• 해양환경안전학회:학술대회논문집
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• 해양환경안전학회 2009년도 춘계학술발표회
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• pp.89-94
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• 2009

본 연구에서는 부산 북항 재개발의 개발 단계별 해수순환 특성을 살펴보고, 이와 동시에 북항으로 유입되는 4개의 하천의 유량을 갈수기, 평수기, 홍수기로 나누어 각 시기별 하천유량의 유입이 북항의 해수순환에 어떠한 영향을 미치는지를 수치모의하고자 하였다. 결과적으로 부산 북항을 중심으로 한 해수유동 수치모의 시 건설 전과 후에 하천유량이 증가할수록 신선대 방향으로의 Flux가 증가하고 이는 건설 전 후와 상관없이 유동방향이 변하지 않기 때문인 것으로 사료된다. 또한 건설 이전의 홍수시 하천 조건에서의 해수교환율은 60%, 건설 전 후의 해수교환율은 하천유량조건과 관계없이 거의 같은 간으로 해수교환율이 증가하였다.

• 한국농공학회지
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• 제12권3호
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• pp.2029-2034
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• 1970

본 시험은 경기도 강화군 길상면 강화간척지에서 1967년부터 3년차에 걸쳐 개거의 깊이와 개거간의 거리가 제염에 미치는 영향을 구명하기 위하여 시험한 것으로 그 결론은 다음과 같다. 1. 관개용수에 의한 토양염분용탈(土壤鹽分溶脫) 깊이는, 지표하 $30{\sim}50cm$까지 영향을 미쳤으며 그이하에서는 토양함수도 및 토양염도의 변화가 미소 하였다. 2. 본 간척지 토양의 지표하 30cm 이하 부터는 수직침투가 점점 감소하고, 그대신 수평으로 침투 현상이 일어 났다. 3. 각처리를 비교할 때 개거의 깊이가 제염률 및 수확량에 영향을 미치는 정도는 미소하였으며, 개거간의 간격에 따라서는 고도의 유의차가 있어 실험 결과로는 깊이 0.9m, 간격 180m로 시설하는 것이 효과적이다. 4. 그러나 개거로 인한 손실면적을 고려하여 수확량을 비교할 때 깊이 0.9m 간격 36m를 시설함이 타당한 것으로 사료 된다.

• 상하수도학회지
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• 제31권6호
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• pp.599-609
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• 2017

Desalination plants have been recently constructed in many parts of the world due to water scarcity caused by population growth, industrialization and climate change. Most seawater desalination plants are designed with a submarine pipeline for intake and discharge. Submarine pipelines are installed directly on the bottom of the water body if the bottom is sandy and flat. Intake is located on a low-energy shoreline with minimal exposure to beach erosion, heavy storms, typhoons, tsunamis, or strong underwater currents. Typically, HDPE (High Density Polyethylene) pipes are used in such a configuration. Submarine pipelines cause many problems when they are not properly designed; HDPE pipelines can be floated or exposed to strong currents and wind or tidal action. This study examines the optimal design method for the trench depth of pipeline, analysis of on-bottom stability and dilution of the concentrate based on the desalination plant conducted at the Pacific coast of Peru, Chilca. As a result of this study, the submarine pipeline should be trenched at least below 1.8 m. The same direction of pipeline with the main wind is a key factor to achieve economic stability. The concentrate should be discharged as much as high position to yield high dilution rate.

• 한국콘크리트학회:학술대회논문집
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• 한국콘크리트학회 2008년도 추계 학술발표회 제20권2호
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• pp.773-776
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• 2008

해양환경에서 철근 콘크리트의 부식은 매우 심하며, 염해는 콘크리트 교량과 항만 구조물의 부식을 일으키는 주요 요인 중 하나이다. 특히 비말대 및 간만대의 수면 부분은 구조물의 안전과 수명의 관점에서 볼 때 매우 중요하다. 지난 수십 년간 토목, 건축분야에서 콘크리트구조물 부식을 억제하기 위한 방식법 중 음극방식(cathodic protection, CP)은 많은 발전을 이룩하였으며 이제 보편화되는 추세에 있다. 최근 해양환경에서 콘크리트구조물의 음극방식을 위해 아연 메쉬 희생양극법이 개발 소개되었으나 아직까지도 이에 대한 구체적 내용이 잘 알려지지 않은 상태이다. 따라서 본 연구에서는 아연 메쉬 음극방식이 환경인자에 따라 콘크리트교각에 어떤 영향을 미치는지에 대하여 조사하였다. 아연 메쉬와 철근의 거리에 따라 음극방식 효과를 측정하기 위하여 약 100cm의 파일 시험편에 10cm 세그먼트 철근 8개를 설치하였으며, 아연 메쉬 희생양극에 의한 음극방식의 설계에 관련된 정보를 얻고자 파일 시험편의 높이에 따른 음극방식 전위의 변화와 전류의 감소치를 측정하였다.

• 한국해양공학회지
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• 제20권6호
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• pp.54-60
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• 2006

This study discusses characteristic of spatiotemporal changes of the sand barrier in the Nakdong estuarine for the last century, focusing on geomarphologic evolution and mobility of sand barriers in the view of coastal engineering. The Nakdong estuarine, the research subject, has a complexly changing natural environment by interaction between ground and marine elements such as ocean wave, tidal current, sediment, etc. Moreover, recently, unnatural geomorphologic changes (e.g., seaside reclamation, new harbor construction, etc.) has been radically increased in this area with increasing desire for coastal development. Because of this, its sand barrier has developed quite unstable condition. Therefore, to identify the development process of geomorphologic changes in this area, required is a close examination on historical characteristics of spatiotemporal changes of the sand barrier in relation to surrounding seaside reclamation and physical environmental changes. This study, based on the marine charts published in between 1927 and 1995 year, analyzes the length and area of the sand barrier for the last hundred years, and investigates the cause of the changes by looking into the change of water depth for the last two years and doing ocean-physical site observations. In conclusion, the sand barrier of the Nakdong estuarine expands toward the open sea by $7.4{\sim}26m$ in annual average, maintaining a fixed distance of $1,241{\sim}1.279m$, and its area is expected to increase about $2.8km^2$ annually. This is characterized by the wocean wave from the open sea and the discharge of Nakdong River.

• Physical Therapy Rehabilitation Science
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• 제5권3호
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• pp.113-119
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• 2016

Objective: The effect of abdominal expansion maneuver (AEM) and abdominal draw-in maneuver (ADIM) on postural control in an unsupported position in stroke patients. Design: Randomized controlled trial. Methods: A total of 36 persons with hemiplegic stroke participated in this study. The subjects were randomly divided into an AEM experimental group (n=12), an experimental ADIM group (n=12), and a control group (n=12). We collected the general characteristics of all subjects and the pre-test results before the intervention and after 4 weeks of the intervention. The trunk stabilization training of the ADIM and AEM group were performed 15 minutes a day, 3 times a week for 4 weeks, and general physical therapy was performed 2 times a day, 30 minutes per session, 5 times a week for all three groups. The control group received joint mobilizations, muscle strengthening, endurance strengthening, and gait exercises along with treatment of the central nervous system, such as neuro-developmental treatment, mat, and gait training. The AEM is an inspiratory phase of tidal breathing expanding the lateral lower ribcage in a lateral direction with minimal superior movements of the chest. Then the lower abdomen expands and the navel moves in an anterior-caudal direction. The ADIM is a repeated contraction and relaxation of the anal sphincter during inspiration. The navel pulls the lower abdomen to the direction of the spine without the movement of the trunk and pelvis. Results: Before and after the interventions, medial-lateral axis movement distance, anterior-posterior axis movement distance, sway mean velocity, and sway area 95% was a statistically significant change in all three groups (p<0.05). The post-hoc test showed a significant improvement in medial-lateral axis movement distance, anterior-posterior axis movement distance, sway mean velocity, and sway area in the AEM group compared with the control group, and in the ADIM group compared with the control group (p<0.05). Conclusions: In conclusion, both AEM training and ADIM training are necessary interventions to maintain the independent sitting position according to the characteristics of the patient.

• 한국해양학회지
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• 제28권3호
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• pp.177-185
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• 1993

장파의 산란이론(Produman, 1914; Longuet-Higgins, 1970)을 대륙붕상의 작은 원 통형 섬주변을 전파하는 조석주기의 Kelvin 파에 적용하였으며, 해저마찰의 효과를 포 함하였다. 이론적 분석에 의하면 산란파의 진폭은 섬주변에서 Kelvin 파의 진폭 감소 율을 변화시킨다. 이러한 진폭의 변화로 비점성 유체의 경우에 섬 연안에 따라 진폭이 균등해지고, 진폭변화는 전향력의 작용으로 설명되어 진다. 해저마찰력은 파가 전파되 어 오는 쪽 연안에서 전파되어 가는 쪽 연안으로 진폭을 감쇄시키나, 연안을 따른 진 폭변화는 상기 연안을 연결하는 선에 대하여 대칭이다. 산란파의 위상은 외해에 비해 전파되어 오고 가는 쪽 연안 부근에서 파의 진행이 빨라지게 한다. 섬 주변에서 파의 위상분포에 미치는 해저면 마찰력의 영향은 무시할만 하다.

• 한국해양학회지:바다
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• 제3권3호
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• pp.103-111
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• 1998

본 연구는 경기만 표층 퇴적물의 지화학적 특징과 입도분포와의 관계를 조사하기 위해서 수행되었다. 1995년 12월에 채집한 총 90 개 퇴적물 시료를 대상으로 입도분포, 유기탄소와 중금속 함량(Al, Fe, Mn, V, Co, Ni, Cr, Zn, Cu)을 분석하였다. 또한 1981년에 조사된 자료와 비교함으로써 그 동안의 변화를 파악하고자 하였다. 퇴적물 입자의 크기는 몇몇 지역에서 1981년과는 다른 양상을 보였다. 1994년에 완공된 시화방조제 부근의 퇴적물은 이전에 비해서 세립해졌다. 공항건설을 위한 매립공사가 진행되고 있는 영종도 부근의 퇴적물의 경우 세립한 퇴적상에서 혼합 퇴적상으로 변하였다. 유기물과 중금속 함량은 전반적으로 입도에 의존적인 분포를 보이고 있지만, 인천북항의 퇴적물에서는 입도와 무관하게 유기물과 Ni, Cr, Zn 그리고 Cu 등의 중금속이 높은 농도로 농축되어 있었다.

• Ocean and Polar Research
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• 제31권1호
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• pp.71-76
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• 2009

Drastic changes in the water quality and phytoplankton community of the new Saemankeum Lakeduring the first decade following the construction of the Saemankeum Sea Wall has been considered to be unavoidable. Input of eutrophicated water through the Mankyeong River and Dongjin River might produce more direct effects on the water quality and phytoplankton community, which lead us to launch a long-term semi-weekly investigation at the "Mankyeong Bridge" monitoring point to resolve its short-term effect as well as long-term stabilization of the ecosystem in the new Saemankeum Lake. During 15 months starting from June 2006, the water temperature varied in accordance with the typical seasonal variations in temperate on the coasts, and no significant daily variations evoked by tidal cycle could be detected. However, there was an inverse relationship between seasonal precipitation and salinity even though the range in annual variation was drastically reduced right after the construction of the Saemankeum Sea Wall. Species richness in the phytoplankton community was also reduced due to the narrowed annual range of salinity, which would eliminate the mid-high salinity species from the Mankyeong Bridge monitoring point. Similarly, species diversity was decreased with increased dominance of the phytoplankton community after the construction. Between the two summer seasons during the present study, species diversity was higher in 2007 than in 2006, which might indicate the early stage of a gradual stabilization in the ecosystem including the phytoplankton community at the monitoring station. The phytoplankton community thus needs to be monitored on a long-term basis to identify indirect signals that can be used to assess the stability of the ecosystem in the young Saemankeum Lake.

• Ocean and Polar Research
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• 제36권2호
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• pp.87-101
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• 2014

Recently, more attention has been paid to the geomorphological changes in the Nakdong River Estuary, because those changes are caused by artificial activities including weirs, reclamation and construction. In order to analyze quantitatively the recent geomorphological variability in the Nakdong River Estuary, we surveyed the depth and elevation of submarine topography near Jinwoodo and Sinjado from March 2007 to February 2012. A statistical method (based on Digital Shoreline Analysis System) and an Empirical Orthogonal Functions method were used to evaluate the morphological changes. According to the statistical variables (DCE, NDC, EPR, LRR), the highest amount and rate of accumulation were recorded around the Gadeokdo whereas the greatest amount of erosion appeared around the coast off the eastern part of Sinjado. In particular, a dynamic variation of morphology was clearly observed in the vicinity of the sub-tidal channel located between Jinwoodo and Sinjado, which seems to be attributable to channel migration. As a result of the EOF method, the first mode (48.7%) is most closely related to the pattern of morphological variability that might be associated with the westerly movement of sediment by longshore current. The spatial variability of the second mode (16.6%) was high in the shoreface of Sinjado, showing a 4-year periodicity of temporal variability. The strong correlation (coefficient 0.73) between the time coefficient and suspended sediment discharge from Nakdong River emphasizes the role of sediment discharge to deposition in this area. The spatial variability of the third mode (11.3%) was distributed mainly around the coast off the eastern part of Sinjado, which is related to the movement of the coastline of Sinjado. Based on the last 5 year's data, our results suggest that the study area is characterized on the whole by a depositional pattern, but the extent of sedimentation is different locally.