Isparta (Senirkent-Uluborlu) havzası hidrojeoloji incelemesi
Hydrogeology investigation of Senirkent-Uluborlu basin
Yazar: FATMA SEYMAN
Danışman: PROF.DR. REMZİ KARAGÜZEL
Süleyman Demirel Üniversitesi / Fen Bilimleri Enstitüsü / Jeoloji Mühendisliği Ana Bilim Dalı
Derece: Yüksek Lisans, 2005
Konu: Jeoloji Mühendisliği = Geological Engineering

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Abstract:
ABSTRACTThis study has been prepared as master thesis in Geological Engineering Section of theGraduate School of Natural and Applied Sciences of Süleyman Demirel University.In this study, hydrogeological basin investigation has been carried out to determine the qualityFEDB@97üÂ¦&530Â¦Â¦&%$ü"Â¦ Â¦üÂ¦Â¤Â¢) 1 C 1 A 8 6 4 2 1 )( ! ' ! Â¥ # # Â© ! Â§ Â¥Â£ Â© Â§ Â¥Â£and potential of groundwater of Senirkent-water basin, which is one of the most important fresh water basins in our country. For thispurpose, geological, hydrology, hydrogeology and hydrochemical features of the Senirkent-Uluborlu basin constrained by surface drainage area have been determined.By using previous works made in the study area, 1/100 000 scale geological map and cross-sections of the study area have been prepared. the lithological units, which make up of thearea were seperated into two groups as autochthonous and allochthonous units.eBd7Â¦Â¡ ba5EXWV0üüTB&B7BÂ¤QP&IG(Y ! cS ` Y 1( U Â©Â£ Â© 6 1 1 6 HS R C Â© ( 1 ' ! Â¥ Â© H Â©Autochthonous units consists from oldestBügÂqY P%Â%pÂGvBWVwüV$ÂVgÂyeVwuvpuVtsÂ¦V&Â¦rqÂ¡bVGbpÂ¦ihd%ü%gü&R 11 6 !f Â¥ Â¥Â¥Â£ Â© Â§ Â¥Â£ Â¢ Y 1 ! Â©( 1 UÂ£Â¥ 1 # !x Y ! Â©( U Â©C1( 1 U Â©Â£ ' ! Â© #1 Â§ U1 Uc16!1 ÂVaqVÂÂ¡rq&Â¦&Â¦i$pwüo$EBdBWw&gm%gg&h@E&%pÂ¦üFQÂ0PuBÂW%$&wiÂ@Â ÂX%$ÂüüÂt Â Â s Â i ÂÂ Â Â f gÂ Â gÂÂ Â eÂ Â Â ÂÂ Â d Â f ÂÂ n Â Â Â l k Â j Â i g Â ÂÂ Â Â fÂ e Â Â Â ÂÂ dÂ Â Â d d Â Â Â Â Â Â ÂÂÂ Â Â Â ÂÂ Â Â ÂÂ Âonly the allochthonous unit in the area:iDVÂdVz70rgüÂeBxv&Â¦&70$BÂÂÂ Â Â ÂÂ Â Â fÂÂ y Â el i Â w u f gÂ Â gÂÂ Â e ÂThe litological units have been evaluated as permeable, semi-permeable, impermeable units interms of their hidrogeological features and 1/100 000 scale hydrogeological map was made.Hydrogeologic parameters (K,T,S) of alluvium aquifer were estimated by using results ofÂ ÂXePbdqÂ¡0ÂGÂÂüd$$Â¤"d&Bp%$%ÂT$VÂügQ"gq"&y&$WI%zwBüv{"ü&iÂ ÂÂ g Â Â d Â Â Â tÂ ÂÂ nÂ e d Â Â Â Â u Â Â Â f Â n Â Â Â Â Â Â Â ÂÂ n Â Â u Â Â Â Â ~ k } Â e Â f Â Â Â fÂ d Â i | Â i f ghydrogelogical parameters for Senirkent area are T= 3.44x10-3 m2/s, K= 3.24x10-5m/s,S=2.81x102, and for Uluborlu area; T= 1.84x10-3 m2/s, K= 6.15x10-6m/s, S=1.95.Groundwater map of the study area shows that direction of groundwater flow is towards the&BÂÂ7üdw&y Âu Â Â Â Â dÂ e dÂBy using precipitation, evaporation-transpiration, flow data of the area, total recharge anddischarge were found as 465,174x106m3/year and 375,84x106m3/year respectively. Waterbudget deficit was calculated as 90x106m3/year and the amount of water, which can be usedsafely, was determined as 54x106m3/year, %60 of water budget deficit.In order to find out the hydrogeochemical features, surface and groundwater samples takenfrom representative locations in the study area were analysed for the hydrochemical features.1/100 000 scale hydrochemical map was made to find out relation of water chemistry withlithological units and to see the differences in regional scale. Waters plut within the Ca-Mg-HCO3 area in Piper diagram and it is throught that this waters are in releation with carbonaterocks. They take place in good-best quality waters in Schöller diagram, in C2S1 class indiagram of USA Salinity Lab., good-best usable waters in Wilcox diagrams.Values of NO3, NO2, NH4 heavy metals analyses made to determine pollution of groundwater,show that water in the basin have been affected from the outer-originated polluters.Key Words: Geology, hydrogeology, Senirkent-Uluborlu, water budget,water chemistry