Aragonite undersaturation in Gwangyang Bay, South Korea: Effects of fresh water input SCIE SCOPUS KCI

DC Field Value Language
dc.contributor.author Kim, Dongseon -
dc.contributor.author Yang, Eun-Jin -
dc.contributor.author Baek, Seung Ho -
dc.contributor.author Kim, Kyung-Hee -
dc.contributor.author Jeong, Jin-Hyun -
dc.contributor.author Kim, Young-Ok -
dc.date.accessioned 2020-04-20T04:40:08Z -
dc.date.available 2020-04-20T04:40:08Z -
dc.date.created 2020-01-28 -
dc.date.issued 2014-09 -
dc.identifier.issn 1738-5261 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/2746 -
dc.description.abstract Dissolved inorganic carbon (DIC) and alkalinity were precisely measured for surface and bottom waters in Gwangyang Bay, Korea, during the four seasons to assess seasonal variations of aragonite saturation state (Omega(arag)). Both the surface and bottom waters were undersaturated with respect to aragonite during summer but were supersaturated during the other seasons. The summertime undersaturation of the surface waters with respect to aragonite may have been a result of the dilution effect caused by higher seasonal river runoff. In the bottom waters, the average DIC concentration increased by 40.6 mu mol kg((TM) 1) from spring to summer, while the average alkalinity decreased by 74.7 mu eq kg((TM) 1). As a result, the alkalinity/DIC ratio decreased from 1.07 in spring to 1.01 in summer and pH also decreased from 7.91 to 7.48, which resulted in the summertime undersaturation of the bottom waters. -
dc.description.uri 1 -
dc.language English -
dc.publisher 한국해양과학기술원 -
dc.title Aragonite undersaturation in Gwangyang Bay, South Korea: Effects of fresh water input -
dc.type Article -
dc.citation.endPage 230 -
dc.citation.startPage 223 -
dc.citation.title OCEAN SCIENCE JOURNAL -
dc.citation.volume 49 -
dc.citation.number 3 -
dc.contributor.alternativeName 김동선 -
dc.contributor.alternativeName 양은진 -
dc.contributor.alternativeName 백승호 -
dc.contributor.alternativeName 김경희 -
dc.contributor.alternativeName 정진현 -
dc.contributor.alternativeName 김영옥 -
dc.identifier.bibliographicCitation OCEAN SCIENCE JOURNAL, v.49, no.3, pp.223 - 230 -
dc.identifier.doi 10.1007/s12601-014-0022-9 -
dc.identifier.scopusid 2-s2.0-84927748968 -
dc.identifier.wosid 000343824400006 -
dc.type.docType Article -
dc.identifier.kciid ART001914852 -
dc.description.journalClass 1 -
dc.description.isOpenAccess N -
dc.subject.keywordPlus CALCIUM-CARBONATE SATURATION -
dc.subject.keywordPlus OCEAN ACIDIFICATION -
dc.subject.keywordPlus SEAWATER -
dc.subject.keywordPlus CO2 -
dc.subject.keywordPlus DISSOCIATION -
dc.subject.keywordPlus CONSTANTS -
dc.subject.keywordPlus ACID -
dc.subject.keywordPlus PH -
dc.subject.keywordAuthor aragonite -
dc.subject.keywordAuthor bay -
dc.subject.keywordAuthor pH -
dc.subject.keywordAuthor alkalinity -
dc.subject.keywordAuthor acidification -
dc.relation.journalWebOfScienceCategory Marine & Freshwater Biology -
dc.relation.journalWebOfScienceCategory Oceanography -
dc.description.journalRegisteredClass scie -
dc.description.journalRegisteredClass scopus -
dc.description.journalRegisteredClass kci -
dc.relation.journalResearchArea Marine & Freshwater Biology -
dc.relation.journalResearchArea Oceanography -
Appears in Collections:
Ocean Climate Solutions Research Division > Ocean Climate Response & Ecosystem Research Department > 1. Journal Articles
Marine Resources & Environment Research Division > Marine Environment Research Department > 1. Journal Articles
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