Application and validation of bivariate GIS-based landslide susceptibility assessment for the Vitravo river catchment (Calabria, south Italy)

被引:56
作者
Conforti, Massimo [1 ]
Robustelli, Gaetano [1 ]
Muto, Francesco [1 ]
Critelli, Salvatore [1 ]
机构
[1] Univ Calabria, Dipartimento Sci Terra, I-87036 Arcavacata Di Rende, CS, Italy
关键词
Bivariate statistics; GIS; Landslide susceptibility; Calabria; South Italy; GRAVITATIONAL SLOPE DEFORMATIONS; HAZARD EVALUATION; FREQUENCY RATIO; BASIN; AREA; INSTABILITY; TECTONICS; EXAMPLE; MASSIF; MODELS;
D O I
10.1007/s11069-011-9781-0
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The Calabria (Southern Italy) region is characterized by many geological hazards among which landslides, due to the geological, geomorphological, and climatic characteristics, constitute one of the major cause of significant and widespread damage. The present work aims to exploit a bivariate statistics-based approach for drafting a landslide susceptibility map in a specific scenario of the region (the Vitravo River catchment) to provide a useful and easy tool for future land planning. Landslides have been detected through air-photo interpretation and field surveys, by identifying both the landslide detachment zones (LDZ) and landslide bodies; a geospatial database of predisposing factors has been constructed using the ESRI ArcView 3.2 GIS. The landslide susceptibility has been assessed by computing the weighting values (Wi) for each class of the predisposing factors (lithology, proximity to fault and drainage line, land use, slope angle, aspect, plan curvature), thus evaluating the distribution of the landslide detachment zones within each class. The extracted predisposing factors maps have then been re-classified on the basis of the calculated weighting values (Wi) and by means of overlay processes. Finally, the landslide susceptibility map has been considered by five classes. It has been determined that a high percentage (61%) of the study area is characterized by a high to very high degree of susceptibility; clay and marly lithologies, and slope exceeding 20A degrees in inclination would be much prone to landsliding. Furthermore, in order to ascertain the proposed landslide susceptibility estimate, a validation procedure has been carried out, by splitting the landslide detachment zones into two groups: a training and a validation set. By means of the training set, the susceptibility map has first been produced; then, it has been compared with the validation set. As a result, a great majority of LDZ-validation set (85%) would be located in highly and very highly susceptible areas. The predictive power of the model is considered reliable, since more than 50% of the LDZ fall into 20% of the most susceptible areas. The reliability of the susceptibility map is also suggested by computing the SCAI index, true positive and false positive rates; nevertheless, the most susceptible areas are overestimated. As a whole, the results indicate that landslide susceptibility assessment based on a bivariate statistics-based method in a GIS environment may be useful for land planning policy, especially when considering its cost/benefit ratio and the need of using an easy tool.
引用
收藏
页码:127 / 141
页数:15
相关论文
共 62 条
[1]  
Aleotti P., 1999, Bull Eng Geol Environ, V58, P21, DOI [10.1007/s100640050066, DOI 10.1007/S1006-40050-066, DOI 10.1007/S100640050066]
[2]   LANDSLIDE HAZARD EVALUATION AND ZONATION MAPPING IN MOUNTAINOUS TERRAIN [J].
ANBALAGAN, R .
ENGINEERING GEOLOGY, 1992, 32 (04) :269-277
[3]  
Antronico L, 2000, P 8 INT S LANDSL LAN, P77
[4]   Landslide types and their relationships with weathering in a Calabrian basin, southern Italy [J].
Calcaterra, D ;
Parise, M .
BULLETIN OF ENGINEERING GEOLOGY AND THE ENVIRONMENT, 2005, 64 (02) :193-207
[5]  
Calcaterra D, 2010, ENG GEOLOGY SERIES S
[6]  
CARRARA A, 1995, ADV NAT TECHNOL HAZ, V5, P135
[7]   GIS TECHNIQUES AND STATISTICAL-MODELS IN EVALUATING LANDSLIDE HAZARD [J].
CARRARA, A ;
CARDINALI, M ;
DETTI, R ;
GUZZETTI, F ;
PASQUI, V ;
REICHENBACH, P .
EARTH SURFACE PROCESSES AND LANDFORMS, 1991, 16 (05) :427-445
[8]  
Carrara A., 1977, Z GEOMORPHOL, V21, P187, DOI DOI 10.1007/978-94-011-2878-0_2
[9]  
CASMEZ, 1971, CART GEOL CAL, V26, P11
[10]  
Catenacci V, 1992, GEOLOGICAL GEOENVIRO, P301