2013
DOI: 10.1007/s10040-013-1032-x
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Simulation of the hydrogeologic effects of oil-shale mining on the neighbouring wetland water balance: case study in north-eastern Estonia

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Cited by 11 publications
(9 citation statements)
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“…Further studies are needed to estimate the hydraulic conductivity of peat at different humification levels in order to model potential impact of groundwater lowering on water levels on the bog surface. Two contrasting opinions have been published and further plans for oil shale mining in mire-rich NE Estonia require a clear answer to that question (Marandi et al 2013(Marandi et al , 2014Orru et al 2013).…”
Section: Discussionmentioning
confidence: 96%
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“…Further studies are needed to estimate the hydraulic conductivity of peat at different humification levels in order to model potential impact of groundwater lowering on water levels on the bog surface. Two contrasting opinions have been published and further plans for oil shale mining in mire-rich NE Estonia require a clear answer to that question (Marandi et al 2013(Marandi et al , 2014Orru et al 2013).…”
Section: Discussionmentioning
confidence: 96%
“…Marandi et al (2013) used a 3-D hydrogeological model that was calibrated according to the extent of the mine, groundwater level observations and water-abstraction rates at two regimes in 2000 and 2010. They concluded that bedrock aquitard does not confine sufficiently and considerable lowering of groundwater takes place below the mire.…”
Section: Introductionmentioning
confidence: 99%
“…The model is a mathematical deterministic conceptual model which' spatial discretisation is based on a fully distributed model discretising the model into a grid of relatively small elements. The model can be used for simulating scenarios for the vertical hydraulic conductivity of the subsurface, which is of critical importance to potential wetland dewatering as a result of mining (Marandi et al 2013).…”
Section: Hydrological Model Classificationmentioning
confidence: 99%
“…Due to the mining activities, about 200,000 m 3 of water are drained daily from the aquifer system and collected into the surface water network. This results in a decrease of the groundwater levels in the bedrock aquifer and also in the Quaternary sediments below the bog, influencing the water regime in the whole area and, thus, endangering the overall functioning of the wetland water budget [85].…”
Section: Selisoo Bog Estoniamentioning
confidence: 99%