قاموا بتحديد العمر التقريبي للمياه

قاموا بتحديد العمر التقريبي للمياه ، تم اخذ اربعة نماذج من مياه الابار ، واربعة نماذج من مياه العيون وذلك لحساب تركيز التريتيوم 3H وهو النظير المشع للمياه الذي يحدد عمر تكوين المياه الجوفيه وبعد ظهور النتائج ومقارنتها مع تصنيف كلارك وفيرتز وجد ان عمر المياه الجوفيه التقريبي هو مياه حديثه ممزوجه مع مياه قديمه قبل سنه 1950 .

النتائج (الإنجليزية) 1:

They identified the age of the approximate water, were taken four models of water wells, and four models of eyes water so as to calculate the concentration of tritium 3H, a radioactive isotope of water that determines the age of the water composition of groundwater and after the appearance of results and compare them with the classification of Clark Wirtz found that the water age of groundwater approximate is water Speaking mixed with old water before 1950.

النتائج (الإنجليزية) 2:

They determined the approximate life of the water, four models of well water, and four models of eye water were taken to calculate the concentration of tritium 3H, the radioactive isotope of water that determines the life of the formation of the aquifer, and after the appearance of the results and compared with the classification of Clark and Virtz found that the age of the groundwater Approximate is modern water mixed with old water before 1950.

النتائج (الإنجليزية) 3:

They determined the approximate age of water, calculated the concentration of tritium 3h, radioisotope water, and determined the formation age of groundwater based on four models of well water and four hole water After the results appear, compared with Clark's and Fritz's classification, it is found that the approximate age of groundwater is mixed with the old water before 1950.