Tilt and self-potential observations of Kibedani Geyser, Japan: Relationship between fluid flow and CO2-driven geyser activity | Research Square window.SnipcartSettings = { analytics: { enabled: false } }; (function() { var accessVector = localStorage.getItem('access_vector') || ''; window.dataLayer = window.dataLayer || []; if (accessVector) { window.dataLayer.push({ user: { profile: { profileInfo: { snid: accessVector } } } }); } })(); (function(w,d,s,l,i){w[l]=w[l]||[];w[l].push({'gtm.start':new Date().getTime(),event:'gtm.js'});var f=d.getElementsByTagName(s)[0],j=d.createElement(s),dl=l!='dataLayer'?'&l='+l:'';j.async=true;j.src='https://www.googletagmanager.com/gtm.js?id='+i+dl;f.parentNode.insertBefore(j,f);})(window,document,'script','dataLayer','GTM-K279D39R'); Browse Preprints In Review Journals COVID-19 Preprints AJE Video Bytes Research Tools Research Promotion AJE Professional Editing AJE Rubriq About Preprint Platform In Review Editorial Policies Our Team Advisory Board Help Center Sign In Submit a Preprint Cite Share Download PDF Article Tilt and self-potential observations of Kibedani Geyser, Japan: Relationship between fluid flow and CO2-driven geyser activity Harutou Tanabe, Koki Aizawa, Takeshi Matsushima This is a preprint; it has not been peer reviewed by a journal. https://doi.org/ 10.21203/rs.3.rs-4617698/v1 This work is licensed under a CC BY 4.0 License Status: Published Journal Publication published 31 May, 2025 Read the published version in Scientific Reports → Version 1 posted 10 You are reading this latest preprint version Abstract Multi-parameter, multi-site observations were undertaken at the Kibedani Geyser, Japan, where the eruption of cold spring-water (20℃) is driven by underground CO2 pressure. Video, temperature, self-potential (SP), ground tilt, and acoustic observations were undertaken. Tilt and SP data display temporal changes related to the geyser cycle of 38 min (32 min between eruptions, with 6 min of eruption). Tilt data indicate that an inclined crack-shaped cavity pressure source expands between eruptions and contracts during eruption, with post-eruption re-expansion beginning ~2.5 min after eruption, when ground tremor has ceased. SP changes suggest groundwater inflow to the pressure source. We conclude that CO2 accumulates in the cavity, uplifting water for eruption. Tilt and SP multi-site observations were effective in estimating fluid flows associated with geyser activity. Earth and environmental sciences/Solid earth sciences Earth and environmental sciences/Solid earth sciences/Geophysics Earth and environmental sciences/Solid earth sciences/Volcanology geyser electric self-potential tilt CO2 groundwater flow Full Text Additional Declarations No competing interests reported. Supplementary Files MovieS1.mp4 Supplementary.docx Cite Share Download PDF Status: Published Journal Publication published 31 May, 2025 Read the published version in Scientific Reports → Version 1 posted Editorial decision: Revision requested 04 Sep, 2024 Reviews received at journal 18 Aug, 2024 Reviewers agreed at journal 22 Jul, 2024 Reviews received at journal 19 Jul, 2024 Reviewers agreed at journal 15 Jul, 2024 Reviewers invited by journal 14 Jul, 2024 Editor assigned by journal 11 Jul, 2024 Editor invited by journal 25 Jun, 2024 Submission checks completed at journal 24 Jun, 2024 First submitted to journal 21 Jun, 2024 You are reading this latest preprint version Research Square lets you share your work early, gain feedback from the community, and start making changes to your manuscript prior to peer review in a journal. As a division of Research Square Company, we’re committed to making research communication faster, fairer, and more useful. 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