شماره مدرك :
6338
شماره راهنما :
5926
پديد آورنده :
نكويي، محسن
عنوان :

مدل سازي تغذيه طبيعي و مصنوعي دشت شهرضا و تاثير تغذيه مصنوعي بر كيفيت منابع آب زيرزميني

مقطع تحصيلي :
كارشناسي ارشد
گرايش تحصيلي :
آبياري و زهكشي
محل تحصيل :
اصفهان: دانشگاه صنعتي اصفهان، دانشكده كشاورزي
سال دفاع :
1390
صفحه شمار :
ده،145ص.: مصور،جدول،نمودار
يادداشت :
ص.ع.به فارسي و انگليسي
استاد راهنما :
جهانگير عابدي كوپايي، سعيد اسلاميان
استاد مشاور :
مهدي حاجيان
توصيفگر ها :
مدل حركت تجمعي بارش , مدل هانتوش
تاريخ نمايه سازي :
14/8/90
استاد داور :
منوچهر حيدرپور، مجيد افيوني
دانشكده :
مهندسي كشاورزي
كد ايرانداك :
ID5926
چكيده فارسي :
به فارسي و انگليسي: قابل رويت در نسخه ديجيتالي
چكيده انگليسي :
AbstractIn order to manage water resources determination of the quantity of recharge in groundwater is a necessary issue Many variable parameters such as soil characteristics topography amount of rainfall evapotranspiration and thedepth of water table are effective factors on the recharge of groundwater Cumulative Rainfall Departure CRD model which is based on the groundwater balance due to its simplicity and minimum need for random parameters is widely used to estimate for groundwater recharge This model needs the data including monthly rainfall watertable statistics aquifer storage coefficient inflow and outflow statistics of the aquifer Moreover water qualitychanges during infiltration through the different geological layers So analyzing the effect of artificial recharge planson the changes in quality of groundwater is of importance The aim of this research was to estimate the quantity ofrecharge in the plain of southern Shahreza and to analyze the effect of artificial recharge plans on the changes ofgroundwater quality in the selected areas The quantity of natural recharge in the southern Shahreza plain area wassimulated using CRD model Also the water table was simulated by this model for each month The results showedthat the trend of simulated water table follows the measured data The differences between the simulated andmeasured diagrams for water table may be attributed to the factors such as lack of data on unauthorized wells overextraction in the authorized wells and the lack of measurement of water table in the area at the same time Thequantity of natural recharge in the southern Shahreza plain was equivalent to 34 61 of rainfall
استاد راهنما :
جهانگير عابدي كوپايي، سعيد اسلاميان
استاد مشاور :
مهدي حاجيان
استاد داور :
منوچهر حيدرپور، مجيد افيوني
لينک به اين مدرک :

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