Evaluation of groundwater flow in the south of the Far East
Abstract
The existing methods of studying and quantifying groundwater flow are practically applicable only if there are long-term observations of the natural water regime on a dense network of reference points. The south of the Far East (FE) is poorly studied hydrologically and hydrogeologically. For complex solution of groundwater flow problem even in regional aspect, not to mention complicated conditions of mountainous areas, these methods are unsuitable.
Область исследования:
(Archived) Without section
References
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