Mixing of brine waste in Puck Bay (the south Baltic Sea) in the light of in-situ measurements

In the north-eastern part of Poland, the underground gas stores are being constructed by diluting salt deposits. Brine, a by-product of the technology applied, is discharged into the coastal waters of the south Baltic Sea by a system of diffusers. To assess the intensity of brine mixing in the near-...

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Veröffentlicht in:Oceanological and hydrobiological studies 2016-03, Vol.45 (1), p.42-54
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description In the north-eastern part of Poland, the underground gas stores are being constructed by diluting salt deposits. Brine, a by-product of the technology applied, is discharged into the coastal waters of the south Baltic Sea by a system of diffusers. To assess the intensity of brine mixing in the near-field of the discharge installation, a monitoring program was carried out. The results demonstrated that under the mildly dynamic conditions of Puck Bay, the discharge of brine (saturation 250 kg m , discharge 300 m h ) leads to salinity excess below 0.5 PSU. For parameters of a real brine discharge, the dilution coefficient estimated by formulas derived from analytical solutions, predictive models and laboratory experiments for stagnant water conditions, varied in the range of 123÷360. The dilution coefficient value estimated on the basis of measurements was 1.27÷3.72 times higher than its value obtained by the use of predictive models, while estimated by formulas obtained from laboratory experiments was in the range of 1.41÷2.26 of the dilution coefficient based on measurements.
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subjects brine discharge
Brines
Coastal waters
Coefficients
Desalination
Diffusers
Dilution
Discharge
Exact solutions
Experiments
in-situ measurements
Laboratories
Laboratory experimentation
Marine
mixing process
Oceanography
Prediction models
Puck Bay
Rivers
Salinity
salinity of water
Salt
Salt deposits
Saturation
Stagnant water
Underground construction
title Mixing of brine waste in Puck Bay (the south Baltic Sea) in the light of in-situ measurements
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