Japan Geoscience Union Meeting 2021

Presentation information

[J] Oral

S (Solid Earth Sciences ) » S-VC Volcanology

[S-VC28] Active Volcanism

Sat. Jun 5, 2021 10:45 AM - 11:30 AM Ch.25 (Zoom Room 25)

convener:Yuta Maeda(Nagoya University), Takahiro Miwa(National research institute for earth science and disaster prevention), Takeshi Matsushima(Institute of Seismology and Volcanology, Faculty of Science, Kyushu University), Chairperson:Urumu Tsunogai(Graduate School of Environmental Studies, Nagoya University), Takeshi Ohba(Department of chemistry, School of Science, Tokia University)

11:15 AM - 11:30 AM

[SVC28-27] Development of an automatic volcanic plume sampler SelPS for UAS

*Urumu Tsunogai1, Ryo Shingubara1, Masanori Ito1, Yuhei Morishita1, Fumiko Nakagawa1, Shin Yoshikawa2, Mitsuru Utsugi2, Akihiko Yokoo2 (1.Graduate School of Environmental Studies, Nagoya University, 2.Graduate School of Science, Kyoto University)

Keywords:fumarolic gases, volcanic plume, carbon dioxide, Unoccupied Aerial Systems, automatic volcanic plume sampler

Both chemical and isotopic compositions of volcanic plumes are highly useful in evaluating the present status of active volcanoes. Monitoring their temporal changes can facilitate the forecasts of volcanic activity as well. In the present study, we developed a drone-borne automatic sampler for volcanic plumes in which an output signal from a sulfur dioxide (SO2) sensor triggered a pump to collect samples when its SO2 concentration exceeded a predefined threshold. We fitted the sampler on a drone at Nakadake central cone, Aso volcano, Japan, where only the crater rim was accessible.

In the sampling campaign done on October 2020, good consistency in isotope ratios (2H/1H) of molecular hydrogen (H2) between samples collected by the automatic sampler and those collected directly into pre-evacuated flasks was obtained. Furthermore, by using the drone-borne sampler at Aso volcano, we obtained plume samples with much higher concentrations of H2 and carbon dioxide (CO2) than those taken directly into flasks at the crater rim. Our sampler can be utilized to collect volcanic plume samples for the determination of stable isotopic compositions in general by subsequent laboratory analysis and the remote establishment of fumarole outlet temperature based on the 2H/1H ratios of hydrogen, including their temporal changes. This study was supported by MEXT Integrated Program for Next Generation Volcano Research and Human Resource Development (Theme B).