| dc.creator |
VAROL, Simge |
|
| dc.creator |
AKSEVER, Fatma |
|
| dc.creator |
DAVRAZ, Ayşen |
|
| dc.date |
2022-12-01T00:00:00Z |
|
| dc.date.accessioned |
2025-02-25T10:32:15Z |
|
| dc.date.available |
2025-02-25T10:32:15Z |
|
| dc.identifier |
75ae117f-ac07-4561-af24-9cde584f4891 |
|
| dc.identifier |
10.1134/s001670292213002x |
|
| dc.identifier |
https://avesis.sdu.edu.tr/publication/details/75ae117f-ac07-4561-af24-9cde584f4891/oai |
|
| dc.identifier.uri |
http://acikerisim.sdu.edu.tr/xmlui/handle/123456789/100187 |
|
| dc.description |
Abstract: In this study, the recharge processes of the springs in the Sandikli and Suhut basins were investigated by stable isotopes, oxygen-18 (δ18O), deuterium (δ2H or δD) and tritium (3H) analysis. The study area consists of volcanics, limestones and clastic rocks. There is a large number of water sources discharged from volcanic origin rocks and clastic limestones in this region. The dominant ions in the springs in the region are Ca2+, Mg2+ and (Formula presented.). The δ18O and δ2H values of the spring waters ranged between –8.0 and –10.8, –53.0 and –69.6 in September-2017, between –7.9 and –10.8, –512.0 and –69.6 in April-2018 respectively. The positions of samples on the δ18O–δ2H diagrams indicate the meteoric origin. The maximum tritium contents of the water samples 5.4 TU in September-2017 and 5.2 TU in April-2018. Deuterium excess (d-excess) values of spring waters were between 9.1 and 17.3‰ in September-2017, between 8.4 and 18.0‰ in April-2018. |
|
| dc.language |
eng |
|
| dc.rights |
info:eu-repo/semantics/closedAccess |
|
| dc.title |
Assessment of Isotopic Characterization (δ18O, δ2H and 3H) and Hydrochemical Processes of the Springs in Kumalar Mountain Region (Afyonkarahisar, Turkey) |
|
| dc.type |
info:eu-repo/semantics/article |
|