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<Article>
<Journal>
				<PublisherName>University of Tehran Press</PublisherName>
				<JournalTitle>Desert</JournalTitle>
				<Issn>2008-0875</Issn>
				<Volume>14</Volume>
				<Issue>2</Issue>
				<PubDate PubStatus="epublish">
					<Year>2009</Year>
					<Month>12</Month>
					<Day>01</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Investigation of the Variations of Soil Factors under Haloxylon aphyllum Cultivation</ArticleTitle>
<VernacularTitle></VernacularTitle>
			<FirstPage>114</FirstPage>
			<LastPage>117</LastPage>
			<ELocationID EIdType="pii">36324</ELocationID>
			
<ELocationID EIdType="doi">10.22059/jdesert.2009.36324</ELocationID>
			
			<Language>EN</Language>
<AuthorList>
<Author>
					<FirstName>B.</FirstName>
					<LastName>Rasooli</LastName>
<Affiliation>Faculty Member, Faculty of Agriculture, Rasht Islamic Azad University, Rasht, Iran</Affiliation>

</Author>
<Author>
					<FirstName>M.</FirstName>
					<LastName>Jafari</LastName>
<Affiliation>Professor, Faculty of Natural Resources, University of Tehran, Karaj, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2006</Year>
					<Month>09</Month>
					<Day>13</Day>
				</PubDate>
			</History>
		<Abstract>Determination of the relationships between soil and plant cover indispensible in the in planning and management&lt;br /&gt;of the arid regions, the aim being to revitalize plant cover, conserve soil and to combat desertification. Among factors&lt;br /&gt;affecting plant cover, particularly in arid and semiarid areas are soil traits. During the present study, the effect of&lt;br /&gt;Haloxylon aphyllum Cultivation on soil physiochemical properties (at different depths) was investigated. A split plot&lt;br /&gt;design was employedin the study, in which cultivated and non-cultivated areas were considered as inter-related&lt;br /&gt;factors, whereas soil depths of(0-10), (10-30) and (30-60) cm as intra- related factors. Soil texture, EC, pH, nitrogen,&lt;br /&gt;phosphorous and organic matter was assessed. Soluble salts of Na, Ca, Mg, Cl, K, carbonate and bicarbonate were&lt;br /&gt;measured. Haloxylon aphyllum has led to a significant difference between Ca, Mg and bicarbonate in the first layer as&lt;br /&gt;compared with the third. A significant difference has been observed between nitrogen in the first soil layer in&lt;br /&gt;comparison with that in the second layer. Significant differences were also observed among all Haloxylon aphyllum&lt;br /&gt;cultivated soil layers as to the contents of Soluble K, absorbable K as well as phosphorous.</Abstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">soil</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Physiochemical properties</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Haloxylon aphyllum</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Split plot</Param>
			</Object>
		</ObjectList>
<ArchiveCopySource DocType="pdf">https://jdesert.ut.ac.ir/article_36324_617b9db10ae00aa85fe4a19db0e03c53.pdf</ArchiveCopySource>
</Article>

<Article>
<Journal>
				<PublisherName>University of Tehran Press</PublisherName>
				<JournalTitle>Desert</JournalTitle>
				<Issn>2008-0875</Issn>
				<Volume>14</Volume>
				<Issue>2</Issue>
				<PubDate PubStatus="epublish">
					<Year>2009</Year>
					<Month>12</Month>
					<Day>01</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Identification of Critical Sediment Source Areas at Regional Scale for Environmental Management (Case Study: Dehnamak Basin, Iran)</ArticleTitle>
<VernacularTitle></VernacularTitle>
			<FirstPage>119</FirstPage>
			<LastPage>125</LastPage>
			<ELocationID EIdType="pii">36327</ELocationID>
			
<ELocationID EIdType="doi">10.22059/jdesert.2009.36327</ELocationID>
			
			<Language>EN</Language>
<AuthorList>
<Author>
					<FirstName>H.</FirstName>
					<LastName>Ahmadi</LastName>
<Affiliation>Professor, Faculty of Natural Resources, University of Tehran, Karaj, Iran</Affiliation>

</Author>
<Author>
					<FirstName>A. A.</FirstName>
					<LastName>Mohammadi</LastName>
<Affiliation>Ph.D. Student of Wartershed Management, Science and Research Branch, Islamic Azad University, Tehran, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2008</Year>
					<Month>05</Month>
					<Day>08</Day>
				</PubDate>
			</History>
		<Abstract>To identify critical sediment sources in large catchments, using easily available terrain information at a regional&lt;br /&gt;scale, a methodology was developed to obtain a qualitative assessment necessary for environmental management.&lt;br /&gt;Fargas et al method was employed in the research. The study was carried out in one of the sub-basins of Hableh Rood&lt;br /&gt;basin called Dehnamak in the arid and semiarid climate of Iran. The main objective of the model is to use basic&lt;br /&gt;terrain data related to the erosive processes that contribute to the production, transportation and accumulation of&lt;br /&gt;sediments throughout the main water paths in the watershed. This model is based on a selection of homogeneous&lt;br /&gt;zones regarding drainage density and lithology, achieved through interrelating the basic units based on a rating&lt;br /&gt;system. The values of drainage density are rated according to an erosion class. The lithology is rated by erosion&lt;br /&gt;indexes, adapted from FAO (1977). The combination and reclassification of the results brings about five qualitative&lt;br /&gt;classes of sediment risk according to Fargas et al (1997). The advantage of this method is that only two main factors&lt;br /&gt;of erosion, namely lithology and drainage density are employed in it, and these factors are available in our geological&lt;br /&gt;and topographic maps in Iran. This methodology has been employed for studying the watershed Dehnamak in NE&lt;br /&gt;Iran with an area of 248 km2. The mapping scale was 1:50000 and the model implemented through a vector GIS (Arc&lt;br /&gt;View). The validation was carried out through interpretation of aerial photos and fieldwork which revealed a viability&lt;br /&gt;of 75.15%. The tested methodology has been proven useful as an initial approach for erosion assessment and soil&lt;br /&gt;conservation planning at regional level, as well as for a selection of priority areas where further analyses can be made&lt;br /&gt;to finally manage the environment.
To identify critical sediment sources in large catchments, using easily available terrain information at a regional&lt;br /&gt;scale, a methodology was developed to obtain a qualitative assessment necessary for environmental management.&lt;br /&gt;Fargas et al method was employed in the research. The study was carried out in one of the sub-basins of Hableh Rood&lt;br /&gt;basin called Dehnamak in the arid and semiarid climate of Iran. The main objective of the model is to use basic&lt;br /&gt;terrain data related to the erosive processes that contribute to the production, transportation and accumulation of&lt;br /&gt;sediments throughout the main water paths in the watershed. This model is based on a selection of homogeneous&lt;br /&gt;zones regarding drainage density and lithology, achieved through interrelating the basic units based on a rating&lt;br /&gt;system. The values of drainage density are rated according to an erosion class. The lithology is rated by erosion&lt;br /&gt;indexes, adapted from FAO (1977). The combination and reclassification of the results brings about five qualitative&lt;br /&gt;classes of sediment risk according to Fargas et al (1997). The advantage of this method is that only two main factors&lt;br /&gt;of erosion, namely lithology and drainage density are employed in it, and these factors are available in our geological&lt;br /&gt;and topographic maps in Iran. This methodology has been employed for studying the watershed Dehnamak in NE&lt;br /&gt;Iran with an area of 248 km2. The mapping scale was 1:50000 and the model implemented through a vector GIS (Arc&lt;br /&gt;View). The validation was carried out through interpretation of aerial photos and fieldwork which revealed a viability&lt;br /&gt;of 75.15%. The tested methodology has been proven useful as an initial approach for erosion assessment and soil&lt;br /&gt;conservation planning at regional level, as well as for a selection of priority areas where further analyses can be made&lt;br /&gt;to finally manage the environment.</Abstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">Dehnamak basin</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Sediment sources</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">aerial photos</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">GIS</Param>
			</Object>
		</ObjectList>
<ArchiveCopySource DocType="pdf">https://jdesert.ut.ac.ir/article_36327_2232e45b0f04506610ffe04f7a377621.pdf</ArchiveCopySource>
</Article>

<Article>
<Journal>
				<PublisherName>University of Tehran Press</PublisherName>
				<JournalTitle>Desert</JournalTitle>
				<Issn>2008-0875</Issn>
				<Volume>14</Volume>
				<Issue>2</Issue>
				<PubDate PubStatus="epublish">
					<Year>2009</Year>
					<Month>12</Month>
					<Day>01</Day>
				</PubDate>
			</Journal>
<ArticleTitle>The Evaluation of Contaminated Soil by Petroleum Mulch in Combating Desertification</ArticleTitle>
<VernacularTitle></VernacularTitle>
			<FirstPage>127</FirstPage>
			<LastPage>132</LastPage>
			<ELocationID EIdType="pii">36332</ELocationID>
			
<ELocationID EIdType="doi">10.22059/jdesert.2009.36332</ELocationID>
			
			<Language>EN</Language>
<AuthorList>
<Author>
					<FirstName>H.</FirstName>
					<LastName>Akbarnia</LastName>
<Affiliation>Scientific Member, Research Institute of Petroleum Industry (RIPI), National Iranian Oil Company, Tehran, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2008</Year>
					<Month>02</Month>
					<Day>05</Day>
				</PubDate>
			</History>
		<Abstract>The most usual type of petroleum mulch, which has been successfully used to combat desertification in large area&lt;br /&gt;in Iran for more than thirty years, is produced by heavy residue petroleum cuts. The petroleum mulch consists of a&lt;br /&gt;wide range of different heavy hydrocarbons such as Polycyclic Aromatic Hydrocarbons (PAHs). PAHs are present at&lt;br /&gt;low level in petroleum mulch, where there is contact with water and soil and the potential for transferring of&lt;br /&gt;compounds into environment. Some of PAHS especially benzo (a) pyrene (BaP) have been recommended for&lt;br /&gt;determining and comparing with standard criteria on causing cancer .Although Iran has a long domestic experience in&lt;br /&gt;sand dune fixation by using petroleum products but so far there is no proper research in probable effects of using&lt;br /&gt;petroleum mulch on environment either in Iran or any other involved countries. In this study it was assumed that&lt;br /&gt;rainfall and temperature would affect mulch disintegration process, then considering these parameters, different&lt;br /&gt;climatic zones in three provinces -Khuzestan, Kerman and Sistan - were selected and samples were prepared from&lt;br /&gt;several sites of any provinces, both in mulch-sprayed sites and non-sprayed sites (observation). In order to estimate&lt;br /&gt;the content of PAHs, several soil samples were taken in different depths from the above-mentioned sites. Quartering&lt;br /&gt;Procedure selected the soil samples beneath mulch layer and the PAHS analysis was performed by solvent extraction&lt;br /&gt;and HPLC method with UV fluorescence detection and results were compared to standard criteria. The results&lt;br /&gt;indicated that the content of PAHs and mostly BaP in petroleum mulch and soil samples beneath mulch layer are less&lt;br /&gt;than the permitted limit in national standards. This component, in the depth of 5 cm, decreased to 1/40 of the initial&lt;br /&gt;even after years. Then, it shows very low penetration. Therefore, the petroleum mulch and contaminated soils can be&lt;br /&gt;considered as safe materials.
The most usual type of petroleum mulch, which has been successfully used to combat desertification in large area&lt;br /&gt;in Iran for more than thirty years, is produced by heavy residue petroleum cuts. The petroleum mulch consists of a&lt;br /&gt;wide range of different heavy hydrocarbons such as Polycyclic Aromatic Hydrocarbons (PAHs). PAHs are present at&lt;br /&gt;low level in petroleum mulch, where there is contact with water and soil and the potential for transferring of&lt;br /&gt;compounds into environment. Some of PAHS especially benzo (a) pyrene (BaP) have been recommended for&lt;br /&gt;determining and comparing with standard criteria on causing cancer .Although Iran has a long domestic experience in&lt;br /&gt;sand dune fixation by using petroleum products but so far there is no proper research in probable effects of using&lt;br /&gt;petroleum mulch on environment either in Iran or any other involved countries. In this study it was assumed that&lt;br /&gt;rainfall and temperature would affect mulch disintegration process, then considering these parameters, different&lt;br /&gt;climatic zones in three provinces -Khuzestan, Kerman and Sistan - were selected and samples were prepared from&lt;br /&gt;several sites of any provinces, both in mulch-sprayed sites and non-sprayed sites (observation). In order to estimate&lt;br /&gt;the content of PAHs, several soil samples were taken in different depths from the above-mentioned sites. Quartering&lt;br /&gt;Procedure selected the soil samples beneath mulch layer and the PAHS analysis was performed by solvent extraction&lt;br /&gt;and HPLC method with UV fluorescence detection and results were compared to standard criteria. The results&lt;br /&gt;indicated that the content of PAHs and mostly BaP in petroleum mulch and soil samples beneath mulch layer are less&lt;br /&gt;than the permitted limit in national standards. This component, in the depth of 5 cm, decreased to 1/40 of the initial&lt;br /&gt;even after years. Then, it shows very low penetration. Therefore, the petroleum mulch and contaminated soils can be&lt;br /&gt;considered as safe materials.</Abstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">Petroleum mulch</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Polycyclic aromatic hydrocarbon</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">contaminated soil</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Desertification</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Sand dune fixation</Param>
			</Object>
		</ObjectList>
<ArchiveCopySource DocType="pdf">https://jdesert.ut.ac.ir/article_36332_de3c3d0c97be17d6327fd3d7866480ad.pdf</ArchiveCopySource>
</Article>

<Article>
<Journal>
				<PublisherName>University of Tehran Press</PublisherName>
				<JournalTitle>Desert</JournalTitle>
				<Issn>2008-0875</Issn>
				<Volume>14</Volume>
				<Issue>2</Issue>
				<PubDate PubStatus="epublish">
					<Year>2009</Year>
					<Month>12</Month>
					<Day>01</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Spatio-Temporal Analysis of Drought Vulnerability using the Standardized Precipitation Index (Case study: Semnan Province, Iran)</ArticleTitle>
<VernacularTitle></VernacularTitle>
			<FirstPage>133</FirstPage>
			<LastPage>140</LastPage>
			<ELocationID EIdType="pii">36333</ELocationID>
			
<ELocationID EIdType="doi">10.22059/jdesert.2009.36333</ELocationID>
			
			<Language>EN</Language>
<AuthorList>
<Author>
					<FirstName>M.</FirstName>
					<LastName>Karimpour Reyhan</LastName>
<Affiliation>Associate Professor, International Desert Research Center, University of Tehran, Tehran, Iran</Affiliation>

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

</Author>
<Author>
					<FirstName>A.</FirstName>
					<LastName>Malekian</LastName>
<Affiliation>Assistant Professor, International Desert Research Center, University of Tehran, Tehran, Iran</Affiliation>

</Author>
<Author>
					<FirstName>N.</FirstName>
					<LastName>Mashhadi</LastName>
<Affiliation>Assistant Professor, International Desert Research Center, University of Tehran, Tehran, Iran</Affiliation>

</Author>
<Author>
					<FirstName>N.</FirstName>
					<LastName>Kamali</LastName>
<Affiliation>MSc. Graduate, Faculty of Natural Resources, University of Tehran, Karaj, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2008</Year>
					<Month>02</Month>
					<Day>04</Day>
				</PubDate>
			</History>
		<Abstract>This study was conducted to identify drought event and its emerging regions in Markazi desert, Iran with focus on&lt;br /&gt;Semnan province in a 30 years statistical period. In this research, 61 stations having adequate data selected and used&lt;br /&gt;after extracting annual statistic from monthly and daily data. Standardized precipitation index values for each station&lt;br /&gt;were calculated and classified. The Results have shown that there was drought condition in 17 studied stations. Also&lt;br /&gt;among 44 stations with no drought condition, there was one humid year in 20 cases. Khareh sarlazor station has the&lt;br /&gt;first position of drought and humid condition among other stations, with 10 drought years and 5 humid years. The&lt;br /&gt;number of common years with normal condition is 3 years and the most extensive drought in 1999 has occurred in 10&lt;br /&gt;dry stations and 1 very dry station. The existence of common trend of variation using study of correlation among&lt;br /&gt;stations has resulted in determination of 7 groups which these results can be useful according to temporal distance of&lt;br /&gt;one or two years in appearing drought in the same group of stations.</Abstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">Drought</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Standardized Precipitation Index</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Semnan</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Iran</Param>
			</Object>
		</ObjectList>
<ArchiveCopySource DocType="pdf">https://jdesert.ut.ac.ir/article_36333_db3045ee86aae100c376bcb89420cd05.pdf</ArchiveCopySource>
</Article>

<Article>
<Journal>
				<PublisherName>University of Tehran Press</PublisherName>
				<JournalTitle>Desert</JournalTitle>
				<Issn>2008-0875</Issn>
				<Volume>14</Volume>
				<Issue>2</Issue>
				<PubDate PubStatus="epublish">
					<Year>2009</Year>
					<Month>12</Month>
					<Day>01</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Solar Radiation Estimation from Rainfall and Temperature Data in Arid and Semi-arid Climates of Iran</ArticleTitle>
<VernacularTitle></VernacularTitle>
			<FirstPage>141</FirstPage>
			<LastPage>150</LastPage>
			<ELocationID EIdType="pii">36334</ELocationID>
			
<ELocationID EIdType="doi">10.22059/jdesert.2009.36334</ELocationID>
			
			<Language>EN</Language>
<AuthorList>
<Author>
					<FirstName>N.</FirstName>
					<LastName>Ghahreman</LastName>
<Affiliation>Asst. Prof., College of Soil and Water Engineering, University of Tehran, Karaj, Iran</Affiliation>

</Author>
<Author>
					<FirstName>B.</FirstName>
					<LastName>Bakhtiari</LastName>
<Affiliation>Shahid Bahonar University of Kerman, Kerman, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2008</Year>
					<Month>05</Month>
					<Day>23</Day>
				</PubDate>
			</History>
		<Abstract>Precipitation and air temperature data, only, are often recorded at meteorological stations, with radiation being&lt;br /&gt;measured at very few weather stations, especially in developing countries. Therefore there arises a need for suitable&lt;br /&gt;models to estimate solar radiation for a completion of data sets. This paper is about an evaluation of eight models for&lt;br /&gt;an estimation of daily solar radiation (Q) from commonly measured variables in six synoptic stations of Iran, namely:&lt;br /&gt;Mashhad, Kerman, Tabriz, Esfehan, Hamedan and Zanjan using daily rainfall and temperature data for a duration of&lt;br /&gt;three years of 2000, 2001 and 2002. These stations represent several arid and semiarid sub-climates of Iran as based&lt;br /&gt;on extended-De Martonne climatic classification (semiarid-cold: Mashhad and Tabriz, arid-cold: Esfehan, Kerman,&lt;br /&gt;semiarid-extracold: Hamedan and Zanjan). The STATISTICA (ver. 6.0) software was employed for non-linear&lt;br /&gt;multivariate regression. The results indicated that most of the models overestimated in lower values of solar radiation&lt;br /&gt;while underestimating in the higher ranges, indicating a systematic error. Performance of the models was evaluated&lt;br /&gt;based on the Root Mean Square Errors (RMSE) as well as R2. RMSE ranged from 1.14 to 7.76 Cal cm-2min-1 for the&lt;br /&gt;whole data range and in all the six stations. Among the eight models, the Richardson model rendered the best&lt;br /&gt;agreement with the measured data in Kerman and Zanjan stations. In case of Hamedan station, Bristow and Campbell&lt;br /&gt;model was the most suitable. As for Tabriz station, De Jong and Stewart model using rainfall and range of daily&lt;br /&gt;temperature data led to the best performance. In Mashhad station, McCaskill equation can be recommended. Analysis&lt;br /&gt;of the data in Esfehan station showed no significant difference among the models. Due to variation in equations&#039;&lt;br /&gt;performances, to come to valid conclusions and to choose the most suitable radiation models, further study would be&lt;br /&gt;required from other climatic regions the country.</Abstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">Radiation models</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Rainfall</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Solar radiation</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">temperature</Param>
			</Object>
		</ObjectList>
<ArchiveCopySource DocType="pdf">https://jdesert.ut.ac.ir/article_36334_3687ed95bf6ed44550c082e8c9f5b219.pdf</ArchiveCopySource>
</Article>

<Article>
<Journal>
				<PublisherName>University of Tehran Press</PublisherName>
				<JournalTitle>Desert</JournalTitle>
				<Issn>2008-0875</Issn>
				<Volume>14</Volume>
				<Issue>2</Issue>
				<PubDate PubStatus="epublish">
					<Year>2009</Year>
					<Month>12</Month>
					<Day>01</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Competition of Different Densities of Wild Mustard (Brassica kaber) and Rapeseed (Brassica napus) in Greenhouse</ArticleTitle>
<VernacularTitle></VernacularTitle>
			<FirstPage>151</FirstPage>
			<LastPage>155</LastPage>
			<ELocationID EIdType="pii">36335</ELocationID>
			
<ELocationID EIdType="doi">10.22059/jdesert.2009.36335</ELocationID>
			
			<Language>EN</Language>
<AuthorList>
<Author>
					<FirstName>R.</FirstName>
					<LastName>Naderi</LastName>
<Affiliation>Former M.Sc. Student, College of Agriculture, Shiraz University, Shiraz, Iran</Affiliation>

</Author>
<Author>
					<FirstName>H.</FirstName>
					<LastName>Ghadiri</LastName>
<Affiliation>Professor, College of Agriculture, Shiraz University, Shiraz, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2008</Year>
					<Month>09</Month>
					<Day>30</Day>
				</PubDate>
			</History>
		<Abstract>A greenhouse experiment was conducted to evaluate the competitive effects of different densities of wild mustard&lt;br /&gt;as against rapeseed. The experiment was performed in a randomized complete block design with four replications&lt;br /&gt;using replacement series in which wild mustard and rapeseed were respectively planted in different ratios of 4:0, 3:1,&lt;br /&gt;2:2, 1:3 and 0:4 plants per pot. Results indicated that the maximum height, number of siliques per plant, silique length&lt;br /&gt;and number of seeds per silique in rapeseed vs. the maximum height, silique length and number of seeds per silique&lt;br /&gt;in wild mustard were obtained in their monoculture states. Overall evaluation of relative yield showed that both&lt;br /&gt;species were exploiting the resources in different ways or even somehow benefiting each other. Relative crowding&lt;br /&gt;coefficient of rapeseed as against wild mustard in the 3:1 treatment was greater than that in the other plant ratio&lt;br /&gt;treatments. Competition indices revealed that rapeseed benefited from a more competitive ability than wild mustard.</Abstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">Competition</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">replacement series</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">rapeseed</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Wild mustard</Param>
			</Object>
		</ObjectList>
<ArchiveCopySource DocType="pdf">https://jdesert.ut.ac.ir/article_36335_489d8603422865de649389c66f50e281.pdf</ArchiveCopySource>
</Article>

<Article>
<Journal>
				<PublisherName>University of Tehran Press</PublisherName>
				<JournalTitle>Desert</JournalTitle>
				<Issn>2008-0875</Issn>
				<Volume>14</Volume>
				<Issue>2</Issue>
				<PubDate PubStatus="epublish">
					<Year>2009</Year>
					<Month>12</Month>
					<Day>01</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Comparison of Some Split-window Algorithms to Estimate Land Surface Temperature from AVHRR Data in Southeastern Tehran,</ArticleTitle>
<VernacularTitle></VernacularTitle>
			<FirstPage>157</FirstPage>
			<LastPage>161</LastPage>
			<ELocationID EIdType="pii">36336</ELocationID>
			
<ELocationID EIdType="doi">10.22059/jdesert.2009.36336</ELocationID>
			
			<Language>EN</Language>
<AuthorList>
<Author>
					<FirstName>S.M. R.</FirstName>
					<LastName>Behbahani</LastName>
<Affiliation>Irrigation and Drainage Engineering Department, College of Abureyhan ,University of Tehran, Tehran, Iran</Affiliation>

</Author>
<Author>
					<FirstName>A.</FirstName>
					<LastName>Rahimikhoob</LastName>
<Affiliation>Irrigation and Drainage Engineering Department, College of Abureyhan ,University of Tehran, Tehran, Iran</Affiliation>

</Author>
<Author>
					<FirstName>M. H.</FirstName>
					<LastName>Nazarifar</LastName>
<Affiliation>Irrigation and Drainage Engineering Department, College of Abureyhan ,University of Tehran, Tehran, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2008</Year>
					<Month>11</Month>
					<Day>01</Day>
				</PubDate>
			</History>
		<Abstract>Land surface temperature (LST) is a significant parameter for many applications. Many studies have proposed&lt;br /&gt;various algorithms, such as the split-window method, for retrieving surface temperatures from two spectrally&lt;br /&gt;adjacent thermal infrared bands of satellite data. Each algorithm is developed for a limited study area and&lt;br /&gt;application. In this paper, as part of developing an optimal split-window method in the southeast of Tehran province,&lt;br /&gt;Iran, four commonly applied algorithms to retrieve the LST from AVHRR were compared. This study was carried&lt;br /&gt;out in a wheat farm site located in the Pakdasht Agricultural Region. Measurements of LST over the farm were made&lt;br /&gt;with a manual infrared radiometer at the time of NOAA overpass for 18 days of May to June 2004. These days were&lt;br /&gt;cloud free over the study area. A total of 18 NOAA images were acquired for the days that LST measurements were&lt;br /&gt;made. The temperatures derived by the different split-window algorithms were compared to ground truth&lt;br /&gt;measurements. The performance of the split window algorithms was checked with three statistical indices: root mean&lt;br /&gt;square error (RMSE), mean bias error (MBE) and coefficient of determination (R2). The results showed that the&lt;br /&gt;Ulivieri split-window algorithm produced the lowest value of RMSE and MBE (2.71 and 0.26 K, respectively) and&lt;br /&gt;its highest value of R2 (0.92) gave more accurate results than the other algorithms.</Abstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">Land surface temperature</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">NOAA</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Split-window</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Iran</Param>
			</Object>
		</ObjectList>
<ArchiveCopySource DocType="pdf">https://jdesert.ut.ac.ir/article_36336_6db54674d2a0dc14f7c5a346e7f80995.pdf</ArchiveCopySource>
</Article>

<Article>
<Journal>
				<PublisherName>University of Tehran Press</PublisherName>
				<JournalTitle>Desert</JournalTitle>
				<Issn>2008-0875</Issn>
				<Volume>14</Volume>
				<Issue>2</Issue>
				<PubDate PubStatus="epublish">
					<Year>2009</Year>
					<Month>12</Month>
					<Day>01</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Effects of Salt Stress on Vegetative Growth and Ion Accumulation of Two alfalfa (Medicago sativa L.) Cultivars</ArticleTitle>
<VernacularTitle></VernacularTitle>
			<FirstPage>163</FirstPage>
			<LastPage>169</LastPage>
			<ELocationID EIdType="pii">36337</ELocationID>
			
<ELocationID EIdType="doi">10.22059/jdesert.2009.36337</ELocationID>
			
			<Language>EN</Language>
<AuthorList>
<Author>
					<FirstName>Y.</FirstName>
					<LastName>Emam</LastName>
<Affiliation>Professor, College of Agricultural, Shiraz University, Shiraz, Iran</Affiliation>

</Author>
<Author>
					<FirstName>E.</FirstName>
					<LastName>Bijanzadeh</LastName>
<Affiliation>Faculty member, College of Agriculture and Natural Resources of Darab, Shiraz University, Shiraz, Iran</Affiliation>

</Author>
<Author>
					<FirstName>R.</FirstName>
					<LastName>Naderi</LastName>
<Affiliation>PhD. student, Shiraz University, Shiraz, Iran</Affiliation>

</Author>
<Author>
					<FirstName>M.</FirstName>
					<LastName>Edalat</LastName>
<Affiliation>PhD. student, Shiraz University, Shiraz, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2008</Year>
					<Month>11</Month>
					<Day>23</Day>
				</PubDate>
			</History>
		<Abstract>Salt stress is one of the most chalanging abiotic stresses affecting natural productivity and causing significant crop&lt;br /&gt;losses worldwide. A greenhouse experiment was conducted to evaluate the response of two alfalfa cultivars (Bami&lt;br /&gt;and Hamedani) to 6 levels of salinity (0 as control, 25, 50, 75, 100, 125 mM NaCl) at the College of Agriculture,&lt;br /&gt;Shiraz University, Shiraz, Iran in 2008. Plant dry weight per pot in both cultivars decreased with increasing salinity&lt;br /&gt;levels. However, Bami as compared to Hamedani, with the lowest Na+ sequestration, produced the greater dry matter&lt;br /&gt;weight. Leaf area per pot was significantly affected by salt stress with Bami cultivar showing a higher leaf area than&lt;br /&gt;Hamedani. Na+ accumulation also increased by increase in the salinity level in either one of the cultivars; however,&lt;br /&gt;Na+ sequestration of Bami as compared to Hamedani, was lower due to Na+ exclusion mechanisms occurring in this&lt;br /&gt;cultivar. Although Cl- accumulation increased with increasing salinity level in either one of the cultivars, Claccumulation&lt;br /&gt;was higher in Hamedani than in the other cultivar. Similar to K+/Na+ ratio, Ca2+/Na+ ratio also&lt;br /&gt;decreased by an increase in salt stress levels and there were highly significant differences observed between 25 and&lt;br /&gt;125 mM of NaCl in either one of the cultivars. There was a strong positive relationship observed between plant dry&lt;br /&gt;matter weight and leaf relative water content for both Bami (R2=0.94) and Hamedani (R2=0.96) cultivars under salt&lt;br /&gt;stress conditions. All in all, it appears that less adverse effect of salinity on Bami cultivar has made it suitable for&lt;br /&gt;growth in saline soils as compared to Hamedani in saline areas prevailent in south Iran.</Abstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">Alfalfa</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">NaCl</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">K+/Na+ Ratio</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">dry weight</Param>
			</Object>
		</ObjectList>
<ArchiveCopySource DocType="pdf">https://jdesert.ut.ac.ir/article_36337_37704257b6b1aef908ce287b3893ea74.pdf</ArchiveCopySource>
</Article>

<Article>
<Journal>
				<PublisherName>University of Tehran Press</PublisherName>
				<JournalTitle>Desert</JournalTitle>
				<Issn>2008-0875</Issn>
				<Volume>14</Volume>
				<Issue>2</Issue>
				<PubDate PubStatus="epublish">
					<Year>2009</Year>
					<Month>12</Month>
					<Day>01</Day>
				</PubDate>
			</Journal>
<ArticleTitle>An Improvement on Land Surface Temperature Determination by Producing Surface Emissivity Maps</ArticleTitle>
<VernacularTitle></VernacularTitle>
			<FirstPage>171</FirstPage>
			<LastPage>184</LastPage>
			<ELocationID EIdType="pii">36338</ELocationID>
			
<ELocationID EIdType="doi">10.22059/jdesert.2009.36338</ELocationID>
			
			<Language>EN</Language>
<AuthorList>
<Author>
					<FirstName>M.</FirstName>
					<LastName>Pahlevani</LastName>
<Affiliation>MSc. student of Remote Sensing, K. N. Toosi University of Technology, Tehran, Iran</Affiliation>

</Author>
<Author>
					<FirstName>M. R.</FirstName>
					<LastName>Mobasheri</LastName>
<Affiliation>Associate Prof., K.N. Toosi University of Technology, Tehran, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2008</Year>
					<Month>12</Month>
					<Day>15</Day>
				</PubDate>
			</History>
		<Abstract>Emissivity mapping of the Earth’s surface is the prerequisite to thermal remote sensing. A precise determination&lt;br /&gt;of a surface&#039;s temperature is dependent upon the availability of precise emissivity data for that surface. The present&lt;br /&gt;study area is a part of sugarcane plantation fields in the west part of Khuzestan province. In this work, Temperature&lt;br /&gt;Emissivity Separation algorithm (TES) was applied to five different ASTER L1B images. It was found out that TES&lt;br /&gt;method overestimates temperature in all the five thermal bands, and underestimates the emissivities as compared to&lt;br /&gt;the laboratory values. The differences in the emissivity values (as compared to laboratory values) varied from 10% in&lt;br /&gt;band 10 to 3% in band 14. The main reasons for these discrepancies were a lack of proper calibration of the thermal&lt;br /&gt;bands, the possible presence of radiometric noises in the calculation of the emissivity Maximum Minimum&lt;br /&gt;Differences (MMD) as well as mixed pixels. To overcome these uncertainties in the TES algorithm, an Improved&lt;br /&gt;TES method (ITES) was introduced. In the ITES method, the surface exiting thermal fluxes were simulated. The&lt;br /&gt;emissivities of four different reference surfaces, along with air temperature measured at nearby weather stations&lt;br /&gt;(believed to represent LST of full vegetated pixels) and the band 14 temperature, were employed as inputs. The&lt;br /&gt;results show noticeable improvements in the predicted emissivity to around 1% for band 10 and less than 1% for&lt;br /&gt;bands 13 and 14 as compared to the corresponding laboratory values. The root mean square error (RMSE) of&lt;br /&gt;emissivities for full vegetation cover was less than 0.015 and less than 0.01 for partial vegetated cover, bare soil, and&lt;br /&gt;sea water surface. Finally, emissivity maps for one sample image, employing the five thermal bands, were produced.&lt;br /&gt;It is believed that these maps can be used in other satellite images as layers of emissivity values for the purpose of a&lt;br /&gt;proper estimation of surface temperatures.</Abstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">remote sensing</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">ASTER</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">TES algorithm</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Emissivity mapping</Param>
			</Object>
		</ObjectList>
<ArchiveCopySource DocType="pdf">https://jdesert.ut.ac.ir/article_36338_51e980c3c7c5ff4808eed78e91767184.pdf</ArchiveCopySource>
</Article>

<Article>
<Journal>
				<PublisherName>University of Tehran Press</PublisherName>
				<JournalTitle>Desert</JournalTitle>
				<Issn>2008-0875</Issn>
				<Volume>14</Volume>
				<Issue>2</Issue>
				<PubDate PubStatus="epublish">
					<Year>2009</Year>
					<Month>12</Month>
					<Day>01</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Long Lead Flood Simulation Using Downscaled GCM Data in Arid and Semi-arid Regions: A Case Study</ArticleTitle>
<VernacularTitle></VernacularTitle>
			<FirstPage>185</FirstPage>
			<LastPage>196</LastPage>
			<ELocationID EIdType="pii">36339</ELocationID>
			
<ELocationID EIdType="doi">10.22059/jdesert.2009.36339</ELocationID>
			
			<Language>EN</Language>
<AuthorList>
<Author>
					<FirstName>M.</FirstName>
					<LastName>Karamouz</LastName>
<Affiliation>Professor, School of Civil Engineering, University of Tehran, Tehran, Iran</Affiliation>

</Author>
<Author>
					<FirstName>M.</FirstName>
					<LastName>Fallahi</LastName>
<Affiliation>M.Sc., School of Civil Engineering, Amirkabir University of Technology, Tehran, Iran</Affiliation>

</Author>
<Author>
					<FirstName>S.</FirstName>
					<LastName>Nazif</LastName>
<Affiliation>Ph.D. Candidate, School of Civil Engineering, University of Tehran, Tehran, Iran</Affiliation>

</Author>
<Author>
					<FirstName>A.</FirstName>
					<LastName>Ahmadi</LastName>
<Affiliation>Ph.D. Candidate, School of Civil Engineering, University of Tehran, Tehran, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2008</Year>
					<Month>12</Month>
					<Day>29</Day>
				</PubDate>
			</History>
		<Abstract>Flood is one of the most calamitous natural disasters that causes extensive property and life damages across the&lt;br /&gt;world. It however, could be a blessing due to its special natural water resources recharging value. By simulating the&lt;br /&gt;magnitude of probable floods considering the anthropogenic and natural effects and implementing contingency plans,&lt;br /&gt;their damages could be reduced. In this paper, the General Circulation Model (GCM) climate change scenarios are&lt;br /&gt;employed to simulate future floods. The GCM scenarios include simulation of climatic signals of the future&lt;br /&gt;considering green house gas emission forces. In this study a statistical downscaling model (SDSM) has been applied&lt;br /&gt;for rainfall downscaling to provide regional results from GCM outputs. Then, a rainfall-runoff model called HECHMS&lt;br /&gt;has been employed to estimate runoff in the region. The maximum simulated rainfall for each year that is of&lt;br /&gt;high enough potential to cause flood, is introduced into the rainfall-runoff model to simulate the plausible&lt;br /&gt;hydrograph of the flood. The proposed procedure is applied to the Kajoo River basin in South Baloochestan region,&lt;br /&gt;south-east of Iran.</Abstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">Downscaling</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">flood simulation</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Rainfall-Runoff model</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">GCM</Param>
			</Object>
		</ObjectList>
<ArchiveCopySource DocType="pdf">https://jdesert.ut.ac.ir/article_36339_1a4dd28b6b2233492da75080c9240b43.pdf</ArchiveCopySource>
</Article>

<Article>
<Journal>
				<PublisherName>University of Tehran Press</PublisherName>
				<JournalTitle>Desert</JournalTitle>
				<Issn>2008-0875</Issn>
				<Volume>14</Volume>
				<Issue>2</Issue>
				<PubDate PubStatus="epublish">
					<Year>2009</Year>
					<Month>12</Month>
					<Day>01</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Studying the Morphologic Maturation of Aeolian Sand Grains During Transportation Process of Wind Erosion (Case study: Khartouran Erg)</ArticleTitle>
<VernacularTitle></VernacularTitle>
			<FirstPage>197</FirstPage>
			<LastPage>207</LastPage>
			<ELocationID EIdType="pii">36340</ELocationID>
			
<ELocationID EIdType="doi">10.22059/jdesert.2009.36340</ELocationID>
			
			<Language>EN</Language>
<AuthorList>
<Author>
					<FirstName>N.</FirstName>
					<LastName>Mashhadi</LastName>
<Affiliation>Assistant Professor, International Desert Research Center, University of Tehran, Tehran, Iran</Affiliation>

</Author>
<Author>
					<FirstName>M. R.</FirstName>
					<LastName>Ekhtesasi</LastName>
<Affiliation>Assistant Professor, Faculty of Natural Resources, University of Yazd, Yazd, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2009</Year>
					<Month>01</Month>
					<Day>28</Day>
				</PubDate>
			</History>
		<Abstract>Wind, in the duration of its erosional process, affects considerable changes in a grain&#039;s morphology&lt;br /&gt;from its removal (detachment) step to sedimentation. In other word, a grain undergoes its gradual&lt;br /&gt;evolution during the transit process. In this project, the maturation of Aeolian sand grains had been&lt;br /&gt;studied upon as based on texture maturity indicator which includes: sorting, mean size grain, roundness as&lt;br /&gt;well as abrasion coefficient parameters. The study area is the transport region of Khartouran Erg&lt;br /&gt;sediments, which founded on the basis of ground index of wind erosion. According to these indicators,&lt;br /&gt;the direction of prevailing or strong winds is notably mentioned. In a later step, four transects are selected&lt;br /&gt;in different area in alignment with wind direction. Samples of sediment grains are taken at varied&lt;br /&gt;distances in any one of the transects. The samples were taken from the windward slope of Rebdou&lt;br /&gt;landform. The samples were evaluated to using granulometry and morphoscopy techniques. Grain size&lt;br /&gt;analysis of was done using dry sieve analysis while morphoscopy of grains carried out by studying the&lt;br /&gt;quartz grains of 150 to 300 μm diameter by using binocular microscope. Results indicate a gradual&lt;br /&gt;maturity (evolution) in sediment texture in all transects starting from the upper parts (near sand source)&lt;br /&gt;toward the lower parts (in transportation area).Also, results indicate that from among the four indicators&lt;br /&gt;of grain maturity namely: sorting, grain size, roundness and abrasion coefficient the respective factors of&lt;br /&gt;either &quot; abrasion coefficient index&quot; or&quot; roundness index &quot; in the first value and then&quot; sorting&quot; and finally&lt;br /&gt;&quot;grain’s mean size index&quot; are the ones accounted for validation for determination of maturity.</Abstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">Khartouran Erg</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Deflation</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Abrasion</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Wind Erosion</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Removal zone</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Transit zone</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">sand dunes</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Wind
erosion indicators</Param>
			</Object>
		</ObjectList>
<ArchiveCopySource DocType="pdf">https://jdesert.ut.ac.ir/article_36340_1004d217c3f2199b76eb5801d6e6d32a.pdf</ArchiveCopySource>
</Article>

<Article>
<Journal>
				<PublisherName>University of Tehran Press</PublisherName>
				<JournalTitle>Desert</JournalTitle>
				<Issn>2008-0875</Issn>
				<Volume>14</Volume>
				<Issue>2</Issue>
				<PubDate PubStatus="epublish">
					<Year>2009</Year>
					<Month>12</Month>
					<Day>01</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Evaluation of the Efficiency of CROPWAT Model for Determining Plant Water Requirement in Arid Regions</ArticleTitle>
<VernacularTitle></VernacularTitle>
			<FirstPage>209</FirstPage>
			<LastPage>215</LastPage>
			<ELocationID EIdType="pii">36341</ELocationID>
			
<ELocationID EIdType="doi">10.22059/jdesert.2009.36341</ELocationID>
			
			<Language>EN</Language>
<AuthorList>
<Author>
					<FirstName>A.</FirstName>
					<LastName>Malekian</LastName>
<Affiliation>Assistant Professor, University of Tehran, Tehran, Iran</Affiliation>

</Author>
<Author>
					<FirstName>H.</FirstName>
					<LastName>Ghasemi</LastName>
<Affiliation>MSc. Graduate of Combating Desertification, Zabol University, Zabol, Iran</Affiliation>

</Author>
<Author>
					<FirstName>A.</FirstName>
					<LastName>Ahmadian</LastName>
<Affiliation>Ph.D. Student , Zabol University, Zabol, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2009</Year>
					<Month>03</Month>
					<Day>15</Day>
				</PubDate>
			</History>
		<Abstract>Shortage of water resources and increasing demand to consumption of this scarce resource, leads to some&lt;br /&gt;noticeable limitations. On the other hand, population growth and consequently, increasing demand for water in arid&lt;br /&gt;and semi arid regions , needs production in exchange of little amount of water consumption. To approach this&lt;br /&gt;objective, an experiment in the complete randomized blocks carried out in four replications for cumin plant growing&lt;br /&gt;in Zabol, southeastern Iran. Experimental treatments included irrigation periods at three levels. Then using&lt;br /&gt;CROPWAT model, the water requirement of the plant is met. Analyzing the data resulted from production gathered&lt;br /&gt;in different times of irrigation and consumption of water in the three times irrigation case with sound efficiency (1750&lt;br /&gt;m3/ha), is more little than the water amount which is simulated by the CROPWAT model in 2003 (6070 m3/ha) and&lt;br /&gt;(5363 m3/ha) in 2004. It then showed that this model is not effective in determining the water requirement of cumin at&lt;br /&gt;this region.</Abstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">Water requirement</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Cumin</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">CROPWAT model</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Efficiency</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Zabol</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">simulation</Param>
			</Object>
		</ObjectList>
<ArchiveCopySource DocType="pdf">https://jdesert.ut.ac.ir/article_36341_b5506d9c85fe0387ce84d4132b117cfa.pdf</ArchiveCopySource>
</Article>
</ArticleSet>
