Hydrological Modeling of Running Water Process and its impact on the size of Sediment Basins the study Area
DOI:
https://doi.org/10.31973/w58etz19Keywords:
Soil Erodiplity index, Soil protection index, Current erosion indicator, Regression index, Heat coefficient indexAbstract
The study aims to know the effect of the running Water Process on the Sediment Volume of the(ALBint, ALYaraa, and ALGhariz) Through the reality of the study of the study area, it was found that these these sediments date back to the Tertiary period and the deposits of the Quaternary period, since the region is part of the eastern edge of the alluvial plain, which belong to the unstable shelf, and its source is the valleys sloping from the eastern side of the Iraqi-Iranian border. Which was formed by heavy rains in the form of torrents sweeping away sand, gravel, clay, and silt. As rainstorms contribute to large part of the erosion and sedimentation process, As rainfall in the form of heavy showers and large water droplets workes to break up soil units particles and form sediments, which it is easily carried by water flow in the valleys and appears clearly on the slopes. As Sediments move to low-lying lands due to gravity, to estimate soil erosion and sedimentation products Gavrilovic Erosion Model (EPM) was relied upon, which he designed during the 1950s. This model is distinguished by the fact that it estimates different types of sediments. Erosion which made it a suitable model for application in different countries of Eastern Europe, Italy, Greece, Switzerland, and Iran. which are highly eroded mountainous countries. especially after the reliaibility of its results was tested in number of studies and compared to the results of field measurements. It was found that there was a great agreement between the results of the model with the results of field measurements, and its application depends on indicators of slop condition of vegetation cover, Soil or surface formations, rainfall, as well as temperature. this model is unque from others in including the temperature factor as an additional indicator to evaluate Water erosion in addition to field information taken from field study.
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References
حسن، إبتهال تقي، (2014)، إستخدام الأدلة لكشف التغيرات في غطاء الأرض لمناطق مختارة من محافظة النجف للحقبة بين (2001-2006) باستخدام بيانات الاستشعار عن بعد، مجلة الكوفة للفيزياء، المجلد (6)، العدد (2).
شعوان، جمال، وآخرون، (2013)، توظيف الاستشعار عن بعد ونظم المعلومات الجغرافية في التقييم الكمي للتعرية المائية في حوض واد أمزاز (الريف الأوسط) من خلال نموذج جافريلوفيك، مجلة جغرافية المغرب، عدد خاص بأعمال المؤتمر الثالث للجغرافيين المغاربة ،مجلد (28) العدد (1 – 2 ).
الغامدي، سعد أبو راس، (2009)، تطبيق نموذج جافريلوفيك لتقدير مخاطر التعرية المائية في حوض وادي نعمان بوسائل تقنيات الأستشعار عن بعد ونظم المعلومات الجغرافية، قسم الجغرافيا، جامعة أم القرى، ص.ب.33006، المجلد 1، العدد1. DOI: https://doi.org/10.21608/egjec.2009.95200
كاظم، محمد احمد، (2017)تصنيف بعض ترب منطقة شط العرب في محافظة البصرة وتقييم ملائمة الأراضي للأغراض الزراعية بالاستعانة بتقانات الاستشعار عن بعد، اطروحة دكتوراه (غير منشورة ) كلية الزراعة , جامعة البصرة.
Amer Zeghmar", Nadir Marouf", Elhadj Mokhtari , ,(2021)Assessment of soil erosion using the GIS-based erosion potential method in the Kebir Rhumel Watershed, Northeast Algeria , JOURNAL OF WATER AND LAND DEVELOPMENT. DOI: https://doi.org/10.24425/jwld.2022.140383
Abdeni Elalui , et al ,(2023). Soil Erosion under Future Climate Change Scenarios in a Semi-Arid Region , Science Agadir, IbnZohr University, Agadir , Morocco.
Eelko.Bergsma,1983,Rain FallErosion,Servers for Conservition Planning,Itc,Nether Journal,VOI-2.
Fournier,F.1960, Climate Erosion, Ia reiation ekter Ie resion du sol parieau et Iesperception, atmospherges,Pairs.
Gavrilovec Z. Stefanovic M. Milojivc M. and Cortic J. (2006)Erosion Potential Method Conference of the Danubian Countries on the Hydrological Forecasting and Hydrological Bases of Water Management, Bled, Sloveni.
Zachar. D.(1982) Soil Erosion Amsterdam: Elsevier science publishing company.
Zoren,M and Komac,B,(2005),Soil erosion on agricultural land in Slovenia merasurements of rill erosion in the besnica valley.Acta geographic slovenica 45-1,Ljubljana. DOI: https://doi.org/10.3986/AGS45103
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