• Ocean and Polar Research
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• 제27권4호
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• pp.433-441
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• 2005

To investigate the characteristics of tidal currents and water circulation in the coastal waters off the Taean Peninsula, tidal currents and sea levels were measured at the study area from 1998 to 2004. In the central waterway to the south of Changan Sand Ridge, mean speed of tidal currents and residual currents were 74.0cm/s, 17.8cm/s respectively; the dominant residual currents flowed northeastward, and the amplitudes of semi-diurnal components $(M_2,\;S_2)$ were larger than diurnal components $(O_1,\;K_1)$. The flood and ebb tidal currents were northeastward and southwestward, respectively, and each period was about 6 hours for them, which was consistent with the period of sea levels at the study area. In the coastal region near Hakampo, Taean, mean velocities of tidal currents and residual currents were 46.1cm/s, 30.8cm/s respectively, and the dominant residual currents flowed southwestward. The amplitudes of shallow water constituents $(M_4,\;MS_4)$ were relatively laige, which were weaker to the northeastern coastal region off Mineodo. The northeastward flow continued for about $2{\sim}3$ hours, while the southwestward flow continued for about $9{\sim}10$ hours near Hakampo during the tidal period. Tidal currents flowed northeastward in the central area of the waterway during the period from the Low Water Level (LWL) to the High Water Level (HWL). While the currents in the coastal region flowed northeastward for the first 3 hours after the LWL, southwestward counter-currents flowed between 3 and 6 hours after the LWL. During the period from the HWL to the LWL, the dominant currents flowed southwestward in the study area except to the northeastern coastal region off Mineodo. Along the shorelines, the counter-currents flowed northward between 4 and 6 hours after the HWL. It seems that the counter-currents near the coastal region are caused by the topography and the geography of the shorelines at the study area.

• 자원환경지질
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• 제27권3호
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• pp.263-279
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• 1994

Paleomagnetic and rock-magnetic data of Cretaceous sedimentary and volcanic rocks from the Euiseong area indicate that the stable components of remanence are carried by single and pseudo-single domain magnetite, with the exception of the Shinyangdong Formation which has been remagnetized. The Hayang Group, except for the remagnetized Shinyangdong Formation, yields the mean characteristic direction of $D/I=22.5^{\circ}/57.2^{\circ}$ (${\alpha}_{95}=4.6^{\circ}$, N=14 sites) and the pole position is $72.0^{\circ}N$, $206.4^{\circ}E$ ($dp/dm=4.9^{\circ}/6.7^{\circ}$). The Yucheon Group shows two polarities and the mean characteristic direction of $D/I=351.2^{\circ}/60.5^{\circ}$ (${\alpha}_{95}=11.2^{\circ}$, N= 19 sites) and the pole position is $81.3^{\circ}N$, $79.0^{\circ}E$ ($dp/dm=13.0^{\circ}/17.0^{\circ}$). The mean directions of both the Hayang and the Yucheon Groups are supported by the McElhinny's fold test at the 99% confidence level and that of the Yucheon Group by a reversal test at the 95% confidence level. A magnetostratigraphic correlation between polarities of the study formations and the Geomagnetic Time Scale indicates that the Hayang Group can be correlated to the Cretaceous Long Normal Superchron (CLNS), and the Yucheon Group to the boundary between the CLNS and the Polarity Chron 33R or later boundaries between normal and reverse polarities. Comparison of the paleopoles from this study with those from the surrounding areas both within the Gyeongsang basin and in the northeastern Asia indicates that the study area was not undergone significant tectonic rotations with respect to the other parts of the Gyeongsang basin and that the Korean Peninsula was the part of the single terrane of the northeastern Asia at least since the CLNS. The Yucheon Group can be divided into four sub-groups based on the paleomagnetic data, suggesting that there were at least four times of volcanic activities in the study area.

• Ocean and Polar Research
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• 제36권4호
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• pp.447-454
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• 2014

In August, 2013, we collected epifaunal megabenthos using a deep sea camera (DSC) around a benthic impact study (BIS) site. This was located in the KR5 block of the Korea Deep Ocean Study (KODOS) area in the Northeastern Pacific. The DSC was positioned at $6.8{\pm}2.9m$ (SD) from the sea bottom and was operated from a position at $131^{\circ}56.85^{\prime}-131^{\circ}55.02^{\prime}W$ for 2.3 h at a speed of 1-2 knot. The geographical features of the study area consisted of two structures; a trough in the middle and hills at the east and west sides. Sediment conditions were consistent within six blocks and were affected by slope and polymetallic nodule deposits. We analyzed 226 megafaunal species. Sipunculida comprised the highest percentage of individuals (39%), and the dominant epifaunal megabenthos were Hormathiidae sp., Primnoidae sp., Hexactinellida sp., Hyphalaster inermis, Freyella benthophila, Paelopatides confundens, Psychropotes longicauda, and Peniagone leander. More than 80% of the total density of megafauna occurred on sea plain (D- and E-blocks). We found two distinct groups in the community, one located on sea plains and the other along both sides of the sea slop. Our results suggest that geographical features such as slope and polymetalic nodule deposits are important in controlling the distribution of the epifaunal megabenthos around the KODOS area.

• Journal of Forest and Environmental Science
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• 제26권3호
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• pp.149-159
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• 2010

This paper analyzes data on the composition, status, diversity, and distribution pattern of invasive forest undergrowth in a protected area (Khadimnagar National Park) of Northeastern Bangladesh. Assessment was done by means of stratified random sampling to diversify the invasive forest undergrowth species. For vegetation survey, 45 plots were taken randomly in ($2m{\times}2m$) circular plot from three topographical regions namely top of the hill, middle slope and plain land (15 plots from each region) and a total of 715 individuals, 22 invasive species belonging to 17 families were recorded from the study site. Among invasive species, shrubs constitute 10 species, herbs 9 species, and vines 3 species respectively. Mass number of invasive undergrowth species was grows in plain land (45.45%) followed by middle slope (31.82%). Based on the survey, invasive undergrowth plants of study areas were also categorized into three degrees of invasiveness e.g., highly invasive, moderately invasive and potentially invasive. Herbs, shrubs, and vines constitute the highest density at Chromolaema odorata (Linn.) King. (1.09), relative density at Chromolaema odorata (Linn.) King. 6.85%; highest and lowest frequency was calculated at Cassia alata L. (64.44%) and Diplazium esculentum (24.44%); for relative frequency the highest was Cassia alata L., which occupies 6.64%. Determination of the abundance of the different species revealed that Cassia alata L., constitutes (3.36) followed by Pteris cretica Wilsonii (3.14) of the area. The presence of invasive undergrowth species always reduced the number of associated species. Therefore, an extensive in-depth long-term investigation, proper policy formulation and management interventions and further study and continuous monitoring on their impacts need to be triggered targeting the control of the invasive undergrowth species of this protected area. In this aspect, national and international organization could help to conserve its biodiversity.

• 한국컴퓨터정보학회논문지
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• 제28권4호
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• pp.121-131
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• 2023

중국의 동북3성(헤이룽장성, 요녕성, 지린성)은 우리나라 신북방정책의 유라시아 복합 물류망 구축을 위한 횡단열차 건설 및 북한과의 무역이 가능한 지역으로, 지리적, 지정학적 및 지경학적 중요성이 크다. 운송학적 관점에서 동북3성은 황해권 국가인 한국-중국-북한 간 해상운송이 가능한 지역이며, 복합운송의 형태로 동북3성을 거쳐 유라시아 및 유럽까지 물품 운송이 가능하다. 본 연구는 신북방정책 연계 중국 동북3성과의 협력 및 우호관계 증진을 통한 물류 거점 지역 확보 필요성을 언급하고자 한다. 특히, 본 연구는 중국 동북3성과의 교역 현황 및 해상물동량을 분석하고, 해상운송 활성화 및 물류거점 확보를 위한 정책적 제언을 하고자 한다. 정책적 제언으로 물류 허브 구축을 위한 항만 공동운영, 항만 인프라 공동건설, 해운사 공동운영을 제안하고자 하며, 문화적 협력 및 콘텐츠 개발을 통한 인적교류 확대로 한국-중국 간의 해상운송여객사업 활성화 방안을 제시하고자 한다.

• 자원환경지질
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• 제28권1호
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• pp.79-88
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• 1995

The gravity measurment has been carried out at 48 gravity stations with intervals of 1.0~1.5 km along the survey line between Samcheog, Gosari and Taebaek to study subsurface geology and geologic structure in the northeastern part of the Ockchon zone. The Bouguer gravity anomaly values were obtained from the measured gravity values through the gravity corrections. The subsurface geology and geologic structure were interpreted quantitatively by means of the Fourier series method and Talwani method for 2.5 dimensional body. In the study area, the depth of Conrad discontinuity is about 10 km at Samcheog, northeastern end of the survey line, and it is increased rapidly to about 12.5 km at Miro, 15 km at Gosari and 15.5 km at Dongjeom, southwestern end of the survey line, respectively. The depth of the basement of the Ockchon zone exposed at Samcheog is increased smoothly to about 2 km at 5 km from Samcheog along the survey line, and is exposed again in the area between Singiry and Gosari. Beyond Gosari its depth is increased to about 1.7 km, and displaced 2.3 km downward by Osipcheon fault near Dogyeri and 0.5 km by Baeksan thrust near Cheolam, respectively. Many V-shaped low Bouguer gravity anomalies resulted from the fracture zone associated with faults imply the existence of Osipcheon fault and several inferred faults. The low Bouguer gravity anomaly zone between Tongdong and Dongjeom is caused by Jurassic gneissose granite. A local high Bouguer gravity anomaly at 35 km along the survey line from Samcheog is interpreted by the effect of iron deposit of high density existed at subsurface. The thickness of Great Limestone Group varies from 0.5 km to 1.4 km, that of Pyeongan Supergroup from 0.4 km to 0.9 km, and that of Yangdeog Group is about 0.3 km. The thickness of Jurassic gneissose granite varies from 1.5 to 3.0 km.

• 한국해양학회지:바다
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• 제1권2호
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• pp.73-79
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• 1996

본 연구는 북동 태평양의 심해저 퇴적물에 서식하는 대형저서동물의 군집 구조와 수평적 및 수직적 분포양상을 보기 위해 1996년 5월에 수행되었다. 생물 시료는 25개 정점에서 box corer를 사용하여 채취된 퇴적물을 0.3 mm 망목의 체 로 걸러 채집하였다. 총 9개 동물문의 17개 분류군에 속하는 363개체의 저서동물이 출현하였고, 이들은 선형동물(30.0%), 유공충류(25.1%), 저서성 요각류(10.2%), Xenophyophorea(5.2%), 다모류(4.7%)순으로 우점하였다. 전형적인 중형동물 분류군 들을 제외하면 다모류가 가장 우점한 동물군이었다. 출현종의 수는 0.01 m$^{2}$ 당 평균 6종류였고, 서식밀도는 1,288개체/m$^{2}$ 로서 심해역으로는 밀도가 높았다. 퇴적물 깊이별 수직분포를 보면 표층에서 최대출현량을 보이고 깊이에 따 라 감소한다. 퇴적물 깊이 10 cm 층 이내에 전체 저서생물의 98% 이상이 출현 하였다.

• 동굴
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• 제73호
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• pp.29-34
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• 2006

Science and technology is the power of impelling the economic and social development. Promoting the international sci-tech communication and cooperation is one of the important ways of pulling the economic development of Northeast Asia area. Sci-tech communication and cooperation between the government and the folk are two wings of international sci-tech communication and cooperation. Both are supplemented mutually and indispensable. In order to promote the economic and social development of Northeast Asia area and further strength, some suggestions are put forward, i.e.fully exerting university the main roles in the sci-tech communication and cooperation of Northeast Asia area and fully exerting Liaoning province the important roles in the sci-tech communication and cooperation of Northeast Asia area.

• 한국환경생태학회지
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• 제17권4호
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• pp.337-345
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• 2004

낙엽활엽수림 개벌 후 벌채지에서 식생구조 회복과정과 변화를 관찰하기 위하여 서울대학교 농업생명과학대학 부속 남부연습림인 백운산의 벌채지를 대상으로 선정하였다. 1994년에 2개의 모니터링 조사구를 설치하였고, 1997년과 1999년, 2001년, 2003년에 식생조사를 하였다. 벌채후 10년간 벌채지의 산림식생변화는 다음과 같다. 벌채지 산림내부에서 벌채 후 1년째에는 잔존 수목인 쪽동백나무, 때죽나무 및 비목나무가 우세하게 나타났으며, 벌채 후 6년째에는 근주맹아목인 때죽나무와 비목나무, 실생목인 두릅나무가 우세하게 나타났고, 벌채 후 8년차부터 벌채 후 10년차 까지 비목나무 때죽나무, 졸참나무 등이 우점종으로 나타났다. 벌채지 산림내부의 종다양도지수는 남서사면에서 계속 낮아졌으며, 북동사면에서는 6년차까지 증가하다가 벌채 후 8년차부터 감소하였다. 흉고직경급(DBH) 분석에서 벌채 후 10년경과시 남서사면의 경우 졸참나무, 때죽나무, 비목나무의 개체수가 출현율이 높았고, 북동사면의 경우 당단풍나무, 쪽동백나무, 함박꽃나무, 비목나무. 두릅나무의 개체수 출현율이 높게 나타났다. 기저면적은 남서사면의 경우 8년차에 비해 감소하였으나, 북동사면 경우는 증가하여 사면간 차이를 보였다.

• Ocean and Polar Research
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• 제26권2호
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• pp.255-263
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• 2004

This study was conducted to investigate the community structure and distributional pattern of meiobenthos in the deep-sea bottom of the Clarion-Clipperton Fracture Zone of the northeastern Pacific during July 2003. The samples were collected using the multiple corer at 13 stations along the transects fiom $5^{\circ}N\;to\;17^{\circ}N$. The most abundant meiobenthos was nematodes and followed by sarcomastigophorans; these two taxa comprised more than 70% of the total abundance at all stations. For size distribution analyses showed that animals which fit into the sieve mesh size of 0.063mm were abundant. The maximum density of meiobenthos was $147inds./10cm^2$ at station located in $7^{\circ}N$, and the minimum density was $6 inds./10cm^2$ at station located in $14^{\circ}N$. More than 60% of meiobenthos were distributed at surface sediment layer within 1.0cm, and the peak abundance was found at $0{\sim}0.25cm$ layer. The latitudinal distribution pattern of meiobenthos in the study area seemed to be related with the primary productivity of the surface water that is also connected to the water circulation pattern of the Pacific Ocean near the Equator, diverging at latitude of $8^{\circ}N$ and conversing at $5^{\circ}N$.