<?xml version="1.0" encoding="utf-8"?>
<journal>
<title>Environmental Erosion Research</title>
<title_fa>پژوهش هاي فرسايش محيطي</title_fa>
<short_title>E.E.R.</short_title>
<subject>Literature &amp; Humanities</subject>
<web_url>http://magazine.hormozgan.ac.ir</web_url>
<journal_hbi_system_id>1</journal_hbi_system_id>
<journal_hbi_system_user>admin</journal_hbi_system_user>
<journal_id_issn>2251-7812</journal_id_issn>
<journal_id_issn_online>2717-3968</journal_id_issn_online>
<journal_id_pii></journal_id_pii>
<journal_id_doi>10.61882/jeer</journal_id_doi>
<journal_id_iranmedex></journal_id_iranmedex>
<journal_id_magiran></journal_id_magiran>
<journal_id_sid>6561</journal_id_sid>
<journal_id_nlai>8888</journal_id_nlai>
<journal_id_science>45855/11/3/90</journal_id_science>
<language>fa</language>
<pubdate>
	<type>jalali</type>
	<year>1402</year>
	<month>9</month>
	<day>1</day>
</pubdate>
<pubdate>
	<type>gregorian</type>
	<year>2023</year>
	<month>12</month>
	<day>1</day>
</pubdate>
<volume>13</volume>
<number>4</number>
<publish_type>online</publish_type>
<publish_edition>1</publish_edition>
<article_type>fulltext</article_type>
<articleset>
	<article>


	<language>fa</language>
	<article_id_doi></article_id_doi>
	<title_fa>ارزیابی کارایی ضرایب اصلاح اریب در روش منحنی سنجه رسوب و مقایسه با مدل‌های هوشمند (ایستگاه جلوگیر خوزستان ـ حوضه کرخه)</title_fa>
	<title>Evaluating the Efficiency of Skew Correction Factors in Sediment Rating Curve and Comparison with Intelligent Models (Case Study: Jelogir Station, Khuzestan - Karkheh Catchment)</title>
	<subject_fa>مدلسازی و تحلیل زمانی و مکانی رخداد انواع مختلف فرسایش محیطی</subject_fa>
	<subject></subject>
	<content_type_fa>مستخرج از پایان‌نامه / رساله / طرح پژوهشی</content_type_fa>
	<content_type></content_type>
	<abstract_fa>&lt;span style=&quot;font-size:10pt&quot;&gt;&lt;span style=&quot;text-autospace:none&quot;&gt;&lt;span style=&quot;direction:rtl&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;b&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span b=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;برآورد مقدار رسوب در رودخانه&amp;shy;ها اهمیت زیادی دارد و متخصصان نیز همواره بدان توجه داشته&amp;shy;اند. منحنی سنجه&amp;shy;رسوب (&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;LTR&quot; lang=&quot;EN-GB&quot; style=&quot;font-size:11.0pt&quot;&gt;SRC&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span b=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;)، از جمله روش&amp;shy;های مرسوم در برآورد میزان بار رسوبات معلق در حوضه&lt;sub&gt;&amp;shy;&lt;/sub&gt;های آبخیز است که رابطه بین دبی جریان و دبی رسوب را بیان می&amp;shy;کند. با توجه به اهمیت این موضوع، در این پژوهش برای ارائه بهترین رابطه دبی رسوب ـ جریان در ایستگاه جلوگیر واقع بر رودخانه کرخه در استان خوزستان، داده&amp;shy;های دبی جریان و رسوب مربوط به سال&amp;shy;های &lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:11.0pt&quot;&gt;&lt;span b=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;1350&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span b=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt; تا &lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:11.0pt&quot;&gt;&lt;span b=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;1397&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span b=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt; تهیه و انواع منحنی سنجه شامل منحنی یک خطی، حد وسط، ماهانه، فصلی و چندخطی (دو خطی و سه خطی) ترسیم شد. همچنین در این پژوهش تلاش شد با استفاده از شاخص درصد بارش نرمال، داده&amp;shy;ها در سه دسته خشک، نرمال و مرطوب، تفکیک و منحنی سنجه برای هر کدام ترسیم شود. در نهایت، مدل بهینه منحنی سنجه&amp;shy;رسوب انتخاب و ضرایب اصلاحی شامل &lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;FAO&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span b=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;، &lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;QMLE&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span b=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;، &lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;Smearing&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span b=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;، &lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;MVUE &lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span b=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;&amp;nbsp;و&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt; (Beta) &amp;beta; &lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span b=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;بر روی مدل اجرا شد. با توجه به معیارهای ارزیابی &lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;RMSE&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span b=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;، &lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;ME&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span b=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt; و &lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;P&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span b=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;، رابطه به دست آمده برای تخمین رسوبات معلق، زمانی که داده&amp;shy;ها به صورت ماهانه تفکیک شد، در ماه مرداد و با اعمال ضریب &lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;MVUE&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span b=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt; دقت بیشتری را به همراه داشت. در ادامه، نتایج به دست آمده از مدل آماری سنجه&amp;shy;رسوب با مدل&amp;shy;های هوش مصنوعی شامل دو مدل شبکه&amp;shy;های عصبی &lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span b=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;پرسپترون چندلایه (&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;LTR&quot; lang=&quot;EN-GB&quot; style=&quot;font-size:11.0pt&quot;&gt;MLP&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span b=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;) و پایه شعاعی&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span b=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt; (&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;LTR&quot; lang=&quot;EN-GB&quot; style=&quot;font-size:11.0pt&quot;&gt;RBF&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span b=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;) مقایسه شد. نتایج نشان داد که مدل شبکه عصبی نسبت به مدل رگرسیونی &lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;LTR&quot; lang=&quot;EN-GB&quot; style=&quot;font-size:11.0pt&quot;&gt;SRC&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span b=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;، نتایج بهتری نشان می&amp;shy;دهد. مدل پرسپترون چندلایه با مقدار &lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;LTR&quot; lang=&quot;EN-GB&quot; style=&quot;font-size:11.0pt&quot;&gt;R&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span b=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt; و &lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;&amp;nbsp;RMSE&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span b=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt; به ترتیب برابر با &lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:11.0pt&quot;&gt;&lt;span b=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;87/0&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span b=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt; و &lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:11.0pt&quot;&gt;&lt;span b=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;0712/0&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span b=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt; نیز دقت خوبی نسبت به سایر مدل&amp;shy;ها دارد. &lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&amp;nbsp;</abstract_fa>
	<abstract>&lt;ol&gt;
	&lt;li align=&quot;left&quot; style=&quot;margin-bottom:11px; margin-left:8px; text-align:left&quot;&gt;&lt;span style=&quot;font-size:10pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span style=&quot;page-break-after:avoid&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;b&gt;&lt;span style=&quot;font-size:11.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span style=&quot;font-size:11.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span style=&quot;letter-spacing:-.5pt&quot;&gt;Introduction&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/li&gt;
&lt;/ol&gt;
&lt;span style=&quot;font-size:10pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span style=&quot;tab-stops:164.25pt&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;Estimation of the sediment load in rivers is one of the important issues in studies related to water quality and transport of pollutants, construction and operation of hydraulic structures, maintenance of reservoirs, water transmission networks, and water resources management. An accurate understanding of the sedimentation of a watershed can provide a correct understanding of soil erosion and its consequences.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:10pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span style=&quot;tab-stops:164.25pt&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;Since sediment changes in the river are often a function of flow discharge changes; therefore, methods of measuring suspended sediment load based on the suspended sediment concentration and flow discharge will be useful in estimating the amount of sediment load.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:10pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span style=&quot;tab-stops:164.25pt&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;The sediment rating curve is one of the methods that is based on flow discharge and sediment discharge and expresses the relationship between these two parameters in the form of power regression (Eq 1).&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:10pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span style=&quot;tab-stops:164.25pt&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;

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			&lt;td style=&quot;width:312px; padding:0cm 7px 0cm 7px&quot; valign=&quot;top&quot;&gt;&lt;span style=&quot;font-size:10pt&quot;&gt;&lt;span style=&quot;text-autospace:none&quot;&gt;&lt;span style=&quot;direction:rtl&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span arial=&quot;&quot; style=&quot;font-family:&quot;&gt;(&lt;/span&gt;&lt;/span&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;&lt;span calibri=&quot;&quot; style=&quot;font-family:&quot;&gt;1&lt;/span&gt;&lt;/span&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span arial=&quot;&quot; style=&quot;font-family:&quot;&gt;)&lt;/span&gt;&lt;/span&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;&lt;span style=&quot;font-family:&quot;Calibri&quot;,sans-serif&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/td&gt;
			&lt;td style=&quot;width:312px; padding:0cm 7px 0cm 7px&quot; valign=&quot;top&quot;&gt;&lt;span style=&quot;font-size:10pt&quot;&gt;&lt;span style=&quot;text-autospace:none&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;font-size:11.0pt&quot;&gt;&lt;span calibri=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;position:relative&quot;&gt;&lt;span style=&quot;top:6.0pt&quot;&gt;&lt;img alt=&quot;&quot; id=&quot;_x0000_i1025&quot; o:ole=&quot;&quot; src=&quot;file:///C:/Users/sana/AppData/Local/Temp/msohtmlclip1/01/clip_image001.wmz&quot; style=&quot;width:47.25pt; height:20.25pt&quot; &gt; &lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span dir=&quot;RTL&quot; lang=&quot;AR-SA&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;font-family:&quot;B Mitra&quot;&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/td&gt;
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&lt;/table&gt;
&lt;span style=&quot;font-size:10pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span style=&quot;tab-stops:164.25pt&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span dir=&quot;RTL&quot; lang=&quot;AR-SA&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:10pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span style=&quot;tab-stops:164.25pt&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;where &lt;/span&gt;&lt;/span&gt;&lt;m:omath&gt;&lt;m:ssub&gt;&lt;m:ssubpr&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span cambria=&quot;&quot; math=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;m:ctrlpr&gt;&lt;/m:ctrlpr&gt;&lt;/span&gt;&lt;/span&gt;&lt;/m:ssubpr&gt;&lt;m:e&gt;&lt;i&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span cambria=&quot;&quot; math=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;m:r&gt;Q&lt;/m:r&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/i&gt;&lt;/m:e&gt;&lt;m:sub&gt;&lt;i&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span cambria=&quot;&quot; math=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;m:r&gt;s&lt;/m:r&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/i&gt;&lt;/m:sub&gt;&lt;/m:ssub&gt;&lt;/m:omath&gt;&lt;span style=&quot;font-size:10.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;position:relative&quot;&gt;&lt;span style=&quot;top:3.0pt&quot;&gt; &lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&amp;nbsp;is the suspended sediment discharge (in tons per day), &lt;/span&gt;&lt;/span&gt;&lt;m:omath&gt;&lt;m:ssub&gt;&lt;m:ssubpr&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span cambria=&quot;&quot; math=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;m:ctrlpr&gt;&lt;/m:ctrlpr&gt;&lt;/span&gt;&lt;/span&gt;&lt;/m:ssubpr&gt;&lt;m:e&gt;&lt;i&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span cambria=&quot;&quot; math=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;m:r&gt;Q&lt;/m:r&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/i&gt;&lt;/m:e&gt;&lt;m:sub&gt;&lt;i&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span cambria=&quot;&quot; math=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;m:r&gt;w&lt;/m:r&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/i&gt;&lt;/m:sub&gt;&lt;/m:ssub&gt;&lt;/m:omath&gt;&lt;span style=&quot;font-size:10.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;position:relative&quot;&gt;&lt;span style=&quot;top:3.0pt&quot;&gt; &lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;is the flow discharge (in cubic meters per second), and a and b are the coefficients of the equation .&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:10pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span style=&quot;tab-stops:164.25pt&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;Rating curves can be drawn in different ways according to the way of data separation. Among these methods, we can refer to one-line, multi-line, mean of categories, seasonal, monthly, annual models, etc.&lt;/span&gt;&lt;/span&gt; &lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;The presence of bias in the sediment discharge relationship makes this relationship unable to show the exact sediment concentration in different flow discharges. This bias causes the amount of sediment to be underestimated. Various researchers have proposed some statistical correction factors to achieve the minimum error, which are applied in the sediment rating equation. In this research, in order to increase the accuracy of sediment estimation by using a sediment rating curve, at first, different types of rating curves were drawn for the station and, finally, correction factors consisting of &lt;/span&gt;&lt;/span&gt;&lt;span style=&quot;font-size:11.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;QMLE, Smearing, MVUE, and (Beta) &amp;beta; &lt;/span&gt;&lt;/span&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;were applied for the selected curve.&lt;/span&gt;&lt;/span&gt; &lt;span lang=&quot;EN-GB&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;Also,&lt;/span&gt;&lt;/span&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt; an attempt was made to separate the data into three categories of dry, normal and wet by using the percentage of normal precipitation and to draw the sediment rating curve for each. At the end, the results obtained from the statistical model (SRC) were compared with artificial intelligence models including two models of multilayer perceptron (MLP) and radial basis set (RBF) neural networks.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;

&lt;ol start=&quot;2&quot;&gt;
	&lt;li style=&quot;margin-bottom:11px; margin-left:8px&quot;&gt;&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;line-height:106%&quot;&gt;&lt;span style=&quot;tab-stops:164.25pt&quot;&gt;&lt;span style=&quot;font-family:Calibri,sans-serif&quot;&gt;&lt;b&gt;Methodology &lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/li&gt;
&lt;/ol&gt;
&lt;span style=&quot;font-size:10pt&quot;&gt;&lt;span style=&quot;line-height:106%&quot;&gt;&lt;span style=&quot;tab-stops:164.25pt&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;line-height:106%&quot;&gt;In this research, the flow and sediment discharge data from 1350 to 1397 for the Jelogir station in Khuzestan province located on the main Karkhe River were prepared from the Khuzestan Regional Water Organization. Sediment rating curve models, including common linear curve (USBR), mean of categories, monthly, seasonal, bilinear, trilinear, dry, normal and wet models were drawn for the station.&lt;/span&gt;&lt;/span&gt; &lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;line-height:106%&quot;&gt;Then, for the drawn curves, evaluation criteria including RMSE, ME and P were checked and, finally, by ranking these criteria, the curve with the least error was selected. In determining the rank of each model, the values of the evaluation indices were compared with each other. In this way, the closest P and ME index value to 1 and the closest RMSE index value to zero, which indicates the least difference between the estimated and observed sediment values, was assigned the first rank. In order to investigate the effect of skew correction coefficients on the accuracy of sediment rating curves, coefficients including MVUE, FAO, QMLE and Smearing were applied on the rating curve which was selected as the optimal model in the previous step.&lt;/span&gt;&lt;/span&gt; &lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;line-height:106%&quot;&gt;The data were processed using neural network models. For this purpose, different structures of neural networks with different layers, neurons and functions were investigated through trial and error.&lt;/span&gt;&lt;/span&gt;&lt;b&gt;&lt;span style=&quot;font-size:11.0pt&quot;&gt;&lt;span style=&quot;line-height:106%&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:10pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span style=&quot;tab-stops:164.25pt&quot;&gt;&lt;span style=&quot;direction:rtl&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span style=&quot;font-family:&quot;B Nazanin&quot;&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;

&lt;ol start=&quot;3&quot;&gt;
	&lt;li style=&quot;margin-bottom:11px; margin-left:8px&quot;&gt;&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;line-height:106%&quot;&gt;&lt;span style=&quot;font-family:Calibri,sans-serif&quot;&gt;&lt;b&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;line-height:106%&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;line-height:106%&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;Results&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/li&gt;
&lt;/ol&gt;
&lt;span style=&quot;font-size:10pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span style=&quot;tab-stops:164.25pt&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;According to the obtained results, the mean categories method has the highest correlation coefficient (0.85). The RMSE in rainy and flooding months (April and March) and also in high flow discharge rates (in bilinear, and trilinear models, at flow discharge greater than 201 and 114 cubic meters per second, respectively), has allocated the largest amount. The lowest value of RMSE is related to the months of August and September, which is reasonable due to the lack of rainfall and flooding in these months and as a result of low erosion of sediments. According to the ranking values, the periods of low rainfall&lt;span style=&quot;color:red&quot;&gt;,&lt;/span&gt; including summer and July, August and September are in the first ranks, and as a result, the sediment rating curve has more accuracy in estimating sediments. Finally, the rating curve of August, which has the lowest total ranking value, was chosen as the optimal curve. According to the ranking of the correction coefficients, it can be seen that the sediment rating curve without applying the correction coefficients (the highest rank) has the highest amount of error and by applying the coefficients, the error of sediment flow estimation can be reduced. Finally, MVUE with the lowest total ranking was chosen as the optimal correction coefficient, and by applying it, the accuracy of the model in estimating the sediment discharge increases.&lt;/span&gt;&lt;/span&gt; &lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;In the neural network model, Lunberg-Marquardt optimization algorithm was used and the number of hidden layer neurons in the best MLP and RBF structure was obtained as 5 and 6, respectively.&lt;/span&gt;&lt;/span&gt; &lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;Also, the activator function in the hidden layer in MLP was selected as sigmoid tangent and Gaussian function in RBF. The results show that by using neural networks of multilayer perceptron, it is possible to predict the amount of suspended sediment with higher accuracy, and the accuracy of the results obtained from the artificial neural network method is far higher than the accuracy of the rating curve method with and without data classification.&lt;/span&gt;&lt;/span&gt; &lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;According to the results, the MLP model has shown a lower error value than the RBF radial base model.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:10pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;b&gt;&lt;span style=&quot;font-size:11.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span calibri=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;letter-spacing:-.2pt&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;

&lt;ol start=&quot;4&quot;&gt;
	&lt;li align=&quot;left&quot; style=&quot;margin-left:8px; text-align:left&quot;&gt;&lt;span style=&quot;font-size:10pt&quot;&gt;&lt;span style=&quot;line-height:106%&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;b&gt;&lt;span style=&quot;font-size:11.0pt&quot;&gt;&lt;span style=&quot;line-height:106%&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span style=&quot;font-size:11.0pt&quot;&gt;&lt;span style=&quot;line-height:106%&quot;&gt;Discussion &amp; &lt;span style=&quot;letter-spacing:-.2pt&quot;&gt;Conclusions&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/li&gt;
&lt;/ol&gt;
&lt;span style=&quot;font-size:10pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span style=&quot;tab-stops:92.15pt&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;In this article, in order to estimate the suspended sediment in the Jelogir station, the data were separated into different forms and the sediment rating curves were drawn into linear curve (USBR), mean of categories, monthly, seasonal, dry, normal, wet, bilinear, and trilinear types. The obtained results showed that the accuracy of the relationship obtained for the classification of data based on August (R2= 0.785) and the total rating of 9 (the lowest value) was more than the other models. And at high flow discharge, the accuracy of the models decreases. It was found that the correction coefficients are effective in increasing the accuracy of the models, and the lowest amount of error for the optimal model is obtained by using MVUE. Comparing the results of statistical methods and neural networks showed that neural network models are more accurate in estimating daily sediment. The better performance of artificial neural networks compared to statistical methods can be expressed in the nonlinear approximation capability of neural networks.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;</abstract>
	<keyword_fa>اصلاح اریب, رسوب معلق, مدل‌های MLP و RBF, مدل SRC.</keyword_fa>
	<keyword>Skew Correction Coefficient, Suspended Sediment, MLP and RBF Models, SRC Model</keyword>
	<start_page>235</start_page>
	<end_page>255</end_page>
	<web_url>http://magazine.hormozgan.ac.ir/browse.php?a_code=A-10-951-1&amp;slc_lang=fa&amp;sid=1</web_url>


<author_list>
	<author>
	<first_name>fatemeh</first_name>
	<middle_name></middle_name>
	<last_name>avazpour</last_name>
	<suffix></suffix>
	<first_name_fa>فاطمه</first_name_fa>
	<middle_name_fa></middle_name_fa>
	<last_name_fa>عوض پور</last_name_fa>
	<suffix_fa></suffix_fa>
	<email>fatemeavazpoor@yahoo.com</email>
	<code>10031947532846008632</code>
	<orcid>10031947532846008632</orcid>
	<coreauthor>No</coreauthor>
	<affiliation>Department of Civil Engineering, Water, and Hydraulic Structure, Yazd University, Yazd, Iran.</affiliation>
	<affiliation_fa>گروه مهندسی عمران ـ آب و سازه‌های هیدرولیکی، دانشکده عمران، دانشگاه یزد، یزد</affiliation_fa>
	 </author>


	<author>
	<first_name>Mohammad Reza</first_name>
	<middle_name></middle_name>
	<last_name>Hadian</last_name>
	<suffix></suffix>
	<first_name_fa>محمدرضا</first_name_fa>
	<middle_name_fa></middle_name_fa>
	<last_name_fa>هادیان</last_name_fa>
	<suffix_fa></suffix_fa>
	<email>mr_hadian@yazd.ac.ir</email>
	<code>10031947532846008633</code>
	<orcid>10031947532846008633</orcid>
	<coreauthor>Yes
</coreauthor>
	<affiliation>Department of Civil Engineering, Water, and Hydraulic Structure, Yazd University, Yazd, Iran.</affiliation>
	<affiliation_fa>گروه مهندسی عمران ـ آب و سازه‌های هیدرولیکی، دانشکده عمران، دانشگاه یزد، یزد</affiliation_fa>
	 </author>


	<author>
	<first_name>Ali</first_name>
	<middle_name></middle_name>
	<last_name>Talebi</last_name>
	<suffix></suffix>
	<first_name_fa>علی</first_name_fa>
	<middle_name_fa></middle_name_fa>
	<last_name_fa>طالبی</last_name_fa>
	<suffix_fa></suffix_fa>
	<email>talebisf@yazd.ac.ir</email>
	<code>10031947532846008634</code>
	<orcid>10031947532846008634</orcid>
	<coreauthor>No</coreauthor>
	<affiliation>Department of Natural Resources and Desert Studies, Yazd University, Yazd, Iran</affiliation>
	<affiliation_fa>گروه مرتع و آبخیزداری، دانشکده منابع طبیعی و کویرشناسی، دانشگاه یزد، یزد</affiliation_fa>
	 </author>


</author_list>


	</article>
</articleset>
</journal>
