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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>انجمن هیدرولیک ایران</PublisherName>
				<JournalTitle>نشریه علمی هیدرولیک</JournalTitle>
				<Issn>2345-4237</Issn>
				<Volume>6</Volume>
				<Issue>3</Issue>
				<PubDate PubStatus="epublish">
					<Year>2011</Year>
					<Month>11</Month>
					<Day>22</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Development of Unsteady State Bed Variations Simulation Model in Gravel Bed Rivers</ArticleTitle>
<VernacularTitle>توسعه مدل شبیه سازی تغییرات بستر رودخانه های شنی تحت جریان ناپایدار با رسوب ورودی از بالادست</VernacularTitle>
			<FirstPage>55</FirstPage>
			<LastPage>72</LastPage>
			<ELocationID EIdType="pii">85488</ELocationID>
			
<ELocationID EIdType="doi">10.30482/jhyd.2011.85488</ELocationID>
			
			<Language>FA</Language>
<AuthorList>
<Author>
					<FirstName>مهدی</FirstName>
					<LastName>باقری نژاد</LastName>
<Affiliation></Affiliation>

</Author>
<Author>
					<FirstName>محمدرضا</FirstName>
					<LastName>مجدزاده طباطبایی</LastName>
<Affiliation>عضو هیات علمی/ پردیس فنی مهندسی شهید عباسپور- دانشگاه شهید بهشتی</Affiliation>
<Identifier Source="ORCID">0000-0002-6205-7868</Identifier>

</Author>
<Author>
					<FirstName>سید سعید</FirstName>
					<LastName>موسوی ندوشنی</LastName>
<Affiliation></Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2011</Year>
					<Month>03</Month>
					<Day>23</Day>
				</PubDate>
			</History>
		<Abstract>Obtaining an analytical solution for bed variation equations, is a hard task and often impossible.&lt;br /&gt;However, if a quasi–steady state is considered for flow condition, analytical solution may not be&lt;br /&gt;unreachable provided that necessary simplifications are made. The main purpose of this paper is to&lt;br /&gt;develop an analytical model to predict bed variations in flood conditions with upstream sediment&lt;br /&gt;supply. In this study, non–uniformity of bed material size has been considered by hiding function. In&lt;br /&gt;addition, governing equations have also been applied and solved to compute values for unknown&lt;br /&gt;parameters such as hydraulic parameters, bed material size, water surface slope and elevation and bed&lt;br /&gt;load at various times from the beginning of flooding. Model validation with observed experimental&lt;br /&gt;data have been made and followed by sensitivity analysis. Finally the effect of flood hydrograph&lt;br /&gt;shapes has also been investigated on bed variations in gravel bed rivers. Results have shown that&lt;br /&gt;hiding function has modeled non–uniformity of the bed materials appropriately while a reasonable&lt;br /&gt;agreement has been found with observed experimental data for flow Froude number of less than 0.8.</Abstract>
			<OtherAbstract Language="FA"></OtherAbstract>
<ArchiveCopySource DocType="pdf">https://jhyd.iha.ir/article_85488_56774c607fa6ae69d2864307508dbce2.pdf</ArchiveCopySource>
</Article>
</ArticleSet>
