• 수산해양기술연구
• /
• 제45권2호
• /
• pp.96-105
• /
• 2009

For an effective management of fisheries resources, we need fisheries informations necessary for the establishment of reasonable fishing effort and TAC distribution. We carried out fishing research using trammel nets in the coastal sea of Susan-port(Yangyang, Gangwondo, Korea) and Hupo-port(Uljin, Gyeongbukdo, Korea) and analyzed fishing power variation of the fishing gear in terms of species composition, condition and so on for both sites. A total of 29 species were caught with most dominant species of Hippoglossoides dubius followed by Pseudopleuronectes herzensteini, Lophius litulon and Alcichthys elongatus in Susan. The total number of species caught in Hupo was 37 species with most dominant species of Todarodes pacifius followed by Lophius litulon, Hexagrammos agrammus and Pseudopleuronectes herzensteini. CPUE of Susan fishing area per trammel net was 12.74 fish and 2.00kg on average, while it was 6.80 fish and 2.27kg on average for Hupo. The fishing power index for both sites was 1, placing the two fishing grounds in a same level.

• 한국수산과학회지
• /
• 제41권6호
• /
• pp.505-510
• /
• 2008

To understand the oceanographic characteristics of Hupo coastal waters as regards the East Korean Warm Current and the North Korean Cold Current, current direction and velocity were investigated by deploying a current meter in Hupo coastal waters during the summer and fall of 2007. Wind data were obtained from the homepage of the Korea Meteorological Administration. Water temperature was measured using a temperature meter attached to the current meter and a mini log. During summer, a south wind prevailed, while during the fall the wind blew from the north. Cold surface waters occurred on a large scale in summer, while in the fall, warm bottom water occurred frequently. After mid-November, when the surface water was cooler than $15^{\circ}C$, there was no difference in water temperature between the surface and bottom layers.

• 한국광물학회지
• /
• 제28권1호
• /
• pp.71-81
• /
• 2015

울릉분지와 후포분지의 퇴적물 코어 시료(각 분지에서 하나씩 03GHP-02와 HB13-2)를 대상으로 광물학적 연구를 수행하였다. 광물조성, 점토광물 성분, 그리고 총 인 성분 및 인의 연속추출법 연구 결과, 두 시료들은 각 값에 대하여 또한 깊이에 따라 어느 정도 차이가 있음을 보이고 있다. 두 시료 모두 광물 종에는 차이를 보이지 않았으며 주로 석영, 미사장성, 장석, 방해석, 오팔A, 황철석, 그리고 점토광물(일라이트, 녹니석, 카올리나이트, 스멕타이트)로 구성되어 있었다. 후포분지의 경우 울릉분지에 비하여 오팔A 함량이 훨씬 많은 것으로 나타났다. 두 시료 모두, 특히 후포분지 시료에서 기존에 동해에서 보고된 것보다 더 많은 스멕타이트가 동정되었는데 이는 고황하강의 영향과 한반도의 제3기 지층 암석에 영향을 받은 것으로 사료된다. 울릉분지 시료의 경우 약 0.7-3.5 m 깊이에 오팔A의 함량 감소 그리고 일라이트 결정도 지수도 낮게 나오며 이는 빙하시대의 추운 기후에 해당된다. 이 깊이의 시료에서는 인의 함량도 상대적으로 낮게 나오고 있다. 이는 이 기간 동안 동해는 해수면의 하강으로 외부 해역과 단절되었고 해협 및 하천을 통한 퇴적물의 유입도 적었기 때문으로 판단된다. 후포분지 시료의 경우 울릉분지에 비하여 깊이에 따른 점토광물 변화와 인의 성분 변화는 크게 관찰되지 않는다. 이러한 경향은 울릉분지에 비하여 비교적 짧은 기간에 퇴적되었거나 퇴적환경의 변화가 별로 없는 환경에서 퇴적되었기 때문으로 해석된다. 점토광물의 결정도 지수는 울릉분지에 비하여 약간 높아 퇴적되었을 당시 비교적 온난한 환경이었을 것으로 추측되며 인의 연구 결과로 미루어 볼 때 비록 어느 정도 변화는 있지만 또한 온난한 환경을 지시한다.

• 한국광물학회지
• /
• 제27권3호
• /
• pp.159-168
• /
• 2014

동해 후포분지의 고환경을 규명하기 위해 HB 13-2 코어를 대상으로 퇴적물의 입도 분석 및 XRD, XRF를 통한 광물 분석을 실시하였다. HB 13-2 코어 퇴적물은 0.4 mbsf를 기준으로 엽리가 미약하고 생교란작용이 나타나는 퇴적상과 생교란작용이 하부로 갈수록 강해지는 두 개의 퇴적상으로 구분된다. 0-0.82 mbsf 구간에서의 비응집성 실트(sortable silt) 함량의 갑작스러운 증가와 상부층준에서의 민감입도 요소의 변화는 대마난류의 영향이 증가하였음을 보여준다. 퇴적물의 주 구성광물은 석영, 미사장석, 정장석, 알바이트와 더불어 녹니석, 캐올리나이트, 일라이트와 같은 점토광물이 포함되어 있으며 이들은 시료의 깊이 및 입도와 크게 연관성이 없는 것으로 나타나는데 이는 코아시료의 퇴적기간 동안 수문학적 변화는 크지 않았음을 시사한다. 1.4 mbsf부터 점토광물의 결정도가 감소하고 S/I 피크가 증가하는 현상은 온난다습한 기후의 영향으로 판단된다.

• 한국석유지질학회지
• /
• 제1권1호
• /
• pp.15-27
• /
• 1993

한반도 동해 대륙주변부에서 취득한 에어건 탄성파 탐사자료에 의하면, 이 지역에는 포항-영덕분지, 묵호분지, 후포분지 등, 세 개의 주요 신제삼기 퇴적분지가 대륙붕 및 대륙사면에 형성되어 있다. 이들 퇴적분지에서의 탄성파층서 및 구조분석 결과, 분지의 형성과 퇴적물 충진은 주향이동신장성(transtensional) 및 차후의 압축성(contractional) 광역지구조운동과 밀접한 관계를 갖고 있는 것으로 보인다. 동해 후열도분지가 확장되기 시작하던 올리고세와 전기 마이오세 동안, 한반도 동해 대륙주변부에는 신장성 전단력(tensional shear stress)이 작용하여 후포단층과 양산단층을 따라 우수주향이동 단 층운동이 일어났으며, 이들 평행한 두 단층 사이의 중첩부에는 당겨열림작용(pull-apart opening)에 의해 포항-영덕 분지가 형성되었다. 한편, 한국대지(Korea Plateau)와 접한 동해 대륙주변부에서는 블럭단층운동으로 인해 융기된 고기저(basement highs) 사이에 묵호분지가 형성되었다. 그 후 중기 마이오세 말에 동해가 닫히기 시작하면서, 연구지역의 응력장은 신장성에서 압축성으로 전환되었으며, 후기 마이오세와 전기 플라이오세, 두 번에 걸쳐 지각변형이 일어나면서 분지를 충진한 퇴적층이 변형되었고, 일부지역에서는 융기가 일어났다. 특히, 전기 플라이오세 동안에는 후포단층이 사교이동양상(oblique-slip sense)을 보이면서 재활성화 되었으며, 이로 인해 반지구(half-graben)형태의 후포분지가 형성되었다.

• 신재생에너지
• /
• 제3권3호
• /
• pp.28-35
• /
• 2007

In this study, the wave power resources at the three locations [Sokcho, Hupo, and Onsan] on the east coast of Korea were estimated by using the field measurement data and were compared with the results of previous researches. It was found that seasonal variation of the wave power is very significant on the east coast of Korean peninsula. The wave power was the smallest in the summer season at all the locations. At Hupo and Onsan, the highest value of the monthly-averaged wave power was observed in September, probably because the pathways of typhoon in September were close to both locations. At the northest location, Sockcho, in contrast, the monthly highest value of the wave power appeared in January, probably owing to the influence of storm waves driven by Donghae twister. The estimated annual average wave power was 4.5 kW/m at Sokcho, which was about two times larger than those at other two locations. It is noteworthy that this result is completely different from past researches based on wave hindcasting data. In addition, the estimates of wave power by the past researches seemed to be smaller than those of the present study, especially at the northern region of the east coast.

• 자원환경지질
• /
• 제15권2호
• /
• pp.65-88
• /
• 1982

In the last ten years, marine geological and geophysical survey and research were conducted by Japanese, Russian and American scientists in the East Sea of Korea (Japan Sea). Many research results were published. However, regional research of the geology of the continental margin of the Korean Peninsula was not conducted. This study has made on attempt to classify submarine strata and stratigraphic boundaries. The study has revealed characters of submarine geology and structure. Isopach maps of each identified stratigraphic unit have been constructed as the results of this study. The study was conducted on the basis of analyses of marine seismic surveys carried out in the continental margin of the East Sea between Kangneung and Pohang. Three depositional basins were identified in the study area and they were named as, Mukho Basin, Hupo Basin and Pohang Basin. The Mukho Basin is developed in continental slope and shelf in the area between Kangneung and Samcheog. Quaternary and Pliocene sediments attain a maximum thickness of 900 m. Basement rocks are interpreted as granite and gneiss. They are correlated with granite-gneiss of the Taebaecksan Series of Pre-cambrian age and the Daebo granite of Jurassic age. The Hupo Basin is developed in the continental shelf between Uljin and Youngdeok. Quaternary and Pliocene sediments attain a maximum thickness of 600 m. Basement rocks were interpreted as granite and gneiss and they are correlated with metamorphic rocks of Pre-cambrian age and the Daebo granites, comprising the Ryongnam Massif. The Pohang Basin is developed in the area between Pohang and Gangu. This basin contains Miocene and older sediments. Basement rocks are not shown. Many faults are developed within the continental shelf and slope. These faults strike parallel with the coast line. A north-south direction is predominant in the southern study area. However, in the northern study area the faults strike north, and north-west. The faults are parallel to each other and are step faults down-thrown to the east or west, forming horst and graben structures which develop into sedimentary basins. Such faults caused the development of submarine banks along the boundary between the continental shelf and slope. This bank has acted as a barrier for deposition in the Hupo Basin. Paleozoic sedimentary rocks distributed widely in the adjacent land area are absent in the Mukho Basin. This suggests that the area of the basin was situated above the sea level until the Pliocene time. The study area contains Pliocene sediments in general. These sediments overlie the basement complex composed of metamorphic rocks, granites, Cretaceous (Kyongsang System) sedimentary rocks and Miocene sedimentary rocks. These facts lead to a conclusion that the continental shelf and slope of the study area were developed as a result of displacements along faults oriented parallel to the present coast line in the post Miocene time.

• Ocean and Polar Research
• /
• 제29권2호
• /
• pp.123-134
• /
• 2007

Distribution patterns of sandy bottom macrobenthic communities were studied around the Hupo coastal area. The seasonal surveys were conducted at 15 chosen sites within a depth range of 10 to 50 m along 10 km of the coastline using a Smith-McIntyre grab $(0.05\;m^2)$ in 2005. Overall depth distribution following the direction of the offshore become deeper parallel to the coastline. A total of 319 macrobenthic species were sampled with a mean density of $1,972\;ind./m^2$, and mean biomass was 82.5 wet-weight $g/m^2$. The major individual-dominant species were three polychaetes Spiophanes bombyx ($436\;ind./m^2$), Scoletoma longifolia ($250\;ind./m^2$) and Magelona japonica ($170\;ind./m^2$), and bivalve Adontorhina subquadrata ($73\;ind./m^2$). Cluster analysis and non-metric multidimensional scaling (nMDS) analysis based on Bray-Curtis similarity identified 2 major station groups which corresponded to macrobenthic faunal assemblages and their characteristic species. In addition, environmental conditions were significantly different between station groups. Group I contained mostly 20 and 50 m deep sites and was associated with sandy mud. Group I was characterized by high abundance of S. bombyx, S. longifolia, A. subquadrata. It was divided into two sub-groups (I-I and I-II) in relation to depth. Sub-group I-I was associated with deeper sites than sub-group I-II. Group II included mostly inshore area shallower than 15 m and was associated with coarse and medium sand. Group II was characterized by Lumbrinerides hayashii and Urothoe grimaldii japonica.

• 한국환경복원기술학회지
• /
• 제12권3호
• /
• pp.21-32
• /
• 2009

Coastal sand dune area is the important ecosystem as an ecotone which located between coastal area and terrestrial area. Moreover, it is very complicate landscape that have geomorphological interaction between erosion and accumulation of sand. Therefore, it is necessary to understand the sand dune ecosystem in view point of landscape scale including background landscape affecting origin of sand dune. Landscape ecological approach in the complicate ecosystem already started in developed countries, and it is applied to land management and biodiversity conservation strategies even in national scale. In this paper, landscape ecological analysis using landscape pattern analysis was carried out on 7 study areas (Yellow Sea : Hakampo and Doksan, South Sea : Namyeol and Balpo, East Sea : Hosan, Hupo and Goraebul) in Korean coastal sand dune ecosystem. Landscape elements were composed by 9 elements in these study areas. Major background landscape elements was the forest land and agricultural field. Namyeol (S06) has larger patch landscape compare to other areas. In patch shape indices, Hupo (E10) shows more complicate patch shapes. The high landscape heterogeneity showed in the Doksan sand dune area and that of Hosan. It shows that these areas were composed by various patch types. However, using landscape indices have to use very carefully because several variables have influence to the result such as scale and spatial pattern of study areas. Although landscape analysis through landscape indices shows sometimes difficult to explain the ecosystem, landscape scale approach on ecosystem assessment still useful to interpret in ecological process in large range of habitat.

• 자원환경지질
• /
• 제43권1호
• /
• pp.1-12
• /
• 2010

동해안의 후포분지에서 채취한 두 개의 피스톤 코어를 이용하여 후포분지에서의 홀로세 퇴적물 내 유기물의 특징 및 동해 해수면 변화와의 관계를 규명하고자 지화학적 접근을 시도하였다. 채취한 시료에 대한 유기물 성분 분석(TOC와 TN)과 유기물 동위원소($\delta^{13}C_{org}$와 $\delta^{15}N_{org}$) 분석 결과들은 코어와 시료 채취 심도에 따라 분석값들이 특징적으로 변화한다. 코어 08HZP-01에서는 4 mbsf(meter below seafloor)에서 코어 표면까지 비교적 채취 심도가 상부로 갈수록 지화학 분석값들이 점이적으로 증가하지만, 코어 08HZP-03에서는 4.71 mbsf를 기준으로 상부와 하부에서 급격한 지화학 분석값들의 변화가 발생한다. 유기물의 TOC/TN과 $\delta^{13}C_{org}$와 $\delta^{15}N_{org}$의 값을 종합적으로 고려하였을 때, 후포분지의 유기물은 해양 조류 기원이 우세한 집단, $C_3$ 육성 식물 기원이 우세한 집단, 해성/육성 조류와 $C_3$ 육성 식물의 혼합기원이 우세한 집단으로 구분할 수 있다. 이러한 퇴적물 내 유기물의 심도에 따른 특성 및 기원 변화는 주로 홀로세 동해 해류와 해수면 등의 변화에 따른 퇴적환경 변화 (퇴적물 이동 포함)에 기인한 것으로 보인다.