The examination of K-1 and K-2 drilling wells located in 2nd Sakarya Organized Industrial Zone by means of geological, geophysical and water characteristics

Our country has a wealth of underground water resources as well as above ground water resources. The geological topographic structure and climate of the region and the ground water level effect result in a linear connection between the well water and its quality. When the relationship between raw water, soft water, cooling water ph and conductivity is examined, it has been observed that fluctuations occurred in the first 6 months of the year and that in the last 6 months there was not much fluctuation except December. During the precipitation and snow melting period, it is seen that the minerals in the water change too much due to environmental effects. This results in the aquifer's superficial flow and precipitation regime. Due to the high ground water level, the lithological structure of the region and the looseness of the layers, coliform and surface pollution can be rapidly penetrated into the wells. Where groundwater flows spontaneously to the ground source The amount and feeding of groundwater, the amount of precipitation, the slope of the surface, the vegetation and the permeability of the stones are determined. Groundwater is abundant in the areas consisting of rainy and permeable stones. In the case of low rainfall, high slope and impermeable ground, the formation of groundwater isdifficult. Sand, gravel, sandstone conglomerate, limestone, volcanic tuffs, alluviums form permeable soils. Therefore alluvial plains and karstic areas are rich in groundwater. Stones such as clay, marl, schist and granite are impermeable. It prevents the formation of groundwater. The water accumulated in the ground is found as Groundwater Artesian Karstic Groundwater. Within the scope of this study made by detay engineering, 66 pieces ground drilling operation, 40 seismic refraction studies and 30 DES studies were used to determine the structure of the study area. The data obtained as a result of all studies, the water characteristics of the well water of the region and the possibility of use in cooling systems have been demonstrated.