JpGU-AGU Joint Meeting 2020

Presentation information

[E] Oral

M (Multidisciplinary and Interdisciplinary) » M-IS Intersection

[M-IS19] Conservation of geoparks, natural geosites, and cultural heritage: weathering and damage assessment

convener:Luigi Germinario(Saitama University), Celine Schneider(University of Reims-Champagne-Ardenne), Chiaki T. Oguchi(Institute for Environmental Science and Technology, Graduate School of Science and Engineering, Saitama University), Tetsuya Waragai(Graduate School of Science and Engineering, Nihon University), Miguel Gomez-Heras(Universidad Autonoma de Madrid), Patricia Vazquez(GEGENAA EA 3795 University of Reims Champagne-Ardenne), Magdalini Theodoridou(Cardiff University), Wonsuh Song(Waseda University)

[MIS19-04] Study on groundwater quality inside of the Taya cavern

*Chiaki T. Oguchi1, Sohyun Ahn1, Yasuhiko TAMURA2 (1.Institute for Environmental Science and Technology, Graduate School of Science and Engineering, Saitama University, 2.Exective Committee for the prevention of Taya Cavern)

Keywords:Taya Cave, groundwater

The Taya Cave, located in the precincts of Josenji Temple, is registered as one of the region historical properties by Yokohama city. This cave originated from the Kamakura period (13th Century). The Buddhist priests excavated and enlarged it to be about 570 m length and 3 floors. There are 11 dome-shaped spaces with various sizes inside, as well as there are more than 300 bas-reliefs engraving Buddhist murals on the walls and ceilings. However, at present, deterioration and weathering have progressed inside the cave in Taya. Salt precipitation, cracks and peeling are observed. In the present study, the geological properties, local environment and the groundwater quality were analyzed for the purpose of salt origin from the viewpoint of water-rock interaction. The results revealed that the temperature inside the cave is kept almost constant, while the humidity varies depending on the location inside the cave because of seasonal changes such as rainfall. The quality of the groundwater in the cave was also affected by seasonal changes which are shown by time-lag, and by location inside of the cave broadly reflecting the difference in depth of from the earth surface.