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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></PublisherName>
				<JournalTitle>Journal of Range and Watershed Managment</JournalTitle>
				<Issn>5044-2008</Issn>
				<Volume>67</Volume>
				<Issue>1</Issue>
				<PubDate PubStatus="epublish">
					<Year>2014</Year>
					<Month>04</Month>
					<Day>21</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Developing Models of Daily Sediment Yield Estimation for Kojur Forest Watershed</ArticleTitle>
<VernacularTitle>Developing Models of Daily Sediment Yield Estimation for Kojur Forest Watershed</VernacularTitle>
			<FirstPage>1</FirstPage>
			<LastPage>15</LastPage>
			<ELocationID EIdType="pii">50824</ELocationID>
			
<ELocationID EIdType="doi">10.22059/jrwm.2014.50824</ELocationID>
			
			<Language>FA</Language>
<AuthorList>
<Author>
					<FirstName>Zakariya</FirstName>
					<LastName>Asadolahi</LastName>
<Affiliation>M.Sc. Student, Department. of Watershed Management,
Faculty of Natural Resources, Tarbiat Modares University, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Mahdi</FirstName>
					<LastName>Vafakhah</LastName>
<Affiliation>Assistant Professor, Department of Watershed Management
Engineering, Faculty of Natural Resources, Tarbiat Modares University, Iran</Affiliation>
<Identifier Source="ORCID">0000-0002-8113-9113</Identifier>

</Author>
<Author>
					<FirstName>Seyed Hamidreza</FirstName>
					<LastName>Sadeghi</LastName>
<Affiliation>Professor, Department of Watershed Management
Engineering, Faculty of Natural Resources, Tarbiat Modares University, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2011</Year>
					<Month>12</Month>
					<Day>18</Day>
				</PubDate>
			</History>
		<Abstract>Todays, dynamic models are supposed as the most important tools in erosion and sediment phenomena&lt;br /&gt;due to their complexities and existence of many affecting factors. Towards, the present study was&lt;br /&gt;conducted in the Kojour watershed for daily sediment modeling using daily rainfall, discharge and&lt;br /&gt;sediment during 2007 to 2010. The modeling process was carried out all data and the monthly and&lt;br /&gt;seasonally classification data in linear and nonlinear models. The results indicated that daily linear and&lt;br /&gt;non-linear models did not indicate a suitable model. The monthly and seasonally classification of the&lt;br /&gt;data led to achievement of better models with determination coefficient significant at 5 percent level&lt;br /&gt;and relative error less than 40 percent as compared with those obtained from no classification. It was&lt;br /&gt;also found out that daily sediment of Kojour watershed was affected by discharge occurred event day&lt;br /&gt;and before four days. The discharge occurred event day is the most effective factor in 80% selected&lt;br /&gt;models in the study watershed. The nonlinear models were better estimation than linear models in&lt;br /&gt;July, September, December and March and autumn but linear models were better than nonlinear&lt;br /&gt;models in other months and seasons.</Abstract>
			<OtherAbstract Language="FA">Todays, dynamic models are supposed as the most important tools in erosion and sediment phenomena&lt;br /&gt;due to their complexities and existence of many affecting factors. Towards, the present study was&lt;br /&gt;conducted in the Kojour watershed for daily sediment modeling using daily rainfall, discharge and&lt;br /&gt;sediment during 2007 to 2010. The modeling process was carried out all data and the monthly and&lt;br /&gt;seasonally classification data in linear and nonlinear models. The results indicated that daily linear and&lt;br /&gt;non-linear models did not indicate a suitable model. The monthly and seasonally classification of the&lt;br /&gt;data led to achievement of better models with determination coefficient significant at 5 percent level&lt;br /&gt;and relative error less than 40 percent as compared with those obtained from no classification. It was&lt;br /&gt;also found out that daily sediment of Kojour watershed was affected by discharge occurred event day&lt;br /&gt;and before four days. The discharge occurred event day is the most effective factor in 80% selected&lt;br /&gt;models in the study watershed. The nonlinear models were better estimation than linear models in&lt;br /&gt;July, September, December and March and autumn but linear models were better than nonlinear&lt;br /&gt;models in other months and seasons.</OtherAbstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">daily discharge</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Kojour forest watershed</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Sediment yield</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">statistic model</Param>
			</Object>
		</ObjectList>
</Article>

<Article>
<Journal>
				<PublisherName></PublisherName>
				<JournalTitle>Journal of Range and Watershed Managment</JournalTitle>
				<Issn>5044-2008</Issn>
				<Volume>67</Volume>
				<Issue>1</Issue>
				<PubDate PubStatus="epublish">
					<Year>2014</Year>
					<Month>04</Month>
					<Day>21</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Prediction of Landslide Hazard in Sikan River Basin Using Logistic Regression Model</ArticleTitle>
<VernacularTitle>Prediction of Landslide Hazard in Sikan River Basin Using Logistic Regression Model</VernacularTitle>
			<FirstPage>17</FirstPage>
			<LastPage>29</LastPage>
			<ELocationID EIdType="pii">50825</ELocationID>
			
<ELocationID EIdType="doi">10.22059/jrwm.2014.50825</ELocationID>
			
			<Language>FA</Language>
<AuthorList>
<Author>
					<FirstName>Mohammad Reza</FirstName>
					<LastName>Sarvati</LastName>
<Affiliation>Professor, Faculty of Earth Sciences,
Shahid Beheshti University, Tehran, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Kazem</FirstName>
					<LastName>Nosrati</LastName>
<Affiliation>Assistant Professor, Faculty of Earth Sciences, Shahid Beheshti
University, Tehran, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Shima</FirstName>
					<LastName>Hassanvandi</LastName>
<Affiliation>M.Sc. Student, Geomorphology in Environmental Planning,
Faculty of Earth Sciences, Shahid Beheshti University, Tehran, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Babak</FirstName>
					<LastName>Mirbagheri</LastName>
<Affiliation>Lecturer of RS &amp; GIS Center, Shahid Beheshti University,
Tehran, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2013</Year>
					<Month>01</Month>
					<Day>20</Day>
				</PubDate>
			</History>
		<Abstract>Landslides and slope instabilities are major hazards for human activities often causing economic&lt;br /&gt;losses and property damages. Sikan River Basin (Ilam province) due to the topography, tectonic,&lt;br /&gt;lithology, and climate has enough potential for occurrence of this phenomenon. The objectives of this&lt;br /&gt;study were to determine effective parameters controlling the landslide occurrence and to prepare&lt;br /&gt;zonation map of landslide risk in Sykan River Basin. In view of this, 11 geophysical characteristics&lt;br /&gt;including (height, slop, slop direction), geomorphologic (the slop of land surface), geology (lithology,&lt;br /&gt;the distance from the fault), hydrography (the distance from the river), coverage, land use (land use&lt;br /&gt;and the distance from road, the distance from village), pedology (soil texture), and dependent variable&lt;br /&gt;(landslide distribution) were selected an independent variable and were analyzed using logistic&lt;br /&gt;regression model. The results showed that the influential factors on landslides occurrence in the basin&lt;br /&gt;are the distance from river, land use, the distance from village, the materials (lithology), slope, and the&lt;br /&gt;shape of land surface. Finally, the study area was classified into five major area based on landslide&lt;br /&gt;occurrence risk which 19.1 km2 of total area had very low risk, 15.9 km2 had low risk, 14.9 km2 had&lt;br /&gt;average risk and 14.6 km2 had high risk and 9.1 km2 had also very high risk. The model evaluation&lt;br /&gt;showed a high accuracy 74.2% in the study area. The results of this study can be useful for landslide&lt;br /&gt;risk management and for controlling the accelerated parameters.</Abstract>
			<OtherAbstract Language="FA">Landslides and slope instabilities are major hazards for human activities often causing economic&lt;br /&gt;losses and property damages. Sikan River Basin (Ilam province) due to the topography, tectonic,&lt;br /&gt;lithology, and climate has enough potential for occurrence of this phenomenon. The objectives of this&lt;br /&gt;study were to determine effective parameters controlling the landslide occurrence and to prepare&lt;br /&gt;zonation map of landslide risk in Sykan River Basin. In view of this, 11 geophysical characteristics&lt;br /&gt;including (height, slop, slop direction), geomorphologic (the slop of land surface), geology (lithology,&lt;br /&gt;the distance from the fault), hydrography (the distance from the river), coverage, land use (land use&lt;br /&gt;and the distance from road, the distance from village), pedology (soil texture), and dependent variable&lt;br /&gt;(landslide distribution) were selected an independent variable and were analyzed using logistic&lt;br /&gt;regression model. The results showed that the influential factors on landslides occurrence in the basin&lt;br /&gt;are the distance from river, land use, the distance from village, the materials (lithology), slope, and the&lt;br /&gt;shape of land surface. Finally, the study area was classified into five major area based on landslide&lt;br /&gt;occurrence risk which 19.1 km2 of total area had very low risk, 15.9 km2 had low risk, 14.9 km2 had&lt;br /&gt;average risk and 14.6 km2 had high risk and 9.1 km2 had also very high risk. The model evaluation&lt;br /&gt;showed a high accuracy 74.2% in the study area. The results of this study can be useful for landslide&lt;br /&gt;risk management and for controlling the accelerated parameters.</OtherAbstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">Darrehshahr City</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Landslides</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Logistic regression</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">risk zonation</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Sikan River Basin</Param>
			</Object>
		</ObjectList>
</Article>

<Article>
<Journal>
				<PublisherName></PublisherName>
				<JournalTitle>Journal of Range and Watershed Managment</JournalTitle>
				<Issn>5044-2008</Issn>
				<Volume>67</Volume>
				<Issue>1</Issue>
				<PubDate PubStatus="epublish">
					<Year>2014</Year>
					<Month>04</Month>
					<Day>21</Day>
				</PubDate>
			</Journal>
<ArticleTitle>The Comparison of Soil Loss and Sediment Yield of Some Geology Formations in Plant Vegetation Gradients
(Case study: Summer Rangelands of Balade in Mazandaran Province)</ArticleTitle>
<VernacularTitle>The Comparison of Soil Loss and Sediment Yield of Some Geology Formations in Plant Vegetation Gradients
(Case study: Summer Rangelands of Balade in Mazandaran Province)</VernacularTitle>
			<FirstPage>31</FirstPage>
			<LastPage>44</LastPage>
			<ELocationID EIdType="pii">50826</ELocationID>
			
<ELocationID EIdType="doi">10.22059/jrwm.2014.50826</ELocationID>
			
			<Language>FA</Language>
<AuthorList>
<Author>
					<FirstName>Shafagh</FirstName>
					<LastName>Rastgar</LastName>
<Affiliation>Assistant Professor, Faculty of Natural Resources, Sari
University of Natural Resources and Agricultural Sciences, Sari, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Hossein</FirstName>
					<LastName>Barani</LastName>
<Affiliation>Associate Professor, Faculty of Natural Resources, Gorgan
University of Natural Resources and Agricultural Sciences, Gorgan, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Ali</FirstName>
					<LastName>Darijani</LastName>
<Affiliation>Assistant Professor., Faculty of Agricultural Economy, Gorgan
University of Natural Resources and Agricultural Sciences, Gorgan, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Vahedberdi</FirstName>
					<LastName>Sheikh</LastName>
<Affiliation>Associate Professor, Faculty of Natural Resources, Gorgan
University of Natural Resources and Agricultural Sciences, Gorgan, Iran</Affiliation>
<Identifier Source="ORCID">0000-0002-9091-2868</Identifier>

</Author>
<Author>
					<FirstName>Jamshid</FirstName>
					<LastName>Ghorbani</LastName>
<Affiliation>Associate Professor, Faculty of Natural Resources, Sari
University of Natural Resources and Agricultural Sciences, Sari, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Mohammad</FirstName>
					<LastName>Ghorbani</LastName>
<Affiliation>Professor, Faculty of Agricultural Economy, Ferdowsi
University of Mashad, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2011</Year>
					<Month>12</Month>
					<Day>23</Day>
				</PubDate>
			</History>
		<Abstract>Vegetation cover as the main factor affecting the water erosion plays an important role in preventing&lt;br /&gt;soil loss. To this end, for better understanding the impact of vegetation cover on soil erosion and&lt;br /&gt;sediment yield over the major existing geological formations in the summer rangelands of Balade in&lt;br /&gt;the Mazandaran province, rainfall simulation studies have been carried out using a portable rainfall&lt;br /&gt;simulator. Among many geological formations across the study area, the three major lithological units&lt;br /&gt;of mica sandstone, clay and shale sandstone with coal seams of “SHEMSHAK”, structures of tuff&lt;br /&gt;shale and dark gray to green shale with volcanic rocks of “KARAJ” and limestone of “LAR” have&lt;br /&gt;been selected as lowly, moderately and highly resisting formations to degradation. For each&lt;br /&gt;combination of geological formation and vegetation cover (low, moderate, and high density) three&lt;br /&gt;sampling plots of 1x1m have been selected and rainfall simulation has been conducted over them. For&lt;br /&gt;each plot, the surface characteristics including the vegetation cover, runoff and sediment yield and soil&lt;br /&gt;texture were measured. The measured data were statistically analyzed. Results showed that&lt;br /&gt;“SHEMSHAK”, “KARAJ” and “LAR” formations were respectively ranked from highest to lowest&lt;br /&gt;with respect to the volume and weight of sediment yield. Also, there was a strong inverse relationship&lt;br /&gt;between vegetation cover percentage and volume of runoff and sediment for all investigated&lt;br /&gt;geological formations specially in poor vegetation situation that indicate interaction effects between&lt;br /&gt;vegetation cover and type of geological formations.</Abstract>
			<OtherAbstract Language="FA">Vegetation cover as the main factor affecting the water erosion plays an important role in preventing&lt;br /&gt;soil loss. To this end, for better understanding the impact of vegetation cover on soil erosion and&lt;br /&gt;sediment yield over the major existing geological formations in the summer rangelands of Balade in&lt;br /&gt;the Mazandaran province, rainfall simulation studies have been carried out using a portable rainfall&lt;br /&gt;simulator. Among many geological formations across the study area, the three major lithological units&lt;br /&gt;of mica sandstone, clay and shale sandstone with coal seams of “SHEMSHAK”, structures of tuff&lt;br /&gt;shale and dark gray to green shale with volcanic rocks of “KARAJ” and limestone of “LAR” have&lt;br /&gt;been selected as lowly, moderately and highly resisting formations to degradation. For each&lt;br /&gt;combination of geological formation and vegetation cover (low, moderate, and high density) three&lt;br /&gt;sampling plots of 1x1m have been selected and rainfall simulation has been conducted over them. For&lt;br /&gt;each plot, the surface characteristics including the vegetation cover, runoff and sediment yield and soil&lt;br /&gt;texture were measured. The measured data were statistically analyzed. Results showed that&lt;br /&gt;“SHEMSHAK”, “KARAJ” and “LAR” formations were respectively ranked from highest to lowest&lt;br /&gt;with respect to the volume and weight of sediment yield. Also, there was a strong inverse relationship&lt;br /&gt;between vegetation cover percentage and volume of runoff and sediment for all investigated&lt;br /&gt;geological formations specially in poor vegetation situation that indicate interaction effects between&lt;br /&gt;vegetation cover and type of geological formations.</OtherAbstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">geological formation</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">lithological units</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Nour-rud</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Rainfall simulator</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">vegetation cover</Param>
			</Object>
		</ObjectList>
</Article>

<Article>
<Journal>
				<PublisherName></PublisherName>
				<JournalTitle>Journal of Range and Watershed Managment</JournalTitle>
				<Issn>5044-2008</Issn>
				<Volume>67</Volume>
				<Issue>1</Issue>
				<PubDate PubStatus="epublish">
					<Year>2014</Year>
					<Month>04</Month>
					<Day>21</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Plant Species Distribution Modeling Using Logistic Regression Models in the North East of Semnan</ArticleTitle>
<VernacularTitle>Plant Species Distribution Modeling Using Logistic Regression Models in the North East of Semnan</VernacularTitle>
			<FirstPage>45</FirstPage>
			<LastPage>59</LastPage>
			<ELocationID EIdType="pii">50827</ELocationID>
			
<ELocationID EIdType="doi">10.22059/jrwm.2014.50827</ELocationID>
			
			<Language>FA</Language>
<AuthorList>
<Author>
					<FirstName>Mohammad Ali</FirstName>
					<LastName>Zare Chahouki</LastName>
<Affiliation>Associate Professor, Faculty of Natural Resources, University of Tehran, Karaj, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Lyla</FirstName>
					<LastName>Khalsi Ahvazi</LastName>
<Affiliation>PhD Student, Faculty of Natural Resources, University of
Gorgan, Karaj, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Hossein</FirstName>
					<LastName>Azarnivand</LastName>
<Affiliation>Professor, Faculty of Natural Resources, University of
Tehran, Karaj, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2011</Year>
					<Month>01</Month>
					<Day>11</Day>
				</PubDate>
			</History>
		<Abstract>The aim of this study was providing plant species predictive habitat models by using logistic&lt;br /&gt;regression method. For this purpose, study area conducted in north east rangelands of Semnan&lt;br /&gt;modeling vegetation data in addition to site condition in formation including topography, and soil was&lt;br /&gt;prepared. sampling was done within each unit of sampling parallel transects and 1 vertical transect&lt;br /&gt;with 750m length, each containing 15 quadrates (according to vegetation variations) were established.&lt;br /&gt;Quadrate size was determined for each vegetation type using the minimal area method. Soil samples&lt;br /&gt;were taken from 0-20 cm and 20-80 cm in starting and ending points of each transect. Logestic&lt;br /&gt;regression (LR) techniques were implemented for plant species predictive modeling. To plant&lt;br /&gt;predictive mapping, it is necessary to prepare the maps of all affective factors of models. To mapping&lt;br /&gt;soil characteristics, geostatistical method was used based on obtained predictive models for each&lt;br /&gt;species (through LR method). The accuracy of the predicted maps was tested with actual vegetation&lt;br /&gt;maps. In this study, the adequacy of vegetation type mapping was evaluated using kappa statistics.&lt;br /&gt;Predictive maps of Astragalus spp. ( κ =0.86), Halocnemum strobilaceum ( κ =0.51), Zygophylum&lt;br /&gt;eurypterum ( κ =0.58) and Seidlitzia rosmarrinus ( κ =0.6) with narrow amplitude is as the same of&lt;br /&gt;actual vegetation map prepared for the study area. Predictive model of Artemisia sieberi ( κ =0.33),&lt;br /&gt;due to its ability to grow in most parts of north east rangeland of Semnan with relatively different&lt;br /&gt;habitat condition, is not possible.</Abstract>
			<OtherAbstract Language="FA">The aim of this study was providing plant species predictive habitat models by using logistic&lt;br /&gt;regression method. For this purpose, study area conducted in north east rangelands of Semnan&lt;br /&gt;modeling vegetation data in addition to site condition in formation including topography, and soil was&lt;br /&gt;prepared. sampling was done within each unit of sampling parallel transects and 1 vertical transect&lt;br /&gt;with 750m length, each containing 15 quadrates (according to vegetation variations) were established.&lt;br /&gt;Quadrate size was determined for each vegetation type using the minimal area method. Soil samples&lt;br /&gt;were taken from 0-20 cm and 20-80 cm in starting and ending points of each transect. Logestic&lt;br /&gt;regression (LR) techniques were implemented for plant species predictive modeling. To plant&lt;br /&gt;predictive mapping, it is necessary to prepare the maps of all affective factors of models. To mapping&lt;br /&gt;soil characteristics, geostatistical method was used based on obtained predictive models for each&lt;br /&gt;species (through LR method). The accuracy of the predicted maps was tested with actual vegetation&lt;br /&gt;maps. In this study, the adequacy of vegetation type mapping was evaluated using kappa statistics.&lt;br /&gt;Predictive maps of Astragalus spp. ( κ =0.86), Halocnemum strobilaceum ( κ =0.51), Zygophylum&lt;br /&gt;eurypterum ( κ =0.58) and Seidlitzia rosmarrinus ( κ =0.6) with narrow amplitude is as the same of&lt;br /&gt;actual vegetation map prepared for the study area. Predictive model of Artemisia sieberi ( κ =0.33),&lt;br /&gt;due to its ability to grow in most parts of north east rangeland of Semnan with relatively different&lt;br /&gt;habitat condition, is not possible.</OtherAbstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">Geostatistical Method</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Kappa statistics</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Logistic regression</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">predictive map</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Semnan rangelands</Param>
			</Object>
		</ObjectList>
</Article>

<Article>
<Journal>
				<PublisherName></PublisherName>
				<JournalTitle>Journal of Range and Watershed Managment</JournalTitle>
				<Issn>5044-2008</Issn>
				<Volume>67</Volume>
				<Issue>1</Issue>
				<PubDate PubStatus="epublish">
					<Year>2014</Year>
					<Month>04</Month>
					<Day>21</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Effects of Agricultural Activities on Land Degradation in the Khatam City</ArticleTitle>
<VernacularTitle>Effects of Agricultural Activities on Land Degradation in the Khatam City</VernacularTitle>
			<FirstPage>61</FirstPage>
			<LastPage>72</LastPage>
			<ELocationID EIdType="pii">50828</ELocationID>
			
<ELocationID EIdType="doi">10.22059/jrwm.2014.50828</ELocationID>
			
			<Language>FA</Language>
<AuthorList>
<Author>
					<FirstName>Gholamreza</FirstName>
					<LastName>Zehtabian</LastName>
<Affiliation>Professor, Faculty of Natural Resources, University of
Tehran, Karaj, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Hassan</FirstName>
					<LastName>Khosravi</LastName>
<Affiliation>Assistance Professor, Faculty of Natural Resources,
University of Tehran, Karaj, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Ali</FirstName>
					<LastName>Azareh</LastName>
<Affiliation>PhD Student, Faculty of Natural Resources, University of Tehran,
Karaj, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2012</Year>
					<Month>03</Month>
					<Day>03</Day>
				</PubDate>
			</History>
		<Abstract>Need to Increasing agricultural land in order to improve food resources in the past two centuries recent&lt;br /&gt;lead to widespread changes in land use and improper management of these lands. Continue this&lt;br /&gt;process can lead to land degradation and desertification, and improve such soils is very costly;&lt;br /&gt;Therefore, prevention of land degradation is more desirable. This function requires to research on the&lt;br /&gt;utilization of land agricultural and how to use. With this aim, the Khatam city was selected as the&lt;br /&gt;study region and various maps of the region, including soil, land use and height maps was prepared to&lt;br /&gt;help ArcGIS9.3 and ENVI software. Four dominant land region mention mono cultivated and multi&lt;br /&gt;cultivated systems under irrigation, garden lands and range lands as control treatments were&lt;br /&gt;considered as the treatments. The soil was sampled and soil factors in two corrective factors, including&lt;br /&gt;correction factors N, P, K, CO, Caco3, Mg and damaging factors Hco3, Cl, Na, pH, EC and SAR at&lt;br /&gt;depth 0 to 30 cm of the soil surface horizons were studied. Factors the design of split plots showed that&lt;br /&gt;there are significant differences between treatments in the region and soil of region is relatively poor&lt;br /&gt;from CO, N, K and P in soils Rdhy. The comparison of treatment means with Duncan Mean&lt;br /&gt;Comparison indicated that the garden lands as the most suitable treatments and range lands as the most&lt;br /&gt;unsuitable one.</Abstract>
			<OtherAbstract Language="FA">Need to Increasing agricultural land in order to improve food resources in the past two centuries recent&lt;br /&gt;lead to widespread changes in land use and improper management of these lands. Continue this&lt;br /&gt;process can lead to land degradation and desertification, and improve such soils is very costly;&lt;br /&gt;Therefore, prevention of land degradation is more desirable. This function requires to research on the&lt;br /&gt;utilization of land agricultural and how to use. With this aim, the Khatam city was selected as the&lt;br /&gt;study region and various maps of the region, including soil, land use and height maps was prepared to&lt;br /&gt;help ArcGIS9.3 and ENVI software. Four dominant land region mention mono cultivated and multi&lt;br /&gt;cultivated systems under irrigation, garden lands and range lands as control treatments were&lt;br /&gt;considered as the treatments. The soil was sampled and soil factors in two corrective factors, including&lt;br /&gt;correction factors N, P, K, CO, Caco3, Mg and damaging factors Hco3, Cl, Na, pH, EC and SAR at&lt;br /&gt;depth 0 to 30 cm of the soil surface horizons were studied. Factors the design of split plots showed that&lt;br /&gt;there are significant differences between treatments in the region and soil of region is relatively poor&lt;br /&gt;from CO, N, K and P in soils Rdhy. The comparison of treatment means with Duncan Mean&lt;br /&gt;Comparison indicated that the garden lands as the most suitable treatments and range lands as the most&lt;br /&gt;unsuitable one.</OtherAbstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">Agriculture</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Khatam city</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Land degradation</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">split plot scheme</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">suitable and unsuitable treatment</Param>
			</Object>
		</ObjectList>
</Article>

<Article>
<Journal>
				<PublisherName></PublisherName>
				<JournalTitle>Journal of Range and Watershed Managment</JournalTitle>
				<Issn>5044-2008</Issn>
				<Volume>67</Volume>
				<Issue>1</Issue>
				<PubDate PubStatus="epublish">
					<Year>2014</Year>
					<Month>04</Month>
					<Day>21</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Effects of Shrubs on Preserving Understory Plants against the Livestock Grazing</ArticleTitle>
<VernacularTitle>Effects of Shrubs on Preserving Understory Plants against the Livestock Grazing</VernacularTitle>
			<FirstPage>73</FirstPage>
			<LastPage>82</LastPage>
			<ELocationID EIdType="pii">50829</ELocationID>
			
<ELocationID EIdType="doi">10.22059/jrwm.2014.50829</ELocationID>
			
			<Language>FA</Language>
<AuthorList>
<Author>
					<FirstName>Tahereh</FirstName>
					<LastName>Sadeghi Shahrakht</LastName>
<Affiliation>M.Sc Student, Department of Range and Watershed Management, Faculty of Natural Resources and Environment, Ferdowsi University of Mashhad, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Mohammad</FirstName>
					<LastName>Jankju</LastName>
<Affiliation>Assistant Professor, Department of Range and Watershed
Management, Faculty of Natural Resources and Environment, Ferdowsi University
of Mashhad, Mashhad, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Mansour</FirstName>
					<LastName>Mesdaghi</LastName>
<Affiliation>Assistant Professor, Department of Range and Watershed
Management, Faculty of Natural Resources and Environment, Ferdowsi University
of Mashhad, Mashhad, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2013</Year>
					<Month>04</Month>
					<Day>26</Day>
				</PubDate>
			</History>
		<Abstract>Rangeland shrubs may provide mechanical facilitation on their understory plants, by protecting them&lt;br /&gt;against the livestock grazing. However, such a facilitation effect may vary depending on the rangeland&lt;br /&gt;utilization rate. In a field research, mechanical facilitation of rangeland shrubs was compared in a&lt;br /&gt;highly grazed, a moderately grazed and an enclosure site; in an arid rangeland, Kakhak, Gonabad,&lt;br /&gt;Iran, during spring to summer 2011. Twenty line transects were established in various directions and&lt;br /&gt;slope aspects. Forage production was measured by clipping method within the paired plots, i.e. under&lt;br /&gt;the canopy of nursing shrubs and their nearby open areas. In the enclosure site, forage production was&lt;br /&gt;similar under the canopy of shrubs and in open areas, whereas in the highly and moderately grazed&lt;br /&gt;sites there were more forage under the canopies. These results indicate increases in mechanical&lt;br /&gt;facilitation of rangeland shrubs by increasing the grazing intensity. The mechanical facilitation was&lt;br /&gt;also varied depending on the life forms of understory species. In the enclosure, the greatest facilitation&lt;br /&gt;was on annual forbs, whereas in the highly grazed site it was on perennial grasses. Results of this&lt;br /&gt;study show important role of rangeland shrubs on preserving understory forage plant against the&lt;br /&gt;intense livestock grazing.</Abstract>
			<OtherAbstract Language="FA">Rangeland shrubs may provide mechanical facilitation on their understory plants, by protecting them&lt;br /&gt;against the livestock grazing. However, such a facilitation effect may vary depending on the rangeland&lt;br /&gt;utilization rate. In a field research, mechanical facilitation of rangeland shrubs was compared in a&lt;br /&gt;highly grazed, a moderately grazed and an enclosure site; in an arid rangeland, Kakhak, Gonabad,&lt;br /&gt;Iran, during spring to summer 2011. Twenty line transects were established in various directions and&lt;br /&gt;slope aspects. Forage production was measured by clipping method within the paired plots, i.e. under&lt;br /&gt;the canopy of nursing shrubs and their nearby open areas. In the enclosure site, forage production was&lt;br /&gt;similar under the canopy of shrubs and in open areas, whereas in the highly and moderately grazed&lt;br /&gt;sites there were more forage under the canopies. These results indicate increases in mechanical&lt;br /&gt;facilitation of rangeland shrubs by increasing the grazing intensity. The mechanical facilitation was&lt;br /&gt;also varied depending on the life forms of understory species. In the enclosure, the greatest facilitation&lt;br /&gt;was on annual forbs, whereas in the highly grazed site it was on perennial grasses. Results of this&lt;br /&gt;study show important role of rangeland shrubs on preserving understory forage plant against the&lt;br /&gt;intense livestock grazing.</OtherAbstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">grazing stress</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">mechanical facilitation</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">nurse shrubs</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">understory</Param>
			</Object>
		</ObjectList>
</Article>

<Article>
<Journal>
				<PublisherName></PublisherName>
				<JournalTitle>Journal of Range and Watershed Managment</JournalTitle>
				<Issn>5044-2008</Issn>
				<Volume>67</Volume>
				<Issue>1</Issue>
				<PubDate PubStatus="epublish">
					<Year>2014</Year>
					<Month>04</Month>
					<Day>21</Day>
				</PubDate>
			</Journal>
<ArticleTitle>The Study of Biological Soil Crust (Mosses) Roles in Protection of Surface Soil in front of Water Erosion
(Case study: Rangelands around Torogh Dam in Khorasan Razavi Province)</ArticleTitle>
<VernacularTitle>The Study of Biological Soil Crust (Mosses) Roles in Protection of Surface Soil in front of Water Erosion
(Case study: Rangelands around Torogh Dam in Khorasan Razavi Province)</VernacularTitle>
			<FirstPage>83</FirstPage>
			<LastPage>92</LastPage>
			<ELocationID EIdType="pii">50830</ELocationID>
			
<ELocationID EIdType="doi">10.22059/jrwm.2014.50830</ELocationID>
			
			<Language>FA</Language>
<AuthorList>
<Author>
					<FirstName>Fariba</FirstName>
					<LastName>Alavizadeh</LastName>
<Affiliation>Msc Student of Range Management, Natural Resources and Environment Faculty, Ferdowsi University of Mashhad, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Kamalledin</FirstName>
					<LastName>Naseri</LastName>
<Affiliation>Professor of Natural Resources and Environment Faculty, Ferdowsi University of Mashhad, Iran</Affiliation>
<Identifier Source="ORCID">0000-0003-3824-4011</Identifier>

</Author>
<Author>
					<FirstName>Ali</FirstName>
					<LastName>Golkarian</LastName>
<Affiliation>Professor of Natural Resources and Environment Faculty,
Ferdowsi University of Mashhad, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Ali</FirstName>
					<LastName>Tavili</LastName>
<Affiliation>Professor, Faculty of Natural Resources, University of Tehran, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2013</Year>
					<Month>10</Month>
					<Day>08</Day>
				</PubDate>
			</History>
		<Abstract>Soil erosion is a main hazard in most area of the country specially in arid and semi-arid regions and it&lt;br /&gt;is very important because of sedimentation, pollution, increased flooding and its negative effects on&lt;br /&gt;soil productivity. One of the features of arid and semi-arid areas is the presence of low cover of&lt;br /&gt;vascular plants. These empty spaces are usually good niches for biological soil crusts or cryptogams&lt;br /&gt;like mosses. These crusts contribute to a variety of ecological functions and have different effects on&lt;br /&gt;soil features and vascular plants. The present study was carried out in the rangelands of Torogh dam&lt;br /&gt;basin of Khorasan- Razavi province in order to find the effects of such kind of plants (mosses) on&lt;br /&gt;water erosion. For this purpose, artificial runoff streams in plots with two intensity (low and high) for&lt;br /&gt;30 minutes. In order to study the effects of different amount of mosses on sedimentation and specific&lt;br /&gt;erosion, four different density of mosses in the same experimental situation were studied: high (60-&lt;br /&gt;75% of plot), medium (35-50% of plot), low (10-20% of plot) and control (0%). The results of&lt;br /&gt;analysis of variance and tukey method by the use of Minitab software showed a significant difference&lt;br /&gt;in 95% level between the four considered density of mosses and the two intensity of water. As mosses&lt;br /&gt;density decrease, sedimentation and specific erosion increased consequently. But there were no&lt;br /&gt;significant differences in infiltration between the different treatments.</Abstract>
			<OtherAbstract Language="FA">Soil erosion is a main hazard in most area of the country specially in arid and semi-arid regions and it&lt;br /&gt;is very important because of sedimentation, pollution, increased flooding and its negative effects on&lt;br /&gt;soil productivity. One of the features of arid and semi-arid areas is the presence of low cover of&lt;br /&gt;vascular plants. These empty spaces are usually good niches for biological soil crusts or cryptogams&lt;br /&gt;like mosses. These crusts contribute to a variety of ecological functions and have different effects on&lt;br /&gt;soil features and vascular plants. The present study was carried out in the rangelands of Torogh dam&lt;br /&gt;basin of Khorasan- Razavi province in order to find the effects of such kind of plants (mosses) on&lt;br /&gt;water erosion. For this purpose, artificial runoff streams in plots with two intensity (low and high) for&lt;br /&gt;30 minutes. In order to study the effects of different amount of mosses on sedimentation and specific&lt;br /&gt;erosion, four different density of mosses in the same experimental situation were studied: high (60-&lt;br /&gt;75% of plot), medium (35-50% of plot), low (10-20% of plot) and control (0%). The results of&lt;br /&gt;analysis of variance and tukey method by the use of Minitab software showed a significant difference&lt;br /&gt;in 95% level between the four considered density of mosses and the two intensity of water. As mosses&lt;br /&gt;density decrease, sedimentation and specific erosion increased consequently. But there were no&lt;br /&gt;significant differences in infiltration between the different treatments.</OtherAbstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">biological crust</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Infiltration</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">moss</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">sedimentation</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Water erosion</Param>
			</Object>
		</ObjectList>
</Article>

<Article>
<Journal>
				<PublisherName></PublisherName>
				<JournalTitle>Journal of Range and Watershed Managment</JournalTitle>
				<Issn>5044-2008</Issn>
				<Volume>67</Volume>
				<Issue>1</Issue>
				<PubDate PubStatus="epublish">
					<Year>2014</Year>
					<Month>04</Month>
					<Day>21</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Comparing the Accuracy of Soil Map Prepared by Geopedology and Usual Method of Iran (Case Study: Kouhin)</ArticleTitle>
<VernacularTitle>Comparing the Accuracy of Soil Map Prepared by Geopedology and Usual Method of Iran (Case Study: Kouhin)</VernacularTitle>
			<FirstPage>93</FirstPage>
			<LastPage>102</LastPage>
			<ELocationID EIdType="pii">50831</ELocationID>
			
<ELocationID EIdType="doi">10.22059/jrwm.2014.50831</ELocationID>
			
			<Language>FA</Language>
<AuthorList>
<Author>
					<FirstName>Zohreh</FirstName>
					<LastName>Alijani</LastName>
<Affiliation>Graduate student, Soil Science Engineering Department,
University of Tehran, Karaj, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Fereydoun</FirstName>
					<LastName>Sarmadian</LastName>
<Affiliation>Professor, Soil Science Engineering Department, University of Tehran, Karaj, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Seyed Rouhollah</FirstName>
					<LastName>Mousavi</LastName>
<Affiliation>Graduate student, Soil Science Engineering Department, University of Tehran, Karaj, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2013</Year>
					<Month>12</Month>
					<Day>24</Day>
				</PubDate>
			</History>
		<Abstract>Today, extensive improvements in fields of soil mapping have increased the purity and accuracy of&lt;br /&gt;soil maps. Usual mapping methods moreover depend on skills and experience of surveyor in&lt;br /&gt;identifying and delineating the boundaries, also need the high cost and time consuming that face the&lt;br /&gt;soil mapping with restrictions. In this study, aerial photographs with 1/40000 scale were used in order&lt;br /&gt;to preparation of the initial interpretive map and determination of sample region. Then, the numbers of&lt;br /&gt;24 profiles were described in determined units. After sampling and necessary physicochemical tests,&lt;br /&gt;soil map of Kouhin (Qazvin) was prepared and accuracy of map was calculated in two methods in all&lt;br /&gt;levels of taxonomy. The first method was formation of error matrix and calculation of kappa index and&lt;br /&gt;second was comparison the geopedological map with described profiles and evaluation the results of&lt;br /&gt;each. Then a part of a geopedological map that had overlapping with map prepared by usual method&lt;br /&gt;was compared with this map. Results showed the overall accuracy of 67.5, 90.5 and 98.5 percent in&lt;br /&gt;levels of family- subgroup and great group- suborder and order of soil for geopedological method&lt;br /&gt;respectively.</Abstract>
			<OtherAbstract Language="FA">Today, extensive improvements in fields of soil mapping have increased the purity and accuracy of&lt;br /&gt;soil maps. Usual mapping methods moreover depend on skills and experience of surveyor in&lt;br /&gt;identifying and delineating the boundaries, also need the high cost and time consuming that face the&lt;br /&gt;soil mapping with restrictions. In this study, aerial photographs with 1/40000 scale were used in order&lt;br /&gt;to preparation of the initial interpretive map and determination of sample region. Then, the numbers of&lt;br /&gt;24 profiles were described in determined units. After sampling and necessary physicochemical tests,&lt;br /&gt;soil map of Kouhin (Qazvin) was prepared and accuracy of map was calculated in two methods in all&lt;br /&gt;levels of taxonomy. The first method was formation of error matrix and calculation of kappa index and&lt;br /&gt;second was comparison the geopedological map with described profiles and evaluation the results of&lt;br /&gt;each. Then a part of a geopedological map that had overlapping with map prepared by usual method&lt;br /&gt;was compared with this map. Results showed the overall accuracy of 67.5, 90.5 and 98.5 percent in&lt;br /&gt;levels of family- subgroup and great group- suborder and order of soil for geopedological method&lt;br /&gt;respectively.</OtherAbstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">accuracy of soil map</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">geopedology</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">soil map units</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">usual method of Iran</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">validation</Param>
			</Object>
		</ObjectList>
</Article>

<Article>
<Journal>
				<PublisherName></PublisherName>
				<JournalTitle>Journal of Range and Watershed Managment</JournalTitle>
				<Issn>5044-2008</Issn>
				<Volume>67</Volume>
				<Issue>1</Issue>
				<PubDate PubStatus="epublish">
					<Year>2014</Year>
					<Month>04</Month>
					<Day>21</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Suitable Species Diversity Abundance Model in Three Grazing Intensities in Dizaj Batchi Rangelands of West
Azerbaijan</ArticleTitle>
<VernacularTitle>Suitable Species Diversity Abundance Model in Three Grazing Intensities in Dizaj Batchi Rangelands of West
Azerbaijan</VernacularTitle>
			<FirstPage>103</FirstPage>
			<LastPage>115</LastPage>
			<ELocationID EIdType="pii">50832</ELocationID>
			
<ELocationID EIdType="doi">10.22059/jrwm.2014.50832</ELocationID>
			
			<Language>FA</Language>
<AuthorList>
<Author>
					<FirstName>Javad</FirstName>
					<LastName>Motamedi</LastName>
<Affiliation>Assistant professor, Department of Range and Watershed
Management, Faculty of Natural Resources, University of Urmia, Urmia, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Esmaeil</FirstName>
					<LastName>Sheidai Karkaj</LastName>
<Affiliation>Ph.D Student Rangeland sciences, Gorgan University of Agricultural Sciences and Natural Resources, Gorgan, Iran</Affiliation>
<Identifier Source="ORCID">0000-0003-2281-0357</Identifier>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2014</Year>
					<Month>03</Month>
					<Day>15</Day>
				</PubDate>
			</History>
		<Abstract>Species diversity is one of the important characteristics shows rangeland ecosystems changes, which is&lt;br /&gt;already under effects of management practices. Thus, this research was conducted to study species&lt;br /&gt;diversity variation and assess suitable distributive abundance model in three rangeland sites in West&lt;br /&gt;Azerbaijan. These sites were almost similar in environmental properties and differ in view point of&lt;br /&gt;grazing intensity (light, moderate and heavy intensities). After selecting sampling areas in each of the&lt;br /&gt;sites, species cover were recorded in 60, one square meter quadrates with 10 meter far from each other&lt;br /&gt;which established along 100 meter transects in sites and then richness, evenness and diversity&lt;br /&gt;(heterogeneity) indices were calculated. Thus, rank-abundance curves were plotted and four&lt;br /&gt;distribution models such as log-normal, geometric, log-series and Brocken stick were fitted to each of&lt;br /&gt;these sites and then best model was selected in 0.05 level of confidence. Means comparison test&lt;br /&gt;showed that richness, evenness and heterogeneity indices have significant differences (P&lt;0.01) in&lt;br /&gt;sites. Highest diversity is observed in the light grazing intensity site and lowest diversity is in heavy&lt;br /&gt;grazing intensity site. Species rank-abundance curves point out that low-abundance species are seen&lt;br /&gt;lower in light grazing site and its curve have gentler slope than moderate and high grazing intensity&lt;br /&gt;sites thus its diversity is higher. There is lowest species number in high grazing intensity site and&lt;br /&gt;evenness is lowest too due to its high number of rare and dominant species. Log-normal model was&lt;br /&gt;fitted to light site implying on sustainable community and high grazing intensity site is fitted with&lt;br /&gt;geometric model which point out on distractive communities with low diversity. Overall results&lt;br /&gt;showed that implementing light grazing can protect species diversity and heavy intensity declines&lt;br /&gt;species diversity that this shows the need considering of management on implementing light grazing&lt;br /&gt;intensity in the rangeland.</Abstract>
			<OtherAbstract Language="FA">Species diversity is one of the important characteristics shows rangeland ecosystems changes, which is&lt;br /&gt;already under effects of management practices. Thus, this research was conducted to study species&lt;br /&gt;diversity variation and assess suitable distributive abundance model in three rangeland sites in West&lt;br /&gt;Azerbaijan. These sites were almost similar in environmental properties and differ in view point of&lt;br /&gt;grazing intensity (light, moderate and heavy intensities). After selecting sampling areas in each of the&lt;br /&gt;sites, species cover were recorded in 60, one square meter quadrates with 10 meter far from each other&lt;br /&gt;which established along 100 meter transects in sites and then richness, evenness and diversity&lt;br /&gt;(heterogeneity) indices were calculated. Thus, rank-abundance curves were plotted and four&lt;br /&gt;distribution models such as log-normal, geometric, log-series and Brocken stick were fitted to each of&lt;br /&gt;these sites and then best model was selected in 0.05 level of confidence. Means comparison test&lt;br /&gt;showed that richness, evenness and heterogeneity indices have significant differences (P&lt;0.01) in&lt;br /&gt;sites. Highest diversity is observed in the light grazing intensity site and lowest diversity is in heavy&lt;br /&gt;grazing intensity site. Species rank-abundance curves point out that low-abundance species are seen&lt;br /&gt;lower in light grazing site and its curve have gentler slope than moderate and high grazing intensity&lt;br /&gt;sites thus its diversity is higher. There is lowest species number in high grazing intensity site and&lt;br /&gt;evenness is lowest too due to its high number of rare and dominant species. Log-normal model was&lt;br /&gt;fitted to light site implying on sustainable community and high grazing intensity site is fitted with&lt;br /&gt;geometric model which point out on distractive communities with low diversity. Overall results&lt;br /&gt;showed that implementing light grazing can protect species diversity and heavy intensity declines&lt;br /&gt;species diversity that this shows the need considering of management on implementing light grazing&lt;br /&gt;intensity in the rangeland.</OtherAbstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">abundance distribution model</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Dizaj Batchi rangelands</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Livestock grazing</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">species diversity</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">West Azerbaijan</Param>
			</Object>
		</ObjectList>
</Article>

<Article>
<Journal>
				<PublisherName></PublisherName>
				<JournalTitle>Journal of Range and Watershed Managment</JournalTitle>
				<Issn>5044-2008</Issn>
				<Volume>67</Volume>
				<Issue>1</Issue>
				<PubDate PubStatus="epublish">
					<Year>2014</Year>
					<Month>04</Month>
					<Day>21</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Determining of Effective Factors on Gully Longitudinal Advancement (Case study: Dareh Koreh Watershed)</ArticleTitle>
<VernacularTitle>Determining of Effective Factors on Gully Longitudinal Advancement (Case study: Dareh Koreh Watershed)</VernacularTitle>
			<FirstPage>117</FirstPage>
			<LastPage>126</LastPage>
			<ELocationID EIdType="pii">50833</ELocationID>
			
<ELocationID EIdType="doi">10.22059/jrwm.2014.50833</ELocationID>
			
			<Language>FA</Language>
<AuthorList>
<Author>
					<FirstName>Aliakbar</FirstName>
					<LastName>Nazari Samani</LastName>
<Affiliation>Assistant Professor, Faculty of Natural Resources, University of Tehran, Karaj, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Fatemeh</FirstName>
					<LastName>Avazadeh Tavakoli</LastName>
<Affiliation>Senior Expert, Agricultural and Natural Resources Research
Center of Bousher Province, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Hassan</FirstName>
					<LastName>Ahmadi</LastName>
<Affiliation>Professor, Islamic Azad University, Science and Research Branch, Tehran, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Gholamreza</FirstName>
					<LastName>Rahi</LastName>
<Affiliation>Ph.D Student of Watershed Management, University of
Mazandaran, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2010</Year>
					<Month>02</Month>
					<Day>24</Day>
				</PubDate>
			</History>
		<Abstract>Gully erosion is one of the most destructive types of channeled water erosion that removes a&lt;br /&gt;considerable volume of soil as it develops. This type of erosion consists of complex a geomorphic&lt;br /&gt;process that has been known as an indicator of accelerated soil erosion. In this research the&lt;br /&gt;advancement of 25 headcuts were assessed through digital interpretation of multi-temporal aerial&lt;br /&gt;photos, field observations and GIS data analysis over the two periods of 1967-1995 and 1995-2008.&lt;br /&gt;Moreover, the stepwise regression analysis procedure was applied to extract the effective factors on&lt;br /&gt;gully head advancement (such as topography, physico-chemical soil attributes and morphology of&lt;br /&gt;gully). The results indicated that the mean of gully head advancement over the periods of 1967-1995,&lt;br /&gt;1995-2008 and the mean of two periods were measured 1.36, 1.23 and 1.3 m/y, respectively. Further,&lt;br /&gt;regression analysis revealed that headcut&#039;s contribution area, distance of gully-head to ridge, height of&lt;br /&gt;gully head cut and SAR are the main factors on gully head advancement. Therefore, distance to ridge,&lt;br /&gt;headcut high and presence of plunge pool could use as suitable criteria to distinguish the active gullies&lt;br /&gt;in order to prioritizing the conservation activities.</Abstract>
			<OtherAbstract Language="FA">Gully erosion is one of the most destructive types of channeled water erosion that removes a&lt;br /&gt;considerable volume of soil as it develops. This type of erosion consists of complex a geomorphic&lt;br /&gt;process that has been known as an indicator of accelerated soil erosion. In this research the&lt;br /&gt;advancement of 25 headcuts were assessed through digital interpretation of multi-temporal aerial&lt;br /&gt;photos, field observations and GIS data analysis over the two periods of 1967-1995 and 1995-2008.&lt;br /&gt;Moreover, the stepwise regression analysis procedure was applied to extract the effective factors on&lt;br /&gt;gully head advancement (such as topography, physico-chemical soil attributes and morphology of&lt;br /&gt;gully). The results indicated that the mean of gully head advancement over the periods of 1967-1995,&lt;br /&gt;1995-2008 and the mean of two periods were measured 1.36, 1.23 and 1.3 m/y, respectively. Further,&lt;br /&gt;regression analysis revealed that headcut&#039;s contribution area, distance of gully-head to ridge, height of&lt;br /&gt;gully head cut and SAR are the main factors on gully head advancement. Therefore, distance to ridge,&lt;br /&gt;headcut high and presence of plunge pool could use as suitable criteria to distinguish the active gullies&lt;br /&gt;in order to prioritizing the conservation activities.</OtherAbstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">aerial photos</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">distance from ridge</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">erosion</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">gully</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">headcut advancement</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Regression</Param>
			</Object>
		</ObjectList>
</Article>

<Article>
<Journal>
				<PublisherName></PublisherName>
				<JournalTitle>Journal of Range and Watershed Managment</JournalTitle>
				<Issn>5044-2008</Issn>
				<Volume>67</Volume>
				<Issue>1</Issue>
				<PubDate PubStatus="epublish">
					<Year>2014</Year>
					<Month>04</Month>
					<Day>21</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Application of Artificial Neural Networks in Simulating and Forecasting of Meteorological Drought Decile
Percentage Index (Case study: Sistan &amp; Balouchestan Province)</ArticleTitle>
<VernacularTitle>Application of Artificial Neural Networks in Simulating and Forecasting of Meteorological Drought Decile
Percentage Index (Case study: Sistan &amp; Balouchestan Province)</VernacularTitle>
			<FirstPage>127</FirstPage>
			<LastPage>139</LastPage>
			<ELocationID EIdType="pii">50834</ELocationID>
			
<ELocationID EIdType="doi">10.22059/jrwm.2014.50834</ELocationID>
			
			<Language>FA</Language>
<AuthorList>
<Author>
					<FirstName>Arash</FirstName>
					<LastName>Malekian</LastName>
<Affiliation>Assistant Professor, Faculty of Natural Resources, University
of Tehran, Karaj, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Mahrou</FirstName>
					<LastName>Dehbozorgi</LastName>
<Affiliation>Ph.D Student, Faculty of Natural Resources, University of Tehran, Karaj, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Amir Houshang</FirstName>
					<LastName>Ehsani</LastName>
<Affiliation>Assistant Professor, Faculty of Environment, University
of Tehran, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Amir Reza</FirstName>
					<LastName>Keshtkar</LastName>
<Affiliation>Assistant Professor, International Desert Research Center,
University of Tehran, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2013</Year>
					<Month>02</Month>
					<Day>02</Day>
				</PubDate>
			</History>
		<Abstract>Consecutive droughts in Sistan and Baloochestan province cause water resources restriction and this is&lt;br /&gt;a very significant problem for this region. In this study, in order to forecast the drought cycle in 9&lt;br /&gt;climatological stations in the province, we used Artificial Neural Networks. The input data were&lt;br /&gt;average of annual rainfall data in all stations and also deciles precipitation index, which the first 30&lt;br /&gt;years from 1971 to 2000 used for training the network and the last 8 years from 2001 to 2008 for&lt;br /&gt;simulating it. The network consists of Multilayer Perceptron (MLP) and Back Propagation Algorithm&lt;br /&gt;(BP) and also sigmoid transfer function. Number of Neurons in hidden layer was 10 with 1-10-1&lt;br /&gt;structure and was calculated based on the lowest RMSE. Then drought prediction was done in neural&lt;br /&gt;network with the trained algorithm and without using actual and observed data in 2009 to 2012.&lt;br /&gt;Results showed that, the network was able to simulate and forecast DPI index with 97% regression&lt;br /&gt;and average RMSE error less than 5%. According to drought indices, results showed that the drought&lt;br /&gt;will have an increasing trend in all stations in this region in 2009 to 2011. Therefore, by using this&lt;br /&gt;method, drought can be predicted in later years without any need to have actual meteorological data&lt;br /&gt;and also can be used in water resources management, drought management and climate changes.</Abstract>
			<OtherAbstract Language="FA">Consecutive droughts in Sistan and Baloochestan province cause water resources restriction and this is&lt;br /&gt;a very significant problem for this region. In this study, in order to forecast the drought cycle in 9&lt;br /&gt;climatological stations in the province, we used Artificial Neural Networks. The input data were&lt;br /&gt;average of annual rainfall data in all stations and also deciles precipitation index, which the first 30&lt;br /&gt;years from 1971 to 2000 used for training the network and the last 8 years from 2001 to 2008 for&lt;br /&gt;simulating it. The network consists of Multilayer Perceptron (MLP) and Back Propagation Algorithm&lt;br /&gt;(BP) and also sigmoid transfer function. Number of Neurons in hidden layer was 10 with 1-10-1&lt;br /&gt;structure and was calculated based on the lowest RMSE. Then drought prediction was done in neural&lt;br /&gt;network with the trained algorithm and without using actual and observed data in 2009 to 2012.&lt;br /&gt;Results showed that, the network was able to simulate and forecast DPI index with 97% regression&lt;br /&gt;and average RMSE error less than 5%. According to drought indices, results showed that the drought&lt;br /&gt;will have an increasing trend in all stations in this region in 2009 to 2011. Therefore, by using this&lt;br /&gt;method, drought can be predicted in later years without any need to have actual meteorological data&lt;br /&gt;and also can be used in water resources management, drought management and climate changes.</OtherAbstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">Artificial Neural Network</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">deciles precipitation index</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Drought</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">perceptron</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">prediction</Param>
			</Object>
		</ObjectList>
</Article>

<Article>
<Journal>
				<PublisherName></PublisherName>
				<JournalTitle>Journal of Range and Watershed Managment</JournalTitle>
				<Issn>5044-2008</Issn>
				<Volume>67</Volume>
				<Issue>1</Issue>
				<PubDate PubStatus="epublish">
					<Year>2014</Year>
					<Month>04</Month>
					<Day>21</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Stakeholders’ Analysis, Social Power and Network Analysis in Natural Resources Co-Management</ArticleTitle>
<VernacularTitle>Stakeholders’ Analysis, Social Power and Network Analysis in Natural Resources Co-Management</VernacularTitle>
			<FirstPage>141</FirstPage>
			<LastPage>157</LastPage>
			<ELocationID EIdType="pii">50835</ELocationID>
			
<ELocationID EIdType="doi">10.22059/jrwm.2014.50835</ELocationID>
			
			<Language>FA</Language>
<AuthorList>
<Author>
					<FirstName>Mahdi</FirstName>
					<LastName>Ghorbani</LastName>
<Affiliation>Assistant Professor, Faculty of Natural Resources, University
of Tehran, Karaj, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Mahrou</FirstName>
					<LastName>Dehbozorgi</LastName>
<Affiliation>Ph.D Student, Faculty of Natural Resources, University of
Tehran, Karaj, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2013</Year>
					<Month>07</Month>
					<Day>11</Day>
				</PubDate>
			</History>
		<Abstract>Nowadays, a lot of natural resource co-management plans due to lack of attention to stakeholders’&lt;br /&gt;characteristics and position in network of social relationships have failed. Actors or key personnel’s&lt;br /&gt;recognition has been one of administrative requirement of natural resources co-management plans.&lt;br /&gt;The most influential actors in environmental decisions making can be identified based on stakeholders&lt;br /&gt;and network analysis. This study is aimed to determine the social powers based on network analysis&lt;br /&gt;approach and stakeholders analysis at the local users level of common rangeland of Nariyan village in&lt;br /&gt;Taleghan region. In this study, first, Rangeland users were identified based on survey methods then&lt;br /&gt;trust and cooperation matrixes are produced and then degree centralities index and betweenness&lt;br /&gt;centrality were computed by questionnaire finally each actor’s topology has shown in the network.&lt;br /&gt;The result of this research is effective in identifying actors with central position that perform a key&lt;br /&gt;role in Nariyan rangeland co-management plan. Also, the result of this study can assist natural&lt;br /&gt;resource managers and planers in identifying social powers in order to organize and implement the&lt;br /&gt;sustainable landscape management plans.</Abstract>
			<OtherAbstract Language="FA">Nowadays, a lot of natural resource co-management plans due to lack of attention to stakeholders’&lt;br /&gt;characteristics and position in network of social relationships have failed. Actors or key personnel’s&lt;br /&gt;recognition has been one of administrative requirement of natural resources co-management plans.&lt;br /&gt;The most influential actors in environmental decisions making can be identified based on stakeholders&lt;br /&gt;and network analysis. This study is aimed to determine the social powers based on network analysis&lt;br /&gt;approach and stakeholders analysis at the local users level of common rangeland of Nariyan village in&lt;br /&gt;Taleghan region. In this study, first, Rangeland users were identified based on survey methods then&lt;br /&gt;trust and cooperation matrixes are produced and then degree centralities index and betweenness&lt;br /&gt;centrality were computed by questionnaire finally each actor’s topology has shown in the network.&lt;br /&gt;The result of this research is effective in identifying actors with central position that perform a key&lt;br /&gt;role in Nariyan rangeland co-management plan. Also, the result of this study can assist natural&lt;br /&gt;resource managers and planers in identifying social powers in order to organize and implement the&lt;br /&gt;sustainable landscape management plans.</OtherAbstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">actors’ centrality</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">natural resources co-management</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Social network analysis</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">social power</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">stakeholders’ analysis</Param>
			</Object>
		</ObjectList>
</Article>

<Article>
<Journal>
				<PublisherName></PublisherName>
				<JournalTitle>Journal of Range and Watershed Managment</JournalTitle>
				<Issn>5044-2008</Issn>
				<Volume>67</Volume>
				<Issue>1</Issue>
				<PubDate PubStatus="epublish">
					<Year>2014</Year>
					<Month>04</Month>
					<Day>21</Day>
				</PubDate>
			</Journal>
<ArticleTitle>English Abstracts</ArticleTitle>
<VernacularTitle>English Abstracts</VernacularTitle>
			<FirstPage>1</FirstPage>
			<LastPage>14</LastPage>
			<ELocationID EIdType="pii">50836</ELocationID>
			
<ELocationID EIdType="doi">10.22059/jrwm.2014.50836</ELocationID>
			
			<Language>FA</Language>
<AuthorList>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2014</Year>
					<Month>07</Month>
					<Day>12</Day>
				</PubDate>
			</History>
		<Abstract></Abstract>
			<OtherAbstract Language="FA"></OtherAbstract>
</Article>
</ArticleSet>
