Research Article

Origin of groundwater salinity and hydrogeochemical processes in a confined coastal karst aquifer: A cause of the Mandalia Bay (southeastern Aegean Sea coasts)

Volume: 2 Number: 1 March 2, 2015
EN

Origin of groundwater salinity and hydrogeochemical processes in a confined coastal karst aquifer: A cause of the Mandalia Bay (southeastern Aegean Sea coasts)

Abstract

There are numerous springs and wells within the context of this research about the part of northern and northeastern in The Mandalia Bay which has an important role regarding tourism and agriculture in Turkey’s Southeastern Aegean coasts. There are an important springs in this basin, as the high discharge with values Ekinambari springs for 5385 l/s, Savrankoy springs for 4215 l/s, Avsar springs for the 1000 l/s, Sucikti springs (Karacahisar) to 400 l/s. The change of the total annual flow observations compatible with each other, an increase was observed in springs of Ekinambari, Savrankoy and Sucikti. The springs group of Ekinambari, is located from the sea about 10 km away in the alluvium. These springs were at the foot of the hill at various points at 46 m altitude, different flow rates and temperatures, allochthonous limestone flows from the broken system. The springs in the investigation area, which was measured in the high current values, of Savrankoy and Ekinambari springs monthly average current value of resources are examined, the difference between the current value is less than by months. In this spring waters of high salinity values (0,5 to 36,2‰) was determined. In this study were questioned as origin of ground water salinity from deep aquifer formations or from current sea water? In the case of salinity, in spring waters have occurred on deep towards the karstic levels of limestones from sea water is saturation. Examined the water was fed by a high level, the transition period is short and in aquifer in contact with shallow circulating water for a short time is. They could say that mixing different amounts of surface water were also. Given these results, the most important spring waters for the region (Savrankoy, Ekinambarı, etc.,) of ground water movement in karstic system pressure and decreasing/increasing rate of interventions performed in the presence of a seawater can be mentioned. 

Keywords

References

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Details

Primary Language

English

Subjects

Engineering

Journal Section

Research Article

Publication Date

March 2, 2015

Submission Date

July 19, 2014

Acceptance Date

September 30, 2014

Published in Issue

Year 2015 Volume: 2 Number: 1

APA
Barut, İ. F. (2015). Origin of groundwater salinity and hydrogeochemical processes in a confined coastal karst aquifer: A cause of the Mandalia Bay (southeastern Aegean Sea coasts). International Journal of Environment and Geoinformatics, 2(1), 25-46. https://doi.org/10.30897/ijegeo.303015
AMA
1.Barut İF. Origin of groundwater salinity and hydrogeochemical processes in a confined coastal karst aquifer: A cause of the Mandalia Bay (southeastern Aegean Sea coasts). IJEGEO. 2015;2(1):25-46. doi:10.30897/ijegeo.303015
Chicago
Barut, İpek F. 2015. “Origin of Groundwater Salinity and Hydrogeochemical Processes in a Confined Coastal Karst Aquifer: A Cause of the Mandalia Bay (southeastern Aegean Sea Coasts)”. International Journal of Environment and Geoinformatics 2 (1): 25-46. https://doi.org/10.30897/ijegeo.303015.
EndNote
Barut İF (March 1, 2015) Origin of groundwater salinity and hydrogeochemical processes in a confined coastal karst aquifer: A cause of the Mandalia Bay (southeastern Aegean Sea coasts). International Journal of Environment and Geoinformatics 2 1 25–46.
IEEE
[1]İ. F. Barut, “Origin of groundwater salinity and hydrogeochemical processes in a confined coastal karst aquifer: A cause of the Mandalia Bay (southeastern Aegean Sea coasts)”, IJEGEO, vol. 2, no. 1, pp. 25–46, Mar. 2015, doi: 10.30897/ijegeo.303015.
ISNAD
Barut, İpek F. “Origin of Groundwater Salinity and Hydrogeochemical Processes in a Confined Coastal Karst Aquifer: A Cause of the Mandalia Bay (southeastern Aegean Sea Coasts)”. International Journal of Environment and Geoinformatics 2/1 (March 1, 2015): 25-46. https://doi.org/10.30897/ijegeo.303015.
JAMA
1.Barut İF. Origin of groundwater salinity and hydrogeochemical processes in a confined coastal karst aquifer: A cause of the Mandalia Bay (southeastern Aegean Sea coasts). IJEGEO. 2015;2:25–46.
MLA
Barut, İpek F. “Origin of Groundwater Salinity and Hydrogeochemical Processes in a Confined Coastal Karst Aquifer: A Cause of the Mandalia Bay (southeastern Aegean Sea Coasts)”. International Journal of Environment and Geoinformatics, vol. 2, no. 1, Mar. 2015, pp. 25-46, doi:10.30897/ijegeo.303015.
Vancouver
1.İpek F. Barut. Origin of groundwater salinity and hydrogeochemical processes in a confined coastal karst aquifer: A cause of the Mandalia Bay (southeastern Aegean Sea coasts). IJEGEO. 2015 Mar. 1;2(1):25-46. doi:10.30897/ijegeo.303015

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