يوضح توازن كتلة الكلوريد الى جانب ن

يوضح توازن كتلة الكلوريد الى جانب نتائج النظائر البيئيه المستقره والمشعه للماء وجود اليات تغذيه للمياه الجوفيه بالاضافه الى الطرق الهيدروجيولوجيه ، واساليب النظائر التي تقدر شحن المياه الجوفيه بالاضافه الى المعلوماتيه حول عمليات اعادة الشحن ويمكن استخدام النظير المشع 3H لتحديد منشا المياه الجوفيه ، التاريخ ، الاثر الفعلي للمياه الجوفيه ، اعادة والمزج بين المياه الجوفيه في مختلف الاعمار.

النتائج (الإنجليزية) 1:

Mass chloride balance shows, along with the results of isotope environmental stable and radioactive water and the presence of the mechanics of feeding of ground water in addition to hydrogeological methods, and methods of isotopes, estimated shipping underground water in addition to INFORMATICS about the re-shipping operations can be used radioactive isotope 3H to determine the origin of underground water, history, the effect of the actual groundwater, re-mixing of ground water at different ages.

النتائج (الإنجليزية) 2:

The balance of the chloride mass, along with the results of stable and radioactive environmental isotopes of water, shows the presence of mechanisms that feed the ground water in addition to hydrogeological methods, and isotope methods that estimate the shipment of groundwater in addition to information about recharging processes and can be used as analogues. Radioactive 3H to determine the aquifer, history, actual impact of groundwater, re-blending of groundwater in various ages.

النتائج (الإنجليزية) 3:

The results of chlorine mass balance and stable environmental isotopes and radioactive water show that the recharge mechanism of groundwater and the hydrological and isotopic methods are used to estimate the recharge of water In addition to the information during the charging process, 3h isotopes can be used to determine the source, date, actual groundwater impact and mix in groundwater Different ages.