Characterization of Rock Samples by A High-Resolution Multi-Technique Non-Invasive Approach

被引:7
作者
Fais, Silvana [1 ,2 ]
Cuccuru, Francesco [1 ]
Casula, Giuseppe [3 ]
Bianchi, Maria Giovanna [3 ]
Ligas, Paola [1 ]
机构
[1] Univ Cagliari, Dept Civil & Environm Engn & Architecture DICAAR, I-09123 Cagliari, Italy
[2] Consorzio Interuniv Ingn Georisorse CINIGeo, I-00186 Rome, Italy
[3] INGV Ist Nazl Geofis & Vulcanol, Sez Bologna, Via Donato Creti 12, I-40128 Bologna, Italy
关键词
non-invasive techniques; comenditic pyroclastic rock; Pietra Forte carbonatic rock; terrestrial laser scanner; photogrammetry; 3D acoustic tomography; petrographic data; integrated interpretation; FROM-MOTION PHOTOGRAMMETRY; ULTRASONIC PULSE VELOCITY; ACOUSTIC PROPERTIES; MECHANICAL-PROPERTIES; BUILDING-MATERIALS; WAVE VELOCITIES; SONIC VELOCITY; CORE SAMPLES; RECONSTRUCTION; POROSITY;
D O I
10.3390/min9110664
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Three different non-invasive techniques, namely Structure from Motion (SfM) photogrammetry, Terrestrial Laser Scanner (TLS) and ultrasonic tomography integrated with petrographic data, were applied to characterize two rock samples of a different nature: A pyroclastic rock and a carbonate rock. We started a computation of high-resolution 3D models of the two samples using the TLS technique supported by a digital SfM photogrammetry survey. The resulting radiometric information available, such as reflectivity maps, SfM photogrammetry textured models and patterns of geometrical residuals, were interpreted in order to detect and underline surface materials anomalies by a comparison of reflectance and natural colour anomalies. Starting from the 3D models from previous techniques, a 3D ultrasonic tomography on each rock sample was accurately planned and carried out in order to detect internal defects or sample heterogeneity. The integration of the above three geophysical non-invasive techniques with petrographical data-especially with the textural characteristics of such materials-represents a powerful method for the definition of the heterogeneity of the rocks at a different scale and for calibrating in situ measurements.
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页数:20
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