2003
DOI: 10.3176/oil.2003.4.04
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Sulphate Balance of Lakes and Shallow Groundwater in the Vasavere Buried Valley, Northeast Estonia

Abstract: Groundwater is an important component of many water resource systems supplying water for domestic use, industry, and agriculture. Management of a groundwater system, an aquifer, means making such decisions as annual withdrawal of the total quantity of water, location of wells for pumping and for artificial recharge and their rates, and control conditions at aquifer boundaries. The decisions related to groundwater quality are of no less importance. In fact, the quantity and quality problems cannot be separated.… Show more

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Cited by 6 publications
(3 citation statements)
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“…On the other hand, the hydrological regime in the valley has been influenced by oil shale mining. The content of sulphate in the surface and groundwater indicates directly the influence of the mining water [22]. The comparatively intensive and uneven water exchange with surrounding mines has been clearly caused by the uneven bedrock topography.…”
Section: Vasavere Valleymentioning
confidence: 99%
“…On the other hand, the hydrological regime in the valley has been influenced by oil shale mining. The content of sulphate in the surface and groundwater indicates directly the influence of the mining water [22]. The comparatively intensive and uneven water exchange with surrounding mines has been clearly caused by the uneven bedrock topography.…”
Section: Vasavere Valleymentioning
confidence: 99%
“…The influence of mining on the lakes has been investigated from the hydrogeological aspect, recommending the usage of infiltration basins and regulation of water flow [10][11][12][13][14]. Water chemistry has been investigated proceeding from the effect of oil shale mining on sulphate content of water [15]. The influence on the landscape and plants has been studied by analysing plant species and mining waste [16][17][18][19].…”
Section: Influence Of Oil Shale Mining On the Area Of Kurtna Landscap...mentioning
confidence: 99%
“…2. Therefore, interaction between all considerable components of water circulation scheme (infiltration of precipitation water into the mines, mine water pumped out into the rivers, groundwater exchange between closed mines and movement at the sites of tectonic damage, total river flow into the Gulf of Finland and Lake Peipsi) for Purtse, Pühajõgi, Vasavere and Rannapungerja rivers is of a combined and developed character [4,14].…”
Section: Total Effect Of Hydrological and Hydrogeological Factorsmentioning
confidence: 99%