@article { author = {Malekian, Arash and Mahdavi, M. and Kholghi, M. and Zehtabian, Gh.R. and Saravi, M. Mohseni and Rouhani, H.}, title = {Optimal Planning for Water Resources Allocation (Case study: Hableh Roud Basin, Iran)}, journal = {Desert}, volume = {17}, number = {1}, pages = {1-8}, year = {2012}, publisher = {University of Tehran}, issn = {2008-0875}, eissn = {2345-475X}, doi = {10.22059/jdesert.2012.32005}, abstract = {The world is facing severe challenges in meeting the rapidly growing demand for water resources. In addition,irrigation water which is the largest use of water in most developing countries and arid and semi arid regions, will likelyhave to be diverted increasingly to meet the needs of the households in urban areas and industry sectors whilst remaining aprime engine of agricultural growth. A Linear Programming (LP) model has been developed to allocate the land and waterresources to different crop activities for maximizing the net return. Application of the model for the irrigation watermanagement revealed that in winter, 89.4% of available channel water was utilized, out of which 55.9% and 18.5% wereallocated for wheat and barley, respectively .The remaining 25.6% channel water was allocated for cotton andwatermelon. Since there were enough channel water supplies in this season, only 10.6% of available groundwater wasutilized. In the absence of constraint on conjunctive use, there would have been no groundwater exploitation, and 100% ofthe channel water, which is much cheaper than groundwater, could have been utilized, if required. During summer season,the entire quantities of water available in channel as well as groundwater resources were utilized. In this season, as therewas limited channel water supply, considerable part of the irrigation requirement was met from available groundwater.Based on the LP analysis, out of total available channel water, 43.2% was allocated to cotton cropping, which was mostprofitable as compared to all other crop activities, followed by 38.3%, 9.5% and 9% to crop activities includingwatermelon, barely and wheat, respectively. Out of total available groundwater, 65.8% was allocated to cotton whoseirrigation water need was high and the remaining 34.2% was shared by wheat, barley and watermelon cropping activities.The model predicts that in the case of changes in irrigation water supply, it will be economic to change the croppingpattern.}, keywords = {Optimization,Hableh Roud basin,surface water,Allocation,Iran}, url = {https://jdesert.ut.ac.ir/article_32005.html}, eprint = {https://jdesert.ut.ac.ir/article_32005_7f85574f4a06d0419f2afabaa57aa1f7.pdf} } @article { author = {Azarnivand, H. and Zare Chahouki, M.A. and Joneidi, H.}, title = {Evaluation of the Effects of Vegetation Characteristics on Desertification (Case Study: Northern Hableh Roud, Iran)}, journal = {Desert}, volume = {17}, number = {1}, pages = {9-13}, year = {2012}, publisher = {University of Tehran}, issn = {2008-0875}, eissn = {2345-475X}, doi = {10.22059/jdesert.2012.32006}, abstract = {One of the characteristics in Iranian Model of Desertification Potential Assessment (IMDPA) is vegetation. Sincevegetation is very important factor in the degradation of land, so some indices were determined for this item in order toevaluate desertification potential of arid, semi arid and arid sub humid areas of Iran. The indices included vegetationcondition, exploit and revegetation. To calibrate the vegetation item in the IMDPA model, above mentioned indices wereassessed in Northern Hableh Rood region as semi arid and arid sub humid region. To do this, in the first stage unit workmap of the study area was prepared based on slope, land use and geological maps. Scores of indices were recorded indifferent study units. At last, using the following formula, VI  3VCI *VUI *VRI , final score of vegetation character(VI) was determined in the study area based on IMDPA. After scoring vegetation character, desertification intensity mapfor vegetation character including four low, medium, intensive and very intensive classes was prepared. The map showedthat 62.2%, 37.2% and 0.6% of the study area are considered as low, medium and high desertification intensity class,respectively. There wasn't very high class based on vegetation character.}, keywords = {IMDPA,soil,Desertification,Hableh Rood,Iran}, url = {https://jdesert.ut.ac.ir/article_32006.html}, eprint = {https://jdesert.ut.ac.ir/article_32006_2363f53d9998b72aec5a84a4c8445fb6.pdf} } @article { author = {Pahlavanravi, A. and Miri, A. and Ahmadi, H. and Ekhtesasi, M.R.}, title = {The Impacts of Different Kinds of Dust Storms in Hot and Dry Climate, A Case Study in Sistan Region}, journal = {Desert}, volume = {17}, number = {1}, pages = {15-25}, year = {2012}, publisher = {University of Tehran}, issn = {2008-0875}, eissn = {2345-475X}, doi = {10.22059/jdesert.2012.32007}, abstract = {Dust storms are catastrophic natural disasters that beside other disasters frequency occur in the arid and semiaridregions worldwide. Drought occurrence, climate aridity, dryness of the Hamoun Lake cause strong winds to below.These conditions have been prepared for dust storms in Sistan region. The damages to Sistan society have beenmeasured using different criteria. The result shows that, peak of dust storms takes place at 10:30 am and the particularminimum was recorded at 6:30 pm. The maximal frequency of dust storms has been occurred in June and July. Sincethe dust storms cause extensive damages, an attempt has been made to quantify the damage costs using an analyticaldescriptivemethod based on questionnaires completed by the local community and organizations. The cumulativelosses in terms of physical damage and loss of productive man-hours have been estimated US$ 99.190 million, over afive year period between 2000-2005.}, keywords = {Dust Storm,Local Community,Damage costs,Sistan}, url = {https://jdesert.ut.ac.ir/article_32007.html}, eprint = {https://jdesert.ut.ac.ir/article_32007_ca9ae3255c51f391a9b6d78b9613c20b.pdf} } @article { author = {Motaghian, H.R. and Mohammadi, J.}, title = {Statistical and Geostatistical Appraisal of Spatial Variability of Aggregate Stability and Aggregate-Associated Organic Carbon Content on a Catchment Scale in a Semi-arid Region, Central Iran}, journal = {Desert}, volume = {17}, number = {1}, pages = {27-39}, year = {2012}, publisher = {University of Tehran}, issn = {2008-0875}, eissn = {2345-475X}, doi = {10.22059/jdesert.2012.32008}, abstract = {In a semiarid region of central Iran, effects of parent materials, physiography and landscape position, land use, andmanagement practices on association of organic carbon with secondary (aggregates) particles and aggregate stability canhave important consequences in terms of carbon sequestration and budgeting, deciding on the proper land use strategy andsuitable soil conservation practices. It was used wet sieved aggregates to evaluate the effects of different factors on soilaggregate stability and organic carbon concentration within three aggregate size fractions (>2 mm, 1-2 mm, <1 mm). 111soil samples were collected to measure water stable aggregates (WSA), aggregate organic carbon concentration (OC), andmean weight diameter (MWD). Some other related soil and terrain properties including bulk density, infiltration rate,saturated hydraulic conductivity and erodibility index were also measured. Analyses of variance indicated that waterstability of aggregates was influenced by aggregate size. Higher percentage of water stable aggregates was found formicroaggregates (< 1 mm), followed by mesoaggregates (1 to 2 mm). Aggregate organic carbon content was highest inmesoaggregates (9 g kg-1), followed by microaggregates (7 g kg-1), while the least OC concentration was found inmacroaggregates (3 g kg-1). Both aggregate size fraction and slope aspect significantly impacted aggregate organic carbonconcentration. Although a significant effect of aggregate size on aggregate organic carbon content was found, however,our findings did not support the model of aggregate hierarchy. Both MWD and GMD were significantly impacted byaggregate size fractions. Geostatistical analysis showed that the measured soil attributes exhibited differences in theirspatial patterns in both magnitude and space at each aggregate size fractions. The relative nugget variance for mostaggregate-associated properties was lower than 45%. The range for water stable aggregates was almost similar (3 km)for the three studied aggregate size classes. The range for aggregate-associated organic carbon contents ranged from about3 km for macroaggregates to about 6.5 km for mesoaggregates. Kriged maps of predicted WSA, OC and MWD for thethree studied aggregate size fractions showed clear spatial patterns. However, a close spatial similarity (coregionalization)was observed between WSA and MWD.}, keywords = {Kriging,organic matter,Variogram,Water stable aggregates}, url = {https://jdesert.ut.ac.ir/article_32008.html}, eprint = {https://jdesert.ut.ac.ir/article_32008_d211bdd05d22e14a450bebc33f298dbe.pdf} } @article { author = {Keshtkar, A.R. and Salajegheh, A. and Najafi Hajivar, M.}, title = {Flood Flow Frequency Model Selection Using L-moment Method in Arid and Semi Arid Regions of Iran}, journal = {Desert}, volume = {17}, number = {1}, pages = {41-48}, year = {2012}, publisher = {University of Tehran}, issn = {2008-0875}, eissn = {2345-475X}, doi = {10.22059/jdesert.2012.32009}, abstract = {Statistical frequency analysis is the most common procedure for the analysis of flood data at a gauged location thatin first step it is needed to select a model to represent the population. Among them, the central moment has been themost common and widely used, and with the using of computers, the application of the maximum likelihood hasincreased. This research was carried out in order to recognition of suitable probability distributions with perviouscommon methods. In order to investigate of suitable probability distribution for flood flow, using L-moment methodthrough the existing hydrometric stations in the region, 17 hydrometric stations were selected for peak dischargesdata studies. According to results of this research for peak discharge, LP3 distribution and ordinary moment method,P3 distribution and L-moment method, LN2 and LN3 distributions and ordinary method have been suitabledistinguished for 53%, 35%, 6% and 6% of stations, respectively. We concluded that L-moment method is suitable todetermine peak series probability distributions in the Iran central plateau and P3 is the best probability distribution formodeling peak series in this region.}, keywords = {Flood flow,Frequency distribution function,Linear moment,Maximum likelihood,Ordinary moment}, url = {https://jdesert.ut.ac.ir/article_32009.html}, eprint = {https://jdesert.ut.ac.ir/article_32009_5b3a0f93c4997ec08d4540104ef9fb0f.pdf} } @article { author = {Fattahi, E. and Noohi, K. and Shiravand, H.}, title = {Study of Dust Storm Synoptical Patterns in Southwest of Iran}, journal = {Desert}, volume = {17}, number = {1}, pages = {49-55}, year = {2012}, publisher = {University of Tehran}, issn = {2008-0875}, eissn = {2345-475X}, doi = {10.22059/jdesert.2012.32010}, abstract = {As widespread deserts is located in west and southwest of Iran plateau, dust storms form due to west andsouthwest systems over Syria or Iraq as well as Arabian Peninsula. These systems severely affect west and southwestregions. Sometimes the fine dusts transmit to central, north east, and east regions. In this study for investigating dustysynoptical patterns, meteorological data at 5 synoptic stations were studied during recent ten years. Mean daily sealevel pressure data were selected from the NCEP reanalysis data encompassing the region from 20°-60°N latitude by20°-80°E longitude, with a 2.5 spatial resolution and for the 10 year period 1961-2003 in dusty days. Selectedterritory is located in a geographical situation that covers all the effecting systems on Iran. For classification anddelineate synoptical patterns Principal Component Analysis (PCA) and clustering method were used. Results showedthat in this region, days with dust have three general circulation patterns. Analyzing these patterns show that there isa trough which restricted to 30-45°E longitude in 850 hPa chart, and at least one relatively strong low pressure overArabian Peninsula in sea level pressure extending to the west, south west and the study region. This study shows thatabove aspects are the major specifications of dusty days.}, keywords = {Synoptical patterns,Dusty systems,Principal component analysis,Iran}, url = {https://jdesert.ut.ac.ir/article_32010.html}, eprint = {https://jdesert.ut.ac.ir/article_32010_0cbaea115b5dbc35546b7304126bbed3.pdf} } @article { author = {Mohammadkhan, Sh.}, title = {Grain Size and Shape of Sand Grains in Ergs of Iran}, journal = {Desert}, volume = {17}, number = {1}, pages = {57-64}, year = {2012}, publisher = {University of Tehran}, issn = {2008-0875}, eissn = {2345-475X}, doi = {10.22059/jdesert.2012.32011}, abstract = {Large areas of Iran are under the influence of wind erosion thus it is important that we recognize three zones ofremoval, transportation and deposition. The deposition zone is very important due to more damages and tangibleeffects. In this study we try to obtain a comprehensive idea to Persian desert with use of laboratory facilities, remotesensing, GIS and field surveying. We survey 28 ergs in this study that they have 6410600 ha area. Area of sand duneis 4172500 ha and we analysis 66 samples from them. the range of grain size is 4000 micron to less than 62 μ. 11%from samples have max grain size of 4000 μ, 3% 1700 μ, 5% 1180 μ13% 600 μ, 58% 300 μ, 9% 150μ, 2% 62μ. 28%samples had min grain size of 75μ, 13% 62μ, and 59% less than 62μ. 3% samples had mod of 600μ, 3% 300μ, 59%150μ, 30%75μ and 3% 62μ. The samples were transport 1 to 5 km, 2% were transport 5 to 20 km, 72% weretransport 20 to 50 km and 23% were transport 50 to 200 km. skewness coefficient of normal charts are -0.2 to 2.95and most coefficients is in range of 2 that shown fine grain.}, keywords = {Sand dune,grain size,Erg}, url = {https://jdesert.ut.ac.ir/article_32011.html}, eprint = {https://jdesert.ut.ac.ir/article_32011_8b4a04107d30b5406fe26e68e82aef7b.pdf} } @article { author = {Fotouhi, F. and Azimzadeh, H.R. and Talebi, A. and Ekhtesasi, M. R.}, title = {Analyzing the Changes of Soil Erodibility Index (K) in the Soils of Arid Regions and the Effective Factors in Central Iran (Case Study: Yazd-Ardakan Plain)}, journal = {Desert}, volume = {17}, number = {1}, pages = {65-75}, year = {2012}, publisher = {University of Tehran}, issn = {2008-0875}, eissn = {2345-475X}, doi = {10.22059/jdesert.2012.32012}, abstract = {One of the main factors of water erosion is the natural characteristics of the soil called "erodibility" or"detachability". The present study aims to analyze the variations of soil erodibility factor in different plains and thefactors related to it. Erodibility is one the key factors in some models of erosion and sediment such as Universal SoilLoss Equation (USLE), Revised USLE (RUSLE), and Modified USLE (MUSLE) and is a function of grain sizedistribution, organic matter, structure and infiltration. To this end, the index of soil erodibility was measured throughfield surveys in 37 spots in the faces of bare pediment, coalescing pediment, and concealed pediment plains usingWischmeier and Smith (1987) method. The infiltration of soil profile and the percentage of desert pavement in thefield were measured as well. Soil grain size distribution, percentage of organic matter, soil structure, gravelvolumetric content, lime, salinity, acidity, and sodium absorption rate were also measured in the laboratory. Thestatistical analysis indicated positive correlations of erodibility with silt, very fine sand (VFS), and negativecorrelation of this factor with gravel, sand, infiltration, organic matter, and lime. The results from Analysis ofVariance (ANOVA) test also indicated that three factors of salinity, acidity, and sodium absorption rate are notsignificantly different in bare pediment, coalescing pediment, and concealed pediment plains. The results suggestedthat in natural conditions of soil surface, desert pavement plays its protective role and land use change throughmixing the soil would thwart effect of the pavement. So, the erodibility of the soil in manipulated and mixedconditions increases up to 10 times.}, keywords = {Geomorphology faces,Desert pavement,Water erosion,Erodibility}, url = {https://jdesert.ut.ac.ir/article_32012.html}, eprint = {https://jdesert.ut.ac.ir/article_32012_0fea249f2133231a42ad499c4eec0acf.pdf} } @article { author = {Yaghmaeian Mahabadi, N. and Givi, J. and Naderi Khorasgani, M. and Mohammadi, J. and Poch Claret, R.M.}, title = {Land Suitability Evaluation for Alfalfa and Barley Based on FAO and Fuzzy Multi-Criteria Approaches in Iranian Arid Region}, journal = {Desert}, volume = {17}, number = {1}, pages = {77-89}, year = {2012}, publisher = {University of Tehran}, issn = {2008-0875}, eissn = {2345-475X}, doi = {10.22059/jdesert.2012.32013}, abstract = {The present research aims to apply several approaches for suitability evaluation of lands under cultivation ofalfalfa and barley in Chaharmil mechanized farming center, Ardestan town, Isfahan province, Iran. Climatic andsoil maps of the climate and soil data were provided in raster format. Land evaluation carried out using maximumlimitation, parametric and multi-criteria (Analytical Hierarchy Process (AHP) and fuzzy AHP) approaches. Landindices, calculated by these methods were correlated with the observed yields. The best relationships were givenby fuzzy AHP for alfalfa and barley, which illustrates the accuracy of this approach for land evaluation. Theresults of fuzzy AHP showed that the majority of the study area is potentially more suitable for alfalfa than forbarley. The membership functions revealed that soil texture is the main constraint for alfalfa and barleyproduction.}, keywords = {land suitability,Multi-criteria,Fuzzy set,AHP,Alfalfa,Barley,Ardestan}, url = {https://jdesert.ut.ac.ir/article_32013.html}, eprint = {https://jdesert.ut.ac.ir/article_32013_e6ceeaa89d08c27adfba7001a3e8c520.pdf} } @article { author = {Saberi, M. and Jafari, M. and Tavili, A. and Zare Chahouki, M.A. and Tahmoures, M.}, title = {Comparison the Amount of Existing Mineral Elements in Plant Aerial Parts, Litter and Soil of Three Range Species in Taleghan Region}, journal = {Desert}, volume = {17}, number = {1}, pages = {91-97}, year = {2012}, publisher = {University of Tehran}, issn = {2008-0875}, eissn = {2345-475X}, doi = {10.22059/jdesert.2012.32014}, abstract = {The aim of this research was to compare the amounts of existing mineral elements in plant aerial parts, litter and soil ofthree range species (Bromus tomentellus, Psathyrostachys fragilis, Agropyron tauri) in order to investigate the litter effectof species on soil properties of Taleghan rangeland. The measured mineral elements include carbon, nitrogen,phosphorous and potassium. After selection of the appropriate plant species and suitable sites, random- systematicsampling method was used to plant aerial part, litter and soil sampling. Soil data were taken of 0-30 cm depth and inaddition to above mineral elements, soil texture, EC, pH and lime percentage was measured in soils of the sites. The datawas analyzed by analysis of variance (ANOVA), Duncan’s test and t-test. Results of analysis of variance of differentelements showed that the amounts of nitrogen, carbon and C/N ratio of the species litter had significant differences, sothat A. tauri had the highest concentration of nitrogen and B. tomentellus had those of Carbon and C/N ratio. Results alsoindicated that there are significant difference among the amounts of nitrogen, phosphorous and carbon in plant aerial partof the mentioned species (P<0.01). P. fragilis had the highest amount of nitrogen and both P. fragilis and B. tomentellushad higher amount of carbon and phosphorous than A. tauri. Soil under the species and control showed significantdifferences so that the mentioned species improve soil productivity. Totally, A. tauri had the highest litter quality anddecomposition rate.}, keywords = {Plant aerial part,litter quality,mineral elements,soil}, url = {https://jdesert.ut.ac.ir/article_32014.html}, eprint = {https://jdesert.ut.ac.ir/article_32014_3171d2f50a58c5fb0d3f220951646b9f.pdf} } @article { author = {Asgari, H.R. and Cornelis, W. and Van Damme, P.}, title = {Wheat (Triticum aestivum L.) Growth and Yield as Influenced by Flooding and Salinity Stresses in Northern Iran}, journal = {Desert}, volume = {17}, number = {1}, pages = {99-104}, year = {2012}, publisher = {University of Tehran}, issn = {2008-0875}, eissn = {2345-475X}, doi = {10.22059/jdesert.2012.32015}, abstract = {Salinity and flooding are as two very important factors of soil degradation. They often occur together and cancause severe damage to plants. However, plant response to environmental stresses may vary with growth stage atwhich exposure occurs. A pot study was conducted in 2005-2006 in northern Aq Qala (northern Iran) to studycombine effects of waterlogging and soil salinity at different growth stages on grain yield and some yield componentsof two Iranian spring wheat genotypes, i.e. Kouhdasht and Tajan. Two salinity treatments were applied, viz. a nonsaline(ECe = 3 dS m-1) and saline soil (ECe= 10 dS m-1). The six waterlogging treatments within each set consistedof: control (no waterlogging), and waterlogging applied at tillering (T); stem elongation (SE); booting (B); grainfilling (GF); and two spells of waterlogging, i.e. at tillering and grain filling stages (T+GF). In this experiment,waterlogging was imposed by keeping pots in hypoxia conditions by adding water daily (during up to two weeks) to110% of available water holding capacity. Results reveal that highest reduction in grain yield; thousand grain weight(TGW) and harvest index (HI) were observed through waterlogging at T+GF for both wheat genotypes. Nonsignificantchanges in grain yield, TGW and HI were observed via waterlogging at B as compared to control.Kouhdasht showed better performance than Tajan under saline and saline × waterlogged conditions}, keywords = {Abiotic stresses,Plant ecophysiology,tolerance,Stress physiology,Semi-arid agriculture}, url = {https://jdesert.ut.ac.ir/article_32015.html}, eprint = {https://jdesert.ut.ac.ir/article_32015_ed691fa4cf1fc472d2ef45af4e18e5e1.pdf} } @article { author = {Ziaei, M.S. and Masoudi, R. and Ghodsi, M. and Khosravi, H.}, title = {Study of the Effect of Management Criterion on Desertification Control (Case Study: Kashan)}, journal = {Desert}, volume = {17}, number = {1}, pages = {105-109}, year = {2012}, publisher = {University of Tehran}, issn = {2008-0875}, eissn = {2345-475X}, doi = {10.22059/jdesert.2012.32016}, abstract = {Desertification is more related to social and anthropogenic issues than natural causes and it becomes moreimportant over the time. Human effects on desertification could be classified as direct and indirect factors. This studyhas focused on the effect of management factor, as a dominant case, on desertification of Kashan region based onIMDPA (IMDPA: Iranian Model of Desertification for Potential Assessment) model. The geometric average weightwas used in order to find out the numerical value of management factor and then; desertification status map of thearea was prepared using GIS. The results showed that about 59.96 percent of the region, based on managementcriterion, is classified in the medium class of desertification which mostly covers central, northern, southeastern andwestern parts of the region. Meanwhile, irrigation systems, rangeland ploughing and the index of evaluationimplemented activity having the numeral value of 3.52, 3.43 and 2.23 are the most important affecting factors ondesertification, respectively. Increasing unwise human activities due to lack of sufficient knowledge on new irrigationand cultivation technologies has been resulted on accelerated degradation and consequent desertification. Then,combination of new extension and traditional knowledge, policy making and planning may lead to desertificationcontrol in the region.}, keywords = {management,IMDPA model,Desertification,GIS,Kashan}, url = {https://jdesert.ut.ac.ir/article_32016.html}, eprint = {https://jdesert.ut.ac.ir/article_32016_70fcd5c1e753692add849b34ce90a6e1.pdf} }