<?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>1404</year>
	<month>6</month>
	<day>1</day>
</pubdate>
<pubdate>
	<type>gregorian</type>
	<year>2025</year>
	<month>9</month>
	<day>1</day>
</pubdate>
<volume>15</volume>
<number>3</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>اثر مسیرهای تردد دام بر نفوذپذیری و رسوب‌زایی مراتع حوضه صنوبر تربت‌حیدریه، خراسان‌رضوی</title_fa>
	<title>The Effect of Livestock Trampling Routes on Permeability and Sediment Production in the Rangelands of the Senobar Watershed, Torbat Heydarieh, Khorasan Razavi</title>
	<subject_fa>تحلیل فضایی عوامل فرساینده، و استخراج الگوهای پراکندگی و انتشار فرسایش</subject_fa>
	<subject></subject>
	<content_type_fa>مستخرج از پایان‌نامه / رساله / طرح پژوهشی</content_type_fa>
	<content_type></content_type>
	<abstract_fa>&lt;div style=&quot;text-align: justify;&quot;&gt;&lt;span style=&quot;font-size:10pt&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 b=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;امروزه میزان بهره&#8204;برداری از آبخیزهای کشور بسیار بالاتر از حدمجاز است که بخشی عمده از این بهره&#8204;برداری به چرای دام اختصاص دارد. چرای زودرس و مفرط اراضی مرتعی توسط دام بر فرایندهایی همچون کمیت و کیفیت پوشش گیاهی، نفوذپذیری، تخلخل، رطوبت خاک، میزان رواناب و فرسایش خاک مراتع با فشردگی و تخریب فیزیکی خاک اثرگذار است. در این راستا پژوهش حاضر به منظور بررسی اثر میکروتراس&#8204;های ایجاد شده در مسیرهای تردد دام بر رواناب، رسوب و نفوذپذیری در شش منطقه از مراتع آبخیز صنوبر تربت حیدریه درون 36 نقطه (18 میکروتراس و 18 شاهد) و با استفاده از شبیه&#8204;ساز باران صحرایی و رینگ&#8204;های دوتایی انجام شد. نتایج تحلیل داده&#8204;های میدانی نشان داد که در متغیرهای نفوذ در هر شش منطقه و در رواناب در پنج منطقه بین تیمار و شاهد اختلاف معنی&#8204;داری (0.05=&lt;/span&gt;&lt;/span&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;P.Value&lt;/span&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;) وجود دارد. اما در متغیرهای بار رسوبی و غلظت رسوب تنها در یک نقطه، بطور معنی&#8204;داری تیمار بالاتر از شاهد است. بین شش منطقه مطالعاتی فقط در متغیر بار رسوبی اختلاف معنی&#8204;داری (0.05=&lt;/span&gt;&lt;/span&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;P.Value&lt;/span&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;) با هم وجود داشت و با در نظر گرفتن توآم هر شش منطقه، بین مقادیر بدست آمده از دو گروه تیمار و شاهد در هر چهار متغیر تحقیق اختلاف معنی&#8204;داری (0.01=&lt;/span&gt;&lt;/span&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;P.Value&lt;/span&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;) مشاهده شد. در نتیجه با توجه به عمومیت داشتن حضور میکروتراس&#8204;های ناشی از لگدکوبی دام در مراتع کشور و اثر معنادار آن بر فرایندهای رواناب، رسوب و نفوذ خاک، لازمست در تدوین و اجرای برنامه مدیریت چرای دام مراتع به نحوی برنامه&#8204;ریزی شود تا توسعه این فرایند متوقف و به خاک مراتع فرصت احیاء مناسب داده شود. &lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/div&gt;
&amp;nbsp;</abstract_fa>
	<abstract>&lt;span style=&quot;font-size:10pt&quot;&gt;&lt;span style=&quot;text-justify:kashida&quot;&gt;&lt;span style=&quot;text-kashida:0%&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;letter-spacing:-.5pt&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;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:10pt&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;letter-spacing:-.5pt&quot;&gt;1- Introduction&lt;/span&gt;&lt;/span&gt;&lt;/b&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;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;span style=&quot;font-size:11.0pt&quot;&gt;&lt;span style=&quot;background:white&quot;&gt;&lt;span style=&quot;letter-spacing:-.3pt&quot;&gt;The most important factors affecting the water infiltration rate on the rangeland surface are livestock trampling and reduced vegetation cover due to excessive grazing. Providing any solution for managing rangeland improvement requires understanding the effect of grazing and enclosure on vegetation cover changes and their relationship with soil parameters, including permeability. Today, the rate of exploitation of the country&amp;#39;s rangelands is much higher than the permissible limit, and the major part of this exploitation is dedicated to livestock. Premature and excessive grazing of rangelands by livestock affects the quantity and quality of vegetation cover, permeability, porosity, soil moisture, runoff, and erosion rate of rangeland soil through compaction and physical destruction of the soil. In this regard, the present study was conducted to investigate the effect of micro-terraces created in livestock traffic routes on runoff, sediment, and permeability in six regions of the rangelands in the Torbat-Heydarieh Senobar watershed within 36 points (18 micro-traces and 18 controls) and using a portable rainfall simulator and double rings.&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;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;background:white&quot;&gt;&lt;span style=&quot;letter-spacing:-.3pt&quot;&gt;2-&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;span style=&quot;font-size:11.0pt&quot;&gt;&lt;span style=&quot;background:white&quot;&gt;&lt;span style=&quot;letter-spacing:-.3pt&quot;&gt; &lt;b&gt;Materials &amp; &lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;b&gt;&lt;span style=&quot;font-size:11.0pt&quot;&gt;&lt;span style=&quot;letter-spacing:-.5pt&quot;&gt;Methods&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;span style=&quot;font-size:11.0pt&quot;&gt;&lt;span style=&quot;background:white&quot;&gt;&lt;span style=&quot;letter-spacing:-.3pt&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;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;span style=&quot;font-size:11.0pt&quot;&gt;&lt;span style=&quot;background:white&quot;&gt;&lt;span style=&quot;letter-spacing:-.3pt&quot;&gt;The rainfall intensity for this study was determined using the Intensity-Duration-Frequency (IDF) curves specific to the region, derived from data collected at the Torbat-Heydariyeh meteorological station near the research area. The intensity was based on runoff observations from preliminary tests, indicating a rainfall rate of 0.9 mm/min, corresponding to a return period of 10 years. During the study, the erosion plots were subjected to simulated rainfall for 15 minutes.&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;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;span style=&quot;font-size:11.0pt&quot;&gt;&lt;span style=&quot;background:white&quot;&gt;&lt;span style=&quot;letter-spacing:-.3pt&quot;&gt;Soil erosion was quantified using an&amp;nbsp;Eijkelkamp rain simulator&amp;nbsp;with a&amp;nbsp;plot area of 30 &amp;times; 30 cm. During precipitation simulation,&amp;nbsp;runoff volume&amp;nbsp;was determined via&amp;nbsp;direct volumetric measurement&amp;nbsp;using a graduated cylinder. The resulting&amp;nbsp;sediment yield&amp;nbsp;was transported to the laboratory, filtered through&amp;nbsp;Whatman 42 filter paper, and subsequently oven-dried at&amp;nbsp;110&amp;deg;C for 24 hours&amp;nbsp;before gravimetric analysis. Additionally,&amp;nbsp;soil permeability&amp;nbsp;was assessed at each sampling point using a&amp;nbsp;double-ring infiltrometer.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt; &lt;span style=&quot;font-size:11.0pt&quot;&gt;&lt;span style=&quot;background:white&quot;&gt;&lt;span style=&quot;letter-spacing:-.3pt&quot;&gt;Following data collection,&amp;nbsp;statistical analyses&amp;nbsp;were performed using&amp;nbsp;SPSS v.27, including&amp;nbsp;one-way ANOVA&amp;nbsp;and&amp;nbsp;independent samples t-test&amp;nbsp;to evaluate significant differences between experimental conditions.&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;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;letter-spacing:-.5pt&quot;&gt;3- Results &lt;/span&gt;&lt;/span&gt;&lt;/b&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;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;span style=&quot;font-size:11.0pt&quot;&gt;&lt;span style=&quot;background:white&quot;&gt;&lt;span style=&quot;letter-spacing:-.3pt&quot;&gt;All selected points for field operations were located in rangelands characterized by hillslopes, specifically within the marl and sandstone geological units. Physiographic factors, such as direction, elevation, and slope, were also carefully chosen to minimize the impact of environmental variability. The normal distribution of data across different groups indicates that environmental changes in the field were not significant. As a result, no interference from external factors was observed, and there was no need for more repetitions in the field experiments.&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;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;span style=&quot;font-size:11.0pt&quot;&gt;&lt;span style=&quot;background:white&quot;&gt;&lt;span style=&quot;letter-spacing:-.3pt&quot;&gt;The results of field data analysis showed a significant difference (P. Value=0.05) in infiltration variables in all six regions and runoff in five regions between the treatment and the control. However, in the sediment load and concentration variables, the treatment was significantly higher than the control at only one point. There was a significant difference (P. Value=0.05) between the six study areas only in the sediment load variable, and considering all six regions together, a significant difference (P. Value=0.01) was observed between the values ​​obtained from the treatment and control groups in all four research variables.&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;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;&amp;nbsp;&lt;b&gt;&lt;span style=&quot;font-size:11.0pt&quot;&gt;&lt;span style=&quot;letter-spacing:-.5pt&quot;&gt;4- Discussion &amp; &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;letter-spacing:-.2pt&quot;&gt;Conclusions&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;letter-spacing:-.5pt&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/b&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;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;span style=&quot;font-size:11.0pt&quot;&gt;&lt;span style=&quot;background:white&quot;&gt;&lt;span style=&quot;letter-spacing:-.3pt&quot;&gt;The analysis of the homogeneous units showed that, with the exception of the sediment load variable and one area affected by lighter soil texture, the six study areas did not exhibit significant differences. However, the four variables -infiltration, sediment load, sediment concentration, and runoff-measured in micro-terraces due to continuous livestock traffic displayed significantly different values compared to the control points.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt; &lt;span style=&quot;font-size:11.0pt&quot;&gt;&lt;span style=&quot;background:white&quot;&gt;&lt;span style=&quot;letter-spacing:-.3pt&quot;&gt;As a result, given the widespread presence of micro-traces caused by livestock trampling in the country&amp;#39;s rangelands and its significant effect on runoff, sediment, and soil infiltration processes, it is necessary to plan in some way in the development and implementation of a rangeland grazing management program to stop the development of soil degradation process and give the rangeland soil a proper recovery opportunity&lt;b&gt;.&lt;/b&gt; Due to the excessive grazing in the country&amp;#39;s rangelands and the pressure on the soil, a fundamental revision of livestock grazing permits and rangeland management plans is necessary. Finally, considering the limitations of the research, it is recommended that the temporal changes in runoff and sediment during the simulation and higher rainfall intensities with different carrying capacities and in heavy soils be examined to summarize the findings.&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>
	<keyword_fa>دبل رینگ, رسوب, روانآب, شبیه‌ساز باران, میکروتراس.</keyword_fa>
	<keyword>Double ring, Micro terrace, Rainfall simulator, Runoff, Sediment.</keyword>
	<start_page>42</start_page>
	<end_page>58</end_page>
	<web_url>http://magazine.hormozgan.ac.ir/browse.php?a_code=A-10-324-4&amp;slc_lang=fa&amp;sid=1</web_url>


<author_list>
	<author>
	<first_name>mehdi</first_name>
	<middle_name></middle_name>
	<last_name>bashiri</last_name>
	<suffix></suffix>
	<first_name_fa>مهدی</first_name_fa>
	<middle_name_fa></middle_name_fa>
	<last_name_fa>بشیری</last_name_fa>
	<suffix_fa></suffix_fa>
	<email>me.bashiri@yahoo.com</email>
	<code>10031947532846009745</code>
	<orcid>10031947532846009745</orcid>
	<coreauthor>Yes
</coreauthor>
	<affiliation>Department of Nature Engineering and Medicinal Plants, Faculty of Agriculture, University of Torbat Heydarieh, Torbat Heydarieh , Iran</affiliation>
	<affiliation_fa>گروه مهندسی طبیعت و گیاهان دارویی، دانشکده کشاورزی، دانشگاه تربت‌حیدریه، تربت‌حیدریه</affiliation_fa>
	 </author>


</author_list>


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