Geophysical and Drill-hole Investigations for Detecting Groundwater Aquifers Around Başiskele-Kocaeli
Abstract
Electrical Resistivity method for groundwater exploration in İzmit-Başiskele district was applied. The investigation involved the utilization of Vertical Electrical Sounding (VES) technique with schlumberger electrode array system. The studied area is located within the sedimentary basin. The data acquired from the 5 DES stations were interpreted. The VES results of the data revealed three layers nameli the topsoil of resitivity 40-70 Ώm, gravely sand of 94-102 Ώm and sandy gravel of 102-150 Ώm. The water of flow 12lt/sec was obtained from the drill-hole drilled up to 80 m of depth within sandy gravel in the investigation area
References
- ARIYO, S.O. ODUWOLE, M.O and MOSURO, G.O., 2003. Hydro-geopghysical,evaluation of groundwater potentials of Awa-Ijebu, Southwestern Nigeria. Journal of the Nigeria Association of Hydrogeologist (NAH) vol. 14 . pp 31-36.
- CARRUTHERS, R.M., 1985. Review of geophysical techniques for groundwater exploration in crystalline basement terrain. British Geological SurveyReport. NORGRG 85/3.
- EMENIKE, E.A., 2001. Geophysical exploration for groundwater in a Sedimentary Environment. A case study from Nanka over Nanka Formation in Anambra Basin, Southeastern Nigeria. Global Journal of Pure and Applied Sciences Vol. 7, No 1.Pp1-11.
- OLAYINKA, A.I and MBACHI, C.N.C, 1992. A technique for The interpretation of electrical sounding from crystalline basement Areas of Nigeria. Journal of Mining and Geology vol. 27. Pp 63-69.
- OLORUNNIWO, M.A and OLORUNFEMI, M.O, 1987. Geophysical investigation for groundwater in Precambrian terrain, a case history from Ikare, Southwestern Nigeria. Jounal of African Earth Sciences 6. Pp787-796.
Abstract
İzmit-Başiskele beldesinde yeraltı suyu araştırmak amacıyla elektriksel özdirenç metodu uygulanmıştır. Çalışma Schlumberger elektrot sistemini uygulayan Düşey Elektrik Sondaj ölçümlerini (DES) kapsamaktadır. Çalışma alanı İzmit kenti doğusunda sedimanter bir alanda yer almaktadır. Veriler 5 adet DES istasyonundan toplanmış ve değerlendirilmiştir. DES verilerinden üstte özdirenci 40-70 Ώm arasında değişen örtü tabakası ile onun altında özdirenci 94-102 Ώm arasında değer alan çakıllı kum tabakası ve en altta ise özdirenci 102-150 Ώm arasında değişen kumlu çakıllı birimin istiflendiği anlaşılmıştır. Burada 80 m derinlikte açılan iki adet su sondaj kuyusunun her birinden saniyede 12 lt su alınmıştır
References
- ARIYO, S.O. ODUWOLE, M.O and MOSURO, G.O., 2003. Hydro-geopghysical,evaluation of groundwater potentials of Awa-Ijebu, Southwestern Nigeria. Journal of the Nigeria Association of Hydrogeologist (NAH) vol. 14 . pp 31-36.
- CARRUTHERS, R.M., 1985. Review of geophysical techniques for groundwater exploration in crystalline basement terrain. British Geological SurveyReport. NORGRG 85/3.
- EMENIKE, E.A., 2001. Geophysical exploration for groundwater in a Sedimentary Environment. A case study from Nanka over Nanka Formation in Anambra Basin, Southeastern Nigeria. Global Journal of Pure and Applied Sciences Vol. 7, No 1.Pp1-11.
- OLAYINKA, A.I and MBACHI, C.N.C, 1992. A technique for The interpretation of electrical sounding from crystalline basement Areas of Nigeria. Journal of Mining and Geology vol. 27. Pp 63-69.
- OLORUNNIWO, M.A and OLORUNFEMI, M.O, 1987. Geophysical investigation for groundwater in Precambrian terrain, a case history from Ikare, Southwestern Nigeria. Jounal of African Earth Sciences 6. Pp787-796.
Details
| Other ID | JA25PB39FA |
|---|---|
| Journal Section | Articles |
| Authors | |
| Publication Date | July 13, 2016 |
| Published in Issue | Year 2010 Volume: 9 Issue: 2 |