An innovative methodology for the non-destructive diagnosis of architectural elements of ancient historical buildings

被引:44
作者
Fais, Silvana [1 ]
Casula, Giuseppe [2 ]
Cuccuru, Francesco [1 ]
Ligas, Paola [1 ]
Bianchi, Maria Giovanna [2 ]
机构
[1] Univ Cagliari, Dept Civil & Environm Engn & Architecture DICAAR, I-09123 Cagliari, Italy
[2] Ist Nazl Geofis & Vulcanol, Sez Bologna, Via Donato Creti 12, I-40128 Bologna, Italy
来源
SCIENTIFIC REPORTS | 2018年 / 8卷
关键词
CARBONATE ROCKS; RECONSTRUCTION; THERMOGRAPHY; REGISTRATION; VELOCITY;
D O I
10.1038/s41598-018-22601-5
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
In the following we present a new non-invasive methodology aimed at the diagnosis of stone building materials used in historical buildings and architectural elements. This methodology consists of the integrated sequential application of in situ proximal sensing methodologies such as the 3D Terrestrial Laser Scanner for the 3D modelling of investigated objects together with laboratory and in situ non-invasive multi-techniques acoustic data, preceded by an accurate petrographical study of the investigated stone materials by optical and scanning electron microscopy. The increasing necessity to integrate different types of techniques in the safeguard of the Cultural Heritage is the result of the following two interdependent factors: 1) The diagnostic process on the building stone materials of monuments is increasingly focused on difficult targets in critical situations. In these cases, the diagnosis using only one type of non-invasive technique may not be sufficient to investigate the conservation status of the stone materials of the superficial and inner parts of the studied structures 2) Recent technological and scientific developments in the field of non-invasive diagnostic techniques for different types of materials favors and supports the acquisition, processing and interpretation of huge multidisciplinary datasets.
引用
收藏
页数:11
相关论文
共 34 条
[1]  
Abbaneo S, 1995, P INT S NOND TEST CI, P253
[2]   Velocity variations in carbonate rocks due to dual porosity and wave-induced fluid flow [J].
Agersborg, Remy ;
Johansen, Tor Arne ;
Jakobsen, Morten .
GEOPHYSICAL PROSPECTING, 2009, 57 (01) :81-98
[3]  
[Anonymous], 2001, GEOLOGIA SARDEGNA NO
[4]   A METHOD FOR REGISTRATION OF 3-D SHAPES [J].
BESL, PJ ;
MCKAY, ND .
IEEE TRANSACTIONS ON PATTERN ANALYSIS AND MACHINE INTELLIGENCE, 1992, 14 (02) :239-256
[5]   CARBONATE LITHOFACIES AS PALEOLATITUDE INDICATORS - PROBLEMS AND LIMITATIONS [J].
CARANNANTE, G ;
ESTEBAN, M ;
MILLIMAN, JD ;
SIMONE, L .
SEDIMENTARY GEOLOGY, 1988, 60 (1-4) :333-346
[6]  
Casula Giuseppe, 2009, International Journal of Microstructure and Materials Properties, V4, P45, DOI 10.1504/IJMMP.2009.028432
[7]  
Cherchi A., 1974, Memoires Bur Rech geol minier, VNo. 78, P433
[8]  
CHOQUETTE PW, 1970, AM ASSOC PETR GEOL B, V54, P207
[9]  
CNR-ICR, 1986, NORM 22 86 MIS VEL P
[10]  
Concu G., 2003, P 3 INT C NOND TEST, P104