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Safranbolu (Zonguldak) kuzeyinin karst hidrojeolojisi incelemesi

Başlık çevirisi mevcut değil.

  1. Tez No: 47128
  2. Yazar: KORAY TÖRK
  3. Danışmanlar: PROF.DR. GÜLTEKİN GÜNAY
  4. Tez Türü: Yüksek Lisans
  5. Konular: Jeoloji Mühendisliği, Geological Engineering
  6. Anahtar Kelimeler: Hidroloji, Karabük-Safranbolu, Karst kaynağı, Hydrology, Karabük-Safranbolu, Karst spring
  7. Yıl: 1995
  8. Dil: Türkçe
  9. Üniversite: Hacettepe Üniversitesi
  10. Enstitü: Fen Bilimleri Enstitüsü
  11. Ana Bilim Dalı: Belirtilmemiş.
  12. Bilim Dalı: Belirtilmemiş.
  13. Sayfa Sayısı: Belirtilmemiş.

Özet

ABSTRACT The aim of the Investigation is to explain the hydrodynamic characteristic of the limestone and the karstic springs which are used for Safranbolu's water necessity. The tectonic movement that resulted from a compression in north- south direction progressed the karstiflcation. Morphologically three relief systems were separated. These are belong to Middle Miocene, Upper Miocene, Pliocene and later periods. The karstiflcation is developed more intensively at the Upper Miocene relief areas. The llthology which settled on this relief is Ökuşme limestone group of Zonguldak Fomıation. The karstiflcation is shallow and developed along horizontal direction because of the underlying impervious rocks. Over the investigation area the mean annua/ precipitation is 600 mm, the temperature 12.5 °C and the actual evaporation 479 mm. The three important springs issue the waters drained from the karstic limestone. These are namely Mencilis, Hızar and Gürleyik springs. Total annual discharge of the springs is 28. 14 x İ06 m3. Mencilis and Hızar springs which are karstic discharge most of the rain failing over the basin. The general ground water direction found that from NW to SE by means of the cave systems. Mencilis spring drained the developed karstic system but Hızar spring also drained by the small fractured systems, sandy-clayey systems which have low tmnsmissMty properties.

Özet (Çeviri)

ABSTRACT The aim of the Investigation is to explain the hydrodynamic characteristic of the limestone and the karstic springs which are used for Safranbolu's water necessity. The tectonic movement that resulted from a compression in north- south direction progressed the karstiflcation. Morphologically three relief systems were separated. These are belong to Middle Miocene, Upper Miocene, Pliocene and later periods. The karstiflcation is developed more intensively at the Upper Miocene relief areas. The llthology which settled on this relief is Ökuşme limestone group of Zonguldak Fomıation. The karstiflcation is shallow and developed along horizontal direction because of the underlying impervious rocks. Over the investigation area the mean annua/ precipitation is 600 mm, the temperature 12.5 °C and the actual evaporation 479 mm. The three important springs issue the waters drained from the karstic limestone. These are namely Mencilis, Hızar and Gürleyik springs. Total annual discharge of the springs is 28. 14 x İ06 m3. Mencilis and Hızar springs which are karstic discharge most of the rain failing over the basin. The general ground water direction found that from NW to SE by means of the cave systems. Mencilis spring drained the developed karstic system but Hızar spring also drained by the small fractured systems, sandy-clayey systems which have low tmnsmissMty properties.

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