Investigation into a Homogenous Rock Slope Response Under Wide Frequency Seismic Loads Using a Large-Scale Shaking Table

preprint OA: closed CC-BY-4.0
📄 Open PDF Full text JSON View at publisher
AI-generated summary by claude@2026-07, 2026-07-17

Shaking table tests on a large-scale rock slope model revealed that acceleration amplification varies with frequency and height, with amplified horizontal motion at the crest and vertical motion at the toe, and nonlinear responses to input amplitude.

One-sentence paraphrase of the abstract; not a substitute for reading it. No clinical advice. How this works

Abstract

Abstract The main objective of this study was to investigate the effect of input earthquake characteristics on the seismic response of a homogenous step-like rock slope. A sequence of shaking table tests was performed in a large-scale physical model with a size of 3.50 m, 0.68 m and 1.20 m in length, width and height, respectively. Results showed that the absolute peak ground acceleration motion amplification factor in horizontal direction (AAF-X) of upper part of the slope was amplified comparison with that at the slope toe while the absolute peak ground acceleration motion amplification factor (AAF-Z) acquired maximum value at the lower position of the slope. With the increasing of the excitation frequencies, the AAF-X around the slope crest increased firstly and then deceased, while the AAF-Z increased continuously. Seismic response of the slope showed strongest amplification when the normalized height of the slope H/λ (ratio of slope height to wavelength) was around 0.2 and AAF-X exhibited a decrease trend when H/λ was larger than 0.2. The AAF showed nonlinear tendency with the increases of the input amplitudes, especially near the shoulder of the slope. This phenomenon can be revealed by the relationship between the calculated resonance frequency or damping ratio of the slope and the amplitude of the input motion. The excitation amplitude has a “double-effect” on the seismic response of a step-like homogeneous rock slope. That is on the one hand, the larger the excitation amplitude, the stronger the acceleration intensity, the greater deterioration of rock slope structure or material and the larger damping ratio of the slope; on the other hand, more energy will be dissipated due to plastic deformation or particle friction of high damping ratio and weaker slope structure. These results could attribute to reveal the dynamic instability mechanism of the homogeneous slope.
Full text 15,995 characters · extracted from preprint-html · click to expand
Investigation into a Homogenous Rock Slope Response Under Wide Frequency Seismic Loads Using a Large-Scale Shaking Table | 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 Investigation into a Homogenous Rock Slope Response Under Wide Frequency Seismic Loads Using a Large-Scale Shaking Table Jianxian He, Zhifa Zhan, Shengwen Qi, Chunlei Li, Bowen Zheng, and 5 more This is a preprint; it has not been peer reviewed by a journal. https://doi.org/ 10.21203/rs.3.rs-770591/v1 This work is licensed under a CC BY 4.0 License Status: Under Review Version 1 posted 6 You are reading this latest preprint version Abstract The main objective of this study was to investigate the effect of input earthquake characteristics on the seismic response of a homogenous step-like rock slope. A sequence of shaking table tests was performed in a large-scale physical model with a size of 3.50 m, 0.68 m and 1.20 m in length, width and height, respectively. Results showed that the absolute peak ground acceleration motion amplification factor in horizontal direction (AAF-X) of upper part of the slope was amplified comparison with that at the slope toe while the absolute peak ground acceleration motion amplification factor (AAF-Z) acquired maximum value at the lower position of the slope. With the increasing of the excitation frequencies, the AAF-X around the slope crest increased firstly and then deceased, while the AAF-Z increased continuously. Seismic response of the slope showed strongest amplification when the normalized height of the slope H/λ (ratio of slope height to wavelength) was around 0.2 and AAF-X exhibited a decrease trend when H/λ was larger than 0.2. The AAF showed nonlinear tendency with the increases of the input amplitudes, especially near the shoulder of the slope. This phenomenon can be revealed by the relationship between the calculated resonance frequency or damping ratio of the slope and the amplitude of the input motion. The excitation amplitude has a “double-effect” on the seismic response of a step-like homogeneous rock slope. That is on the one hand, the larger the excitation amplitude, the stronger the acceleration intensity, the greater deterioration of rock slope structure or material and the larger damping ratio of the slope; on the other hand, more energy will be dissipated due to plastic deformation or particle friction of high damping ratio and weaker slope structure. These results could attribute to reveal the dynamic instability mechanism of the homogeneous slope. Planetary Geology Seismology Seismic response of the slope Wide frequency effect topography effect Shaking table test Resonance effect Full Text Cite Share Download PDF Status: Under Review Version 1 posted Reviewers agreed at journal 24 May, 2022 Reviews received at journal 21 Nov, 2021 Reviewers invited by journal 18 Aug, 2021 Editor invited by journal 11 Aug, 2021 Editor assigned by journal 04 Aug, 2021 First submitted to journal 30 Jul, 2021 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. Our growing team is made up of researchers and industry professionals working together to solve the most critical problems facing scientific publishing. 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-770591","acceptedTermsAndConditions":true,"allowDirectSubmit":false,"archivedVersions":[],"articleType":"Research Article","associatedPublications":[],"authors":[{"id":46744881,"identity":"fa009a19-f748-4a98-9f99-44429f241da6","order_by":0,"name":"Jianxian He","email":"","orcid":"","institution":"Southwest Jiaotong University","correspondingAuthor":false,"submittingAuthor":false,"prefix":"","firstName":"Jianxian","middleName":"","lastName":"He","suffix":""},{"id":46744882,"identity":"e94752e4-3bc7-4cee-b8dd-b7f9ba4d8b17","order_by":1,"name":"Zhifa Zhan","email":"","orcid":"","institution":"China Renewable Energy Engineering Institute","correspondingAuthor":false,"submittingAuthor":false,"prefix":"","firstName":"Zhifa","middleName":"","lastName":"Zhan","suffix":""},{"id":46744883,"identity":"2bb7c95d-1c2c-4292-9f9e-f29ed36fdcda","order_by":2,"name":"Shengwen Qi","email":"data:image/png;base64,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","orcid":"https://orcid.org/0000-0002-0967-7582","institution":"Institute of Geology and Geophysics Chinese Academy of Sciences","correspondingAuthor":true,"submittingAuthor":false,"prefix":"","firstName":"Shengwen","middleName":"","lastName":"Qi","suffix":""},{"id":46744884,"identity":"9980a4b0-87c8-4e8f-868c-0f9b8ab57504","order_by":3,"name":"Chunlei Li","email":"","orcid":"","institution":"IWHR: China Institute of Water Resources and Hydropower Research","correspondingAuthor":false,"submittingAuthor":false,"prefix":"","firstName":"Chunlei","middleName":"","lastName":"Li","suffix":""},{"id":46744885,"identity":"cc43792a-090b-41f3-bc4e-bbeea3930e62","order_by":4,"name":"Bowen Zheng","email":"","orcid":"","institution":"Institute of Geology and Geophysics Chinese Academy of Sciences","correspondingAuthor":false,"submittingAuthor":false,"prefix":"","firstName":"Bowen","middleName":"","lastName":"Zheng","suffix":""},{"id":46744886,"identity":"cb3f87d1-e989-409e-b889-8dd5de7da6f8","order_by":5,"name":"Guoxiang Yang","email":"","orcid":"","institution":"China University of Geosciences","correspondingAuthor":false,"submittingAuthor":false,"prefix":"","firstName":"Guoxiang","middleName":"","lastName":"Yang","suffix":""},{"id":46744887,"identity":"ca945464-47c4-4f38-abd3-62cf300c7bc8","order_by":6,"name":"Songfeng Guo","email":"","orcid":"","institution":"Institute of Geology and Geophysics Chinese Academy of Sciences","correspondingAuthor":false,"submittingAuthor":false,"prefix":"","firstName":"Songfeng","middleName":"","lastName":"Guo","suffix":""},{"id":46744888,"identity":"8be22731-a08c-4f14-9de7-af1d4f4dcbc7","order_by":7,"name":"Xiaolin Huang","email":"","orcid":"","institution":"Institute of Geology and Geophysics Chinese Academy of Sciences","correspondingAuthor":false,"submittingAuthor":false,"prefix":"","firstName":"Xiaolin","middleName":"","lastName":"Huang","suffix":""},{"id":46744889,"identity":"c74f11f2-b7a6-4d8a-bf4a-a3a8294ce681","order_by":8,"name":"Yu Zou","email":"","orcid":"","institution":"Institute of Geology and Geophysics Chinese Academy of Sciences","correspondingAuthor":false,"submittingAuthor":false,"prefix":"","firstName":"Yu","middleName":"","lastName":"Zou","suffix":""},{"id":46744890,"identity":"ea496239-4e4f-42c8-a248-09b34354b8b1","order_by":9,"name":"Ning Liang","email":"","orcid":"","institution":"Institute of Geology and Geophysics Chinese Academy of Sciences","correspondingAuthor":false,"submittingAuthor":false,"prefix":"","firstName":"Ning","middleName":"","lastName":"Liang","suffix":""}],"badges":[],"createdAt":"2021-08-01 08:56:51","currentVersionCode":1,"declarations":"","doi":"10.21203/rs.3.rs-770591/v1","doiUrl":"https://doi.org/10.21203/rs.3.rs-770591/v1","draftVersion":[],"editorialEvents":[],"editorialNote":"","failedWorkflow":false,"files":[{"id":13670228,"identity":"70c4e472-8b5c-40b6-b3df-3931a72d9502","added_by":"auto","created_at":"2021-09-17 11:04:27","extension":"pdf","order_by":1,"title":"","display":"","copyAsset":false,"role":"manuscript-pdf","size":1859791,"visible":true,"origin":"","legend":"","description":"","filename":"MaintextSeismicresponseofarockslopenomark.pdf","url":"https://assets-eu.researchsquare.com/files/rs-770591/v1_covered.pdf"},{"id":12623775,"identity":"12bab3fc-3ffa-4e3a-bf8e-24e9386a6242","added_by":"auto","created_at":"2021-08-20 20:10:16","extension":"pdf","order_by":1,"title":"","display":"","copyAsset":false,"role":"manuscript-pdf","size":1855909,"visible":true,"origin":"","legend":"","description":"","filename":"MaintextSeismicresponseofarockslopenomark.pdf","url":"https://assets-eu.researchsquare.com/files/rs-770591/v1_covered.pdf"}],"financialInterests":"","formattedTitle":"\u003cp\u003eInvestigation into a Homogenous Rock Slope Response Under Wide Frequency Seismic Loads Using a Large-Scale Shaking Table\u003c/p\u003e","fulltext":[{"header":"Full Text","content":"This preprint is available for \u003ca href='/article/rs-770591/latest.pdf' target='_blank'\u003edownload as a PDF\u003c/a\u003e."}],"fulltextSource":"","fullText":"","funders":[],"hasAdminPriorityOnWorkflow":false,"hasManuscriptDocX":false,"hasOptedInToPreprint":true,"hasPassedJournalQc":"","hasAnyPriority":false,"hideJournal":false,"highlight":"","institution":"","isAcceptedByJournal":true,"isAuthorSuppliedPdf":true,"isDeskRejected":"","isHiddenFromSearch":false,"isInQc":false,"isInWorkflow":false,"isPdf":false,"isPdfUpToDate":true,"isWithdrawnOrRetracted":false,"journal":{"display":true,"email":"[email protected]","identity":"natural-hazards","isNatureJournal":false,"hasQc":true,"allowDirectSubmit":false,"externalIdentity":"nhaz","sideBox":"Learn more about [Natural Hazards](https://www.springer.com/journal/11069)","snPcode":"11069","submissionUrl":"https://submission.nature.com/new-submission/11069/3","title":"Natural Hazards","twitterHandle":"","acdcEnabled":true,"dfaEnabled":true,"editorialSystem":"em","reportingPortfolio":"Springer Hybrid","inReviewEnabled":true,"inReviewRevisionsEnabled":false},"keywords":"Seismic response of the slope, Wide frequency effect, topography effect, Shaking table test, Resonance effect","lastPublishedDoi":"10.21203/rs.3.rs-770591/v1","lastPublishedDoiUrl":"https://doi.org/10.21203/rs.3.rs-770591/v1","license":{"name":"CC BY 4.0","url":"https://creativecommons.org/licenses/by/4.0/"},"manuscriptAbstract":"\u003cp\u003eThe main objective of this study was to investigate the effect of input earthquake characteristics on the seismic response of a homogenous step-like rock slope. A sequence of shaking table tests was performed in a large-scale physical model with a size of 3.50 m, 0.68 m and 1.20 m in length, width and height, respectively. Results showed that the absolute peak ground acceleration motion amplification factor in horizontal direction (AAF-X) of upper part of the slope was amplified comparison with that at the slope toe while the absolute peak ground acceleration motion amplification factor (AAF-Z) acquired maximum value at the lower position of the slope. With the increasing of the excitation frequencies, the AAF-X around the slope crest increased firstly and then deceased, while the AAF-Z increased continuously. Seismic response of the slope showed strongest amplification when the normalized height of the slope \u003cem\u003eH/λ \u003c/em\u003e(ratio of slope height to wavelength)\u003cem\u003e \u003c/em\u003ewas around 0.2 and AAF-X exhibited a decrease trend when \u003cem\u003eH/λ\u003c/em\u003e was larger than 0.2. The AAF showed nonlinear tendency with the increases of the input amplitudes, especially near the shoulder of the slope. This phenomenon can be revealed by the relationship between the calculated resonance frequency or damping ratio of the slope and the amplitude of the input motion. The excitation amplitude has a “double-effect” on the seismic response of a step-like homogeneous rock slope. That is on the one hand, the larger the excitation amplitude, the stronger the acceleration intensity, the greater deterioration of rock slope structure or material and the larger damping ratio of the slope; on the other hand, more energy will be dissipated due to plastic deformation or particle friction of high damping ratio and weaker slope structure. These results could attribute to reveal the dynamic instability mechanism of the homogeneous slope.\u003c/p\u003e","manuscriptTitle":"Investigation into a Homogenous Rock Slope Response Under Wide Frequency Seismic Loads Using a Large-Scale Shaking Table","msid":"","msnumber":"","nonDraftVersions":[{"code":1,"date":"2021-08-20 20:10:06","doi":"10.21203/rs.3.rs-770591/v1","editorialEvents":[{"type":"communityComments","content":0},{"type":"reviewerAgreed","content":"","date":"2022-05-24T07:18:38+00:00","index":0,"fulltext":""},{"type":"editorInvitedReview","content":"","date":"2021-11-21T12:07:59+00:00","index":0,"fulltext":""},{"type":"reviewersInvited","content":"","date":"2021-08-18T08:55:38+00:00","index":"","fulltext":""},{"type":"editorInvited","content":"Natural Hazards","date":"2021-08-11T05:40:24+00:00","index":"","fulltext":""},{"type":"editorAssigned","content":"","date":"2021-08-04T05:42:38+00:00","index":"","fulltext":""},{"type":"submitted","content":"Natural Hazards","date":"2021-07-31T00:58:49+00:00","index":"","fulltext":""}],"status":"published","journal":{"display":true,"email":"[email protected]","identity":"natural-hazards","isNatureJournal":false,"hasQc":true,"allowDirectSubmit":false,"externalIdentity":"nhaz","sideBox":"Learn more about [Natural Hazards](https://www.springer.com/journal/11069)","snPcode":"11069","submissionUrl":"https://submission.nature.com/new-submission/11069/3","title":"Natural Hazards","twitterHandle":"","acdcEnabled":true,"dfaEnabled":true,"editorialSystem":"em","reportingPortfolio":"Springer Hybrid","inReviewEnabled":true,"inReviewRevisionsEnabled":false}}],"origin":"","ownerIdentity":"5ee7b51e-374d-47d7-bf24-f1e1e1047350","owner":[],"postedDate":"August 20th, 2021","published":true,"recentEditorialEvents":[],"rejectedJournal":[],"revision":"","amendment":"","status":"under-review","subjectAreas":[{"id":6605857,"name":"Planetary Geology"},{"id":6605858,"name":"Seismology"}],"tags":[],"updatedAt":"2022-12-12T13:05:21+00:00","versionOfRecord":[],"versionCreatedAt":"2021-08-20 20:10:06","video":"","vorDoi":"","vorDoiUrl":"","workflowStages":[]},"version":"v1","identity":"rs-770591","journalConfig":"researchsquare"},"__N_SSP":true},"page":"/article/[identity]/[[...version]]","query":{"redirect":"/article/rs-770591","identity":"rs-770591","version":["v1"]},"buildId":"FbvkV6FR0MCFSLy54lSbu","isFallback":false,"isExperimentalCompile":false,"dynamicIds":[84888],"gssp":true,"scriptLoader":[]}

Text is read by the "Ask this paper" AI Q&A widget below. Extraction quality varies by source — PMC NXML preserves structure cleanly, OA-HTML may include some navigation residue, and OA-PDF can have broken hyphenation. The publisher copy (via DOI) is the canonical version.

My notes (saved in your browser only)

Ask this paper AI returns verbatim quotes from the full text · source: preprint-html

Answers must be backed by verbatim quotes from this paper's full text. Hallucinated quotes are dropped automatically; if no verbatim passage answers the question, we say so. How this works

Citation neighborhood (no data yet)

We don't have any in-corpus citations linked to this paper yet. The paper's references may be in our DB but unresolved to ``paper_id`` (resolution happens at ingest when the cited DOI matches a row we already have). Run the cross-source citation reconcile pass to retry.

Source provenance

europepmc
last seen: 2026-05-19T01:45:01.086888+00:00
unpaywall
last seen: 2026-06-04T02:00:05.705006+00:00
License: CC-BY-4.0