Analysis of infrasound signals generated by quarry blasts | 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 Research Article Analysis of infrasound signals generated by quarry blasts Ulrike Mitterbauer, Ewald Brückl, Peter Carniel, Stefan Mertl This is a preprint; it has not been peer reviewed by a journal. https://doi.org/ 10.21203/rs.3.rs-8260268/v1 This work is licensed under a CC BY 4.0 License Status: Under Review Version 1 posted 9 You are reading this latest preprint version Abstract The ISCO infrasound array has been installed at the Conrad Observatory (Austria, ~ 50 km SSW Vienna) since January 2021. Among the signals detected, regularly recurring signals can be attributed to blasting in a limestone quarry located ~ 16 km away. The characteristic signal shape and the availability of blasting data provided a basis for an in-depth analysis of these signals. We consider the interaction of the rock mass set in motion by an explosion with the atmosphere to be the source of the signals. We derive the kinematics of the blasted rock masses, in particular the change in volume, from photogrammetric documentation of the deposits and numerical modeling of the ejection process. We limit ourselves to 1D modeling of the blasts as an infrasound source, since the dominant wavelength of the signal, at ~ 500 m, is a factor of 10 greater than the dimensions of the blasted rock masses. A source function based on the ‘vibrating sphere’ model in conjunction with a transfer function corresponding to reverberation allows excellent modeling of the signal shape. As the cause of the reverberation, we present an analogy between the shape and acoustics of classical amphitheaters and the shape of the open-cast mine and its possible acoustic effectiveness. The amplitude of the source function based on the ‘vibrating sphere’ model correlates very well with the total amount of explosives used in a blast (R2 = 0.87). There is considerable variation between these two parameters and the peak-to-peak amplitude of the infrasound signal (R2 = 0.37). Infrasound blasting photogrammetry numerical modeling. Green’s function reverberation Full Text Additional Declarations No competing interests reported. Supplementary Files SupplementDec25.docx Cite Share Download PDF Status: Under Review Version 1 posted Editorial decision: Revision requested 30 Jan, 2026 Reviews received at journal 29 Jan, 2026 Reviews received at journal 15 Jan, 2026 Reviewers agreed at journal 11 Jan, 2026 Reviewers agreed at journal 06 Jan, 2026 Reviewers invited by journal 10 Dec, 2025 Editor assigned by journal 03 Dec, 2025 Submission checks completed at journal 03 Dec, 2025 First submitted to journal 02 Dec, 2025 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. We do this by developing innovative software and high quality services for the global research community. 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Also discoverable on Platform About Our Team In Review Editorial Policies Advisory Board Help Center Resources Author Services Accessibility API Access RSS feed Manage Cookie Preferences © Research Square 2026 | ISSN 2693-5015 (online) Privacy Policy Terms of Service Do Not Sell My Personal Information {"props":{"pageProps":{"initialData":{"identity":"rs-8260268","acceptedTermsAndConditions":true,"allowDirectSubmit":false,"archivedVersions":[],"articleType":"Research Article","associatedPublications":[],"authors":[{"id":559906750,"identity":"b4c2538a-4436-4a17-af3a-6852da82a823","order_by":0,"name":"Ulrike 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[email protected]","identity":"pure-and-applied-geophysics","isNatureJournal":false,"hasQc":true,"allowDirectSubmit":false,"externalIdentity":"paag","sideBox":"Learn more about [Pure and Applied Geophysics](https://www.springer.com/journal/24)","snPcode":"24","submissionUrl":"https://submission.nature.com/new-submission/24/3","title":"Pure and Applied Geophysics","twitterHandle":"","acdcEnabled":true,"dfaEnabled":true,"editorialSystem":"em","reportingPortfolio":"Springer Hybrid","inReviewEnabled":true,"inReviewRevisionsEnabled":false},"keywords":"Infrasound, blasting, photogrammetry, numerical modeling. Green’s function, reverberation","lastPublishedDoi":"10.21203/rs.3.rs-8260268/v1","lastPublishedDoiUrl":"https://doi.org/10.21203/rs.3.rs-8260268/v1","license":{"name":"CC BY 4.0","url":"https://creativecommons.org/licenses/by/4.0/"},"manuscriptAbstract":"\u003cp\u003eThe ISCO infrasound array has been installed at the Conrad Observatory (Austria, ~\u0026thinsp;50 km SSW Vienna) since January 2021. Among the signals detected, regularly recurring signals can be attributed to blasting in a limestone quarry located\u0026thinsp;~\u0026thinsp;16 km away. The characteristic signal shape and the availability of blasting data provided a basis for an in-depth analysis of these signals.\u003c/p\u003e\u003cp\u003eWe consider the interaction of the rock mass set in motion by an explosion with the atmosphere to be the source of the signals. We derive the kinematics of the blasted rock masses, in particular the change in volume, from photogrammetric documentation of the deposits and numerical modeling of the ejection process. We limit ourselves to 1D modeling of the blasts as an infrasound source, since the dominant wavelength of the signal, at ~\u0026thinsp;500 m, is a factor of 10 greater than the dimensions of the blasted rock masses. A source function based on the \u0026lsquo;vibrating sphere\u0026rsquo; model in conjunction with a transfer function corresponding to reverberation allows excellent modeling of the signal shape. As the cause of the reverberation, we present an analogy between the shape and acoustics of classical amphitheaters and the shape of the open-cast mine and its possible acoustic effectiveness.\u003c/p\u003e\u003cp\u003eThe amplitude of the source function based on the \u0026lsquo;vibrating sphere\u0026rsquo; model correlates very well with the total amount of explosives used in a blast (R2\u0026thinsp;=\u0026thinsp;0.87). There is considerable variation between these two parameters and the peak-to-peak amplitude of the infrasound signal (R2\u0026thinsp;=\u0026thinsp;0.37).\u003c/p\u003e","manuscriptTitle":"Analysis of infrasound signals generated by quarry blasts","msid":"","msnumber":"","nonDraftVersions":[{"code":1,"date":"2025-12-15 09:55:14","doi":"10.21203/rs.3.rs-8260268/v1","editorialEvents":[{"type":"communityComments","content":0},{"type":"decision","content":"Revision requested","date":"2026-01-30T15:13:22+00:00","index":"","fulltext":""},{"type":"editorInvitedReview","content":"","date":"2026-01-29T20:04:25+00:00","index":"hide","fulltext":""},{"type":"editorInvitedReview","content":"","date":"2026-01-15T14:28:53+00:00","index":"hide","fulltext":""},{"type":"reviewerAgreed","content":"235878360846048641076077169942622947777","date":"2026-01-11T23:11:10+00:00","index":"hide","fulltext":""},{"type":"reviewerAgreed","content":"34288568560286179290955929728752953994","date":"2026-01-06T10:44:16+00:00","index":"hide","fulltext":""},{"type":"reviewersInvited","content":"","date":"2025-12-10T10:11:57+00:00","index":"","fulltext":""},{"type":"editorAssigned","content":"","date":"2025-12-03T14:03:07+00:00","index":"","fulltext":""},{"type":"checksComplete","content":"","date":"2025-12-03T06:50:06+00:00","index":"","fulltext":""},{"type":"submitted","content":"Pure and Applied Geophysics","date":"2025-12-02T11:55:55+00:00","index":"","fulltext":""}],"status":"published","journal":{"display":true,"email":"
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