An Analysis of Vertical Infiltration Responses in Unsaturated Soil Columns

preprint OA: closed
Full text JSON View at publisher
Full text 12,021 characters · extracted from preprint-html · click to expand
An Analysis of Vertical Infiltration Responses in Unsaturated Soil Columns | 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 An Analysis of Vertical Infiltration Responses in Unsaturated Soil Columns Lincui Li, Cheng Li, Xi-An Li, Yonghong Li, Yong Li, Yiping He, and 2 more This is a preprint; it has not been peer reviewed by a journal. https://doi.org/ 10.21203/rs.3.rs-4943413/v1 This work is licensed under a CC BY 4.0 License Status: Posted Version 1 posted You are reading this latest preprint version Abstract Rainfall infiltration affects slope stability by changing the pore water pressure in soil. In this study, indoor vertical infiltration tests were performed on silt columns. The instantaneous profile method and filter paper method were used to obtain the soil water characteristic curve (SWCC) and hydraulic conductivity function(HCF). During the rainfall infiltration test, the vertical patters of volumetric moisture contents, total hydraulic head or suction and the wetting front were recorded. Advancing displacement and rate of the wetting front, the cumulative infiltration, the instantaneous infiltration rate, the average infiltration rate were determined to assess rainfall infiltration process comprehensively, combining with SWCC and HCF. Additionally, the effects of dry density and runoff on the one-dimensional (1D) vertical infiltration process of soil columns were evaluated. The results showed that the variation curve of the wetting front displacement versus time obeys a power function relationship, the infiltration rate–time relationship curve and the unsaturated permeability curve could be roughly divided into three stages, and the SWCC and HCF calculated by volumetric moisture content are more sensitive to changes in dry density than to changes in runoff or hydraulic head height. Physical sciences/Engineering/Civil engineering Earth and environmental sciences/Hydrology Horizontal infiltration Soil–water characteristic curve Soil moisture profile Hydraulic conductivity Pore water pressure Rainfall Full Text Additional Declarations No competing interests reported. Cite Share Download PDF Status: Posted Version 1 posted 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-4943413","acceptedTermsAndConditions":true,"allowDirectSubmit":true,"archivedVersions":[],"articleType":"Article","associatedPublications":[],"authors":[{"id":356899389,"identity":"1db7f13d-3f48-4b52-a0d4-b17bf699fd43","order_by":0,"name":"Lincui Li","email":"data:image/png;base64,iVBORw0KGgoAAAANSUhEUgAAAZAAAAAyAQMAAABI0h/eAAAABlBMVEX///8AAABVwtN+AAAACXBIWXMAAA7EAAAOxAGVKw4bAAAA/ElEQVRIie3NMWrDMBTGcQmBvLwmq4yLewUVrYZcoIfQI5ApQ6bQrTICZ2l3h16iUOjs1BAvbmYNXbJ4TvHSqTSZW+R066A/fMuDH4+QUOgfNmZ09alvMxhHtmKEH0/VAIlX1ohDO0vj+60+j8i2MfG6eFXS3cjzCHFoFPAKjYOPfrEk6chp2i88gpZopgDvmD8+PCfljqjYaZaUHsIEmhpEh/by7YVdFASfnOYMPIQLzC3IGgsx707kbpAAbCwtda1AzPmJaDlERJQX5FDNUgFblcBOXK/bvU18ZFJHHcGvDCaN3fewzK5GzXTT+8iPr8dR8wcQCoVCod/6Bpe+T/7NdT8pAAAAAElFTkSuQmCC","orcid":"","institution":"Shaanxi Geological Environment Monitoring Station","correspondingAuthor":true,"prefix":"","firstName":"Lincui","middleName":"","lastName":"Li","suffix":""},{"id":356899390,"identity":"91465191-2775-4703-b59c-0c2cb6285590","order_by":1,"name":"Cheng Li","email":"","orcid":"","institution":"Shaanxi Geological Environment Monitoring Station","correspondingAuthor":false,"prefix":"","firstName":"Cheng","middleName":"","lastName":"Li","suffix":""},{"id":356899391,"identity":"e66e0b22-d5ab-42d4-ade0-f6226ef64202","order_by":2,"name":"Xi-An Li","email":"","orcid":"","institution":"Chang'an University","correspondingAuthor":false,"prefix":"","firstName":"Xi-An","middleName":"","lastName":"Li","suffix":""},{"id":356899392,"identity":"d7ef2b11-b99e-4499-aacf-86c5c5ed9efc","order_by":3,"name":"Yonghong Li","email":"","orcid":"","institution":"Shaanxi Geological Environment Monitoring Station","correspondingAuthor":false,"prefix":"","firstName":"Yonghong","middleName":"","lastName":"Li","suffix":""},{"id":356899393,"identity":"dba8e1e6-1392-4776-9e8a-7d709ef68f14","order_by":4,"name":"Yong Li","email":"","orcid":"","institution":"Shaanxi Geological Environment Monitoring Station","correspondingAuthor":false,"prefix":"","firstName":"Yong","middleName":"","lastName":"Li","suffix":""},{"id":356899394,"identity":"8f039f16-d192-4528-bbc4-f3ff4b3f6cda","order_by":5,"name":"Yiping He","email":"","orcid":"","institution":"Shaanxi Geological Environment Monitoring Station","correspondingAuthor":false,"prefix":"","firstName":"Yiping","middleName":"","lastName":"He","suffix":""},{"id":356899395,"identity":"71608524-ce86-4d40-9d63-ba0976172218","order_by":6,"name":"Chaowei Yao","email":"","orcid":"","institution":"Shaanxi Geological Environment Monitoring Station","correspondingAuthor":false,"prefix":"","firstName":"Chaowei","middleName":"","lastName":"Yao","suffix":""},{"id":356899398,"identity":"b5dcaa08-36f6-471a-8026-5740863a30f1","order_by":7,"name":"Li Wang","email":"","orcid":"","institution":"Xi'an University of Science and Technology","correspondingAuthor":false,"prefix":"","firstName":"Li","middleName":"","lastName":"Wang","suffix":""}],"badges":[],"createdAt":"2024-08-20 08:44:27","currentVersionCode":1,"declarations":"","doi":"10.21203/rs.3.rs-4943413/v1","doiUrl":"https://doi.org/10.21203/rs.3.rs-4943413/v1","draftVersion":[],"editorialEvents":[],"editorialNote":"","failedWorkflow":false,"files":[{"id":65820850,"identity":"b0650fb3-5147-432c-b203-dbf02cdf2fdc","added_by":"auto","created_at":"2024-10-03 07:32:02","extension":"pdf","order_by":1,"title":"","display":"","copyAsset":false,"role":"manuscript-pdf","size":1710195,"visible":true,"origin":"","legend":"","description":"","filename":"ManuscriptScientificReports.pdf","url":"https://assets-eu.researchsquare.com/files/rs-4943413/v1_covered_530c943b-99f9-4f3a-903e-d8ebb647ac42.pdf"}],"financialInterests":"No competing interests reported.","formattedTitle":"An Analysis of Vertical Infiltration Responses in Unsaturated Soil Columns","fulltext":[],"fulltextSource":"","fullText":"","funders":[],"hasAdminPriorityOnWorkflow":false,"hasManuscriptDocX":false,"hasOptedInToPreprint":true,"hasPassedJournalQc":"","hasAnyPriority":false,"hideJournal":true,"highlight":"","institution":"","isAcceptedByJournal":false,"isAuthorSuppliedPdf":true,"isDeskRejected":"","isHiddenFromSearch":false,"isInQc":false,"isInWorkflow":false,"isPdf":true,"isPdfUpToDate":true,"isWithdrawnOrRetracted":false,"journal":{"display":true,"email":"[email protected]","identity":"researchsquare","isNatureJournal":false,"hasQc":true,"allowDirectSubmit":true,"externalIdentity":"","sideBox":"","snPcode":"","submissionUrl":"/submission","title":"Research Square","twitterHandle":"researchsquare","acdcEnabled":true,"dfaEnabled":false,"editorialSystem":"","reportingPortfolio":"","inReviewEnabled":false,"inReviewRevisionsEnabled":true},"keywords":"Horizontal infiltration, Soil–water characteristic curve, Soil moisture profile, Hydraulic conductivity, Pore water pressure, Rainfall","lastPublishedDoi":"10.21203/rs.3.rs-4943413/v1","lastPublishedDoiUrl":"https://doi.org/10.21203/rs.3.rs-4943413/v1","license":{"name":"CC BY 4.0","url":"https://creativecommons.org/licenses/by/4.0/"},"manuscriptAbstract":"\u003cp\u003eRainfall infiltration affects slope stability by changing the pore water pressure in soil. In this study, indoor vertical infiltration tests were performed on silt columns. The instantaneous profile method and filter paper method were used to obtain the soil water characteristic curve (SWCC) and hydraulic conductivity function(HCF). During the rainfall infiltration test, the vertical patters of volumetric moisture contents, total hydraulic head or suction and the wetting front were recorded. Advancing displacement and rate of the wetting front, the cumulative infiltration, the instantaneous infiltration rate, the average infiltration rate were determined to assess rainfall infiltration process comprehensively, combining with SWCC and HCF. Additionally, the effects of dry density and runoff on the one-dimensional (1D) vertical infiltration process of soil columns were evaluated. The results showed that the variation curve of the wetting front displacement versus time obeys a power function relationship, the infiltration rate–time relationship curve and the unsaturated permeability curve could be roughly divided into three stages, and the SWCC and HCF calculated by volumetric moisture content are more sensitive to changes in dry density than to changes in runoff or hydraulic head height.\u003c/p\u003e","manuscriptTitle":"An Analysis of Vertical Infiltration Responses in Unsaturated Soil Columns","msid":"","msnumber":"","nonDraftVersions":[{"code":1,"date":"2024-09-27 07:58:04","doi":"10.21203/rs.3.rs-4943413/v1","editorialEvents":[{"type":"communityComments","content":0}],"status":"published","journal":{"display":true,"email":"[email protected]","identity":"researchsquare","isNatureJournal":false,"hasQc":true,"allowDirectSubmit":true,"externalIdentity":"","sideBox":"","snPcode":"","submissionUrl":"/submission","title":"Research Square","twitterHandle":"researchsquare","acdcEnabled":true,"dfaEnabled":false,"editorialSystem":"","reportingPortfolio":"","inReviewEnabled":false,"inReviewRevisionsEnabled":true}}],"origin":"","ownerIdentity":"b4aae5e9-0afb-4fcf-b70f-4c5e5a794e3e","owner":[],"postedDate":"September 27th, 2024","published":true,"recentEditorialEvents":[],"rejectedJournal":[],"revision":"","amendment":"","status":"posted","subjectAreas":[{"id":37963003,"name":"Physical sciences/Engineering/Civil engineering"},{"id":37963004,"name":"Earth and environmental sciences/Hydrology"}],"tags":[],"updatedAt":"2024-10-03T07:23:51+00:00","versionOfRecord":[],"versionCreatedAt":"2024-09-27 07:58:04","video":"","vorDoi":"","vorDoiUrl":"","workflowStages":[]},"version":"v1","identity":"rs-4943413","journalConfig":"researchsquare"},"__N_SSP":true},"page":"/article/[identity]/[[...version]]","query":{"redirect":"/article/rs-4943413","identity":"rs-4943413","version":["v1"]},"buildId":"qtupq5eGEP_6zYnWcrvyt","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. This is a recent paper (2024) — citers typically take a year or two to land, and the OpenAlex reference graph may still be filling in.

Source provenance

europepmc
last seen: 2026-05-20T01:45:00.602351+00:00