이 연구는 구(舊)일본해군의 군사적 요충지 역할을 맡은 군항도시 사세보 (佐世保)가 관광도시로 전환되는 과정에 기반을 두고 있다. 사세보는 1889 년 7월 진수부(鎮守府)가 개청된 이래 군사 전략적 요충지로 자리잡았다. 1946년 다나카 마사스케(田中正輔) 시장의 취임 이후, 군항도시의 이미지 를 벗고자 평화산업항만도시의 실현을 위해 관광산업을 추진하였고 사세보 주변 해역을 포함한 서해 일대를 국립공원으로 지정받기 위해 최선의 노력 을 다했다. 하지만 사이카이(西海)국립공원 지정 논의가 한창 진행된 시기 인 1950년 한국전쟁이 발발하였고 미국에 의해 일본의 재무장을 촉진 시 키는 계기가 된다. 1950년 7월 맥아더에 의해 해상보안청이 설치되었고 그 총감부가 사세보에 배치된다. 니시오카(西岡) 현(県)지사와 다나카(田中) 시 장은 지역경제를 고려하여 군상(軍商)항이라는 두 마리 토끼를 잡겠다는 목표로 의지를 표명했다. 1955년 여러 난관을 뚫고 서해 일대가 만장일치 로 국립공원 1순위로 결정되었고 3월 16일 정식으로 지정되었다. 본 논문 은 사세보시가 군항도시에서 관광도시로 전환하기 위하여 추진했던 사이카 이(西海)국립공원 유치 활동과 지정 과정을 고찰하고자 한다. 아울러 동아 시아의 역사 속에서 사세보라는 군항도시가 평화산업항만도시로 변천되어 가는 과정을 규명하고자 한다.

서해병 폐기물 배출해역 오염심화구역의 퇴적물 정화·복원을 위해 2013, 2014, 2016, 2017년에 준설토를 피복하였다. 피복 효과 평 가를 위해 배출해역 내 피복구역(5개 정점)과 자연회복구역(2개 정점)을 설정하고 2014년부터 2020년까지 연 1회 구역별 표층 퇴적물을 채취 하여 퇴적물 물리·화학적 특성 및 저서동물상을 분석하였다. 퇴적물 평균 입도(Mz)는 자연회복구역에서 5.91~7.64 Φ로 세립질이었고 피복구 역에서는 준설토의 영향으로 1.47~3.01 Φ의 조립질 퇴적물로 구성되어 있었다. 유기물 및 중금속 함량은 피복구역에서 자연회복구역 대비 약 50 % 낮아(p<0.05) 준설토 피복 효과가 있는 것으로 판단되었다. 대형저서동물 분석 결과에서는 피복구역의 출현종수, 생태지수가 자연회 복구역보다 낮게 나타났다(p<0.05). 피복구역의 출현종수 및 생태지수의 시계열 분석 결과에서는 2013, 2014년 피복 이후 초기 4년간 증가하 다가 이후 감소하는 경향을 보였다. 이는 피복으로 인해 빠른 성장과 짧은 수명의 특징을 보이는 기회종 생물들이 피복 초기에 우세하다가 2016, 2017년에 추가로 피복이 진행됨에 따라 서식환경이 다시 교란되어 나타난 현상으로 추정된다. AMBI는 자연회복구역 및 피복구역에서 모두 2등급(Good), BPI는 1~2등급 수준을 유지하고 있어 건강한 저서상태로 평가되었다. 따라서 폐기물 배출해역의 오염퇴적물 정화 및 저 서생태계 복원을 위한 준설토 피복은 오염도 저감효과는 나타나지만 저서생태계의 측면에서는 장기적인 모니터링을 통해 회복추이를 관찰 해야 할 것으로 판단된다. 또한 향후 배출해역의 오염심화구역 정화 복원 사업 확대 시 적응적 관리가 필요할 것으로 판단된다.

A survey was conducted to analyze seasonal dynamics of the phytoplankton community at 22 stations on the surface and bottom layers in the Anma Islands of Yeonggwang (AIY) in the southern West Sea, Korea from the spring of 2020 to the winter of 2021, using a marine survey vessel Ed Ocean. Based on the survey results, there were 87 phytoplankton species in 52 genera, diatoms accounted for 67.8%, dinoflagellates 26.5%, silicoflagellates 3.5%, and cryptomonads and euglenoids accounted for 1.1% each. By season, it was simple in spring and relatively varied in winter. The phytoplankton standing crop on the surface was low (28.8±30.1 cells mL-1) in summer and high (87.0±65.1 cells mL-1) in spring. In the phytoplankton community, diatoms showed a high share (over 80%) throughout the year, and Skeletonema costatum-ls was the dominant species with a dominance of more than 60% in spring and winter, and 34.6% and 24.2% in summer and autumn, respectively. The diversity expressing the characteristics of the community structure was high (2.79±0.45) in autumn and low (1.82±0.18) in spring, unlike the phytoplankton standing crop. However, the dominance was high at (0.86±0.08) in spring and low (0.44±0.13) in autumn. Based on the results of principal component analysis (PCA) using environmental and phytoplankton-related factors, it was estimated that the biological oceanographic environmental characteristics seen through the phytoplankton community in the AIY were dominated by nutrients supplied from open seawater and surface sediments by seawater mixing, such as tidal mixing.

본 연구에서는 강한 한파가 발생했던 2018년과 온난 한파가 발생했던 2019년의 기온에 따른 수온의 반응 및 지연시간과 북풍계 열 바람 빈도와의 상관관계를 분석하였다. 사용된 시간 자료는 국립수산과학원에서 제공하는 7개 지점 해역별 수온자료와 수온관측소 인 근 7개 지점 AWS 기온자료를 이용하였다. 관측되지 못한 자료는 내삽법으로 근사값을 계산하였고, FIR Filter를 이용하여 자료의 주기성을 파악하였다. 그 결과, 강한 한파가 발생했던 2018년은 북풍계열 바람을 통해 차가운 공기가 남하하면서 기온을 하강시켜 전 해역에 저수온을 유발한 반면 온난 한파가 발생했던 2019년은 평년 수준의 기온으로 하강하였지만 수온은 크게 변화하지 않았다. 강한 한파가 발생했 던 2018년 기온 하강에 따른 수온의 지연시간은 평균 14시간으로 0.7 이상의 높은 상관성을 나타냈고 온난 한파가 발생했던 2019년은 평균 지연시간이 20시간으로 0.44-0.67 사이의 상관성을 보였다. 본 연구를 통해 해역별로 기온 하강에 따른 표층수온의 반응을 해석하였고 지연시간을 파악함으로써 양식생물의 피해를 최소화하고 한파 피해의 신속한 대응에 기여할 수 것으로 기대한다.

본 연구는 2019년 8월 한반도 주변해역(동해, 서해, 남해, 동중국해)에서 탄소 및 질소 안정동위원소 기법을 활용하여 하위영양 단계에서의 먹이망 구조를 파악하였다. 입자성 유기물(POM)의 δ13C 범위는 -26.18 ~ 20.61 ‰, δ15N 범위는 5.36 ~ 15.20 ‰의 넓은 범위를 보였다. POM과 각 생물별 개체군 사이의 δ13C 분별작용의 결과는 대부분 micro-POM을 섭식하는 것으로 확인하였으나 해역 간 차이를 보였 다. 각 생물별 영양단계는 chaetognaths (3.40±0.61)가 가장 높은 영양단계에 있음을 확인하였다. 동위원소 혼합모델을 적용한 결과에서 chaetognaths의 먹이원으로 copepods (13 ~ 48 %)와 euphausiids (20 ~ 51 %)가 가장 높은 기여도를 나타냈다. 본 연구결과 각 해역별 먹이원의 제한적 공급 및 다양성의 차이가 먹이망 구조 및 각 생물별 동위원소 비에 영향을 미친 것으로 판단된다.

Species composition and seasonal variations of fish in the Five West Sea Islands in Korea, were investigated by using otter trawls and bongo nets from 2014 to 2015. During the surveyed period using an otter trawl, a total of 53 species, 147,253 ind./km2 and 2,721,296 g/km2 of fish were collected by otter trawls. The individual dominant species were Chaeturichthys stigmatias (30.3%), Coilia nasus (18.2%), Engraulis japonicus (12.3%), and Setipinna tenuifilis (12.2%). Moreover, the biomass dominant species in biomass were Liparis tanakae (21.3%), Beringraja pulchra (18.5%), Engraulis japonicus (8.3%) and Okamejei kenojei (8.1%). Eggs by bongo nets included 1,748 ind./1,000 m3 of Engraulis japonicus and 64,691 ind./1,000 m3 of unidentified species. A total of 15 species and 2,015 ind./1,000 m3 of fish larvae were collected, and the dominant species were Johnius belengerii and Pholis fangi.

We conducted a seasonal field survey to analyze the distribution patterns of a phytoplankton community and biological oceanographic characteristics in the Geum river estuary in 2018. The results showed that the phytoplankton community consisted of 58 genera and 116 species, showing a relatively simple distribution. It was controlled by diatoms at 70.2%, a low number of species in winter and spring, and a high number in summer and autumn. The phytoplankton cell density ranged from 10.0 to 2,904.0 cells mL-1, with an average layer of 577.2 cells mL-1, which was low in autumn and high in winter. The seasonal succession of phytoplankton dominant species was mainly centric diatoms from winter to summer, including Thalassiosira nordenskioeldii, Cerataulina bergonii, and Skeletonema costatum-ls in winter, S. costatum-ls and C. bergonii in spring, and Eucampia zodiacus and Th. nordenskioeldii in summer. However, the autumn species depended upon the regions, with the inner bay dominated by the centric diatom, Aulacoseira cf. granulata, the mixed areas by S. costatum-ls, and the open sea by the dinoflagellate, Lingulodinium polyedra. According to principal component analysis (PCA), the phytoplankton community was greatly affected by the inflow and expansion of freshwater, including high nutrients, which are introduced annually through the rivermouth weir in Geum river estuary. However, the estuary, which is strongly affected by annual freshwater, was limited to areas near Geumran Island, which is adjacent to the river-mouth weir.

The feeding habits of the bighead croaker Collichthys niveatus were studied using 745 specimens collected by bottom trawl net in the West Sea, Korea, in April and October of 2016, 2017 and 2018. The size of C. niveatus ranged from 4.8 to 16.0 cm in total length. The stomach contents analysis indicated that C. niveatus consumed mainly euphausiids and copepods. C. niveatus consumed mainly euphausiids and copepods in all size classes. The dietary compositions of C. niveatus was not significantly different among size classes (One-way ANOVA, P > 0.05). As body size of C. niveatus increased, the mean weight of prey per stomach (mW/ST) tended to increase.

In order to understand the tidal current and mean flow at the west channel of Yeoja Bay in the South Sea of Korea, numerical model experiments and vorticity analysis were carried out. The currents flow north at flood and south at ebb respectively and have the reversing form in the west channel. Topographical eddies are found in the surroundings of Dunbyong Island in the east of the channel. The flood currents flow from the waters near Naro Islands through the west channel and the coastal waters near Geumo Islands through the east channel. The ebb currents from the Yeoja Bay flow out along the west and the east channels separately. The south of Nang Island have weak flows because the island is located in the rear of main tidal stream. Currents are converged at ebb and diverged at flood in the northwest of Jeokgum Island. Tidal current ellipses show reversing form in the west channel but a kind of rotational form in the east channel. As the results of tide induced mean flows, cyclonic and anticyclonic topographical eddies at the northern tip but eddies with opposite spin at the southern tip are found in the west channel of Yeoja Bay. The topographical eddies around the islands and narrow channels are created from the vorticity formed at the land shore by the friction between tidal currents and the west channel.

This study is aimed to compare stock assessment models depending on how the models fit to observed data. Process-error model, Observation-error model, and Bayesian state-space model for the Korean Western coast fisheries were applied for comparison. Analytical results show that there is the least error between the estimated CPUE and the observed CPUE with the Bayesian state-space model; consequently, results of the Bayesian state-space model are the most reliable. According to the Bayesian State-space model, potential yield of fishery resources in the West Sea of Korea is estimated to be 231,949 tons per year. However, the results show that the fishery resources of West Sea have been decreasing since 1967. In addition, the amounts of stock in 2013 are assessed to be only 36% of the stock biomass at MSY level. Therefore, policy efforts are needed to recover the fishery resources of West Sea of Korea.

Acoustic surveys were conducted in the seas surround the South Korea (South Sea A, South Sea B (waters around the Jeju Island), West Sea and East Sea) in spring and autumn in 2016. First, the vertical and horizontal distributions of fisheries resources animals were examined. In most cases vertical acoustic biomass was high in surface water and mid-water layers other than South Sea A in autumn and West Sea. The highest vertical acoustic biomass showed at the depth of 70-80 m in the South Sea A in spring (274.4 m2/nmi2) and the lowest one was 10-20 m in the West Sea in autumn (0.4 m2/nmi2). With regard to the horizontal distributions of fisheries resources animals, in the South Sea A, the acoustic biomass was high in eastern and central part of the South Sea and the northeast of Jeju Island (505.4-4099.1 m2/nmi2) in spring while it was high in eastern South Sea and the coastal water of Yeosu in autumn (1046.9-2958.3 m2/nmi2). In the South Sea B, the acoustic biomass was occurred high in the southern and western seas of Jeju Island in spring (201.0-1444.9 m2/nmi2) and in the southern of Jeju Island in autumn (203.7-1440.9 m2/nmi2). On the other hand, the West Sea showed very low acoustic biomass in spring (average NASC of 1.1 m2/nmi2), yet high acoustic biomass in the vicinity of 37 N in autumn (562.6-3764.2 m2/nmi2). The East Sea had high acoustic biomass in the coastal seas of Busan, Ulsan and Pohang in spring (258.7~976.4 m2/nmi2) and of Goseong, Gangneung, Donghae, Pohang and Busan in autumn (267.3-1196.3 m2/nmi2). During survey periods, fish schools were observed only in the South Sea A and the East Sea in spring and the West Sea in autumn. Fish schools in the South Sea A in spring were small size (333.2 ± 763.2 m2) but had a strong SV (–49.5 ± 5.3 dB). In the East Sea, fish schools in spring had low SV (–60.5 ± 14.5 dB) yet had large sizes (537.9 ± 1111.5 m2) and were distributed in the deep water depth (83.5 ± 33.5 m). Fish schools in the West Sea in autumn had strong SV (–49.6 ± 7.4 dB) and large sizes (507.1 ± 941.8 m2). It was the first time for three seas surrounded South Korea to be conducted by acoustic surveys to understand the distribution and aggregation characteristics of fisheries resources animals. The results of this study would be beneficially used for planning a future survey combined acoustic method and mid-water trawling, particularly deciding a survey location, a time period, and a targeting water depth.

In this study, total mercury (THg) variations of Black-tailed Gull (Larus crassirostris) eggs laid on Baengnyeongdo, West Sea of Korea were compared between within- and among clutch in order to ensure statistical representativeness of an egg sampling method. In the ANOVA analysis, the THg variation (59%) among clutches was much higher than within-clutch (27%). This means that the mercury variation of sampled eggs was significantly influenced by the mercury variation among female individuals occupying different nests. In spite of relatively smaller variation of THg in the within-clutch, the THg concentration depending on an egg-laying sequence within a clutch significantly appeared higher in the first-laid eggs rather than the second-laid eggs. Therefore, it is necessary to take one egg from one nest in order to sample more nests in terms of better sampling representativeness. Also, one egg selection from one nest should be consistently applied in order to ensure comparability of mercury concentrations among monitoring sites and monitoring years.

Distribution and composition of the seabed litters in the exclusive economic zone of the West Sea of South Korea including 18 sea-blocks were investigated using a bottom trawl gear of the R/V Tamgtu 20 (National Institute of Fisheries Science) from 24th April 2011 to 4th May 2012. Each trawl shot was conducted for an hour in each sea-block and the total trawl shots was 18. As a result, 325.6 kg of seabed litter in total has been collected.　The quantity of the seabed litter was highest at No. 202 of the sea-block, close to the Heuksan-Do. The highest occupied sea material was plastic (83.1% of entire seabed litters), the second highest material was metal combined with plastic (10.6%), and glass (2.9%), metals (2.3%), vinyl (0.6%), cloth (0.4%) and wood (0.2%) in order. The origin of seabed litters was from fishing gear (89.0% of all seabed litters). Therefore, it could be assumed that most seabed litters were derived from the fishing activity for example fishing nets and ropes.

2011~2012년 보령연안 수온의 시공간적 변동특성을 장기 연속수온관측 자료를 이용하여 분석하였다. 수온은 반일 또는 일일의 단주기 변동이 전 계절에 탁월하고 그 진폭은 하계와 춘계에 크고 추계에 작다. 수온과 기온의 연변동 진폭은 기온 12.9℃, 수온 10.9℃로 기온이 더 크며, 연변동 최고위상은 기온 8월 2일, 수온 8월 22일로 기온이 20일 앞선다. 수온의 연변동 진폭은 원산도와 대천항 연안에서 가장 크다. 수온변동 중 일일주기는 대천항과 무창포항, 반일주기는 원산도 주변 협수로에서 탁월하며, 대천천 하구는 천해조 비율이 높 다. 표층수온과 기온은 대체로 풍향 변동에 따라 변동한다. 하천수가 방출되면 수온은 상승 후 하강 또는 하강 후 상승한다. 수온 탁월주 기는 0.5일, 1.0일, 15일 주기와 7~10일 전후이다. 수온변동특성에 따라 해역을 분류하면 ①원산도 남동연안의 혼합수역 ②삽시도~용도, 장 고도~삽시도, 장고도~안면도 남쪽의 서쪽 외해수역 ③용도~독산의 남쪽 외해수역 ④송도~대천항~무창포항의 조간대 연안수역으로 구분 된다.