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)

16:30 〜 16:45

[HTT22-05] Application of repeated impacts method of the Schmidt hammer test to coastal cliff surface at Shimane, Japan: evaluation of the degree of weathering

★招待講演

*小暮 哲也1田中 一臣2大平 寛人1仲 優太朗1塚本 崚一1 (1.島根大学大学院総合理工学研究科地球資源環境学領域、2.島根大学総合理工学部地球資源環境学科)

キーワード:Schmidt hammer test, tafoni, rockfall, salt weathering

The processes by which two types of cliff surface develop have been discussed in order to shed light on the mechanism of rockfalls on the Isotake coast of Shimane, Japan. We found that the cause, which differentiates the two types of surface topography, is salt weathering due to the precipitation of calcareous sinter, leading to the development of tafoni formed by small-scale fragmentation of cliff materials. The weathered surface is frequently removed by salt weathering in the tafoni, keeping the surface fresher. This is reflected in the results of the Schmidt hammer rebound test, which clearly distinguish two types of weathered surfaces, with higher rebound values at the surface of the tafoni than at the surface of cliffs without tafoni. Continuous fragmentation of the pyroclastic rock due to the salt weathering by calcareous sinter causes the recession of the coastal cliff, but this fragmentation also keeps the cliff surface relatively intact, preventing rockfall disasters. The analysis of the results of the Schmidt hammer test in this study can be applied to any kind of rock surface, because the condition of the weathered surface was extremely fragile. Data from different kinds of rock with differing degrees of weathering will improve this method and future estimates of the characteristics of weathering determined via the Schmidt hammer test.