Mahin Hanifapour; Gholamreza Zehtabian; Hasan Ahmadi; Aliakbar Nazari Samani; Hassan Khosravi
Volume 29, Issue 2 , July 2022, , Pages 186-195
Abstract
Wind erosion and dust storms are one of the natural disasters that are increasingly facing the arid and desert areas of central Iran. Improper management in natural resources has also had a high impact on this phenomenon. One of the basic principles of controlling and combating ...
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Wind erosion and dust storms are one of the natural disasters that are increasingly facing the arid and desert areas of central Iran. Improper management in natural resources has also had a high impact on this phenomenon. One of the basic principles of controlling and combating wind erosion is to know the areas of sediment harvesting. The purpose of this study is to identify the areas of wind sediment harvesting in the facies of the Mallard region in the west of Tehran province. Based on topographic maps, satellite imagery, geological map, and field surveys, the geomorphologic facies map was prepared and then the sampling was done and analyzed in a GIS environment. The interpretation of the anemometer data using Windrose & Stormrose showed the wind direction of the dominant and eroding from the northwest. The results obtained from the study's Sandrose indicated that variation in wind direction is low to high, and Qazvin station (the station closest to the critical centers) had high variability and included multi-directional winds with sharp angles. The 83 samples of different facies of the study area are graded by the ASTM (Dry Sieve) method. The granulation results indicate the local origin of the harvest. The prioritization map of the critical centers of the region showed that 16.4% of the area is low intensity, 3.4% medium intensity, and 3% high intensity. Finally, it was found that saline clay with no vegetation cover or with little vegetation covered with saline in the plain had the highest percentage of particles sensitive to wind erosion.
MAHSA abdolshahnejad; Hassan Khosravi; Aliakbar Nazari Samani; Amir Alambeigi
Volume 29, Issue 1 , February 2022, , Pages 36-52
Abstract
The importance of paying attention to sustainable development and biosafety in areas that effected by an environmental disaster such as dust storms has increased the need for new methods to find coping strategies. For this purpose, cross-structural analysis is an effective tool for studying system behavior. ...
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The importance of paying attention to sustainable development and biosafety in areas that effected by an environmental disaster such as dust storms has increased the need for new methods to find coping strategies. For this purpose, cross-structural analysis is an effective tool for studying system behavior. Based on the results of structural analysis and future study approaches, stability strategies can be proposed in the affected area by high-risk dust. The method of the research is according to the applied and future study approach. The sample population of this research was composed of 22 experts and managers in the field of agriculture and dust. Based on collecting data through expert interview and brainstorming method, the effective drivers were identified. According to the opinion of experts, the final drivers were extracted as a 26 × 26 matrix. Then, the cross-impact matrix was scored by experts. To determine the key drivers affecting the resilience of farming communities affected by dust in Ahvaz County, the future research approach was performed using MICMAC software in three groups of economic, social, and natural-physical components and 26 indicators. Research variables were divided into three categories »key, Independent and Regulative« based on the degree of relationship between influence and dependence. Key drivers include »Change of Quality and Quantity of Agricultural Products, Income Risk, Unemployment and Poverty Rise, Access to Financial Credits, Alternative livelihood and Immigration«. The results showed that the system of this study is unstable and in order to make management decisions and increase sustainability, it is necessary to develop strategies based on key drivers affecting farmer’s resilience.
Mahsa Abdolshahnejad; Ali Akbar Nazari Samanni; Mehdi Ghorbani; Aziz Orsham; feridoon Taheri
Volume 26, Issue 2 , July 2019, , Pages 325-339
Abstract
The effects of human activities on the land use and landscape and its subsequent effects on the natural environment have always been considered. Therefore, to have a sustainable landscape planning, knowing about such changes would be essential. Satellite images of TM sensor in ...
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The effects of human activities on the land use and landscape and its subsequent effects on the natural environment have always been considered. Therefore, to have a sustainable landscape planning, knowing about such changes would be essential. Satellite images of TM sensor in 1990, ETM+ Sensor in 2002 as well as OLI Landsat 8 in 2013 were used to investigate the trend of changes and preparation of cover maps. The executive phase of the study included the analysis of the gradient of land use structure in eight geographical directions for class area (CA), number of patch (NP), and mean patch size (MPS) in seven classes such as woodland) low-density forest and garden), water zone, agriculture, bare land, rangeland, urban and sand dunes. The results showed that the land use of woodland, urban, and sand dunes had an increasing trend, while the bare land showed a decreasing trend. The results of gradient analysis of land use structure in eight geographical directions indicated that the most changes were in the west and center of the region. Based on the analysis of changes rate of metrics, the most changes were recorded for rangeland, bare land, and urban during 1990 to 2002; the woodland, agriculture, and urban during 2002 to 2013; and rangeland, woodland and urban during 1990 to 2013. Therefore, given that some aspects of land use change depend on human aspects, the relationship between these quantitative indicators can be used to determine the sustainability level as well as the future trend of land use change to identify the critical affected areas. Metrics of area, number of patches and mean patch size were recognized as the important indices in discussions of monitoring land use and mosaic changes.
Mohammadreza Rahdari; Hasan Ahmadi; Ali Tavili; Mohammad Jafari; Aliakbar Nazari Samani; mohammad khosroshahi; Shahrooz Sharifi
Volume 26, Issue 1 , June 2019, , Pages 226-240
Abstract
Due to vast desert area in Iran, wind regime studies are important for the railway safe design as well as aeolian sediment transport. In this study wind regime and sand drift potential (DP) were calculated with Fryberger method in nine meteorological stations located near to the Qom –Tehran railway ...
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Due to vast desert area in Iran, wind regime studies are important for the railway safe design as well as aeolian sediment transport. In this study wind regime and sand drift potential (DP) were calculated with Fryberger method in nine meteorological stations located near to the Qom –Tehran railway (178 km). For this reason, hourly wind speed and direction data were analyzed. Annual wind roses showed that West and Northwest winds were predominantly about 40%, 50%, 42% and 57% at the stations of Tehran, Shahriyar, Qom, and Imam Khomeini airport, respectively. The highest amount of sand drift potential was at the Imam Airport station (DP= 574, UDI=0.8) in the west and its lowest value was at Qom station (DP= 109, UDI= 0.47) in the south of the region. The drift potential (DP) for aeolian deposits was generally high (DP >400) in the Garmsar (DP= 481), Salafchegan (DP= 485), Saveh (DP= 552) and Imam Khomini airport (DP=574) climatological stations. DP was relatively moderate (200>DP>400) at the Shariyar and Kahak stations in the northwest and south of study area, respectively; and weak (DP<200) in the Tehran and Qom climatological stations. There was an increasing trend in the transport of sand when moving from Namakzar railway station to the Imam Khomeini railway station. Also field evaluations indicated the sensitivity of the Separ Rostam-Namakzar block to entry of sand, which was 21.3 kilometers long. Finally, it is suggested to railway directors of the Islamic Republic of Iran to proceed with the assessment of sand drift potential near railways station for control of sand deposition.
Ali Akbar Nazari Samani; leila Biabani; Hamidreza Abbasi; Hasan Khosravi
Volume 25, Issue 3 , November 2018, , Pages 594-612
Abstract
Wind, as a major driving factor on soil erosion in arid and semi-arid areas, needs to be investigated precisely to prevent its undesirable effects. The main purpose of this research was to determine the spatial variability of wind erosivity and sand drift around Urmia Lake. For this aim, ...
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Wind, as a major driving factor on soil erosion in arid and semi-arid areas, needs to be investigated precisely to prevent its undesirable effects. The main purpose of this research was to determine the spatial variability of wind erosivity and sand drift around Urmia Lake. For this aim, the anemometry data of eight synoptic stations adjusted to the Lake were analyzed for the whole period time. Annual wind-roses showed that despite the very high spatial and temporal changes of wind variables (speed and direction), major prevailing winds were blown from the East and West, respectively. Also, annual storm-roses depicted that the erosive winds blew mainly from South and Southwest direction. These winds had a unidirectional regime in summer and spring, while in fall and winter, a multi directional regime was observed. The results of calculated sand drift power by Fryberger and Dean Formula indicated a low to moderate class of wind erosion potential and the final direction of sediment transport was mainly to northeast. According to the Letu-Letu equation, sand transport flux is varied between 0.05 to 0.76 Ton/m/year. Although the windiness of study area is moderate, the Tsoar sand mobility index is less than one, indicating inactive sand dunes. However, due to the low vegetation established on the sand dunes surface, it can be drawn that the role of human factors (especially cattle grazing and trampling) as well as the salinity caused by the drying of the Lake are responsible for this situation.
ali Nazari; asghar tavakoli; hoda ghasemieh; naser mashhadi; mohammadreza rahdari
Volume 24, Issue 1 , May 2017, , Pages 67-79
Abstract
Wind erosion is one of the most important natural processes in arid and semi-arid areas, occurring as a result of erosive winds. Wind speed, frequency and duration should be considered in studies related to wind erosion. Kashan Erg is one of the most important sand dunes complexes in Iran. To study the ...
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Wind erosion is one of the most important natural processes in arid and semi-arid areas, occurring as a result of erosive winds. Wind speed, frequency and duration should be considered in studies related to wind erosion. Kashan Erg is one of the most important sand dunes complexes in Iran. To study the relationship between the wind characteristics (Uni- directional index, windness index, wind duration and frequency) with Erg morphology and also study the changes of sand flow rate in various regions, anemometers data were obtained from synoptic stations of Kashan, Ardestan, Jangalbani Badrod, Garmsar and Qom. Then, the interpolation map of sand transport and interpolation map of average and maximum wind in Kashan Erg were drawn using GIS software. Finally, the analysis results showed that the interpolation map of sand transport corroborated the results obtained from interpolation map of average wind, because sand transport rate and average wind speed were reduced from east to west of the Erg. Therefore, it is found that wind frequency and duration have more important role in the sand transport and morphology of the study area as compared with the wind speed. In addition, the comparison of Erg morphology and anemometer results in different stations showed that the spring and summer winds had the highest role in the Erg morphology.
ali nazari; hamidreza abbasi; hasan ahmadi; mohammadreza rahdari
Volume 24, Issue 1 , May 2017, , Pages 210-223
Abstract
This research was aimed to modeling the height and distance of sand dunes in central deserts of Iran (Kashan Erg and Jen Erg) as well as their classification. Results of identifying sand dunes in the study areas showed that there were considerable variations in formation of sand dunes in central ...
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This research was aimed to modeling the height and distance of sand dunes in central deserts of Iran (Kashan Erg and Jen Erg) as well as their classification. Results of identifying sand dunes in the study areas showed that there were considerable variations in formation of sand dunes in central deserts of Iran. Quantitative modeling of height based on DEM (80 × 80m) showed that the average height of sand dunes in Kashen Erg and Jen Erg was 35m and 6.84m, respectively. The reduced height in Jen Reg was due to the 37% frequency of sand dunes area and regardless of these dunes, the average height was calculated to be 8.63 m in Jen Reg, of which 90% was in a height class less than 20 m. On the other hand, the frequency percentage variation of sand dunes height classes is higher in Kashan Erg, so that over 80% of Kashan Erg is in a height class less than 50m, while 87% of Jen Erg is in a height class less than 10m. In Kashan Erg, the height of sand dunes is low and gradually increases in the center of Erg, reaching to the highest height of sand dunes. Quantitative modeling of relations between the height and distance of dunes in Jen Erg indicated that the sand dunes activity was restricted to the upper part of the dunes. In Kashan ERG, the comparison of fixed, linear and compound dunes showed that the fixed dunes would be formed at a closer distance as compared with two other types.