Sinking Particle Flux in the Subtropical Oligotrophic Northwestern Pacific from a Short-term Sediment Trap Experiment

김형직,김종욱,김동선,Michael T. Chandler,손승규 한국해양과학기술원 2018 Ocean science journal Vol.53 No.2

Time-series sediment traps were deployed in the subtropical oligotrophic northwestern Pacific (SONP) at three depths from August to September 2015 to better understand vertical flux of sinking particles. Sinking particles were collected at 5-day intervals over the sediment trap deployment period. The average total mass flux at water depths of 400 m, 690 m, and 1,710 m was 9.1, 4.4, and 4.1 mg m-2day-1, respectively. CaCO3 materials constituted 50 to 70% of sinking particles while in comparison particulate organic carbon (POC) constituted up to 20%. A synchronous variation of total mass flux was observed at the three depths, indicating that calcite-dominated particles sank from 400 to 1,710 m within a 5-day period. POC flux at these water depths was 2.4, 0.38, and 0.31 mg m-2day-1, respectively. Our results indicate low transfer efficiencies of 16% from 400 to 690 m and 13% for the 400 to 1,710 m depth range. The estimated transfer efficiencies were significantly lower than those observed at the K2 station in the northwest Pacific subarctic gyre, presumably because of a prevalence of pico-cyanobacteria in the SONP. Because cyanobacteria have a semi-permeable proteinaceous shell, they are more readily remineralized by bacteria than are siliceous phytoplankton in the northwest Pacific subarctic gyre. Continued surface water warming and expansion of the SONP will likely have a profound impact on ocean acidification in the northwest Pacific, possibly affecting the transfer efficiency of sinking POC to the deep-sea.

동태평양 열대해역에서 2009-2010년 침강입자 플럭스의 수직 변화

김형직,조소설,김동선,김경홍,유찬민,Kim, Hyung Jeek,Cho, Sosul,Kim, Dongseon,Kim, Kyeong Hong,Yoo, Chan Min 한국해양과학기술원 2022 Ocean and Polar Research Vol.44 No.3

A sediment trap had been deployed at 1250 m depth in the Eastern Tropical Pacific (ETP) from September 2009 to July 2010, with the aim of understanding the temporal and vertical variability of particle flux. During the monitoring period, total particle flux varied from 12.4 to 101.0 mg m^-2day^-1, with the higher fluxes in January-March 2010. Biogenic particle flux varied in phase with the total particle flux. The increase in total particle flux during January-March 2010 was attributed to the enhanced biological production in the surface layer caused by wind-driven mixing in response to the seasonal shifts in the location of the Intertropical convergence zone. The export ratio (e-ratio) was estimated using the particulate organic carbon flux and satellite-derived net primary production data. The estimated e-ratios changed between 0.8% and 2.8% (1.4±0.6% on average). The ratio recorded in the negative phase of Pacific decadal oscillation (PDO) was similar to the previous results obtained from the ETP during the 1992/93 periods in the positive phase of PDO. This suggests that the regime shift of the PDO is not related to the carbon export ratio.

애드혹 네트워크에서 경로 안정성 향상을 위한 라우팅 프로토콜

김형직,최선웅,Kim, Hyungjik,Choi, Sunwoong 한국정보통신학회 2015 한국정보통신학회논문지 Vol.19 No.7

Nodes of Mobile ad-hoc network usually use the energy-limited battery. Balanced energy consumptionis important to maintain path's stability. In this paper, we focus on improving the stability of the routing path in mobile ad-hoc networks. For that purpose, we propose a new routing protocol to find the highest minimum node residual energy path among shortest paths. The largest path of minimum value of the remain energy has a longer life than other paths to improve the reliability to data-transmission. Using ns-3 simulator, we show that the proposed routing protocol can provide more long-life stable routing path than AODV and EA-AODV. 모바일 애드혹 네트워크의 노드는 일반적으로 에너지의 용량이 제한된 배터리를 사용한다. 경로의 안정성을 유지하기 위해 균형 잡힌 에너지 소비가 중요하다. 본 논문에서는 애드혹 네트워크에서 데이터 전송 경로의 안정성을 향상시키는 것을 목표로 한다. 이를 위해 데이터를 전송할 수 있는 최단 전송 경로 중에서 노드 에너지 잔량의 최소값이 가장 큰 경로를 선택하는 새로운 라우팅 프로토콜을 제안한다. 에너지 잔량의 최소값이 가장 큰 경로는 다른 경로보다 상대적으로 긴 수명을 갖게 되어 데이터 전송에 안정성을 향상 시킬 수 있다. NS-3 시뮬레이터를 사용하여 제안하는 라우팅 프로토콜이 AODV와 EA-AODV보다 수명이 긴 안정적인 경로를 제공하는 것을 확인한다.

북서태평양 아열대 해역에서 침강입자 플럭스의 시·공간 변동

김형직,형기성,유찬민,전동철,정진현,김부근,김동선 한국해양과학기술원 2011 Ocean and Polar Research Vol.33 No.3

Time-series sediment traps were deployed at 1,000 m water depth of the northwestern subtropical Pacific from July 2009 to June 2010, with the aim of understanding temporal and spatial variations of sinking-particle fluxes. The opening and closing of the traps was synchronized at 18-day periods for 20 events. Total mass fluxes showed distinct seasonal variations with high values for the summer-fall seasons and relatively low values for winter-spring. This seasonal variation at two stations was characterized by a distinct difference in CaCO3 fluxes between the two seasons. The enhanced CaCO3 flux in the summer - fall seasons might be attributed to an increased planktonic foraminiferal flux. Total mass flux at FM10 station was nearly 50% higher than that at FM1 station. The difference in CaCO3 fluxes between two stations contributed nearly 70% of the difference of total mass fluxes. The CaCO3 flux was a major component controlling temporal and spatial variation of sinking - particle fluxes in the western subtropical Pacific Ocean.

케이블 모뎀 상향 채널을 위한 S-DMT의 성능 비교 분석

김형직,김성준,최형진 한국통신학회 2003 韓國通信學會論文誌 Vol.28 No.4B

[고찰과 연구] 우리 말에 들어오는 외래어를 어떻게 대할것인가?

김형직 길림성민족사무위원회 1996 중국조선어문 Vol.84 No.-

[중앙인민방속국전문란] 법률용어번역을 더욱 정확하게

김형직 길림성민족사무위원회 1994 중국조선어문 Vol.71 No.-

중국 조선민족의 민속실태

김형직 재외한인학회 1994 在外韓人硏究 Vol.4 No.1

북동태평양 심해에서 관측된 퇴적물 입자 플럭스의 계절적 변동

김형직,김동선,형기성,김경홍,손주원,황상철,지상범,김기현,김부근,Kim, Hyung-Jeek,Kim, Dong-Seon,Hyeong, Ki-Seong,Kim, Kyeong-Hong,Son, Ju-Won,Hwang, Sang-Chu,Chi, Sang-Bum,Kim, Ki-Hyun,Khim, Boo-Keun 한국해양학회 2008 바다 Vol.13 No.3

2003년 7월부터 2005년 6월까지 약 24 개월 동안 북동태평양 대한민국 망간단괴 개발광구 내에 위치한 정점 KOMO(Korea Deep-Sea Environmental Study Long-Term Monitoring Station, $10^{\circ}30'N,\;131^{\circ}20'W$)에서 시계열 퇴적물 포집장치를 설치하여 물질 플럭스를 측정하였다. 약 4,960 m 수심에서 획득된 침강입자의 총질량 플럭스는 겨울(12월-2월)과 봄(3월-5월)에 높고, 여름(6월-8월)과 가을(9월-11월)에 낮은 뚜렷한 계절변동을 보였다. 생물기원 물질플럭스도 총질량 플럭스와 유사하게 뚜렷한 계절변동을 나타냈다. 특히, 겨울과 봄에 관측된 탄산염 플럭스는 여름과 가을보다 두 배가량 높게 측정되어, 다른 생물기원 구성성분들의 계절변동에 비해 가장 크게 나타났다. 심해저층에서 관측된 침강입자의 총질량 플럭스와 생물기원 물질플럭스는 표층 해양 일차 생산력의 계절변동을 반영하는 것으로 생각된다. 겨울과 봄에는 강한 바람의 영향으로 혼합층 아래로부터 영양염의 공급이 증가되어 일차생산력이 높아진 것으로 생각되며, 여름과 가을에는 바람의 약화와 강한 성층으로 인하여 영양염 공급이 약해져서 일차생산력이 감소한 것으로 판단된다. 침강입자의 총질량 플럭스와 생물기원 물질플럭스의 계절적 변동은 이전에 연구된 엘니뇨/라니냐와 같은 환경변화에 따른 물질플럭스의 변화보다 크게 나타났다. 따라서 북동태평양 적도지역에서 엘니뇨와 라니냐 같은 환경변화의 영향에 의한 해양 물질플럭스의 변화를 이해하기 위해서는 일반적인 계절적 변동을 정확하게 측정하여야 한다. Particle fluxes were measured with a time-series sediment trap from July 2003 to June 2005 at the St. KOMO(KOMO; Korea Deep-Sea Environmental Study Long-Term Monitoring Station, $10^{\circ}30'N,\;131^{\circ}20'W$) in the northeastern Pacific. Total mass fluxes at a depth of 4,960 m showed distinct seasonal variations with high values in the winter(December-February) and spring(March-May) and low values in the summer(June-August) and fall(September-November). Biogenic origin fluxes also displayed distinct seasonal variations similar to total mass fluxes. Particularly, calcium carbonate fluxes in winter and spring were more than two times greater than those in summer and fall. The prominent seasonal variations of total mass and biogenic fluxes were closely related with the seasonal changes of primary production in the surface waters; in winter and spring, primary production increased due to the enhanced supply of nutrients below the surface mixed layer by strong wind and less stratification, whereas it decreased as a result of the less supply of nutrient by reduced wind speed and strong stratification in summer and fall. The seasonal variations of total mass and biogenic fluxes in this study were higher than the differences of total mass and biogenic fluxes caused by the environmental changes such as El $Ni\tilde{n}o$ and La $Ni\tilde{n}a$ events in the previous studies. In order to understand the effects of El $Ni\tilde{n}o$ and La $Ni\tilde{n}a$ on the particle flux, therefore, the seasonal variation of particle flux in the northeastern equatorial Pacific needs to be well defined.

북동태평양 수온약층 융기대에서 강한 엘니뇨 현상에 따른 침강입자 물질플럭스의 변동

김형직,형기성,유찬민,지상범,김동선,김부근 대한조선학회 2011 대한조선학회 학술대회자료집 Vol.2011 No.6