JpGU-AGU Joint Meeting 2017

講演情報

[EE] 口頭発表

セッション記号 H (地球人間圏科学) » H-TT 計測技術・研究手法

[H-TT22] [EE] Non destructive techniques applied to stone cultural heritages

2017年5月22日(月) 15:30 〜 17:00 105 (国際会議場 1F)

コンビーナ:小口 千明(埼玉大学大学院理工学研究科)、Celine Elise Thomachot-Schneider(GEGENAA (Groupe d etude des geomateriaux et environnements naturels, anthropiques et arch?ologiques), EA3795, University or Reims (France))、Patricia V?zquez(GEGENAA - Universit? Reims-Champagne-Ardenne)、青木 久(東京学芸大学)、座長:Vazquez patricia(GEGENAA - Université Reims-Champagne-Ardenne)、座長:Schneider Céline(GEGENAA)、座長:青木 久(東京学芸大学)、座長:小口 千明(埼玉大学大学院理工学研究科)

15:30 〜 15:45

[HTT22-01] Close-range remote sensing for monitoring the weathering in wall surfaces of a historical building at Orval Abbey, Belgium

★招待講演

*早川 裕弌1小口 千明2Celine Thomachot-Schneider3Patricia Vázquez3Soizic Gibeaux3 (1.東京大学空間情報科学研究センター、2.埼玉大学、3.ランス大学)

キーワード:TLS, weathering, point cloud, digital elevation model

Monitoring and evaluation of weathering processes of materials in historical buildings are crucial for the maintenance and conservation of such cultural heritage. For this purpose, spatial distribution of the surface condition, including the area, depth, and volume of weathering, should be examined. Detection and quantitative evaluation of changes in the surface condition of rocks have become possible by the availability of terrestrial laser scanning (TLS), and structure-from-motion multi-view stereo (SfM-MVS) photogrammetry approaches. We applied these technologies to the detailed, multi-temporal morphological measurements of a wall surface at a test site in the Orval Abbey, a historical building in Belgium. Time series of the high-definition topographic data including point clouds and digital elevation models (DEMs) were registered to each other, and the millimeter- to centimeter-scale changes were detected for the time periods of the surveys in three years. The changes are most likely induced by salt weathering. The spatial distribution of the surficial changes indicates the spatial variability in the surrounding condition of wetness and temperature, which significantly affects the rate of weathering.