• 수산해양교육연구
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• 제16권1호
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• pp.110-123
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• 2004

Five Islands in the West Sea of Korea (Baekryeong-do, Daecheong-do, Socheong-do, Yeonpyeong-do, and Woo-do) are located very close to the North Korea's coast and all of them are under the jurisdiction of South Korea. The North and South Korean naval vessels clashed twice in the West Sea of Korea on June 15, 1999 and on June 29, 2002. These incidents were resulted from conflicts over the validity of the Northern Limit Line(NLL) and the appropriate maritime boundary between the two Koreas. From the viewpoint of South Korea, the North Limit Line is a lawful Maritime Military Demarcation Line under the Korean Military Armistice Agreement and it must be maintained as a maritime boundary between two Koreas until being substituted by a peace treaty. In conclusion, the maritime boundary between two Koreas cannot be settled easily by the principles of the International Law of the Sea at present.

• 한국환경생태학회지
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• 제21권2호
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• pp.107-112
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• 2007

한라산 국립공원의 양서 파충류상을 파악하기 위하여 1100고지, 어승생악, 돈내코, 어리목, 영실, 관음사, 성판악 주변을 2006년 4월부터 2007년 1월까지 조사하였다. 한라산 국립공원에서 발견된 양서류는 총 4과 5종, 파충류는 4과 8종이었다. 내륙 지방에서는 개체수가 적은 대륙유혈목이(Amphiesma vibakari ruthveni), 줄장지뱀(Takydronus wolteri), 도마뱀(Scincella vandenburghi), 실뱀(Coluber spinalis), 제주도룡뇽(Hynobius quelpartensis)과 한반도에서는 제주도에만 서식하는 비바리뱀(Sibynophis chinensis)을 확인하였다. 제주도는 한반도에서 유일하게 남방한계와 북방한계인 양서 파충류가 서식한다. 제주도의 양서 파충류는 오랜 격리와 기후에 의한 차이를 보이며 생물지리학적으로 매우 중요한 위치에 있다. 또한 기존 문헌에 기록되어 있지만, 서식여부가 명확하지 않은 두꺼비(Bufo gargarizans), 옴개구리(Rana rugosa), 금개구리(R. plancyi). 무자치(Elaphe rufodorsata), 아무르장지뱀(T. amurensis)의 현황에 대한 연구는 시급히 이루어져야 한다.

• 건축역사연구
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• 제24권3호
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• pp.31-41
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• 2015

This study aims to draw out planning principles and structure of Iksan imperial capital city in late Baekje, especially in view of the relationship among imperial capital city planning area, skeletal axis and the location of royal castle. With site survey and analysis of historical records, old maps, topographical maps, archeological excavation data, land registration map of 1915, some significant inferences were drawn out. Firstly from the point of topological conditions, the contiguous line of a stratum from Mireuk mountain(彌勒山) to Wangkung-ri castle(王宮里遺蹟) and two waterways made a topological axis of Iksan Imperial capital city. Secondly district of Iksan imperial capital city can be deduced to the inner area north to Kummado soil wall(金馬都土城), south to the confluence of Iksan river(益山川) and Busang river(扶桑川), west to Okum mountain fortress(五金山城) and Galjeon river(葛田川), east to line near to eastern wall of Jesuksa temple(帝釋寺). Iksan ssang-reung(益山雙陵) was located outside western boundary line of capital city. Thirdly axis from Wangkung-ri castle to northern Kummado soil wall made a skeletal axis of city structure. It got through northern lowland along Buk river(北川) between Yonghwa(龍華山) and Mireuk mountain. Fourthly the location of royal palace can be deduced to the north part of the city around Kumma town area along the planning principle of northern royal palace.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 1997년도 추계 국제학술심포지움 논문집
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• pp.97-142
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• 1997

The Seoguipo Formation occurs only in a small exposure along the coast of the Seoguipo City, but in the subsurface, underlies tile western part of the Bugcheon-Pyoseon Line in the northeastern part of tile island. The Bugcheon-Pyoseon Line is presumed to be a facies boundary that reflects tile distribution of hyaloclastites resulted from submarine volcanic activity. The Seoguipo Formation is distributed in the subsurface along the part which is lower than 400m in average altitude, and occurs at El. -5.76∼-46.63m in tile southern area, El. -41.89∼-57.97m in the western area, El. -13.15∼-50.59m in the northern area. Therefore, the southern area was uplifted after the deposition of the Seoguipo Formation. In the subsurface, the vertical depth of the volcanic rocks of the Cheju Volcanic Edifice is El. -40.6m in the southern area, El. -111.3m in the western area, El. -81.5m in the northern area and El. -134.7m in the eastern area. The unconsolidated U Formation, which is, overlying the basement and about 70∼250m thickness underlies the whole island. There is a positive correlation between tile groundwater level and the depth of the subsurface distribution of the Seoguipo Formation. Consequently, it is conformed that the subsurface distribution of the Seoguipo Formation plays important role for controlling the characteristics of the reservoir of tile groundwater in Cheju Island.

• 수산해양교육연구
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• 제23권2호
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• pp.141-152
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• 2011

This study was investigated the species composition of demersal fishes by a bottom trawler GAYA, in order to be used basic data for resources management of fishery in the jointly controlled waters of the West sea. We caught 39 species, 5,532 individuals and 322.518kg in biomass. The number of species was the fewest of the jointly controlled waters of the East china sea and boundary zone between Busan and Tsushima. The first dominant species in individuals in summer was Oregonia gracilis, and in biomass was angler. But angler was the first dominant species in 7 stations of 12 stations. It was a peculiar phenomenon that cod which lives in a cold current was caught in the northern part of the West sea. In this connection it seems to be needs for oceanographic research. Catch per unit effort (kg/hr) of bottom trawl was the higher in northern part and in right line of all surveyed area respectively.

• 농촌계획
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• 제7권1호
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• pp.61-76
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• 2001

During the performance of large scale tidal land reclamation project along the coast line, the construction of large scale structures such as sea-dikes, closing estuaries will induce big changes of near-shore hydraulic behavior. In this paper, its is aimed to verify the change of tide and currents after the construction of sea-dike of the Saemangeum project along the coast line. Numerical scale model "TRISULA" which development by Delft Hydraulics in the Netherlands was used. "TRISULA" is adopting the finite difference numerical scheme, and mostly using for hydro-dynamic solution along the sea and estuaries. Model boundary is covering $100{\times}170$ Km and constructed with $133{\times}337$ grids. Outer side boundary is divided 48 sections, and input 37 tidal components are gained from another big scale numerical "Yellow Sea" model. Model calibrations & verifications were performed th field tide & current datas which were measured along sea-dike alignment during Aug. $1997{\sim}Apr$. 1999. And then, numerical simulation with the tide condition dated 17 Apr. 1999 was performed with & without sea-dike construction condition for the comparison. Evaluated boundary is 20 km out-side from sea-dike alignment. Four cross lanes were set up, each of lane contains 3 points, for the comparison of sea-dike construction effects. Results showing the tidal amplitude is reducing approximately 20 cm after the construction of sea-dike during spring tide condition, amplitude 6.9m. Currents after construction of sea-dikes along the alignment, the northern part shows 50%(inner), 90%(outer) and the southern part shows 10%(inner) 50%(outer) of the currents before construction.

• Strategy21
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• 통권31호
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• pp.27-56
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• 2013

The United Nations Command (UNC) and the communist North failed to reach an agreement on where the maritime demarcation line should be drawn in the process of signing a truce after the Korean War because of the starkly different positions on the boundary of their territorial waters. As a result, the Armistice Treaty was signed on July 1953 without clarification about the maritime border. In the following month, Commander of the UNC unilaterally declared the Northern Limit Line (NLL) as a complementing measure to the Armistice. Referring to this, North Korea and its followers in South Korea wrongfully argue that the NLL is a "ghost line" that was established not based on the international law. However, one should note that the waters south of the NLL has always been under South Korea's jurisdiction since Korea's independence from Japan on August 15, 1945. There is no need to ask North Korea's approval for declaring the territorial waters that had already been under our sovereign jurisdiction. We do not need North Korea's approval just as we do not need Japan's approval with regard to our sovereign right over Dokdo. The legal status of the NLL may be explained with the following three characteristics. First, the NLL is a de facto maritime borderline that defines the territorial waters under the respective jurisdiction of the two divided countries. Second, the NLL in the West Sea also serves as a de facto military demarcation line at sea that can be likened to the border on the ground. Third, as a contacting line where the sea areas controlled by the two Koreas meet, the NLL is a maritime non-aggression line that was established on the legal basis of the 'acquiescence' element stipulated by the Inter-Korea Basic Agreement (article 11) and the Supplement on the Non-aggression principle (article 10). Particularly from the perspective of the domestic law, the NLL should be understood as a boundary defining areas controlled by temporarily divided states (not two different states) because the problem exists between a legitimate central government (South Korea) and an anti-government group (North Korea). In this sense, the NLL problem should be viewed not in terms of territorial preservation or expansion. Rather, it should be understood as a matter of national identity related to territorial sovereignty and national pride. North Korea's continuous efforts to problematize the NLL may be part of its strategy to nullify the Armistice Treaty. In other words, North Korea tries to take away the basis of the NLL by abrogating the Armistice Treaty and creating a condition in which the United Nations Command can be dissolved. By doing so, North Korea may be able to start the process for the peace treaty with the United States and reestablish a maritime line of its interest. So, North Korea's rationale behind making the NLL a disputed line is to deny the effectiveness of the NLL and ask for the establishment of a new legal boundary. Such an effort should be understood as part of a strategy to make the NLL question a political and military dispute (the similar motivation can be found in Japan's effort to make Dokdo a disputed Island). Therefore, the South Korean government should not accommodate such hidden intentions and strategy of North Korea. The NLL has been the de facto maritime border (that defines our territorial waters) and military demarcation line at sea that we have defended with a lot of sacrifice for the last sixty years. This is the line that our government and the military must defend in the future as we have done so far. Our commitment to the defense of the NLL is not only a matter of national policy protecting territorial sovereignty and jurisdiction; it is also our responsibility for those who were fallen while defending the North-Western Islands and the NLL.

• 한국지역지리학회지
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• 제15권3호
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• pp.317-327
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• 2009

본 연구는 환경부의 전국자연환경조사를 통하여 수집된 비무장지대와 그 인접 지역의 지형분야 조사의 결과를 분석하고, 활용 방안을 모색하는데 그 목적이 있다. 조사된 총 356개의 지형 중 가장 많이 관찰된 지형은 하안단구였으며, 전체 지형 중 1 등급은 57개(16.01%)로 나타났다. 본 지형 조사는 북방한계선까지 접근하여 비무장지대 및 그 인접 지역의 지형을 파악하는데 큰 의의가 있다. 이러한 비무장지대 및 그 인접지역의 지형경관은 비무장지대라는 세계에서 유일한 공간적 특성과 함께 유네스코에서 지정하는 지오파크로 활용될 수 있는 가능성이 매우 높다.

• 한국환경생태학회지
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• 제20권4호
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• pp.464-472
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• 2006

월출산국립공원 금생골의 식생구조 분석을 실시하기 위해 30개 조사구를 설치하고, 식생조사를 실시하였다. Classification 기법 중 하나인 TWINSPAN을 이용하여 군락분리를 시도한 결과, 굴참나무군락(I),상수리나무군락(II), 소나무군락(III), 소나무-상수리나무군락(IV)의 4개 군락으로 분리되었다. 이상의 분석결과 월출산국립공원 금생골의 식생은 군락 I 과 II의 경우 소나무에서 굴참나무와 상수리나무 등 참나무류로 천이가 진행된 발전단계였으며, 군락 III과 IV는 소나무가 참나무류와 경쟁관계에 있는 것으로 판단된다.

• 한국해양학회지:바다
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• 제5권4호
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• pp.320-334
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• 2000

북동 태평양의 위도별(131$^{\circ}$30'W, 5${\sim}$12$^{\circ}$N) 각 지점에서 다중 주상시료 채취기(multiple corer)로 획득된 31개 표층 퇴적물의 지질공학적 특성을 분석하였다 환경연구지역을 포함한 연구지역 북부(9${\sim}$12$^{\circ}$N)퇴적물은 대부분 규질퇴적상을 보인다. 반면 남쪽지역(5${\sim}$6$^{\circ}$N)에서는 탄산질 퇴적물이 산출되는데, 이는 수층 생산성이 높고 이 지역 탄산염 보상심도(CCD: 4,400 m)보다 수심이 얕은데 기인된 결과이다. 지질공학적 특성은 7$^{\circ}$N을 경계로 남-북 퇴적물간 뚜렷한 차이를 보인다. 남쪽지역의 탄산질 퇴적물은 낮은 함수율, 공극율, 전단강도, 그리고 높은 입자 밀도 및 전밀도의 원인이 된다. 반면에 망간단괴가 고밀도로 분포하고 있는 북쪽지역 퇴적물은 주로 생물기원 규질 퇴적물로 구성되어 있으며, 이는 높은 함수율, 공극율, 전단강도 그리고 낮은 입자 밀도 및 전밀도의 일반적 원인이 된다. 퇴적물의 활성도(activity)는 북쪽 퇴적물에서 매우 높게 나타난다. 한편, 북쪽지역 퇴적물들은 표층에서 약 5${\sim}$8 cm를 경계로 준액상(semi-liquid)인 상부층과 단단하게 굳어진 하부층으로 뚜렷이 구분되며, 깊이에 따라 급격한 지질공학적 특성 변화를 보인다. 반면 남쪽 지역에서는 이러한 깊이에 따른 지질공학적 특성 변화가 적다. 이러한 남-북 지역 퇴적물중 지질공학적 특성의 위도별, 깊이별 변화는 탄산질 퇴적물과 규질 퇴적물의 분포, 수층의 생산성 및 수심변화에 따른 용해도와 퇴적을 차이 그리고 침식 및 재퇴적작용 등 퇴적 과정이 위도별로 달랐기 때문으로 판단된다.