مطالعه نرخ فرونشست و توزیع اندازه ذرات گردوغبار با توجه به خصوصیات اراضی در کانون فوق بحرانی هویزه-خرمشهر

نوع مقاله : مقاله پژوهشی

نویسندگان

1 گروه علوم و مهندسی خاک، دانشکده کشاورزی، دانشگاه شهید چمران اهواز، اهواز، ایران

2 گروه علوم و مهندسی خاک، دانشکده کشاورزی، دانشگاه شهید چمران اهواز، اهواز، ایران.

چکیده

طوفان­های گردوغبار را می­توان یکی از مهم‌ترین دلایل آلودگی هوا در مناطق دارای کانون­های ریزگرد و مناطق همجوار آن­ها دانست. این پژوهش با هدف بررسی تغییرات نرخ فرونشست و الگوی توزیع اندازه ذرات گردوغبار با توجه به عوامل اقلیمی مؤثر در اطراف کانون غبار هویزه انجام شد. بدین منظور ۳۰ ایستگاه برای نصب تله­های رسوب‌گیر تیله­ای در شهرهای هویزه و سوسنگرد انتخاب و هرماه پس از جمع‌آوری نمونه‌های غبار، نرخ فرونشست و الگوی توزیع اندازه ذرات گردوغبار تعیین شد. نتایج نرخ فرونشست ذرات گردوغبار نشان داد که بیشترین و کمترین مقدار فرونشست ماهانه گردوغبار به ترتیب در اردیبهشت و اسفندماه رخ‌ داده است. نتایج توزیع اندازه ذرات نشان داد که بیش از ۸۰ درصد ذرات گردوغبار ته‌نشست­شده را اجزای سیلت تشکیل می­دهد. تشابه در بافت ذرات گردوغبار با بافت خاک کانون غبار هویزه- خرمشهر و از طرفی با توجه به الگوی جهت باد منطقه مورد مطالعه، می­توان منشأ این طوفان­های گردوغبار را از مناطق همجوار استان خوزستان و احتمالاً از کانون غبار هویزه و تالاب­های خشک‌شده در مرز ایران و عراق دانست.

کلیدواژه‌ها

موضوعات


عنوان مقاله [English]

Study of Deposition Rate and Dust Particle Size Distribution with Attention to Soil Properties in Hoveizeh-Khorramshahr Supercritical Source

نویسندگان [English]

  • Reza Aminfar 1
  • Ahmad Landi 2
  • Saeid Hojati 1
1 Department of Soil Science and Engineering, Faculty of Agriculture, Shahid Chamran University of Ahvaz, Ahvaz, Iran
2 Department of Soil Science and Engineering, Faculty of Agriculture, Shahid Chamran University of Ahvaz, Ahvaz, Iran
چکیده [English]

Dust storms can be one of the most important causes of air pollution in areas with dust sources and also in nearby areas. The purpose of this study was to investigate the changes rate of deposition and the pattern of particle size distribution of dust due to climatic factors around the dust. For this purpose, 30 stations were selected to install marine sediment Marbles traps in the city of Hoveizeh and Susangerd. Each month after collecting the dust samples, the rate of deposition and particle size distribution pattern of the dust were determined. The results of the dust particle deposition showed that the highest and the lowest monthly dust deposition occurred in May and March, respectively. The particle size distribution results showed that silt components form more than 80% of the deposited dust particles. Regarding the similarity of the texture of dust particles with the soil texture of the Hoveizeh-Khorramshahr dust source and also the land features and wind direction pattern of the study area, the origin of these dust storms is known to be from the neighboring areas of Khuzestan province, and probably from the Hoveizeh dust source and the dried wetlands in Iran-Iraq border.

کلیدواژه‌ها [English]

  • Deposition
  • Dust
  • Origin
  • Particle size
  • Temporal variation
Akbari, A., Azimzadeh, H. R., and Bahan Dayyani, S. (2012). Determination of pollution and geoaccumulation index of Pb heavy metal in soils around Behbahan cement factory.
Al-Dousari, A.M., and Al-Awadhi, J. (2012). Dust fallout in northern Kuwait, major sources and characteristics. Kuwait Journal Science. 39, 171-187.
Al-Harbi, M. (2015). Characteristics and composition of the falling dust in urban environment. International Journal of Environmental Science and Technology. 12 (2), 641- 652.
Artieda, O., Herrero, J., and Drohan, P.J. (2006). Refinement of the Differential Water Loss Method for Gypsum Determination in Soils. Soil Science Society of America Journal. 70(6), 1932-1935.
Beit-lafte, R., Landi, A., Hojati, S., and Sayyad, GH. (2015). Deposition Rate, Mineralogy and Size Distribution Pattern of Dust Particles Collected Around the Houralazim Marshland, Khuzestan Province, Journal of Water and Soil. 29, 695-707. (In Farsi).
Karimian, B., Hojati, S., Landi, A., and Ahadian, J. (2016). Investigation of physicochemical and mineralogical characteristics of Ahvaz dust. Journal of Water and Soil Research. 47, 159-173. (In Farsi).
Bouyoucos, G.J. (1962). Hydrometer method improved for making particle size analysis of soil. Agronomy Journal. 54, 464-465.
Chapman, H. D. (1965). Cation exchange capacity. Methods of soil analysis, American Society of Agronomy. 2, 891-901.
Ganor, E. (1975). Atmospheric dust in Israel. Sedimentological andmeteorological analysis of dust deposition. Ph. D. dissertation, University of Jerusalem.
Gholampour, A., Nabizadeh, R., Hassanvand, M.S., Taghipour, H., Nazmara, S., and Mahvi, A.H. (2015). Characterization of saline dust emission resulted from Urmia Lake drying. Journal of Environmental Health Science and Engineering. 13, 1-11
Hagen, L.J., S. Van Pelt and B. Sharratt. (2010). Estimating the saltation and suspension components from field wind erosion. Aeolian Research, 1:147-153.
Hojati, S., Khademi, H., Faz Cano, A., and Landi, A. (2012). Characteristics of dust deposited along a transect between central Iran and the ZagrosMountains. Catena. 88, 27-36.
Jackson, M. L. (1973). Soil chemical analysis. New Delhi. Prentice Hall of India Private Limited.
Liu, L.Y., X.L. Li, P.J. Shi, S.Y. Gao, J.H. Wang, W.Q. Ta, Y. Song, M.X. Liu, Z. Wang and B.L. Xiao.  (2007). Wind  erodibility  of major  soils  in  the  farming-pastoral  ecotone  of China.  Journal  of  Arid Environments, 68:611-623.
Lopez-Bermudez, F., Romero-Diaz, A., Martinez-Fernandez,  J., Martinez-Fernandez, J. (1998). Vegetation and soil erosion under a semi-arid Mediterranean climate: a case study from Murcia (Spain). Geomorphology 24, 51-58.
Mahmoudi, Z., and Khademi, H. (2012). The Recognition of Atmospheric Dust Origins in Isfahan Using Chemical and Mineralogical Properities of Dust. Water and Soil Conservation Researches. 21, 1-18. 
McTainsh, G.H. (1999). Dust transport and deposition. PP. 181-211. In: Goudie, A., S. Livingstone and I. Stokes, Aeolian Environments, Sediments and Landforms. John wiley and Sons, Ltd, Chichester.
Modaihsh, A. S. (1997). Characteristics and com position of the falling dust sediments on Riyadh city, Saudi Arabia. J. Arid Environ. 36: 211-223.
Norouzi, S., Khademi, H., Faz Cano, A., Acosta, J.A. (2015). Using plane tree leaves for biomonitoring of dust borne heavy metals: a case study from Isfahan, Central Iran. Ecol. Indic. 57, 64-73.
Nelson, R.E. (1982). Methods of Soil Analysis. 6td ed. American Society of Agronomy.
Rashki, A., Eriksson, P.G., de Rautenbach, C.J.W., Kaskaoutis, D.G., Grote, W., and Dykstra, J. (2013). Assessment of chemical and mineralogical characteristics of airborne dust in the Sistan region. Iran. Chemosphere. 90, 227-236.
Shahsavani, A., Yarahmadi, M., Mesdaghinia, A., Younesian, M., Jaafarzadeh, N., and Naimabadi, M. (2012). Analysis of Dust Storms Entering Iran with Emphasis on Khuzestan Province. Hakim Research Journal. 15(3), 192- 202.
Shi, Z.H., N.F. Fang, F.Z. Wu, L. Wang, B.J. Yue  and G.L. Wu. (2012). Soil  erosion processes  and sediment sorting associated with  transport mechanism on steep slopes. Journal of Hydrology, 454- 455: 123-130.
Ta, W., Xiao, H., Qu, J., Xiao, Z., Yang, G., Wang, T., and Zhang, X. (2004). Measurements of dust deposition in Gansu province, China. Geomorphology. 57, 41-51.
Wang, R., Zou, X., Cheng, H., Wu, X., Zhang, C., and Kang, L. (2015). Spatial distribution and source apportionment of atmospheric dust fall at Beijing during spring of 2008-2009. Environmental Science and Pollution Research. 22, 35-47.
Zarasvandi, A., Carranza, E.J.M., Moore, F., and Rastmanesh, F. (2011). Spatio-temporal occurrences and mineralogical-geochemical characteristics of airborne dusts in Khuzestan Province (southwestern Iran). Journal of Geochemical Exploration. 111, 138-151.
Zolfaghari, H., and Abedzadeh, H. (2005). Synoptic Analysis of Dust Systems in western Iran. Journal of Geography and Urban Space Development. 3, 173-188. (In Farsi).