심해채광을 위한 C-C지역 퇴적물의 지질공학적 특성연구

DC Field Value Language
dc.contributor.author 지상범 -
dc.contributor.author 김기현 -
dc.contributor.author 이현복 -
dc.contributor.author 주세종 -
dc.contributor.author 유찬민 -
dc.date.accessioned 2020-07-17T02:30:14Z -
dc.date.available 2020-07-17T02:30:14Z -
dc.date.created 2020-02-11 -
dc.date.issued 2007-12-10 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/30126 -
dc.description.abstract Recently the market price of valuable metals are rapidly increased due to the high demand and limited resources. Therefore, manganese (Mn)-nodules (Polymetallic nodules) in the Clarion-Clipperton fracture zone have stimulated economic interest. Nickel, copper, cobalt and manganese are the economically most interesting metals of Mn-nodules. In order to mine Mn-nodules from sea floor, understanding the geotechnical properties of surface sediment are very important for two major reasons. First, geotechnical data are required to design and build the stable and environmentally acceptable mining vehicles. Second, deep-sea mining activity could significantly effect on the surface layer of deep sea floor. For example, surface sediments will be redistributed through the resuspension and redeposition. Reliable sedimentological and soil mechanical baseline data of the undisturbed benthic environment are essential to assess and evaluate these environmental impacts by mining activity using physical and numerical modeling. The 225 times deployments of the multiple corer guaranteed undisturbed sediment samples in which geotechnical parameters were measured including sediment grain size, density, water content, shear strength. The sea floor sediments in this study area are generally characterized into three different types as follow. The seabed of the middle part (8-12° N) of this study area is mainly covered with biogenic siliceous sediment compared with pelagic red clays in the northern part (16-17° N). However, the southern part (5-6° N) is dominant with calcareous sediments because its water depth is shallower than the carbonate compensation depth (CCD). This result suggests that middle area, covered with siliceous sediment, is more feasible for commercial mining than northern area, covered with pelagic red clay, with the consideration of the nodule miner maneuverability and the environmental impact. Especially, middle part with the highest nodule abundance and valuable meta -
dc.description.uri 1 -
dc.language English -
dc.publisher AGU(American Geophysical Union) -
dc.relation.isPartOf 2007 AGU (American Geophysical Union) fall meeting -
dc.title 심해채광을 위한 C-C지역 퇴적물의 지질공학적 특성연구 -
dc.title.alternative The Study of Geotechnical Properties of Sediment in C-C Zone in the Northeastern Pacific for Deep-sea Mining -
dc.type Conference -
dc.citation.conferencePlace US -
dc.citation.endPage 0978 -
dc.citation.startPage OS53A -
dc.citation.title 2007 AGU (American Geophysical Union) fall meeting -
dc.identifier.bibliographicCitation 2007 AGU (American Geophysical Union) fall meeting, pp.OS53A - 0978 -
dc.description.journalClass 1 -
Appears in Collections:
Marine Resources Research Division > Deep-sea Mineral Resources Research Center > 2. Conference Papers
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