• Title/Summary/Keyword: 표층수

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속초연안 해양환경의 시공간적 변동특성

  • Park, Seung-Yun;Park, Jin-Il;Sim, Jeong-Min;Kim, Yeong-Suk;Jin, Hyeon-Guk;Hwang, Un-Gi;Kim, Gwi-Yeong;Jeong, Chang-Su
    • Proceedings of the Korean Environmental Sciences Society Conference
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    • 2006.05a
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    • pp.280-281
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    • 2006
  • 속초연안의 수온은 18개년 평균 표층수 $14.10\pm0.34^{\circ}C$, 저층수 $12.56\pm0.28^{\circ}C$, 염분은 표층수 $31.66\pm0.18$, 저층수 $32.68\pm0.10$, pH은 표층수 $8.05\pm0.01$, 저층수 $8.02\pm0.01$, BO는 표층수 $8.48\pm0.11mg/L$, 저층수 $8.16\pm0.12mg/L$, COD는 표층수 $1.54\pm0.07mg/L$, 저층수 $1.33\pm0.06mg/L$, SS는 표층수 $13.75\pm0.80mg/L$, $PO_4$-P는 표층수 $0.74\pm0.05{\mu}M$, 저층수 $0.61\pm0.04{\mu}M$, $NH_4$-N는 표층수 $2.49\pm0.18{\mu}M$, 저층수 $2.01\pm0.15{\mu}M$, $NO_2$-N는 표층수 $0.72\pm0.05{\mu}M$, 저층수 $0.58\pm0.04{\mu}M$, $NO_3$-N는 표층수 $4.39\pm0.24{\mu}M$, 저층수 $3.63\pm0.20{\mu}M$, DIN는 표층수 $7.64\pm0.38{\mu}M$, 저층수 $6.22\pm0.29{\mu}M$, DIN/DIP비 표층수 $23.91\pm3.42$, 저층수 $23.43\pm3.38$이었으며, 전반적으로 해역별 수질기준 I등급 내지는 II등급을 유지하고 있었고, 공간적으로는 외해측으로 갈수록 외해수와 혼합 확산되어 양호한 수질을 나타내었다. 장기적인 변동특성은 세그룹으로 구분되어진다.

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In Summer , the Origin of Tsushima Warm Current Water in Western Channel of the Korea Strait ( 1 ) - On the Water in Surface Layer - (하계 대한해역 서수도에 유입되는 쓰시마 난류수의 기원 ( 1 ) - 표층수에 대한 고찰 -)

  • Jo, Gyu-Dae;Yun, Jong-Hwi
    • Journal of the Korean Society of Fisheries and Ocean Technology
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    • v.26 no.2
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    • pp.184-191
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    • 1990
  • 하계 대한해협 서수도에는 연직적으로 특성이 서로 다른 세 개의 수괴가 존재한다. 그 중 표층수에 대하여 인접 해역의 해수 특성과 상호 비교함으로써 그 기원과 유로를 추정하였다. 그 결과, 표층수는 동지나해의 대륙붕 상에서 형성된 Kuroshio수와 중국대륙연안수의 혼합수로써, 중국대륙연안수의 영향을 더 많이 받는 것으로 나타났다. 대부분의 표층수는 Kyushu Island의 서쪽 해역, 경도 126$^{\circ}$E와 127$^{\circ}$E 사이 해역과 제주도 동쪽 해역을 거쳐 유입되고, 한국 연안 부근에 있는 일부 표층수는 제주도 서쪽해협을 거쳐 유입된 것으로 나타났다.

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Seawater Quality of Jinhae Bay and Adjacent Sea of Gaduk Island, Korea (진해만 및 가덕도 주변 해역의 수질 환경)

  • Kim, Kyung-Tae;Kim, Eun-Soo
    • Proceedings of KOSOMES biannual meeting
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    • 2009.06a
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    • pp.137-143
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    • 2009
  • 진해만과 가덕도 주변 해역에서 2007년 2회(하계와 추계)에 걸쳐 표층 및 저층수 조사를 실시하여 수질 환경 특성을 파악하였다. 수온은 표층이 저층보다 높았는데 여름이 가을보다 표 저층간의 차이가 컸으며, 염분은 가덕도 남쪽에서 낙동강 물의 유입 영향으로 저염분을 나타내었다. 부유물질은 표층수의 경우 진해만 및 연안에서 높고 외해에서 낮았으며, 과거의 조사 농도 범위에 속하였다. POC는 계절별로 분포 차이가 있지만 유기물 유입원에 대한 근접성과 기초 생산아 영향을 받는 것으로 나타났다. COD는 표층에서 오염원의 영향이 많은 진해만에서 높고 외해로 가면서 낮아졌다. 여름에 진해만 일부 정점은 해역별 수질기준 III등급이었다. DO는 저층이 표층보다 낮았는데 특히 진해만 내완 외해의 깊을 수심 정점에서 차이가 크고, 하계에 성층에 의하여 수증간에 큰 자이를 나타내었다. 인산염-인과 규산염-규소는 저층수에서 용존산소가 낮아짐에 따라 높은 농도를 나타내는 경향이 강하였으며, 암모니아-질소도 내만의 저산소층에서 높은 농도를 보였다. 표층수의 용존 무기질소는 신항과 가덕도 주변에서 높고 진해만 서쪽 및 외해로 갈수록 낮아졌으며, 과거 조사 농도보다 낮고 좁은 변동 범위를 보였다. 총 질소와 총인도 외해역에서 낮은 농도였으며, 표층보다 저층이 높은 추세였고 여름에 더욱 뚜렷하였다. 총질소 평균 농도로는 해역별 수질기준과 I등급을 만족하였으나 정점별로는 $I{\sim}III$등급까지 변화가 컸는데 진해만 내의 저층 또는 외해의 깊은 수심을 갖는 정점에서 등급이 좋지 알았다. Chl-a는 진해만 내 또는 가덕수도에서 높은 분포였으며, 신항과 가덕도 남쪽에서는 과거보다 낮은 농도였다.

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Korean Surface Realizer Based on Topic-Comment Structure (토픽-코멘트 구조에 기반한 한국어 표층 생성기)

  • Kim, Jung-Eun;Choi, Key-Sun
    • Annual Conference on Human and Language Technology
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    • 2001.10d
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    • pp.503-508
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    • 2001
  • 본 논문은 자연언어생성 기술을 이용하여 질병에 대한 기술문을 생성해 내는 시스템에서 사용되는 표층 생성기에 대해서 다루고 있다. 표층 생성기는 문장의 추상적인 표현으로부터 통사적으로, 형태론적으로 올바른 텍스트로 생성하여 내는 것을 목표로 한다. 질병에 관한 기술문에 있는 문장들은 두가지 특징을 가지고 있다. 첫번째로, 질병 기술문의 문장들은 토픽-코멘트 구조로 나타내어질 수 있다. 두번째로, 같은 의미 범주에 속하는 문장들은 같은 토픽을 가진다. 따라서, 토픽은 의미범주로부터 유추될 수 있으므로 표층 생성기의 입력인 구 명세 (phrase specification)에 표현될 필요가 없다. 본 논문에서는 이런 특징을 이용하여 효율적인 표층 생성기를 만들기 위하여 표층 생성의 단계를 내부 표현 생성과 외부 문장 생성의 두 단계로 나누었다. 내부 표현 생성 단계에서는 코멘트에 해당하는 부분을 생성하고 외부 문장 생성 단계에서 의미범주 태그에 따라 토픽을 첨가하여 최종 문장으로 생성하였다. 이런 방법으로 실험한 결과, 본 표층 생성기는 문법에 맞으면서 자연스러운 텍스트를 생성해 낸다는 것을 알 수 있었다.

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LNG-Vessels Hybrid Engine Seawater Desalination Complex System (LNG 선박 하이브리드 엔진 및 해수 담수화 복합 시스템)

  • Lim, Jae Jun;Lee, Dong-Heon;Byun, Gi-Sik;Kim, Gwan-Hyung
    • Proceedings of the Korean Institute of Information and Commucation Sciences Conference
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    • 2016.10a
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    • pp.663-664
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    • 2016
  • Temperature difference power generation using sea water is a method repeatedly closed liquefaction and gasification by using the ammonia (refrigerant) of the deep sea water and surface water with a temperature difference between turning the turbine. The larger the temperature difference between the nature of the temperature characteristic energy generation development, the better. This is the story that the surface waters of the deep-water temperature difference is large. But the winter is not large temperature difference between surface water and deep water has lowered energy efficiency. And desalination technologies accounted for 97% of the earth, but we can not eat the technology to convert sea water into fresh water, fresh water produced by the desalination technology that is available for various industries such as irrigation, drinking water in the vessel.In this paper, LNG transport vessels, based on the LNG transport ship to the temperature difference power generation using cold energy of thermal energy and LNG marine diesel engines, which use the existing order to improve the temperature of the surface waters of the season that is the current problem we propose that a complex development of desalination and desalination of seawater freezing research into hybrid research and utilizing the cold energy of the engine.

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Hydrographic Analysis of Surface Water Using Radium Isotopes Signature in the East and South China Sea in Summer (여름철 동중국해 및 남중국해 표층수의 Ra 동위원소를 이용한 수계분석)

  • Yang, Han-Soeb;Lee, Tong-Sup
    • The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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    • v.4 no.4
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    • pp.305-311
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    • 1999
  • This study aims to decipher surface water mass interaction in summer in the South China Sea and East China Sea by radium isotope distribution pattern. Salinity and activity ratio of radium ($^{228}Ra/^{226}Ra$) showed gradual changes, which were adequate to apply simple two end-member mixing between Kuroshio surface water and Changjiang Dilute Water for the East China Sea and the former and Nearshore Diluted Watermass (NDW) for the South China Sea. Two tracer methods, salinity and Ra isotope ratio, were compared for East China Sea. Results showed remarkable consistency for waters near Kuroshio, however, discrepancy were noticeable after Tsushima Warm Current branching. Mixing with subsurface waters may cause the discrepancy. When mixed with subsurface waters, salts and radium isotope ratio are expected to be biased in opposite direction, i. e. prone to underestimate the fraction of less saline water in the case of salts and vice versa for Ra isotope ratio. Taking the mean values of two different results seems more realistic to estimate fraction of end-members.

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Performance Comparison of R134a Organic Rankine Cycle (ORC) Using Hot Wastewater and Surface Seawater (온배수와 표층수를 이용하는 R134a용 유기 랭킨사이클의 성능 비교)

  • Yoon, Jung-In;Son, Chang-Hyo;Baek, Seung-Moon;Kim, Hyeon-Ju;Lee, Ho-Saeng
    • Journal of Advanced Marine Engineering and Technology
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    • v.36 no.6
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    • pp.768-773
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    • 2012
  • This study was performed to find out the possibility that hot waste water from a thermoelectric power plant can be applied to Organic Rankine Cycle (ORC) by comparing the performance characteristics for use of the ocean surface water ($25^{\circ}C$) and hot waste water ($35^{\circ}C$) as a secondary fluid. The parameters considered in this study are four; superheating temperature, subcooling temperature, turbine efficiency, and pump efficiency. Main results of this study are summarized as follows : Overall efficiency of applying hot waste water to ORC is 87% higher than that of surface water. Thus it could be confirmed that hot waste water of the thermoelectric power plant can be applied to ORC.

Seasonal Distribution of Vibrio spp. in the Jeonam Archipelago Marine Ranching Ground (전남 다도해 바다목장 비브리오속 세균의 계절적 분포)

  • Kim, Mal-Nam;Lee, Han-Woong
    • Journal of fish pathology
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    • v.20 no.3
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    • pp.229-235
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    • 2007
  • Cell number of Vibrio spp. was examined for the surface and bottom sea water harvested from the 9 stations in the Jeonam Archipelago Marine Ranching Ground in 2006~2007. Species population composition and dominant species were analyzed as well. The largest number of Vibrio spp. was detected in summer (June, 2007) among the 4 seasons with the surface and bottom sea water samples of 5.4~93.2 cfu㎖-1 and 1.0~53.1 cfu㎖-1. respectively. In winter (January, 2007), Vibrio spp. was not detected at all except that one station from which 0.2 cfu㎖-1 of Vibrio spp. was counted in the surface sea water sample. Cell numbers were 0~11.9 cfu㎖-1 and 0~8.3 cfu㎖-1, respectively, in the surface and bottom sea water samples retrieved in spring (April, 2007), and the corresponding sea water samples in autumn(November, 2006) were contaminated with 0.1~21.4 cfu㎖-1 and 0~2.9 cfu㎖-1, respectively. Species population composition of Vibrio spp. was found to be V. parahaemolyticus, V. alginolyticus and V. cholerae non-01 among which V. parahaemolyticus and V. alginolyticus were dominant in all seasons. V. alginolyticus was detected from all stations even in the winter season indicating that this species seems to be less temperature dependent than the other Vibrio spp..

Distributions of $^{226}Ra$\;and\;^{228}Ra$in the Surface Waters of East Sea of Korea (한국 동해 표층수중 $^{226}Ra$$^{228}Ra$의 농도분포)

  • YANG Han-Soeb;KWON Yeoung-Ann;KIM Gue-Buem;KIM Seong-Soo
    • Korean Journal of Fisheries and Aquatic Sciences
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    • v.25 no.5
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    • pp.399-405
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    • 1992
  • Using $MnO_2-coated$ fiber extraction and gamma counting techniques, we measured the distributions of $^{226}Ra$\;and\;^{228}Ra$ in the surface waters at 14 stations of East Sea of Korea in September, 1988. The concentrations of $^{226}Ra$\;and\;^{228}Ra$ in the surface waters ranged $70-110\;dpm/10^3l$ and 102=232 $dpm/10^3l$, respectively. In general, the concentrations of Ra isotopes were shown higher in the coastal and southern stations than those in the outer and northern stations in our observed area. Also, the concentrations of Ra isotopes in the study area were significantly higher than values in the other area of the East Sea and Kuroshio surface water, but much lower than the concentrations in the surface water of Yellow Sea reported previously. There was an inverse relationship between the $^{226}Ra/^{228}Ra$ ratio and salinity in the surface waters of Kuroshio, Yellow Sea and East Sea of Korea. This indicates that the continental shelf waters such as Yellow Sea and East China Sea are main source of Ra isotopes in surface waters of the East Sea of Korea.

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Heavy metals in the surface waters and sediments of Jinhae Bay, Korea (진해만 표층수와 표층 퇴적물 중의 중금속 분포)

  • Kim, Kyung-Tae;Kim, Eun-Soo;Cho, Sung-Rok;Kim, Jong-Kun;Park, Jun-Kun
    • Proceedings of KOSOMES biannual meeting
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    • 2007.05a
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    • pp.27-33
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    • 2007
  • Heavy metals in the surface seawaters and sediments were measured in Jinhae Bay. The high concentrations of heavy metals in the seawaters were found at the stations near the islands. In the sea waters, the mean concentrations of dissolved heavy metals except for Pb were not higher than previous data in this bay. Higher heavy metal contents in the surface sediments were observed at the stations adjacent to the Kojedo or Kadukdo of the Kadoksudo. The contents of Co, Ni, Zn, Cu, As and Cd in the surface sediments showed relatively high correlation coefficients with IL and COD. The order of enrichment factors(EFs) of heavy metals in the sediments was As>Cd>Pb>Zn>Co>Cu>Hg>Ni, and the EFs of As, Cd, Pb and Zn were higher than 1.

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