• 한국환경생물학회:학술대회논문집
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• 한국환경생물학회 2001년도 학술대회
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• pp.84-84
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• 2001

• Ocean and Polar Research
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• 제43권2호
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• pp.65-72
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• 2021

In order to evaluate the dissolved organic carbon (DOC) and fluorescent dissolved organic matter (FDOM), as indicators of organic matter in the coastal environments, we measured the concentrations of DOC, FDOM, and chemical oxygen demand (COD) in saline groundwater (Woljeong, Pyoseon, and Hwasun beaches) and coastal seawater (Haengwon, Gwideok, Pyoseon, and Yeongnak) in Jeju, Korea. The highest concentrations of DOC and COD in groundwater were found in Woljeong and Pyoseon, and those in coastal water were observed in Haengwon and Pyoseon, indicating that the higher concentrations of DOC and COD seem to be associated with saline groundwater-driven dissolved organic matter (DOM) and/or biogeochemical processes. According to origin and optical properties of DOM using FDOM as a tracer, proportion of humic-like FDOM, more refractory DOM, was relatively greater in the groundwater than in the coastal water. With regard to this result, there was no relationship between DOC and COD in groundwater, while DOC showed a good positive correlation (r² = 0.66) with COD in coastal water. This result indicates that COD as an indicator of assessment of DOM has a limitation in which it is difficult to quantify refractory DOM. Although DOC is a potential alternative to COD in the coastal environments, particulate organic carbon cannot be negligible due to relatively higher concentration compared to the open ocean. Therefore, the use of total organic carbon (TOC) as a replacement of COD in the coastal ocean is important, and the evaluation criterion of the TOC is necessary in order to evaluate of organic matter indicator in the various coastal environments.

• 한국해안해양공학회:학술대회논문집
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• 한국해안해양공학회 2001년도 한국해안해양공학발표논문집 Proceedings of Coastal and Ocean Engineering in Korea
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• pp.146-151
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• 2001

• 대한토목학회논문집
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• 제44권4호
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• pp.465-482
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• 2024

The global use of groundwater in coastal areas has increased. Events such as seawater intrusion (SWI) are expected to increase along with the acceleration of natural disasters owing to environmental changes such as climate change, resulting in large-scale damage worldwide. Current trends in the research of coastal groundwater and related natural disasters include testing and verifying technologies using major case studies from individual countries. We identified global research trends in coastal groundwater, related these trends to changing environments and climate, and confirmed the qualitative and quantitative growth of these studies. This study describes the theoretical background and techniques for coastal groundwater analysis and details regional-scale SWI indicators based on analytical and numerical studies. This review highlights recent technologies that consider uncertainty and promotes discussions on field data obtained using new technologies. Finally, the research findings and trends for a regional coastal aquifer in Korea are discussed to describe recent SWI approaches for groundwater resources.

• 한국지구과학회지
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• 제40권4호
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• pp.428-435
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• 2019

In the shallow coastal area, located off the northwestern Taean Peninsula of the eastern Yellow Sea, geoacoustic models with two layers were reconstructed for underwater acoustic experimentation and modeling. The Yellow Sea experienced glacio-eustasy sea-level fluctuations during Quaternary period. Coastal sedimentation in the Yellow Sea was characterized by alternating terrestrial and shallow marine deposits that reflected the fluctuating sea levels. The coastal geoacoustic models were based on data from piston, grab cores and the high-resolution 3.5 kHz, chirp seismic profiles (about 70 line-kilometers, respectively). Geoacoustic data of the cores were extrapolated down to 3 m in depth for geoacoustic models. The geoacoustic property of seafloor sediments is considered a key parameter for modeling underwater acoustic environments. For simulating actual underwater environments, the P-wave speed of the models was adjusted to in-situ depth below the sea floor using the Hamilton method. The proposed geoacoustic models could be used for submarine acoustic inversion and modeling in shallow-water environments of the study area.

• 한국해안해양공학회:학술대회논문집
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• 한국해안해양공학회 1992년도 정기학술강연회 발표논문 초록집
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• pp.158-165
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• 1992

Bottom sediments, in various types of sediment transport models, have been usually assumed to be horizontally and/or vertically homogeneous. The assumption may be appropriate in well-sorted sedimentary environments including sand beaches and high turbid regions of fine grained cohesive sediments. (omitted)

• 한국지형학회지
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• 제23권3호
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• pp.79-92
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• 2016

Samples from two boreholes of coastal dune field at Jangho-ri coast, Gochang was studied. These were analyzed by grain size analysis geochemical analysis, and the application of OSL dating method to understand the development during the Holocene. The boreholes SB8 and SB9 were classified into three different sedimentary layers by their mean grain size and geochemical characteristics. The results revealed that the upper sand layer is equivalent to the present coastal dune layer, which developed since 1,200 years ago; the silt layer in the middle to the dune slack or lagoon sedimentation layer, which developed between 1,200 and 6,000 years ago; and the sand layer at the bottom to the paleo coastal dune that developed between 6,000 and 7,000 years ago. It was proposed that the forming material of current coastal dune was supplied from the sandy flat in coastal area, while the middle silt layer was supplied from the weathered soil of a bed rock by the comparison with material of surrounding area. In the case of coastal dune, concentrated layer of sands were identified which were buried about 300 and 1,200 years ago, which is identified as the little ice age. This study confirmed the development of Jangho-ri coastal dunes after Holocene Climate Optimum period, and it is likely to assist in the understanding of coastal dunes development.

• 한국군사과학기술학회지
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• 제27권3호
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• pp.346-354
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• 2024

Deep learning models require high computing power due to a substantial amount of computation. It is difficult to use them in devices with limited computing environments, such as coastal surveillance equipments. In this study, a lightweight model is constructed by analyzing the weight changes of the convolutional layers during the training process based on MobileNet and then pruning the layers that affects the model less. The performance comparison results show that the lightweight model maintains performance while reducing computational load, parameters, model size, and data processing speed. As a result of this study, an effective pruning method for constructing lightweight deep learning models and the possibility of using equipment resources efficiently through lightweight models in limited computing environments such as coastal surveillance equipments are presented.

• 한국해양환경ㆍ에너지학회지
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• 제11권3호
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• pp.113-123
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• 2008

유독성 Cochlodinium polykrikoides 적조의 최초발생해역으로 알려져 있는 나로도 주변 해역의 해양환경적 특징을 조사하기 위해서 1992년부터 2007년까지 국립수산과학원이 실시한 해양환경측정망 자료 및 적조정보자료와 고흥지방의 기후자료 등을 분석하였다. Cochlodinium polykrikoides 적조는 8월에 나로도 주변 해역에서 최초로 발생한 경우가 가장 많았고, 그 발생시기는 해마다 빨라지고 있는 경향을 보였다. 또한 나로도 주변 해역에서의 표층 염분도 계속 증가하는 추세를 보여, Cochlodinium polykrikoides 적조 발생시기의 빨라짐과의 어떤 관련성을 시사하였다. 한편 나로도 주변 해역에서 Cochlodinium polykrikoides 적조가 최초로 발생할 때는 동일한 시기의 가막만 또는 진해만 해역에 비해 상대적으로 일사량은 많았고 강수량은 적었다. 8월의 나로도 주변 해역의 평균 수온 및 염분은 동일한 시기의 가막만 및 진해만에 비하여 평균 수온은 $0.2{\sim}0.6^{\circ}C$, 염분은 $1.84{\sim}3.91psu$ 각각 더 높았으며, 두 해역에 비해 상대적으로 고온, 고염을 나타내었다. 또한 나로도 주변 해역은 부영양화 해역으로 알려진 진해만에 비해서는 영양염이나 식물플랑크톤의 농도가 현저히 낮았으나, 전체적인 수질환경은 가막만과 크게 다르지 않은 것으로 판단되었다. 주성분 분석결과, 나로도 주변 해역에서 최초로 발생하는 Cochlodinium polykrikoides 적조 요인으로서는 기상인자와 물리적 환경인자인 일사량과 수온이 가장 중요하며, 부차적으로 수질요소인 COD와 용존산소의 농도가 여기에 관여하고 있음을 보여주었다. 태풍 또한 Cochlodinium polykrikoides 적조 발생에 있어 중요한 요인 중의 하나로 생각되었다.

• 한국구조물진단유지관리공학회 논문집
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• 제13권6호통권58호
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• pp.176-182
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• 2009

단조롭고 자연친화적이지 못한 기존 연안블록의 설계 및 시공으로 인하여, 연안침식방지 블록이 효과적으로 제 기능을 발휘하지 못하고 또 다른 피해가 발생되고 있다. 국민소득의 증대와 Waterfront 개념의 빠른 확산으로 연안 어항의 낙후된 시설개선 등에 많은 사업이 추진되고 있으나 이러한 용도에 맞는 자연 친화형 구조물이 개발된 바 없어 기존의 Solid Block, Igloo Block, Tunnel Block 등이 일부 현장에 적용되고 있는 실정이다. 선박이 계류하는 안벽이나 물양장 등에서 항내 진입파와 항파 등으로 인한 반사파의 발생에 의한 공진현상으로 항내파고가 높아져 정온도유지가 어렵고 선박의 계류 및 하역에 지장을 주게 되며, 선박과의 충돌 발생으로 인한 소형선박의 손괴 발생율이 높은 실정이므로 새로운 형태의 블록(Block)개발이 필요하다. 이에 따라 개발한 C.E.(Coastal Environments)블록을 현장에서 사용하기 위해서는 전단키 부분의 내하력 평가가 요구 된다. 따라서, 본 연구는 C.E. 블록의 연결부 시험편을 제작하여 C.E.블록 경계면의 마찰실험을 실시하였으며, 실험에서 얻은 C.E.블록 연결부의 마찰계수를 유한요소 해석에 사용하여 C.E.블록의 블록과 블록 접촉면의 마찰 계수를 산정하고자 한다.