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<!DOCTYPE ArticleSet PUBLIC "-//NLM//DTD PubMed 2.7//EN" "https://dtd.nlm.nih.gov/ncbi/pubmed/in/PubMed.dtd">
<ArticleSet>
<Article>
<Journal>
				<PublisherName>Sharif University of Technology</PublisherName>
				<JournalTitle>Scientia Iranica</JournalTitle>
				<Issn>1026-3098</Issn>
				<Volume>29</Volume>
				<Issue>5</Issue>
				<PubDate PubStatus="epublish">
					<Year>2022</Year>
					<Month>10</Month>
					<Day>01</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Integrated numerical study of rainfall-induced landslides from initiation to propagation using saturation-based rheological model</ArticleTitle>
<VernacularTitle></VernacularTitle>
			<FirstPage>2304</FirstPage>
			<LastPage>2316</LastPage>
			<ELocationID EIdType="pii">22686</ELocationID>
			
<ELocationID EIdType="doi">10.24200/sci.2022.58125.5577</ELocationID>
			
			<Language>EN</Language>
<AuthorList>
<Author>
					<FirstName>R.</FirstName>
					<LastName>Ghorbani</LastName>
<Affiliation>School of Mechanical Engineering, Sharif University of Technology, Tehran, P.O. Box 11155/9567, Iran</Affiliation>

</Author>
<Author>
					<FirstName>M.T.</FirstName>
					<LastName>Manzari</LastName>
<Affiliation>School of Mechanical Engineering, Sharif University of Technology, Tehran, P.O. Box 11155/9567, Iran</Affiliation>

</Author>
<Author>
					<FirstName>A.</FirstName>
					<LastName>Hajilouy-Benisi</LastName>
<Affiliation>School of Mechanical Engineering, Sharif University of Technology, Tehran, P.O. Box 11155/9567, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2021</Year>
					<Month>04</Month>
					<Day>17</Day>
				</PubDate>
			</History>
		<Abstract>This paper presents an integrated two-dimensional numerical framework for simulating rainfall-induced landslides from instability initiation to post-failure flow. To describe the entire process, three steps are considered in this study: 1) a coupled hydro-stability analysis which detects the failure plane using the Finite Element Method (FEM) (pre-failure stage), 2) computing the local rheology of the failed mass (wet sandy soil) based on the water saturation at the onset of failure, using the saturation-based rheological model (transition stage), and 3) a continuum-based propagation analysis which solves the flow of the wet material by employing the Smoothed Particle Hydrodynamics (SPH) method (post-failure stage). Finally, to investigate the influence of rheological model on the post-failure behavior, the computed final deposition profile and flow kinetic energy are compared with those of a viscoplastic model.</Abstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">Rainfall-induced landslide</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Slope stability</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Saturation-based rheological model</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Propagation</Param>
			</Object>
		</ObjectList>
<ArchiveCopySource DocType="pdf">https://scientiairanica.sharif.edu/article_22686_06cdf564433704ef25a87c329c00475c.pdf</ArchiveCopySource>
</Article>
</ArticleSet>
