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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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. |
doi_str_mv | 10.1515/ohs-2016-0005 |
format | Article |
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, 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.</description><identifier>ISSN: 1897-3191</identifier><identifier>ISSN: 1730-413X</identifier><identifier>EISSN: 1897-3191</identifier><identifier>DOI: 10.1515/ohs-2016-0005</identifier><language>eng</language><publisher>Berlin: De Gruyter</publisher><subject>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</subject><ispartof>Oceanological and hydrobiological studies, 2016-03, Vol.45 (1), p.42-54</ispartof><rights>Copyright Walter de Gruyter GmbH 2016</rights><rights>This work is published under http://creativecommons.org/licenses/by-nc-nd/4.0 (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><rights>2016. This work is published under http://creativecommons.org/licenses/by-nc-nd/4.0 (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c444t-9de79f421cefc66cee69d60e3163485d9b101e47c62f7bb8030ae69fe51220423</citedby><cites>FETCH-LOGICAL-c444t-9de79f421cefc66cee69d60e3163485d9b101e47c62f7bb8030ae69fe51220423</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,860,27903,27904</link.rule.ids></links><search><creatorcontrib>Robakiewicz, Małgorzata</creatorcontrib><title>Mixing of brine waste in Puck Bay (the south Baltic Sea) in the light of in-situ measurements</title><title>Oceanological and hydrobiological studies</title><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. 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water</subject><subject>Salt</subject><subject>Salt deposits</subject><subject>Saturation</subject><subject>Stagnant water</subject><subject>Underground 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Małgorzata</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c444t-9de79f421cefc66cee69d60e3163485d9b101e47c62f7bb8030ae69fe51220423</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2016</creationdate><topic>brine discharge</topic><topic>Brines</topic><topic>Coastal waters</topic><topic>Coefficients</topic><topic>Desalination</topic><topic>Diffusers</topic><topic>Dilution</topic><topic>Discharge</topic><topic>Exact solutions</topic><topic>Experiments</topic><topic>in-situ measurements</topic><topic>Laboratories</topic><topic>Laboratory experimentation</topic><topic>Marine</topic><topic>mixing process</topic><topic>Oceanography</topic><topic>Prediction models</topic><topic>Puck Bay</topic><topic>Rivers</topic><topic>Salinity</topic><topic>salinity of water</topic><topic>Salt</topic><topic>Salt deposits</topic><topic>Saturation</topic><topic>Stagnant water</topic><topic>Underground 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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.</abstract><cop>Berlin</cop><pub>De Gruyter</pub><doi>10.1515/ohs-2016-0005</doi><tpages>13</tpages><oa>free_for_read</oa></addata></record> |
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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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