Journals / Yerbilimleri / 1998 / Cilt: 0 - Sayı: 20

Hydrogeological investigation of Yedigöz (Elazığ) Spring

Yedigöz (Elazığ) Kaynağı' nın hidrojeoloji incelemesi

Pages
31–40
Publication Date
2022-11-05
DOI
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AI Summary & Key Takeaways

AI Insight
⚡ TL;DR(Too Long; Didn't Read)

In autumn and winter, the cation and anion orders are as follows: r( Na+K) > rCa > rMg, rCI > rHCO3 > rSO4While, during spring and summer these orders are as follows: rCa > r(Na+K) > rMg , rHCO3> rCI >rSO4 Anioris and cations of Yedigöz Springs are generally gathered in fifth and nineth areas on Piper Diagram.

📌 3 Key Takeaways

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Objective & Hypothesis:The study area is located in NE of city of Elazığ, Mesozoic and Senozoic aged formations cropout in the study area.
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Key Findings & Data:The volume of water discharged above the discharge level of the spring was estimated as $2.33*10^5$ m3 during the period between July 1 and October 28, 1995.
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Conclusion & Impact:In autumn and winter, the cation and anion orders are as follows: r( Na+K) > rCa > rMg, rCI > rHCO3 > rSO4While, during spring and summer these orders are as follows: rCa > r(Na+K) > rMg , rHCO3> rCI >rSO4 Anioris and cations of Yedigöz Springs are generally gathered in fifth and nineth areas on Piper Diagram.
🔬Design:Research Article
📍Scope:Comprehensive Sample
⚙️Variables:Domain Parameters

Abstract

The study area is located in NE of city of Elazığ, Mesozoic and Senozoic aged formations cropout in the study area. These are Elazığ Magmatics, Harami Formation, Kırkgeçit Formation and Karabakır Formation. Long - term measurements of discharge and ion content were carried out in Yedigöz Karstic Spring. The volume of water discharged above the discharge level of the spring was estimated as $2.33*10^5$ m3 during the period between July 1 and October 28, 1995. The volume of water in storage above the discharge level of the Yedigöz Spring was estimated as $1.27*10^6$ m3 during the period between May .10 and September 29, 1996. In autumn and winter, the cation and anion orders are as follows: r( Na+K) > rCa > rMg, rCI > rHCO3 > rSO4While, during spring and summer these orders are as follows: rCa > r(Na+K) > rMg , rHCO3> rCI >rSO4 Anioris and cations of Yedigöz Springs are generally gathered in fifth and nineth areas on Piper Diagram.

Özet

İnceleme alanı Elazığ il merkezinin kuzeydoğusunda yeralmaktadır. İnceleme alanı Mesozoyik ve Senozoyik yaşlı birimlerden oluşmaktadır. Bunlar Elazığ Mağmatitleri, Harami Formasyonu, Kırkgeçit Formasyonu ve Karabakır Formasyonu'dur. Yedigöz Karstik Kaynağı'nda uzun süreli debi ve iyon değişimi kontrol edilmiştir. Kaynağını Temmuz - 28 Ekim 1995 tarihleri arasındaki boşalım kodu üzerinde boşalttığı su miktarı 233 000 m3 , 10 Mayıs - 29 Eylül 1996 tarihleri arasındaki boşalım kodu üzerinde depolama gücü ise $1.27*10^6$ m3 ' tür.Kaynak suyunda katyon ve anyonların sıralanışı sonbahar ve kış aylarında: r( Na+K) > rCa > rMg , rCI > rHCO3 > rSO4ilkbahar ve yaz aylarında ; rCa > r(Na+K) > rMg , rHCO3 > rCI > rSO4 şeklindedir. Yedigöz Kaynak suyunda Piper diyagramı esas alınarak katyon ve anyonlar genel olarak 5. ve 9. bölgede gruplanmışlardır.

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Cite This Article

ÇETİNDAĞ, B., CANİK, B., PASVANOĞLU, S. (2022). Hydrogeological investigation of Yedigöz (Elazığ) Spring. Yerbilimleri, Cilt: 0 - Sayı: 20, 31–40. https://ajindex.com/articles/647121

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