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해양심층수와 지하염수 자원의 비교분석

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dc.contributor.author문덕수-
dc.contributor.author정동호-
dc.contributor.author김현주-
dc.contributor.author신필권-
dc.date.accessioned2021-12-09T00:41:03Z-
dc.date.available2021-12-09T00:41:03Z-
dc.date.issued20031128-
dc.identifier.urihttps://www.kriso.re.kr/sciwatch/handle/2021.sw.kriso/7218-
dc.description.abstractDeep Ocean Water is formed within restricted area including polar sea (high latitude) by cooling of surface seawater and globally circulated in the state of insolation with surface seawater. Although not as obvious as estuaries mixing, Brine groundwater is mixture of recirculated seawater and groundwater. Seawater having high osmotic pressure infiltrate into unconfined aquifer where is connected to the sea. The ions dissolved in seawater are present in constant proportions to each other and to the total salt content of seawater. However deviation in ion proportions have been observed in some brine groundwater. Some causes of these exception to the Rule of constant proportions are due to many chemical reactions between periphery soil and groundwater. While Deep Ocean Water (DOW) have a large quantity of functional trace metals and biological affinity relative to brine groundwater, DOW have relatively small amount of harmful bacteria and artificial pollutants.-
dc.language한국어-
dc.language.isoKOR-
dc.title해양심층수와 지하염수 자원의 비교분석-
dc.title.alternativeComparative analysis of resources characteristics for deep ocean water and brine groundwater-
dc.typeConference-
dc.citation.title한국해양환경공학회-
dc.citation.volume2003-
dc.citation.number11-
dc.citation.startPage185-
dc.citation.endPage189-
dc.citation.conferenceName한국해양환경공학회-
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