• 한국마린엔지니어링학회:학술대회논문집
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• 한국마린엔지니어링학회 2001년도 추계학술대회 논문집(Proceeding of the KOSME 2001 Autumn Annual Meeting)
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• pp.98-104
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• 2001

Recently, the researches on the prevention of marine oil pollution being strengthened. Sludge oils were unavoidably produced in ship's operations, therefore it is necessary to manage the sludge oils inside the ship itself with the view to prevent marine oil pollution from ship. The present study deals with the ultrasonic breaking systems that recycle the sludge oil from ships into usable oil to be burnt. At the first instanceexperimental studies were carried out to investigate the homogenizing effect of the marine oils and the erosion aspect of horn disc by repeated vibration of ultrasonic transducer. The erosion damages for horn disc SS41 steel with weight loss rate and the irradiation time to max. erosion rate were examined according to the variation of the transducer amplitude, the oil temperature and the immersing depth of horn disc. As the result of it, the erosion aspects of horn disk were varied with oil environments and testing time.

• 한국전기전자재료학회논문지
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• 제13권2호
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• pp.163-169
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• 2000

In this paper, we showed the erosion characteristic of MgO protector layer releated to lifetime of plasma display panel(PDP). We observed MgO erosion characteristic as a functions of deposition conditions, pressure and distance between electrodes. In RIE condition of Xe gas, the lowest erosion rate appears in the conditions of no heating bias voltage -30V and pressure 5mtorr. In general, as deposition rate increases, erosion rate decreases. In real panel, when the gap distance between electrodes is narrow and the pressure is low, the heavy plasma damage appears. Also, the surfaces between electrodes and on the bus electrode are extremely damaged.

• 아시안잔디학회지
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• 제10권1호
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• pp.31-40
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• 1996

The mechanical expresion provides for the use of Soil property reserves and permanent protec-tion or improvement of soil resources in accordance with measurable standards. If the functions I (initial soil property), E (soil erosion), R (soil renewal), and M. (minimum allowable value) are assumed to be integrable in region A, erosion tolerance over a region is leaded to ${\int}_A{\int}I(m, cl, re, ch, b)dA-{\int}_A{\int}{\{\int}_{to}^{\infty}[E(w, re, c, re, ch, b, t)-R(m, ch, re, b, t)]dt}\dA{\geqq}{\int}_A{\int}M_i(m, cl, re, ch, b)dA$ were variable factors are m=parent material of soil, cl=climate, re=relief or topography, ch=soil characteristics, r=rain or water, w=wind, b=biota, and t=time.

• 항공우주시스템공학회지
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• 제11권5호
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• pp.42-49
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• 2017

고체추진 로켓(SRM)은 모터케이스, 점화기, 추진제, 노즐, 절연체, 제어 및 구동장치 등으로 구성되어 있으며 액체로켓과 다르게 노즐을 냉각시킬 수 없어 고온 및 고속의 연소가스에 의해 침식(Erosion)이 발생한다. 이러한 침식현상은 노즐목의 형상 변화를 일으키며 로켓의 추력 성능을 감소시킨다. 로켓 노즐의 재질은 침식현상을 최소화하고 열을 차단시키는 효과가 있어야 하며 용융 상태에서 소실되지 않고 전단력이나 압력에 견딜 수 있어야 한다. 본 연구는 실험을 통하여 고체로켓 노즐의 재질에 대하여 연소시간별 침식특성을 파악한다. 그리고 Graphite와 C-C 복합재료의 각 재질별 조직검사를 통하여 침식 후의 미세특징을 비교 분석하여 침식특성을 규명한다.

• 한국세라믹학회:학술대회논문집
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• 한국세라믹학회 2003년도 추계총회 및 연구발표회 초록집
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• pp.115.2-115
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• 2003

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2006년도 학술발표회 논문집
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• pp.333-337
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• 2006

본 연구에서는 원격탐사와 GIS 기술을 이용하여 지형특성을 분석하고 효과적인 토양보존계획 및 관리를 위해 검토되어야 할 토사유실 원인지역을 선정하기 위한 전략적 접근방법을 제시하였다. 이를 위해 지형학적으로 인접되어 있지만 저수지의 탁도에는 매우 큰 차이를 보이고 있는 안동과 임하호 유역을 선정하였다. 각 유역에 대한 효과적인 토양보존계획 및 관리를 위해서는 강우발생에 따른 토사유실의 전반적인 거동을 파악하는 것이 중요하다. 또한 토양보존 프로그램의 효용성을 증가시키기 위해서는 각 유역을 구성하고 있는 소유역별 토사유실 잠재성을 심도 있게 분석해야 한다. 특히 본 연구에서는 안동호와 임하호 유역을 상류, 중류, 하류로 구분하여 토양침식인자, 지형인자, 식생피복인자 그리고 토사유실량의 거동을 분석하였다. 여기서 제시된 접근방법은 토양보존계획을 위해 검토되고 관리되어야 할 우선지역 선정을 위한 가이드라인을 제공 할 것이다.

• 한국안전학회지
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• 제31권2호
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• pp.70-75
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• 2016

Recently, coastal erosion has been widely in progress and the erosion level becomes also serious in the world wide, espeically in East Sea in Korea. Since it would threaten the life, economics and security risk, it is necessary to much comprehend the reason why coastal erosion has occurred according to the geographical characteristics. Meanwhile, analysis about hydrodynamics of the solitary wave such as tunami in swash zone is needed for the best management practice of coastal erosion. Solitary wave is nonlinear wave and can be reproduced in the laboratoy scale by openning suddenly a sluice gate with water head difference, of which methodology was found in the literature, since it could be simply determined by a significant wave height. Thus, in this sutdy the generation of solitary wave was experimentalized using the sluice gate. Experimental conditions were classified by angles of a beach slope, a water level in a beach slope and a difference of water level between in a headtank and a channel bed. Two kinds of dimensionless analyses based from experimental results in this study were presented; the first analysis indicates nondimensionalization between the wave height and the water level in a beach slope in order to investigate characteristics of solitary wave approaching the beach. The second shows the other nondimensionalization between dynamic pressure and static pressure on a beach slope to investigate the relationship between wave breaking and wave pressure. Under the same conditions as laboratory experiments, the numerical results computed with a SWAN model embedded in FLOW 3D were compared in terms of wave height, and pressure on the beach slope, which shows good agreement with each other. Overall results from this study could provide fundamental hydraulic data for the reliabile verification of numerical simulation results about coastal erosion in swash zone caused by solitary waves.

• 한국해양공학회지
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• 제31권1호
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• pp.60-68
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• 2017

In this study, we analyzed the real time video image obtained from the video monitoring system to grasp the shoreline, beach width, and area change of Haeundae beach. The video monitoring techniques enabled continuous monitoring for a long period at a much lower cost than general survey methods. It was possible to grasp quantitative beach variation characteristics of Haeundae beach through image acquisition, rectification, and image processing of video images. According to the monitoring results, the erosion rate of Haeundae beach in spring and summer was -19.8% in 2014 and -6.7% in 2015. The erosion rate in 2016 was -6.4%, which showed that the erosion rate in spring and summer continued to decrease. In particular, the influence of the erosion at the time of typhoon CHABA was revealed to be smaller than in the past. It can be concluded that these variations were due to beach width expansion by beach nourishment and the installation of submerged breakwaters.

• 한국표면공학회지
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• 제45권6호
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• pp.272-277
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• 2012

The hull of a fast sailing aluminium ship are generally prone to erosion owing to the impact of seawater. At this time, synergistic effects of the erosion and the corrosion by aggressive ions such as chlorides tend to aggravate the damage. There have been various attempts, including selection of erosion-resistant materials, cathodic protection and addition of corrosion inhibitors, to overcome damage by erosion or corrosion under marine environments. These approaches, however, have limits on identifying the damage mechanism clearly, because they depend on analogical interpretation by correlating two damage behaviors after the individual studies are assessed. In this research, it was devised a hybrid testing apparatus that integrates electrochemical corrosion test and cavitation test, and thus the erosion-corrosion behavior by cavitation was investigated more reliably. As a result, the slightest damage was observed at the potentials between -1.6 V and -1.5 V. This is considered to be due to a reflection or counterbalancing effect caused by collision of the cavitation cavities and the hydrogen gas formed by activation polarization.

• 한국지형학회지
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• 제19권3호
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• pp.71-82
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• 2012

이 연구는 태안 파도리 해식애 사면을 대상으로 침식기준목을 이용하여 연간 침식 후퇴율을 산정하고, 계절적 변화의 특성과 원인을 파악하고자 하였다. 연구결과, 해식애는 봄철에서 여름철까지 침식 후퇴율이 증가하였고, 다시 8~10월 사이에 급격히 증가하였는데, 이는 집중호우 및 태풍 등과 같은 극한기후사상의 영향으로 판단된다. 그 후 해식애의 침식 후퇴율은 점차 감소하다가 겨울철에 다시 증가하는데, 이것은 겨울철 폭풍해일과 기반암이 동결 해빙작용을 반복하면서 기계적 풍화가 활발히 진행된 결과이다. 해식애의 침식 후퇴율에 영향을 미치는 요소는 선행강수일수 및 일최대파고이다. 특히, 태풍 및 폭풍해일시 강한 파랑에너지에 의해 침식이 가속화되는 것으로 나타났다. 연구지역의 지난 2년간(2010년 5월~2012년 5월) 연간 침식 후퇴율은 각 지점마다 지형 지질학적 특성이 다르지만, 대략 44~60cm/yr 정도이다. 이러한 침식 후퇴율은 기존 연구결과보다 증가하였는데, 그 원인은 극한기후사상에 의한 해안 침식력이 강화되었기 때문으로 판단된다. 연구지역의 해식애 침식 후퇴과정의 특징은 해성작용(파랑에너지) 이외에도 육상의 삭박작용이 함께 작용하여 침식이 진행되고 있다.