한국 중부 조간대 퇴적물의 닫힌챔버법을 이용한 메탄방출량 평가
DC Field | Value | Language |
---|---|---|
dc.contributor.author | 이준호 | - |
dc.contributor.author | 정갑식 | - |
dc.contributor.author | 우한준 | - |
dc.contributor.author | 강정원 | - |
dc.contributor.author | 이동헌 | - |
dc.date.accessioned | 2020-07-16T05:52:29Z | - |
dc.date.available | 2020-07-16T05:52:29Z | - |
dc.date.created | 2020-02-11 | - |
dc.date.issued | 2014-02-28 | - |
dc.identifier.uri | https://sciwatch.kiost.ac.kr/handle/2020.kiost/26412 | - |
dc.description.abstract | A closed flux chamber technique method was used for measuring methane (CH<sub>4</sub>) gas from intertidal flat sediments at Taean in mid-west south Korea for 3 days of March 2013. Methane emissions were measured 3 sites (Hwang-do, Sindu-ri, and Sogeun-ri at Taean) during the ebb tide hours only. The 3 sites surface sediment were analyzed for size parameters in the laboratory by Fork analysis. And the methane fluxes were calculated based on the methane concentration rate (Gas Chromatography 6890 FID detector) of change measured inside a closed chamber. The methane fluxes were 0.23 mg m<sup>-2</sup> h<sup>-1</sup> (silty Sand, Hwang-do), 0.45 mg m<sup>-2</sup> h<sup>-1</sup> (Sand, Sindu-ri), and 0.60 mg m<sup>-2</sup> h<sup>-1</sup> (slightly gravelly Sand, Sogeun-ri), respectively. Methane fluxes in environment of surface layer possessed a correlation with sediment sizes. But the variations of methane fluxes was related to several factors depending upon field conditions such as amount of sunshine, bio-activity, water conductivity, sediment/air temperature, and tide level., and Sogeun-ri at Taean) during the ebb tide hours only. The 3 sites surface sediment were analyzed for size parameters in the laboratory by Fork analysis. And the methane fluxes were calculated based on the methane concentration rate (Gas Chromatography 6890 FID detector) of change measured inside a closed chamber. The methane fluxes were 0.23 mg m<sup>-2</sup> h<sup>-1</sup> (silty Sand, Hwang-do), 0.45 mg m<sup>-2</sup> h<sup>-1</sup> (Sand, Sindu-ri), and 0.60 mg m<sup>-2</sup> h<sup>-1</sup> (slightly gravelly Sand, Sogeun-ri), respectively. Methane fluxes in environment of surface layer possessed a correlation with sediment sizes. But the variations of methane fluxes was related to several factors depending upon field conditions such as amount of sunshine, bio-activity, water conductivity, sediment/air temperature, and tide level. | - |
dc.description.uri | 1 | - |
dc.language | English | - |
dc.publisher | Ocean Science Meeting (OSM)/AGU/ASLO | - |
dc.relation.isPartOf | Ocean Sciences Meeting/2014 Ocean Sciences Meeting | - |
dc.title | 한국 중부 조간대 퇴적물의 닫힌챔버법을 이용한 메탄방출량 평가 | - |
dc.title.alternative | Evaluation for methane Emissions of the Intertidal Flat Sediments Using Enclosure Chamber Technique Method, Mid-west South Korea | - |
dc.type | Conference | - |
dc.citation.conferencePlace | US | - |
dc.citation.endPage | 142 | - |
dc.citation.startPage | 142 | - |
dc.citation.title | Ocean Sciences Meeting/2014 Ocean Sciences Meeting | - |
dc.contributor.alternativeName | 이준호 | - |
dc.contributor.alternativeName | 정갑식 | - |
dc.contributor.alternativeName | 우한준 | - |
dc.contributor.alternativeName | 강정원 | - |
dc.contributor.alternativeName | 이동헌 | - |
dc.identifier.bibliographicCitation | Ocean Sciences Meeting/2014 Ocean Sciences Meeting, pp.142 | - |
dc.description.journalClass | 1 | - |