Digital photogrammetric analysis and electrical resistivity tomography for investigating the Picerno landslide (Basilicata region, southern Italy)

被引:45
作者
de Bari, Claudia [1 ,2 ]
Lapenna, Vincenzo [1 ]
Perrone, Angela [1 ]
Puglisi, Claudio [3 ]
Sdao, Francesco [2 ]
机构
[1] CNR, Ist Metodol Anal Ambientale, Tito, PZ, Italy
[2] Univ Basilicata, Dipartimento Strutture Geotecn & Geol Applicata A, I-85100 Potenza, Italy
[3] Ctr Ric Casaccia, Dipartimento Ambiente Cambiamenti Climat & Svilup, ENEA, Rome, Italy
关键词
Roto-translational slide; Aerial photos; Analytical and digital photogrammetry; ERT; DEM difference; MASS-WASTING PROCESSES; SAR INTERFEROMETRY; AERIAL PHOTOGRAPHS; ELEVATION MODELS; APENNINE CHAIN; URBAN AREA; EVOLUTION; MOVEMENTS; LIDAR; SUSCEPTIBILITY;
D O I
10.1016/j.geomorph.2011.06.013
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Digital photogrammetric analysis and Electrical Resistivity Tomography (ERT) techniques were applied to evaluate the volume of material involved in a complex roto-translational slide occurred in the territory of Picerno (Basilicata region, southern Italy). Analytical and digital photogrammetric techniques facilitated a multi-temporal analysis of aerial photos for the years 1997, 2004 and 2006. In order to identify different geomorphologic features (scarps, terraces and trenches) of the landslide and their development, the analytical and digital photo interpretation was performed at the maximum scale of 1:5000. Geological and geomorphological surveys were carried out to verify photo-interpretation results. Digital Elevation Models (DEMs) for 1997, 2004 and 2006 were produced by applying the Grid Adaptive method. The differential DEMs (2006-1997; 2006-2004; 2004-1997) for the most dangerous part of the landslide allowed us to recognize the areas affected either by deposition or erosion and also estimate any altitudinal changes in each geomorphologic unit. To detect the sliding surface and estimate the thickness of the sliding material, several transversal and longitudinal ERT profiles were obtained. The electrical images of subsurface supported by stratigraphical data from boreholes were integrated with the information from the DEMs. The altitudinal changes and the sizes of the source and accumulation areas allowed us to estimate the volume of material involved in the mass movement. The fusion of data from different sensors allows us to gather indications on the surface and subsurface characteristics of the landslide providing useful information for landslide mitigation activities. Such an approach can help both to improve our knowledge and overcome the drawbacks of each methodology. (C) 2011 Elsevier B.V. All rights reserved.
引用
收藏
页码:34 / 46
页数:13
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