The role of fluid mud in the formation of extensive mud sheets during summer on the Duuri macrotidal flat, west coast of Korea SCIE SCOPUS KCI

DC Field Value Language
dc.contributor.author Baek, Young Sook -
dc.contributor.author Chun, Seung Soo -
dc.contributor.author Chang, Tae Soo -
dc.contributor.author Kim, Jung Kwan -
dc.date.accessioned 2020-04-16T09:40:03Z -
dc.date.available 2020-04-16T09:40:03Z -
dc.date.created 2020-01-28 -
dc.date.issued 2018-02 -
dc.identifier.issn 1226-4806 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/1026 -
dc.description.abstract On the Duuri macrotidal flat along the west coast of Korea, mud sheets exceeding 20 cm in thickness form during summer, and are completely eliminated in the course of the following winter. This cyclical seasonal deposition/erosion of mud on the extensive intertidal flat of Korea has to date not been plausibly explained. To elucidate the responsible mechanism, vertical profiles of suspended sediment concentrations (SSCs) were obtained from March to August 2008 using an ASM-IV, which comprises a vertical array of OBS sensors mounted within a 1.44-m-long pole. The measurements reveal that a high-concentration mud layer begins to develop in mid-May, and reaches concentrations over 10 g/l (fluid mud) by August. SSCs are observed to be generally higher at spring tide than at neap tide. The fluid mud (SSCs > 10 g/l) clearly responds to wave action: the calm period being characterized by a two-layer profile, whereas a gradational one-layer profile during the rough summer season. The fluid mud sheet blanketing the exposed flat is supposed to be semi-consolidated mainly by organic processes and solar radiation during low-water slack tide. The differential response of the fluid mud to the variable seasonal wave-energy conditions thus plays a key role in the rapid and widespread formation of ephemeral mud flats in the study area during summer. The available evidence, however, suggests that the summer mud sheet has a very low potential for preservation in the rock record. -
dc.description.uri 1 -
dc.language English -
dc.publisher GEOLOGICAL SOCIETY KOREA -
dc.subject SOUTHEASTERN YELLOW-SEA -
dc.subject FINE-SEDIMENT TRANSPORT -
dc.subject SUSPENDED SEDIMENT -
dc.subject SEVERN ESTUARY -
dc.subject WADDEN SEA -
dc.subject GOMSO BAY -
dc.subject DYNAMICS -
dc.subject FACIES -
dc.subject MATTER -
dc.subject SHELF -
dc.title The role of fluid mud in the formation of extensive mud sheets during summer on the Duuri macrotidal flat, west coast of Korea -
dc.type Article -
dc.citation.endPage 32 -
dc.citation.startPage 19 -
dc.citation.title GEOSCIENCES JOURNAL -
dc.citation.volume 22 -
dc.citation.number 1 -
dc.identifier.bibliographicCitation GEOSCIENCES JOURNAL, v.22, no.1, pp.19 - 32 -
dc.identifier.doi 10.1007/s12303-017-0063-z -
dc.identifier.scopusid 2-s2.0-85038622959 -
dc.identifier.wosid 000423583800003 -
dc.type.docType Article -
dc.description.journalClass 1 -
dc.subject.keywordPlus SOUTHEASTERN YELLOW-SEA -
dc.subject.keywordPlus FINE-SEDIMENT TRANSPORT -
dc.subject.keywordPlus SUSPENDED SEDIMENT -
dc.subject.keywordPlus SEVERN ESTUARY -
dc.subject.keywordPlus WADDEN SEA -
dc.subject.keywordPlus GOMSO BAY -
dc.subject.keywordPlus DYNAMICS -
dc.subject.keywordPlus FACIES -
dc.subject.keywordPlus MATTER -
dc.subject.keywordPlus SHELF -
dc.subject.keywordAuthor tidal flat -
dc.subject.keywordAuthor summer mud -
dc.subject.keywordAuthor fluid mud -
dc.subject.keywordAuthor suspended sediments concentration -
dc.subject.keywordAuthor vertical profile of SS -
dc.subject.keywordAuthor wave effect -
dc.relation.journalWebOfScienceCategory Geosciences, Multidisciplinary -
dc.description.journalRegisteredClass scie -
dc.description.journalRegisteredClass scopus -
dc.description.journalRegisteredClass kci -
dc.relation.journalResearchArea Geology -
Appears in Collections:
Marine Environmental & Climate Research Division > Marine Active Fault Research Unit > 1. Journal Articles
Files in This Item:
There are no files associated with this item.

qrcode

Items in ScienceWatch@KIOST are protected by copyright, with all rights reserved, unless otherwise indicated.

Browse