<?xml version="1.0" encoding="utf-8"?>
<journal>
<title>Journal of Spatial Analysis Environmental Hazards</title>
<title_fa>تحلیل فضایی مخاطرات محیطی</title_fa>
<short_title>Journal of Spatial Analysis Environmental Hazards</short_title>
<subject>Literature &amp; Humanities</subject>
<web_url>http://jsaeh.khu.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>2423-7892</journal_id_issn>
<journal_id_issn_online>2588-5146</journal_id_issn_online>
<journal_id_pii></journal_id_pii>
<journal_id_doi>10.61882/jsaeh</journal_id_doi>
<journal_id_iranmedex></journal_id_iranmedex>
<journal_id_magiran></journal_id_magiran>
<journal_id_sid></journal_id_sid>
<journal_id_nlai></journal_id_nlai>
<journal_id_science></journal_id_science>
<language>fa</language>
<pubdate>
	<type>jalali</type>
	<year>1402</year>
	<month>2</month>
	<day>1</day>
</pubdate>
<pubdate>
	<type>gregorian</type>
	<year>2023</year>
	<month>5</month>
	<day>1</day>
</pubdate>
<volume>10</volume>
<number>1</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>پهنه بندی پتانسیل خطر وقوع سیلاب در حوضه نکارود، نکا- مازندران</title_fa>
	<title>The zoning of flood risk potential in the Nekarod Cachment, Neka- Mazandaran</title>
	<subject_fa>تخصصي</subject_fa>
	<subject>Special</subject>
	<content_type_fa>پژوهشي</content_type_fa>
	<content_type>Research</content_type>
	<abstract_fa>&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;direction:rtl&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span calibri=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span lang=&quot;AR-SA&quot; style=&quot;font-size:13.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span b=&quot;&quot; nazanin=&quot;&quot; style=&quot;font-family:&quot;&gt;سیل به &amp;shy;عنوان یکی از مخرب&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:13.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&amp;shy;&lt;/span&gt;&lt;/span&gt;&lt;span lang=&quot;AR-SA&quot; style=&quot;font-size:13.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span b=&quot;&quot; nazanin=&quot;&quot; style=&quot;font-family:&quot;&gt;ترین و مهم&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:13.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&amp;shy;&lt;/span&gt;&lt;/span&gt;&lt;span lang=&quot;AR-SA&quot; style=&quot;font-size:13.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span b=&quot;&quot; nazanin=&quot;&quot; style=&quot;font-family:&quot;&gt;ترین بلایای طبیعی می&amp;shy;باشد که براساس آمارهای سالیانه خسارات زیاد جانی و مالی را به خود اختصاص می&amp;shy;دهد. یکی از اقدامات کلیدی، شناخت مناطق دارای پتانسیل وقوع سیلاب می&amp;shy;باشد. در این پژوهش احتمال وقوع سیلاب رودخانه نکارود واقع در استان مازندران با استفاده از &lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:13.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span b=&quot;&quot; nazanin=&quot;&quot; style=&quot;font-family:&quot;&gt;تحلیل تصمیم&amp;shy;&amp;shy; گیری چند معیاره &lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span b=&quot;&quot; nazanin=&quot;&quot; style=&quot;font-family:&quot;&gt;(&lt;/span&gt;&lt;span dir=&quot;LTR&quot; new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;MCDA&lt;/span&gt;&lt;span b=&quot;&quot; nazanin=&quot;&quot; style=&quot;font-family:&quot;&gt;)&lt;/span&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:13.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span b=&quot;&quot; nazanin=&quot;&quot; style=&quot;font-family:&quot;&gt; مطالعه شده&amp;shy; است. باتوجه به روش، از 4 معیار اصلی شامل ارتفاع، شیب، فاصله از رودخانه و کاربری اراضی در این پژوهش استفاده شده &amp;shy;است. پس از آماده&amp;shy; سازی معیارها، هرمعیار به صورت نزولی در 9 کلاس ارزش&amp;shy; گذاری و&amp;nbsp; با توجه به تاثیر هر معیار در احتمال وقوع سیلاب طبقه&amp;shy; بندی شدند. سپس شاخص وزن نرمال&amp;shy; شده &lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;(&lt;/span&gt;&lt;span dir=&quot;LTR&quot; new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;NWI&lt;/span&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;)&lt;/span&gt; &lt;span lang=&quot;FA&quot; style=&quot;font-size:13.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span b=&quot;&quot; nazanin=&quot;&quot; style=&quot;font-family:&quot;&gt;محاسبه شد و نقشه نهایی پهنه&amp;shy; بندی پتانسیل خطر وقوع سیلاب با تلفیق معیارها به روش وزن&amp;shy;دهی خطی &lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;(&lt;/span&gt;&lt;span dir=&quot;LTR&quot; new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;WLC&lt;/span&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;)&lt;/span&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:13.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span b=&quot;&quot; nazanin=&quot;&quot; style=&quot;font-family:&quot;&gt; در 5 طبقه تهیه گردیده&amp;shy; است. نتایج بدست آمده، نشان می&amp;shy;دهد که، حدود 982.58 کیلومتر مربع (51.42 درصد) از دو طرف رودخانه نکارود دارای پتانسیل احتمال خطر زیاد و خیلی&amp;shy;زیاد وقوع سیلاب است. قسمت ورودی شهر نکا و محدوده&amp;shy; هایی که دارای کاربری مسکونی و زراعی هستند، به دلیل تراکم بالای شبکه آبراهه و همینطور شب 6 تا 10 درجه&amp;nbsp; دارای بیشترین میزان خطر می&amp;shy;باشند. نتایج حاصل از این پژوهش نشان&amp;shy; می&amp;shy;دهد که تحلیل تصمیم&amp;shy;&amp;shy; گیری چند معیاره ، روشی سریع و کم هزینه برای استفاده در تهیه نقشه&amp;shy; های پهنه &amp;shy;بندی احتمال وقوع سیلاب در حوضه &amp;shy;های فاقد اطلاعات هیدرومتری می&amp;shy;باشند.&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;br&gt;
&amp;nbsp;</abstract_fa>
	<abstract>&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;line-height:normal&quot;&gt;&lt;span calibri=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;b&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;Introduction&lt;/span&gt;&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;line-height:normal&quot;&gt;&lt;span calibri=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;A flood is a natural disaster caused by heavy rainfall, which causes casualties and damage to infrastructure and crops. Trend of floods in the world increasing due to climate change, changing rainfall patterns, rising sea levels in the future, and in addition, population growth and urban development and human settlements near river have caused floods to become a threat to humans. One of the most important and necessary tasks in catchments is to prepare flood risk maps and analyze them. In recent decades, researchers have been using remote sensing techniques and geographic information systems to obtain flood risk maps in an area. Due to the numerous floods that have occurred in the Neka river catchment, it is necessary to conduct a study entitled zoning of flood sensitivity in Neka river catchment for more effective management in this area.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;line-height:normal&quot;&gt;&lt;span calibri=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;font-family:&quot;Times New Roman&quot;,serif&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;line-height:normal&quot;&gt;&lt;span calibri=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;b&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;Materials and methods&lt;/span&gt;&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;line-height:normal&quot;&gt;&lt;span calibri=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;Study area: Neka river catchment area with an area of ​​1922 &lt;/span&gt;&lt;m:omath&gt;&lt;m:ssup&gt;&lt;m:ssuppr&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;/m:ssuppr&gt;&lt;m:e&gt;&lt;i&gt;&lt;span cambria=&quot;&quot; math=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;m:r&gt;Km&lt;/m:r&gt;&lt;/span&gt;&lt;/i&gt;&lt;/m:e&gt;&lt;m:sup&gt;&lt;i&gt;&lt;span cambria=&quot;&quot; math=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;m:r&gt;2&lt;/m:r&gt;&lt;/span&gt;&lt;/i&gt;&lt;/m:sup&gt;&lt;/m:ssup&gt;&lt;/m:omath&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&amp;nbsp;is part of Mazandaran province in terms of political divisions. This basin is between 53&amp;ordm; 17&amp;acute; 54 &amp;ordm;44&amp;acute; east and 36 &amp;ordm; 28 &amp;acute;to 36 &amp;ordm; 42&amp;acute; of north latitude. The highest point of the basin is 3500 m (Shahkuh peak) and the height of the lowest point of the basin in the Ablo station is about 50 m and at the connection to the Caspian Sea is -27 meters. The seven sub-basins of this basin are Laksha, Golord, Burma, Metkazin, Kiasar, Alarez and Sorkh Griyeh. Geologically, the basin is mostly of calcareous and marl formations. In the south and southwest of Neka River, the rock material is mostly clay and calcareous marl, which makes this basin has a high erosion potential&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;line-height:normal&quot;&gt;&lt;span calibri=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;To study the flood zoning of the area using a multi-criteria decision model, 1: 25000 maps of the surveying organization and a digital elevation model with a resolution of 12.5 meters (Alos Palsar) were extracted. In order to study the flood risk in Neka river, 4 criteria of height, distance from the river, land use and slope have been used. In the present study, modeling and preparation of flood risk zoning map in 4 stage including descending valuation, normalization of each class, normalized index weight and integration of criteria has been done by the following linear weighting method. Performing linear weighting operations depends on the weighted average of a number of selected parameters in the opinion of the expert. According to the weight assigned to each criterion based on the expert opinion, each of the criteria was multiplied by the assigned weight and at the end the criteria were added together and the final zoning map was obtained.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;line-height:normal&quot;&gt;&lt;span calibri=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;font-family:&quot;Times New Roman&quot;,serif&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;line-height:normal&quot;&gt;&lt;span calibri=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;b&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;Results and Discussion&lt;/span&gt;&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;line-height:normal&quot;&gt;&lt;span calibri=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;In this study, using a multi-criteria decision-making system model, a flood risk zoning map in the Neka river catchment was prepared. According to the weight assigned to each criterion based on expert opinion, the final risk probability map has a value between 0.02 to 0.2, which is ultimately divided into 5 classes in terms of flood risk. Value range 0.02 to 0.06 component of very low risk zone, range 0.08 to 0.11 component of low-risk zone, range 0.11 to 0.13 component of medium-risk zone, range 0.13 to 0.16 component of high-risk zone, and finally domain 0.16 to 0.20 components of the area with very high risk potential have been obtained. According to the final divisions in the flood risk zoning map of the catchment area, a safe area means areas where the probability of flooding is very low and close to zero, and in contrast, the area with a high and very high risk potential for flooding has the probability of high-risk floods. According to the final flood risk zoning map, about 982 &lt;/span&gt;&lt;m:omath&gt;&lt;m:ssup&gt;&lt;m:ssuppr&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;/m:ssuppr&gt;&lt;m:e&gt;&lt;i&gt;&lt;span cambria=&quot;&quot; math=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;m:r&gt;Km&lt;/m:r&gt;&lt;/span&gt;&lt;/i&gt;&lt;/m:e&gt;&lt;m:sup&gt;&lt;i&gt;&lt;span cambria=&quot;&quot; math=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;m:r&gt;2&lt;/m:r&gt;&lt;/span&gt;&lt;/i&gt;&lt;/m:sup&gt;&lt;/m:ssup&gt;&lt;/m:omath&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&amp;nbsp;(51%) has high and very high vulnerability, as well as about 510 &lt;/span&gt;&lt;m:omath&gt;&lt;m:ssup&gt;&lt;m:ssuppr&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;/m:ssuppr&gt;&lt;m:e&gt;&lt;i&gt;&lt;span cambria=&quot;&quot; math=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;m:r&gt;Km&lt;/m:r&gt;&lt;/span&gt;&lt;/i&gt;&lt;/m:e&gt;&lt;m:sup&gt;&lt;i&gt;&lt;span cambria=&quot;&quot; math=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;m:r&gt;2&lt;/m:r&gt;&lt;/span&gt;&lt;/i&gt;&lt;/m:sup&gt;&lt;/m:ssup&gt;&lt;/m:omath&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&amp;nbsp;(26.69%) has medium vulnerability in Neka catchment area.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;line-height:normal&quot;&gt;&lt;span calibri=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;font-family:&quot;Times New Roman&quot;,serif&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;line-height:normal&quot;&gt;&lt;span calibri=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;b&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;Conclusion&lt;/span&gt;&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;line-height:normal&quot;&gt;&lt;span calibri=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;The results obtained from the model indicates that the highest risk of flooding points are located in the western parts of the Neka catchment area and the end of the catchment area that reach the city of Neka. According to the research findings, the most important factors in increasing the risk of floods were the slope in this area and the distance from the drainage network. According to the results of the model, a large area of ​​the basin is a component of high risk zone, that means the Neka river watershed has a high potential for floods. Evidence and documented reports show that the Neka river Basin has experienced several floods in the last two decades. The major part of the occurrence of floods is due to the natural conditions of the basin, thus it is necessary to reduce flood damage by changing the locations of various land uses based on flood vulnerability maps. Using multi-criteria decision making method can be used to prepare flood risk zoning maps in basins that do not have hydrometric data; It is also a more cost-effective method in terms of time. One of the important issues in the final result of this model is due to the weight of the layers, which should be used by experts, who are familiar with the region and this method and adapt to field evidence.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;line-height:normal&quot;&gt;&lt;span calibri=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;font-family:&quot;Times New Roman&quot;,serif&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;line-height:normal&quot;&gt;&lt;span calibri=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;b&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;Keyworlds:&lt;/span&gt;&lt;/b&gt; &lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;Flood, Multi-criteria decision making system(MCDA), &lt;/span&gt;&lt;span lang=&quot;EN&quot; new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;Hazard zoning,&lt;/span&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt; Nekarod, Natural hazard.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&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;font-size:9.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span style=&quot;font-family:&quot;Times New Roman&quot;,serif&quot;&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:11pt&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;font-size:10.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span style=&quot;font-family:&quot;Times New Roman&quot;,serif&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;br&gt;
&amp;nbsp;</abstract>
	<keyword_fa>سیل, تحلیل تصمیم‌‌گیری چند معیاره , پهنه بندی خطر, نکارود, مخاطرات طبیعی</keyword_fa>
	<keyword>Flood, Multi-criteria decision making system(MCDA), Hazard zoning,  Nekarod, Natural disaster ,</keyword>
	<start_page>23</start_page>
	<end_page>40</end_page>
	<web_url>http://jsaeh.khu.ac.ir/browse.php?a_code=A-10-1451-1&amp;slc_lang=fa&amp;sid=1</web_url>


<author_list>
	<author>
	<first_name>Mohammad Mahdi</first_name>
	<middle_name></middle_name>
	<last_name>Hosseinzadeh</last_name>
	<suffix></suffix>
	<first_name_fa>محمد مهدی</first_name_fa>
	<middle_name_fa></middle_name_fa>
	<last_name_fa>حسین زاده</last_name_fa>
	<suffix_fa></suffix_fa>
	<email>m_hoseinzadeh@sbu.ac.ir</email>
	<code>100319475328460011122</code>
	<orcid>100319475328460011122</orcid>
	<coreauthor>Yes
</coreauthor>
	<affiliation>Earth Sciences Faculty, Shahid Beheshti University, Tehran</affiliation>
	<affiliation_fa>دانشکده علوم زمین، دانشگاه شهید بهشتی</affiliation_fa>
	 </author>


	<author>
	<first_name>ali reza</first_name>
	<middle_name></middle_name>
	<last_name>Salehipor Milani</last_name>
	<suffix></suffix>
	<first_name_fa>علیرضا</first_name_fa>
	<middle_name_fa></middle_name_fa>
	<last_name_fa>صالحی پور میلانی</last_name_fa>
	<suffix_fa></suffix_fa>
	<email>ar.salehipour@googlemail.com</email>
	<code>100319475328460011123</code>
	<orcid>100319475328460011123</orcid>
	<coreauthor>No</coreauthor>
	<affiliation>Earth Sciences Faculty, Shahid Beheshti University, Tehran</affiliation>
	<affiliation_fa>دانشکده علوم زمین، دانشگاه شهید بهشتی</affiliation_fa>
	 </author>


	<author>
	<first_name>fateme</first_name>
	<middle_name></middle_name>
	<last_name>Rezaian Zarandini</last_name>
	<suffix></suffix>
	<first_name_fa>فاطمه</first_name_fa>
	<middle_name_fa></middle_name_fa>
	<last_name_fa>رضائیان زرندینی</last_name_fa>
	<suffix_fa></suffix_fa>
	<email>aidarezaei13@gmail.com</email>
	<code>100319475328460011124</code>
	<orcid>100319475328460011124</orcid>
	<coreauthor>No</coreauthor>
	<affiliation>Earth Sciences Faculty, Shahid Beheshti University, Tehran</affiliation>
	<affiliation_fa>دانشکده علوم زمین، دانشگاه شهید بهشتی</affiliation_fa>
	 </author>


</author_list>


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