<abstract xmlns="http://www.w3.org/1999/xhtml">

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-3, discharge 300 m3 h-1) 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.
</abstract>

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-3, discharge 300 m3 h-1) 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.

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

Department of Coastal Engineering and Dynamics

Oceanological and Hydrobiological Studies

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License.

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,...

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

Article Category: Original research paper

Publié en ligne: 10 mars 2016

Pages: 42 - 54

Reçu: 05 mai 2015

Accepté: 01 sept. 2015

DOI: https://doi.org/10.1515/ohs-2016-0005

Mots clés
brine discharge, in-situ measurements, Puck Bay, mixing process, salinity of water

© Faculty of Oceanography and Geography, University of Gdañsk, Poland. All rights reserved.

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License.

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

Article Category: Original research paper

Publié en ligne: 10 mars 2016

Pages: 42 - 54

Reçu: 05 mai 2015

Accepté: 01 sept. 2015

DOI: https://doi.org/10.1515/ohs-2016-0005

Mots clésbrine discharge, in-situ measurements, Puck Bay, mixing process, salinity of water

© Faculty of Oceanography and Geography, University of Gdañsk, Poland. All rights reserved.

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License.

Mots clés
brine discharge, in-situ measurements, Puck Bay, mixing process, salinity of water