11–23.,
Abstract
During the Space Shuttle Endeavour mission in October 1994, a remote-sensing campaign was carried out ...
During the Space Shuttle Endeavour mission in October 1994, a remote-sensing campaign was carried out with the objectives of both radiometric and polarimetric calibration and ground truth data acquisition of bare soils. This paper presents the results obtained in the experiment. Polarimetric cross-talk and channel imbalance values, as well as radiometric calibration parameters, have been found to be within the science requirements for SAR images. Regarding ground truth measurements, a wide spread in the height rms values and correlation lengths has been observed, which has motivated a critical revisiting of surface parameters descriptors.
DEL GAUDIO V., PIERRI P., e WASOWSKI J., 2001, Un approccio per la valutazione della probabilità temporale di frane sismo-indotte a scala regionale,
20° Convegno Nazionale GNGTS, pp. 289–292, Roma, 2001,
A. REFICE, F. BOVENGA, J. WASOWSKI, 2001, Monitoring landslide activity in a peri-urban area by SAR Interferometry,
EGU 2001, 2001,
Refice, A; Bovenga, F; Guerriero, L; Wasowski, J, 2001, DInSAR applications to landslide studies,
IGARSS 2001, pp. 144–146, Sydney, Australia, 9-14 July 2001,
Abstract
Operational monitoring of slope instabilities by SAR Interferometry poses a number of challenges due to ...
Operational monitoring of slope instabilities by SAR Interferometry poses a number of challenges due to the limited spatial extent of the landsliding areas and the rainy conditions usually associated with mass movement events. In this work, we present applications of DInSAR techniques to the assessment of the stability of landslide-prone areas.
Petrucci O., Taddei A. e Minervino I., 2001, WP6000: Selection of Case studies in the Cosenza province,
2001,
Sorriso-Valvo M., Petrucci O., Capparelli G., Silvestri F., Varra' V., Versace P., 2001, Literature survey on landslide types, activity and models,
2001,
PETRUCCI O., 2001, L’analisi dei dati storici per lo studio delle catastrofi idrogeologiche,
22° Corso di aggiornamento_ Tecniche per la difesa dall'inquinamento. Gruppo Italiano di Idraulica, GUARDIA PIEMONTESE, 20 GIUGNO 2001,
Iovine G., Petrucci O., Ferrari E., 2001, Eventi di dissesto idrogeologico nell’Alto Jonio calabrese (CS),
Emergenze ambientali di carattere geomorfologico e tettonico. Comunità Montana Alto Ionio e Min. LL. PP., Oriolo Calabro, 01/02/2001,
Iovine G., Petrucci O., Ferrari E., 2001, Eventi di dissesto idrogeologico nell’Alto Jonio calabrese,
Emergenze ambientali di carattere geomorfologico e tettonico, pp. 15–31, Oriolo Calabro, 1-2 Febbraio 2001,
GENEVOIS R., GALGARO A., TECCA P.R., 2001, Image Analysis for Debris Flow Properties Estimation.,
Physics and chemistry of the earth (2002) 26 (2001): 623–631. doi_10.1016/S1464-1917(01)00059-9,
DOI: 10.1016%2FS1464-1917(01)00059-9
D'Agostino V.
Marchi L., 2001, Debris flow magnitude in the Eastern Italian Alps_ data collection and analysis,
Physics and chemistry of the earth. Part C_ Solar-terrestrial and planetary science 26 (2001): 657–663.,
Polemio M, 2001, Valutazione del dissesto idrogeologico nell’ abitato di Bovino – Relazione,
2001,
Abstract
Valutazione del dissesto idrogeologico nell' abitato di Bovino ...
Valutazione del dissesto idrogeologico nell' abitato di Bovino
Petrucci O., Polemio M., 2001, The use of historical data in the characterisation of hydrogeological multiple hazard,
Geophysical research abstracts 3 (2001): 223–223.,
M. Polemio (1), O. Petrucci (2), 2001, Landslides triggered by rainfall_ a critical analysis of international experiences,
XXVI EGS General Assembly, Nice (Francia), 25-30/3/2001,
Polemio, M., Petrucci, O., 2001, Landslides triggered by rainfall_ a critical analysis of international experiences,
Geophysical research abstracts (Online) 3 (2001): 334.,
Arattano M., 2001, Monitoring, modelling and mapping of mass movements,
Physics and chemistry of the earth. Part C_ Solar-terrestrial and planetary science 26 (2001): 621–621. doi_10.1016/S1464-1917(01)00058-7,
DOI: 10.1016%2FS1464-1917(01)00058-7
Delle Rose M., Parise M., Proietto G., Tartarelli M., 2001, L’àviso Neviera (Pu 196) a Sogliano Cavour (provincia di Lecce).,
Puglia grotte (2001): 35–42.,
Rizzo V., Fragale F., Terranova O., 2001, Widespread landslide and flood events in the Catanzaro isthmus (Calabria, Italy). Relationship with rainfall data.,
Natural Hazards and Hydrological Science Symposium of the XXIV general assembly of the European Geophysica Society, pp. 169–183, The Hague (NL), 19-23 Aprile 1999,
Luino F., 2001, Raccogliamo ciò che abbiamo seminato…,
Nimbus (Torino) (2001): 100–111.,
MARAGA F., LUINO F., TURITTO O., 2001, Flooding sediment grain size on flood prone plains (po River basin, Northern Italy),
7th International Conference on Fluvial Sedimentology, Lincoln, 6-10 Agosto 2001,
Luino F., 2001, Come un fiume in piena,
Costruire (Milano) (2001): 68–70.,
Gullà G., Antronico, L., Sorriso-Valvo M., Borrelli L., Greco R., Niceforo D., Aceto L, Terranova O., Naccarato G., 2001, Progettazione esecutiva per la rete nazionale di monitoraggio frane – Sezione territoriale della Regione Calabria,
2001,
Abstract
Svolto per la Presidenza del Consiglio dei Ministri-DSTN-Servizio Geologico Nazionale, P.O. Assistenza tecnica del Q.C.S. ...
Svolto per la Presidenza del Consiglio dei Ministri-DSTN-Servizio Geologico Nazionale, P.O. Assistenza tecnica del Q.C.S. Obiettivo 1 - 1994-1999 - Misura 2.5 Studio di fattibilità e progettazion.
Antronico L., Gullà G., Oddo B., 2001, Considerazioni preliminari sulla caratterizzazione di soil slip in alcune zone di studio della Stretta di Catanzaro (Calabria),
Bollettino della Società Geologica Italiana (Testo stamp.) 56 (2001): 1–10.,
Abstract
In a study area of Calabria multidisciplinary researches are in progress in order to test ...
In a study area of Calabria multidisciplinary researches are in progress in order to test procedures devoted to define the geo-environmental contexts with homogeneous characteristics with respect to specific types of slope instability.
In the study area, that falls inside a graben structure, sedimentary and metamorphic rocks crop out. Both rocks are affected by widespread slope instability, shallow and deep seated landslides, and erosion processes (from moderate to intense).
The shallow failures in the slopes (from 0.5 to 2 m in depth) assume particular importance in the area. This type of instability, indicated as "soil slips", involves small volumes of soil and can produce serious damage to property and danger to people.
The hazard that this type of instability represents is determined by their kinematic mechanism (slide and immediately subsequent rapid flow) and by their spreading during particularly severe rainstorms.
The high incidence of such type of slope instability, has suggested a research aimed at defining a methodological approach to quickly identify their features. These features are essential for the development of forecasting models and subsequent definition of remedial measures, aimed at preventing or reducing risks.
For this reason, in three sample zones of the study area where soil slips involving sedimentary terrains detailed geo-morphological reliefs and geotechical surveys have been carried out. This survey, analyzed together with the photographic documentation acquired during about ten years of observation, has produced a satisfactory definition of the geometric characteristics of the shallow failures.
The knowledge of the dates of some mobilization occurred in the period considered and the rainfall time series, allowed to assess the characteristics of the triggering rainstorm events.
Moreover, the results of some accurate topographic surveys carried out in order to obtain important information about the geometry of the slopes, are shown.
Finally, the results of geotechnical tests enabled to define the particle size envelopes and the index properties of the soil covers involved in shallow instabilities.
ANTRONICO L, SORRISO-VALVO M., TANSI C., GULLA' G., 2001, Carta litologico-strutturale e dei movimenti in massa della Stretta di Catanzaro (Scala 1_50000),
2001,
GULLA' G., ANTRONICO L, COSTA P., D'AMBROSIO R., 2001, Banche dati nell’ingegneria geotecnica_ l’applicativo Geotec.da.ba,
Convengno "GIS: strumenti avanzati ed applicazioni per la gestione ed il controllo del territorio", Università degli Studi del Sannio, pp. 79–83, Benevento, 14 novembre 2001,
Glade T., Guzzetti F., Reichenbach P., Cardinali M., De Vita P., 2001, Regional rainfall and hydrologic thresholds for landslide occurrence. Examples from New Zealand and central Italy,
2nd Plinius Conference on Mediterranean Storms, 2001,
Antonini G., Ardizzone F., Cacciano M., Cardinali M., Castellani M., Galli M., Guzzetti F., Reichenbach P., Salvati P., 2001, Procedura per la perimetrazione delle aree a rischio da frana e per la valutazione delle condizioni di rischio specifico e totale,
2001,
Antonini G., Cardinali M., Galli M., Guzzetti F., Reichenbach P., 2001, Cartografia dei movimenti franosi per il bacino del Torrente Staffora, Provincia di Pavia, Lombardia,
2001,
Abstract
Cartografia dei movimenti franosi per il bacino del Torrente Staffora, Provincia di Pavia, Lombardia ...
Cartografia dei movimenti franosi per il bacino del Torrente Staffora, Provincia di Pavia, Lombardia
SORRISO-VALVO M. (Responsabile scientifico), GULLA' G., et al., 2001, Studio e monitoraggio della frana di Serra di Buda (Acri)-Relazione finale.,
2001,
Abstract
Studio e monitoraggio ...
Studio e monitoraggio
GULLA' G., SDAO F. (curatori); Autori vari, 2001, Dissesti Prodotti o Aggravati dal Sisma del 9 Settembre 1998 nei Territori del Confine calabro-lucano,
Perugia: CNR, GNDCI, 2001,
Loredana Antronico, Giovanni Gullà e Oreste Terranova, 2001, L’evento pluviometrico dell’8-10 settembre 2000 nella Calabria Ionica Meridionale_ dissesti sui versanti e processi in alveo in alcune aree campione,
Il dissesto idrogeologico_ inventario e prospettive, Roma, Accademia dei Lincei, 5 giugno 2001,
Ardizzone F., Sterlacchini S., 2001, Procedure per la realizzazione della banca dati del CNR,
pp.1–54, 2001,
M.V. Avolio (1), G. D. D'Ambrosio (1), S. Di Gregorio (1), R. Rongo (1), W. Spataro (1), G. Iovine (2), V. Lupiano (2), 2001, Simulating different complexity landslides with cellular automata methods,
Geophysical research abstracts (Online) 3 (2001).,
IOVINE G. (1), PETRUCCI O. (1) & FERRARI E. (2), 2001, Eventi di dissesto idrogeologico nell’Alto Jonio calabrese (CS).,
Conv. Naz. "Emergenze ambientali di carattere geomorfologico e tettonico. Le frane, le alluvioni, i terremoti"., pp. 15–31, Oriolo Calabro (CS), 1-2 febbraio, 2001,
D'AMBROSIO D. (1), DI GREGORIO S. (1), IOVINE G. (2), LUPIANO V. (2), RONGO R. (3) & SPATARO W. (1), 2001, Simulation of flow-like landslides through cellular automata.,
"ROCC - International Conference on Coastal Rock Slope Instability_ Geohazard and Risk Analysis", pp. 49–51, Le Havre, 30-31 maggio 2001,
AVOLIO M.V. (1), D'AMBROSIO D. (1), DI GREGORIO S. (1), RONGO R. (2), SPATARO W. (1), IOVINE G. (3), LUPIANO V. (3), MERENDA L. (3) & NARDI G. (4), 2001, Simulating landslides of different complexity with hexagonal cellular automata.,
"IAMG 2001 - International Association for Mathematical Geology", Session M, Cancùn, Mexico, 6-12 settembre 2001,
Abstract
The paradigms of acentrism and parallelism that are embedded in the definition of Cellular
Automata (CA) ...
The paradigms of acentrism and parallelism that are embedded in the definition of Cellular
Automata (CA) can be easily and efficiently applied in the simulation of very complex natural
processes like landslides. This permits a phenomenological description that is able to overcome
resource computational limits, placed in a classical approach and therefore based on the resolution
of differential equation systems.
We present a general frame and the latest developments of a CA based model for the
simulation of debris flow type landslides.
Landslides are here viewed as a dynamical system that is subdivided in parts which
components evolve exclusively on the basis of "local interactions" in a spatial and temporal
discretum, where space is represented by hexagonal cells, which specifications (namely substates)
describe the average physical characteristics of the respective area. Such a method permits to start
from simple landslides, that can be modeled using few substates and simple local interactions; a
more complex landslide can be modeled from the previous model, adding substates and local
interactions.
SCIDDICA can be considered to exhibit great flexibility in modeling and simulating debris
flows. Furthermore it can be applied in some field of intervention such as_ The creation of risk
maps also with a statistical approach; the simulation of the possible effects of intervention on
flows for stream deviation, introducing data which represent alterations of the original conditions
(e.g., the construction of a canal or embankment, occlusion of a mud canal etc.). Examples of
practical applications on real events involved_ the 1992 reactivation of the Tessina landslide in
Italy, the 1984 Ontake volcano debris avalanche in Japan and a first partial application to the
landslides occurred in the Sarno area of Campania Region (Italy) in the May of 1998.
Chiarle M., 2001, Analisi dei pericoli naturali in ambiente glaciale,
2001,
Abstract
Tesi di Dottorato di Ricerca, Politecnico di Torino, Dipartimento Georisorse e Territorio, XII ciclo, 206 ...
Tesi di Dottorato di Ricerca, Politecnico di Torino, Dipartimento Georisorse e Territorio, XII ciclo, 206 pp
CHIARLE M. & MORTARA G., 2001, Esempi di rimodellamento di apparati morenici nell’arco alpino italiano,
Atti dell'VIII Convegno Glaciologico Italiano, "Risposta dei ghiacciai alpini ai cambiamenti climatici", pp. 41–54, Bormio, 9-12 Settembre 1999,
CHIARLE M. & MORTARA G., 2001, Bòsmattò (Gressoney Saint Jean), il giorno del disastro,
Nimbus (Torino) 21/22 (2001): 88–92.,
O. Petrucci, 2001, Social and economic impact of slope instability in Italy and in Calabria,
2001,
Lorenzo M. (1), Schiattarella M. (1), Sdao F. (1), Tansi C. (2), 2001, Inquadramento geologico, condizioni di stabilità dei versanti dell’area interessata dal sisma del 9 settembre 1998.,
pp.9–35, 2001,
Tansi C., 2001, I dissesti in località Giardini Nuova del Comune di Castelluccio Superiore (PZ).,
pp.87–93, 2001,
Polemio, M.
Ricchetti, E., 2001, Vulnerability Mapping of an Apulian Deep Carbonate Aquifer Using GIS,
2nd Symposium "Protection of groundwater from pollution and seawater intrusion", pp. 291–302, BARI, 27/09-01/10/1999,
Abstract
Computer techniques such as Geographic Information Systems are applied to the evaluation of the vulnerability ...
Computer techniques such as Geographic Information Systems are applied to the evaluation of the vulnerability of a deep carbonate aquifer.
The study area, of about 150 km2, is located in the low Murgia Plateau (Apulia) and characterized by Mesozoic limestone and dolomite rocks of several thousand meters thickness. A wide and thick aquifer resides in these carbonate rocks. Its groundwater flows toward the sea mainly under pressure and with maximum piezometric level of about 200 m a.s.l.. Due to their high quality, the water resources of this aquifer are particularly valuable for the local communities and therefore must be protected from pollution and inappropriate use.
The vulnerability map of the aquifer is an indispensable tool for the effective management of groundwater resources and to support environmental planning. Several approaches have been proposed by different authors to evaluate intrinsic vulnerability. Most of the methods for detailed vulnerability mapping are based on the integrated analysis of several variables using different algorithms. Geographic Information Systems are advanced computer tools for the analysis of georeferenced data in 2D and 3D and can be effectively applied to the implementation of evaluation models. In this study the SINTACS evaluation method was implemented in a GIS and a digital vulnerability map produced.
The different data taken into consideration in this analysis, such as depth to water, actual infiltration, pollution attenuation capacity of unsaturated zone, land cover, hydrogeological features of saturated aquifer, hydraulic conductivity, terrain slope, geology and geological structures, were georeferenced and converted into digital form. Each variable corresponds to a separate data layer made of graphic and attribute data.
The computerized multilayer analysis performed by the GIS is time effective and leads to more comprehensive and accurate results with better spatial resolution.
Paolucci R., Petrucci O., Polemio M., 2001, L’evoluzione delle pianure costiere e il dissesto idrogeologico in un’area campione della Calabria,
Conoscenza e salvaguardia delle aree di pianura_ il contributo delle Scienze della Terra, Ferrara, 2001,
Tansi C. (1), 2001, I dissesti in località Giardini Nuova del Comune di Castelluccio Superiore (PZ),
Dissesti prodotti o aggravati dal sisma del 9 settembre 1998 nei territori del Confine calabro-lucano, edited by Gullà G., Sdao F., pp. 87–93. Soveria Mannelli_ Rubbettino, 2001,
Bianca M. (1), Monaco C. (1), Tansi C. (2), Tortorici G. (1), Tortorici L. (1), 2001, Quaternary normal faulting and marine terracing in the area of Capo Vaticano and S. Eufemia Gulf (southern Calabria),
3° Forum Italiano di Scienze della Terra, Chieti, 5-8 Settembre 2001,
