Document Type : Research Paper

Authors

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 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.

Keywords

Ahmadi, H., 2006. Applied Geomorphology (wind erosion). University of Tehran Press, 706p.
Ekhtesasi, M. R., Saremi Nainii, M. and Saremi Nainii, A., 2005. Preparation of sand rose graph 2.0 for soil erosion and sand drift potential. 1st National conference on wind erosion,Yazd University, 23-24 February:12p.
Ekhtesasi, M. R., Ahmadi, H., Khalili, H., Saremi Nainii, M. and Rajabi, M. 2006. Application of wind rose, storm rose and sand rose for wind erosion analysis and sand movement direction (a case study: Yazd-Ardakan plain). Iranian Journal of Natural Resources, 59(3): 533-541.
Ekhtesasi, M. R., Azimzadeh, H., 2004. Threshold velocity relation to soil physical and chemical properties in Iranian central plain (Case study: Yazd- Ardakan plain). Iranian Journal of Natural resources, 57(2):1-11.
Eric j. R. P., Duranb, O., Tsoar, H., Schwammle, V. and Hermann, H. J., 2009. Dune formation under bimodal winds. Applied Physical Sciences, 106(52): 22085-22089.
Fryberger, S. G., 1979. Dune forms and wind regime. 137–169 In: McKee, E. D. (Eds.), A study of global sand seas. United States Geological Survey, Washington, DC
Fryberger, S. G., Ahlbrandt, T. S. and Andrews, S., 1979. Origin, sedimentary features, and significance of low-angle aeolian sand sheet deposits, Great Sand Dunes National Monument and vicinity, Colorado. Journal of Sedimentary Research, 49 (3): 733-746.
Hangen, L. J., 1976. A wind erosion predication system to meet user needs. soil water conserve journal, 46(2):106-111.
Saremi Nainii, M., 2006. Comparison analysis of spatial distribution of wind rose, storm rose and sand rose through GIS technique. (Case study: Yazd- Ardakan plain). M.Sc. Thesis, Faculty of Natural Resources, University of Tehran.
Stewart, D. A. and Essenwanger. O. M., 1987. Freqeuncy distribution of wind speed near the surface, Appl. Meteor journal, 17:1633-1642.
Tavoosi, T. and Raeispoor, K. 2011. Statistical analysis and prediction of occurrence probability of violent Storms using partial – series analysis method (Case study: sistan area). Arid Regions Geographic Studies, 1(2):93-105.
Webb, N. P., McGowan, H. A., Phinn, S. R. and McTainsh, G. H., 2006. AUSLEM (Australian Land Erodibility Model): A tool for identifying wind erosion hazard in Australia. Geomorphology, 78(3):179-200.
Yamani, M., 2000. Relationship between sand grain size and frequency of wind threshold velocity in band rig Kashan, Journal of geographical researches, 38: 115-132.
Yamani, M., Nazouri, Z. and Gourabi, A., 2011. Morphometry and causes of Kerman Erg establishment through wind analysis and granolometry. Journal of arid region geographical studies. 1(4): 17-33.
Zobeck, T. M., 1991. Soil properties affecting wind erosion. Soil and Water Conserve Journal, 46(2):112-118.