KaydedilenlerDerginizi ekleyin

Dergiler / Turkish Journal of Earth Sciences / 1995 / Cilt: 4 - Sayı: 2

Geochemistry of Regional Groundwater Flow In the Aladag Karstic Aquifer, Eastern Taurids-Turkey: Effect of Flow Conditions

Türker KURTTAŞ
C. Serdar BAYARI
Sayfa
29–37
Yayın Tarihi
2022-11-05
DOI
—
🏛️Bu makalenin bibliyografik verileri ve tam metin bağlantısı DergiPark üzerinden sağlanmıştır.
DergiPark Kaydı ↗
✨

Yapay Zeka Hızlı Bakış & Çıkarımlar

AI Insight
⚡ TL;DR(1 Cümlede Hızlı Çıkarım)

However. gypsum dissolution allong the regional flow path seems to be independent of hydraulic conditions.

📌 3 Maddede Bu Makale

🎯
Amaç & Hipotez:The geochemistry of regional groundwater flow along the Aladag karstic aquifer indicates a remarkable correlation between the hydraulic and geochemical conditions.
📊
Temel Bulgular & Veri:The varition of physical and chemial proper­ ties of the karstic effluents implies that although the carbonate dissolution is perpetual along the flow system. dissolution rates decrease where confined flow conditions start to prevail.
💡
Sonuç & Katkı:However. gypsum dissolution allong the regional flow path seems to be independent of hydraulic conditions.
🔬Tür:Araştırma Makalesi
📍Kapsam:Genişletilmiş Akademik Örneklem
⚙️Değişkenler:Alan Parametreleri

Abstract

The geochemistry of regional groundwater flow along the Aladag karstic aquifer indicates a remarkable correlation between the hydraulic and geochemical conditions. The Aladag karstic aquifer. in between the recharge area and the regional ero­ sion base. comprises unconfined and confined sections. A transition zone along which semi-comfined flow conditions dominate also occurs between these sections. The parts of the aquifer in which unconfined and confined flow conditions dominate seem to be anal· ogous of geochemically open and closed systems of carbonate dissolution. respectively. The varition of physical and chemial proper­ ties of the karstic effluents implies that although the carbonate dissolution is perpetual along the flow system. dissolution rates decrease where confined flow conditions start to prevail. However. gypsum dissolution allong the regional flow path seems to be independent of hydraulic conditions.

🔖

Bu Makaleye Atıf Yap

KURTTAŞ, T., BAYARI, C. S. (2022). Geochemistry of Regional Groundwater Flow In the Aladag Karstic Aquifer, Eastern Taurids-Turkey: Effect of Flow Conditions. Turkish Journal of Earth Sciences, Cilt: 4 - Sayı: 2, 29–37. https://ajindex.com/articles/603298

📄 Tam Metin PDF Okuyucu

📄

PDF görüntüleyici hazırlanıyor...

Kaynakça (1)

  1. Appelo. C.A.J. and Postma. D. 1992. Groundwater. Geochemistry and Pollution. Vrije Universiteic. Amstertam. 51Op. APHA. AWINA and wPCr. 1989. Standard Methods for the Analysis of Water and Waste Water: APHA Publication. 1015th Street. N. w.Wash­ ington D.C. 2005. Ayhan. A. 1988. Geological Map of Turkey Senes. Kozan.i21 Plate­ MTA Publication. Ankara. 12p. (in Turkish). Back. W. and Lesser. J.M. 1981. Geochimcal wnstraints of groundwa­ ter management m the Yucatan Peninsula. Mexico: J. Hydrol. 51. pp. 119-13:>. Back. W. Cherry. R.N. and Hanshaw. B.B. 1982. Chenical equilibnum between water and minerals m carbonate aquifers: (translated bY: G. Aac1k). DSI Teknik B1Jlteni.50. s. 37-41. (in Turkish). Back. W. Hanshaw. B.B. Plummer. N.L. Rahn. P.R. and Rightmire. 1983. Process and rate of de·dolomit1zation: Mass transfer and C-14 dating in a regional carbonate aquifer: Geel. Soc. Am. Bull. 94. pp. 11J 15 1Ll29. Bayan. C.S. 1991. Karst hydrogcological investigation of the Lower Zamant1 Basin (Aladalar): Ph. D. Thesis. Hacettepe University. lnslitute of Pure and Applied Sciences. t 64p. (Unpublished. abstract in English). Bayan. C.S. and Denizman. C. 1993. Preliminal)' hydrogeologtc evalua­ tion of the travertine-depositing karst1c springs 1n the Lower Zamant1 Basin. Eastern Taurids. Turkey· Geosound. Bull. of Depts. of Geological and Mining Engmeenngm. Bayan. C.S. and G(irer. I. 1993. Use of hydrochemical andisotopic techniques m the 1dent1flcat1on of karst groundwarer flow patterns in the Lower Zamant1 Basin:OOCA. Turkish J. Earth. Sci. 2. pp. 37-47. Bogh. A. 1980. Kare• Hydrology and Physical Speleology (rranslated ryy c. Sch1mld). Springer-Verlag. Berlin. 284p. Buhmann. D. and Dreybrodt. W. 1985. The kinetics of calcite dissolu tion and prec1p1tatt0n m geologically relevant s1tuati0ns of karst areas: Chemical Geology. 48. pp. 189 211. •ord. D.C. and W1lhams. P. 1989. Karst Geomorphology and Hydrol­ ogy. Unwin Hyman Publ. Boston. 601p. Gunay. G. and Bayan. C.S. 1991. Isotope survey of the Lower Zamant1 Basin: HU-IAEA Prcyect. Progress Report no. 2. Int. Res. and Applic. Center for Karst Water Resources. Ilacettepe University. Ankara. 31p. Hanshaw. B.B. Back. w. and Deike. R.G. 1971. A geochemical hypothesis for dolomitization by groundwater: Economic Geology. 66. pp. 710-72.ll. Hanshaw. B.B. and Back. W. 1979. Major geochemical processes in the evolution of carbonate aquifer system: J. Hydrol. 43. pp.287-312. Hem. J.D. 1985. Study a