Japan Geoscience Union Meeting 2015

Presentation information


Symbol B (Biogeosciences) » B-GM Geomicrobiology

[B-GM22] Microbial ecology in earth and planetary sciences

Tue. May 26, 2015 9:00 AM - 10:45 AM 105 (1F)

Convener:*Michinari Sunamura(University of Tokyo Dept. of Earth & Planetary Science), Ken Takai(Extremobiosphere Research Center, Japan Agency for Marine-Earth Science & Technology), Keisuke Koba(Tokyo University of Agriculture and Technology), Natsuko Hamamura(Ehime University), Chair:Takuro Nunoura(Research and Development Center for Marine Biosciences, Japan Agency for Marine-Earth Science & Technology (JAMSTEC)), Michinari Sunamura(University of Tokyo)

9:00 AM - 9:15 AM

[BGM22-01] Multiple analyses to chase the signature of direct impact of rainfall into groundwater in Mt. Fuji

Ayumi SUGIYAMA1, Kazuyo NAGAOSA1, *Kenji KATO1 (1.Shizuoka University, Graduate School of Science)

Keywords:groundwater, strong rainfall, abnormal flash out

A huge amount of groundwater is stored in subsurface environment of Mt. Fuji, the largest volcanic (basalt) mountain in Japan. There distribute many springs flushing out between lava (high permeability) and underlying older lava (low permeability) at various points of the foot. Based on the concept of piston flow transport an apparent residence time was estimated to ca. 30 years by 36Cl/Cl ratio (Tosaki et al., 2011). However, this number represents an averaged value of the residence time of groundwater mixed before flushing out. On the other hand, we found that pH of spring water in the lower part of the foot of Mt. Fuji decreased shortly after the typhoon in August 2011 which suggested the newly supplied rainwater was mixed into groundwater. Thus, we try to chase signature of direct impact of rainfall into groundwater from multiple analyses to elucidate the routes of groundwater under the torrential rainfall. Though analyses of groundwater chemistry show just an averaged value, microbial DNA analysis could suggest the routes of transport; if thermophilic microbial DNA is detected this suggests at least a part of groundwater must originated from the environment >ca. 40oC (=600 m deep in Mt. Fuji). Thus, we employed three different tracers; stable isotopic analysis (δ18O and δD), chemical analysis (concentration of silica) and microbial DNA analysis.
Stable oxygen isotopic ratio of shallow groundwater became higher than usual value reflecting torrential rainfall and the concentration of silica decreased after the torrential rainfall amounting more than 300 mm. In addition, the density of Prokaryotes in shallow groundwater apparently increased. These findings indicate a direct impact of rainfall into groundwater was observed after torrential rainfall with more than 300 mm in the studied geological setting. This did not appear when rainfall did not exceed 100 mm/day. Increase in the density of Archaea at deep groundwater after the torrential rainfall suggests a possible mixing of deep groundwater which was pushed by piston flow transport as an indirect impact of rainfall into deep groundwater, if it is true to this geological setting that Archaea is predominant in deep subsurface environment as was suggested. Microbial DNA can give possible information about the route of groundwater.