Примеры использования Groundwater flow на Английском языке и их переводы на Русский язык
{-}
-
Official
-
Colloquial
Jurassic karstic limestones; groundwater flow occurs in both directions; weak links to surface waters.
the deeper aquifers may consist of a number of laterally and/or vertically interconnected groundwater flow systems of various orders of magnitude.
In parts of the region, mining of hard coal has also significantly changed the groundwater flow.
leaching and subsequent groundwater flow.
pumping tests, groundwater flow model, Kaliningrad region.
KuČnica aquiFeR(no.83)59 austria Slovenia Type 2; Quaternary carbonate-silicate alluvium.; groundwater flow direction from Austria to Slovenia;
Natural groundwater flow from the Genevese aquifer(No. 123)- the main transboundary aquifer in the basin- to the Lake Geneva is about 789,000 m3/year
strong links to surface water systems, groundwater flow from Serbia to Bosnia
strong links to surface water system; groundwater flow from Bosnia and Herzegovina to Croatia.
in strong connection; groundwater flow from Slovenia to Croatia
weakly linked to surface waters; groundwater flow from Montenegro to Bosnia and Herzegovina.
dominant groundwater flow direction from Slovenia to Italy
The greatest variations in groundwater flow patterns occur where changes in rock types-- for example,
dominant groundwater flow direction: Bulgaria from South to North.
with local Eocene flysch; groundwater flow from Bosnia and Herzegovina to Croatia;
little groundwater flow across the border.
dominant groundwater flow is from Bulgaria towards Turkey
medium to strong link with surface water systems, groundwater flow from the former Yugoslav Republic of Macedonia to Greece
How fast groundwater flows depends on the characteristics of the aquifer.