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Manisa Alaşehir graben sistemi içerisinde yer alan Kuvaterner Alüvyon akiferin yıllık beslenim miktarı yeraltısuyu seviye verilerine göre belirlenmiştir. Bunun için alana 10 adet pompaj kuyusu, 30 adet araştırma kuyusu açılmıştır. Akiferin karekterizasyonu yapılmış ve sahada akifer temsil edecek şekilde kuyulara otomatik seviye kaydedici ve 3 noktada meteoroloji istasyonu kurularak veriler elde edilmiştir. Bir hidrolojik dönemde elde edilen seviye verileri kullanılarak en düşük seviye ve en yüksek seviyeler belirlenmiş ve bu verilerden akiferin beslenim miktarı belirlenmiştir. Seviye izleme verisi sonuçlarına göre akiferin yıllık beslenim değerinin 39,6 mm ile 588,99 mm arasında değişmekte ve ortalaması 290 mm’dir. En yüksek beslenme miktarı jeolojik yapıya uyumlu olarak akiferin batı kesimlerindeki geçirimli alüvyonel yelpazelerin dağılım sunduğu alanlarda belirlenmiştir. Seviye değişim yöntemi zaman alıcı ve uzun dönem izleme gerektiren bir yöntem olmasına karşın akiferdeki beslenimin daha doğruya yakın hesaplanmasına yardımcı olan bir yöntem olarak karşımıza çıkmaktadır.
The annual nutrition amount of the Kuvaterner Alüvyon akiferin located within the Manisa Alicir graben system is determined by the level data of the subterranean. For this purpose there are 10 pumping holes, 30 research holes opened in the area. The data were obtained by automatic level recording to the hills in order to represent the hills in the field and installing a meteorological station at 3 points. By using the level data obtained in a hydrological period, the lowest level and the highest levels were determined, and from these data the nutritional amount of acifers was determined. According to the level monitoring data, the annual nutritional value of the acrylic varies between 39.6 mm and 588.99 mm and its average is 290 mm. The highest amount of nutrition is determined in the areas where the distribution of passive alvial varieties in the western parts of the acrylic is in accordance with the geological structure. Although the level change method is a time-consuming and long-term monitoring method, it appears to us as a method that helps to calculate the nutrition in the ends closer.
The annual recharge of the Quaternary Alluvium aquifer in the Manisa Alaşehir graben system was determined according to groundwater level data. For this purpose, 10 pumping wells and 30 research wells were drilled in the area. The characterization of the aquifer was made and the data were obtained by installing an automatic level recorders in wells and meteorology stations to represent the aquifer in the field. Using the level data obtained in a hydrological period, the lowest level and the highest levels were determined and from these data the recharge of the aquifer was calculated. According to the results of monitoring wells, it has been calculated that the annual recharge value of the aquifer varies between 39,6 mm and 588,99 mm with 290 mm on average. The highest recharge value was determined permeable alluvial fans materials in the western parts of the aquifer in accordance with the geological structure. Although the level change method requires long-term monitoring and time, this method helps us to calculate the inflow in the aquifer more accurately.
Alan : Mühendislik; Fen Bilimleri ve Matematik
Dergi Türü : Ulusal
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