The evaluation of karstic aquifer recharge from spring hydrographs; Kazanpınarı spring (Elmalı Polje, Antalya)
Küçük Resim Yok
Tarih
1996
Yazarlar
Dergi Başlığı
Dergi ISSN
Cilt Başlığı
Yayıncı
Erişim Hakkı
info:eu-repo/semantics/openAccess
Özet
Karstik kaynak hidrografları değerlendirilerek, karst akifer sistemlerinin beslenme, boşalım ve akış şekilleri hakkında önemli bilgiler sağlanmaktadır. Burada, kaynak hidrograflarının düşüş dönemlerinden yararlanarak Maillet' e (1905) göre kaynağın boşalım katsayıları hesaplanmış ve 16 yıllık ortalaması 6,92 $10^{-3} gün^{-l}$ olarak bulunmuştur. Kazanpınarı kaynağının aylık boşalımlarından ve su yılındaki dinamik rezerv değişimlerinden yararlanarak allokton karstik kireçtaşı akiferinin beslenmesi tahmin edilmiş olup yıllık ortalaması 76,66 $l0^6$ m3' tür. Yeraltı suyu beslenmesi; alana düşen yağış miktarı ve mevsimsel dağılımına, akiferin beslenme alanı büyüklüğüne, hava sıcaklığına, akiferin geçirimliliği ve akifer tipi vb faktörlere bağlıdır.
Karstic spring hydrographs have been useful tools in providing valuable information about the recharge, discharge, and flow processes of karstic aquifer systems. In this study, spring discharge coefficients were evaluated based on recession periods of spring hydrographs using Maillet (1905) approach and a mean value of 16 years were evaluated as 6.92 $10^{-3} day^{-l}$- Recharge of alloctonous karstic limestone aquifer were estimated using monthly discharge of Kazanpınarı spring and dynamic reserve changes in the hydrology year and annually average recharge was evaluated as 76.66 $l0^6$ m3. Ground water recharge is affected by such parameters as the precipitation per unit area and its seasonal distribution; size of recharge area of the aquifer; air temperature; hydraulic conductivity of aquifer; the type of aquifer, and other factors.
Karstic spring hydrographs have been useful tools in providing valuable information about the recharge, discharge, and flow processes of karstic aquifer systems. In this study, spring discharge coefficients were evaluated based on recession periods of spring hydrographs using Maillet (1905) approach and a mean value of 16 years were evaluated as 6.92 $10^{-3} day^{-l}$- Recharge of alloctonous karstic limestone aquifer were estimated using monthly discharge of Kazanpınarı spring and dynamic reserve changes in the hydrology year and annually average recharge was evaluated as 76.66 $l0^6$ m3. Ground water recharge is affected by such parameters as the precipitation per unit area and its seasonal distribution; size of recharge area of the aquifer; air temperature; hydraulic conductivity of aquifer; the type of aquifer, and other factors.
Açıklama
Anahtar Kelimeler
Yerbilimleri, Ortak Disiplinler
Kaynak
Geosound
WoS Q Değeri
Scopus Q Değeri
Cilt
Sayı
28
