Hydrogeological parameters used in determining karstic features of Konya-Karapinar basin

The study area, near the town of Konya- Karapınar and into the area of 2500 km2 is an area due. The study area has suitable resolution Bolkardağı Units which composed of Jurassic-Cretaceous limestones and Miocene and after units. Konya Basin, into an interior basin of the biggest causes of climatic changes, as well as karst development model characteristic shape of the cave-shaped obruks or obruks are through the sudden discharge of water. Some of the obruks in the area in case fossils, some of the becomes actives. In some areas, the new obruks are formed or in formation stage. In short, obruk development is ongoing in the region and that prevent the development is not possible. This continuity, in some regions will threaten the security of life and property has reached proportions.In this study, using the hydrogeological parameters, collapse may occur when identification of possible areas to be; work in the field every 25 km2 best considered to be representative of the level of the wells by taking measurements, and especially to date Akkuyu İnoba obruks and around the well level measurements often enabling the underground water table map was drawn. According to the in-situ tests, where the 72 points of measured values; dissolved oxygen, pH, temperature distribution and specific electrical conductivity maps were made. In line with this map is defined as Akkuyu-inoba corridor probable depression was defined a dangerous line. Hydrochemical studies within the scope of the 31 points taken from the water samples was performed, the major anion-cation analysis Piper, Schoeller, U.S.A. Salinity and Wilcox diagrams have been evaluated, water origin, type and classification are interpreted.