• 한국환경과학회지
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• 제27권8호
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• pp.677-688
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• 2018

The purpose of this study was to minimize salt water intrusion into freshwater aquifers and limit the development of freshwater aquifers, by selecting an appropriate excavation depth of in the western coastal area of Jeju Island. The study site was mostly basaltic lava, which was mainly composed of trachy basalt. A vertical logging test was conducted to investigate the vertical distribution of the groundwater and saline groundwater interface in the study well. It was found that freshwater groundwater, saline groundwater, and freshwater groundwater are distributed from the surface to approximately 16 m, 16~50 m, and 50~60 m, below the ground, respectively. In order obtain saline groundwater and minimize the inflow of freshwater into this well, the drilling depth should be limited in the range of 16~50 m from the surface. Thus, saline groundwater well development should be carried out with reference to the measurement results, which depend on the drilling depth and EC (electrical conductivity) obtained with drilling apparatus for geology and ground handling.

• The Korean Journal of Physiology
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• 제25권2호
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• pp.189-200
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• 1991

During the past few years it has been proposed that lithium clearance can be used as a reliable measure for the outflow of tubular fluid from the proximal tubule. This study was aimed to characterize the inflow dependent reabsorption of Na in renal tubule beyond the proximal tubule. For this purpose, lithium clearance was used as a measure for the inflow from the proximal tubule and the changes in reabsorption fraction of Na and water were determined in rabbits. Rabbits were pretreated with hypotonic saline solutions for an hour (50 mM/L NaCl, 20 ml/hr/kg). And then a hypertonic solution of 500 mM/L NaCl (20 ml/kg) was administered intraperitoneally in conjunction with a bolus of LiCl solution (2 mM/kg, i.v.) for conditioning the $C_{Li}$ and urine flow rate. To rule out the effect of $Li^+$ on tubular functions, a bolus of NaCl solution (2 mM/kg, i.v.) was administered. Fifteen, thirty, and sixty minutes after injection of hypertonic saline arterial blood and urine samples were taken. Urinary and plasma concentrations as well as urinary output of $Li^+,\;Na^+\;and\;K^+$ were measured. From these $C_{Li},\;C_{Na}$ and the reabsorption fraction of Na and water $(Fr_{Na}\;&\;FrH_2O)$ were calculated. These results were compared with those from control groups in which the same amount of isotonic saline (145 mM/L NaCl) and of 15% dextran solution were administered in the same way as that in experimental group. Followings are the results obtained. 1) The plasma concentration of $Na^+$ in rabbits injected with hypertonic saline reached the peak value after 15 min and thereafter no significant change was observed. Hematocrit values did not show any change, while urinary excretion of $Na^+$ increased markedly during the first 15 min and decreased thereafter. These results were not affected by an injection of a small amount of LiCl. 2) The clearances of $Li^+,\;Na^+\;and\;K^+$ in rabbits injected with hypertonic saline and LiCl solution decreased. 3) In spite of the variation in $C_{Li},\;Fr_{Na}$ did not show any significant change while $FrH_2O$ increased gradually. 4) $C_{Li}$ decreased also in rabbits received isotonic saline. $Fr_{Na}$ tended to be higher than that in hypertonic saline group, while $FrH_2O\;and\;Fr_{Na}$ did not associated with the decrease in $C_{Li}$. 5) $C_{Li}$ of the rabbits received dextran solution fluctuated persistently and $Fr_{Na}\;and\;FrH_2O$ did not change in along with $C_{Li}$ although $Fr_{Na}$ had a tendency to be higher than that in hypertonic saline group. 6) From the above results it was concluded that: (a) In rabbits with normal body store of $Na^+$, the $Fr_{Na}$ of renal tubule beyond proximal tubule. calculated from $C_{Li}$ as a measure of inflow from proximal tubule is constant in spite of variations in $C_{Li}$. (b) The $FrH_2O$ calculated from $C_{Li}$ is dependent largely upon ADH rather than inflow from proximal tubule. (c) When there is a decrease in plasma $Na^+$ concentration or ineffective body fluid. $Li^+$ reabsorption may occur in the thick segnent of Henle's loop and hence the determination of $Fr_{Na}$ and $FrH_2O$ will not be easy one, but $Fr_{Na}$ is constant under the same experimental conditions.

• 한국환경과학회지
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• 제17권2호
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• pp.141-148
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• 2008

In order to investigate the effect of inflow of Yangze river on the distribution of chlorophyll-${\alpha}$, the results of serial oceanographic observation during 2000-2005 were used. The oceanographic conditions in the northern East China Sea is influenced by the Tsushima Warm Current and low saline water derived from the Yangze river. The distributions of these water masses vary significantly by the season in the northern East China Sea. The sea surface temperature and salinity were stable and concentrations of chlorophyll-${\alpha}$ were low in the eastern part of $126^{\circ}E$. On the contrary, the salinity was significantly influenced by the low saline water derived from Yangze river with the high concentrations of chlorophyll-${\alpha}$. It is suggested that the low saline water inflowed from the Yangze river affects high concentrations of chlorophyll-${\alpha}$ in the northern East China Sea in summer.

• 한국관개배수논문집
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• 제9권1호
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• pp.38-47
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• 2002

The Lake Sihwa gradually changes from freshwater lake to saline lake due to inflow of seawater by sluice gates . The changes of lake water are closely related to characteristic and distribution of turbidity and suspended matter. During the period April-Ma

• 한국해양학회지:바다
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• 제5권4호
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• pp.295-304
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• 2000

수리적인 환경 요인(조석, 바람 등)에 따른 하계 서남극 킹조지섬 마리안 소만의 수층 특성과 부유물질 분산을 이해하기 위해 내만에 유빙이 점유했던 시기에 30분 간격으로 CTDT연속 관측을 수행하였고 공간적인 표층 해수의 특성(수온과 염분)과 부유물질농도가 측정되었다. 소만 중앙의 수층은 탁도의 관점에서 크게 1)저온 ${\cdot}$ 저염 ${\cdot}$ 고탁도의 표층 플름과 2)고온 ${\cdot}$ 고염 ${\cdot}$ 저탁도의 맥스웰 만 유입수로 나누어진다. 소만 안쪽의 빙벽 앞과는 달리 빙하기저부 유출에 의한 담수성 수층이 나타나지 않았다. 고온의 맥스웰 만 표층수와 조수빙하/유빙의 열적 융빙은 표층 혼합층을 발달시키며 특히 소만 내 유빙의 점유와 거동으로 인해 맥스웰 만 유입수의 수층 특성이 불안정해진다. 이러한 수층의 불안정으로 인해 조석주기에 따른 맥스웰 만 유입수와 표층 플름의 거동은 나타나지 않았다. 소만 북부 연안에 나타나는 표층 플름에 비해 고온 ${\cdot}$ 고염 ${\cdot}$ 고탁도 표층 플름은 강한 북서풍 계열의 바람으로 위버 반도 서부 연안을 따라 중앙 분지로 유입되는 연안류이다. 표층 플름의 육성기원 쇄설물은 주로 급경사 연안의 빙벽 가장자리와 일부 해안가의 융설수류로부터 유입되며 조석과 바람에 의해 분산되고 조절된다. 특히 대조차 시기의 북서풍은 고탁도의 표층 플름을 내만에 체류시키며 소만 분지에 육성기원 쇄설성입자의 퇴적을 증가시킨다.

• 항공우주시스템공학회지
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• 제11권2호
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• pp.43-50
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• 2017

한반도의 근해는 다양한 해양변화가 있으며, 작전을 수행하는 해군함정, 함재기, 해상운용 비행기, 공군의 전투기, 해안에 위치한 공항 및 비행장 등이 영향을 받는다. 특히 해양환경의 직접적인 영향인 염분은 가스터빈엔진과 같이 고온/고속으로 운용되는 장비에 연료의 황성분과 화학적 변화로 고온부식(Hot Corrosion)이 발생시킨다. 한계값으로 정의 할 수 없지만 염분에 의한 부식은 디미스터(공기흡입구) 높이가 7m 이하일 경우 해상에서 유입되는 염분이 증가하여 부식이 급격하게 증가하였다. 또한 서해보다 동해에서 작전임무를 수행하는 무기체계는 염분도, 풍량, 파고에 의해 비산되는 염분이 상대적으로 많아 부식율이 17% 증가함을 확인하였다. 해상에서 가스터빈엔진을 운용하는 해상무기체계는 염분유입을 최소화하기 위해 해상으로부터 13m이상에서 운용되어야 급격한 고온부식을 최소화 될 것으로 본다.

• 한국추진공학회:학술대회논문집
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• 한국추진공학회 2017년도 제48회 춘계학술대회논문집
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• pp.137-138
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• 2017

한반도의 근해는 다양한 해양변화가 있으며, 작전을 수행하는 해군함정, 함재기, 해상운용 비행기, 공군의 전투기, 해안에 위치한 공항 및 비행장 등이 영향을 받는다. 특히 해양환경의 직접적인 영향인 염분은 가스터빈엔진과 같이 고온/고속으로 운용되는 장비에 연료의 황성분과 화학적 변화로 고온부식(Hot Corrosion)이 발생시킨다. 한계값으로 정의 할 수 없지만 염분에 의한 부식은 디미스터(공기흡입구) 높이가 7m 이하일 경우 해상에서 유입되는 염분이 증가하여 부식이 급격하게 증가하였다. 또한 서해보다 동해에서 작전임무를 수행하는 무기체계는 염분도, 풍량, 파고에 의해 비산되는 염분이 상대적으로 많아 부식율이 17% 증가함을 확인하였다. 해상에서 가스터빈엔진을 운용하는 해상무기체계는 염분유입을 최소화하기 위해 해상으로부터 13m이상에서 운용되어야 급격한 고온부식을 최소화 될 것으로 본다.

• 대한응급의학회지
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• 제29권6호
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• pp.641-648
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• 2018

Objective: This study examined the incidence and amount of air inflow during central venous catheter (CVC) insertion. Methods: This study was an experimental study aimed at designing an apparatus to implement blood vessel and blood flow in the human body. A 1.5-m long core tube with a Teflon tube, suction rubber tube, and polyvinyl chloride tube were made. This core tube was assumed to be the blood vessel of the human body. Blood was replaced with a saline solution. The saline solution was placed higher than the core tube and flowed into the inside of the tube by gravity. The CVC was injected 15-cm deep into the core tube. The air was collected through a 3-way valve into the upper tube. The experiments were carried out by differentiating the pressure in the tube, CVC insertion step, and diameter of the end of the catheter. The experiment was repeated 10 times under the same conditions. Results: The amount of air decreased with increasing pressure applied to the tube. Air was not generated when the syringe needle was injected, and the amount of air increased with increasing size of the distal end catheter. Conclusion: To minimize the possibility of air embolism, it is necessary to close the distal end catheter at the earliest point as soon as possible.

• Journal of the korean society of oceanography
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• 제33권3호
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• pp.41-52
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• 1998

A seasonal circulation pattern in the eastern Yellow Sea (EYS) is suggested from the water mass analysis and geostrophic calculation using the hydrographic data collected by National Fisheries Research and Development Institute during the years of 1970 to 1990. This research focuses on the presence of inflow of warm (and saline) waters into EYS in summer. EYS is divided into two regions in this paper: the west coast of Korea (WCK) and the central Yellow Sea (CYS). In CYS, waters are linked with warm waters near Cheju Island in winter, but with cold waters from the north in summer (in the lower layer). It is not simple to say about WCK because of the influences of freshwater input and tidal mixing. Nevertheless, water mass analysis reveals that along WCK, waters have the major mixing ratios (40-60%) of warm waters in summer, while the dominant mixing ratios (50-90%) of cold waters in winter. Such a seasonal change of water mass distribution can be explained only by seasonal circulation. In winter, warm waters flow northward into CYS and cold waters flow southward along WCK. In summer, warm waters flow northward along WCK and cold waters flow southward into CYS. This circulation pattern is supported by both statistical analysis and dynamic depth topography. Accordingly, Yellow Sea Warm Current may be defined as the inflow of warm waters to CYS in winter and to WCK in summer.

• Ocean and Polar Research
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• 제28권2호
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• pp.153-161
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• 2006

To investigate inflow path of the East Sea Intermediate Water (ESIW) into the Ulleung Basin, hydrographic data surveyed in July 2005 were analyzed. The ESIW was characterized by the Salinity Minimum Layer (SML) within a depth range of 100 to 360 meters. Averaged potential temperature and salinity of the SML were $1.835^{\circ}C$ and 34.049 psu, respectively. Mean potential density $({\sigma}_{\theta})$ of the SML was 27.221 with a standard deviation of 0.0393. On isopycnal surfaces of 27.14 and 27.18 $({\sigma}_{\theta})$ which correspond to upper layers of the ESIW, the coastal low salinity water was separated from the offshore low salinity water by the relatively warm and saline water which might be affected by the Tsushima Warm Current Water. Relatively cold and fresh water, however, intruded into the Ulleung Basin from the region of Korean coast on isopycnal surfaces of 27.22 and 27.26 which was lower layer of the ESIW. The salinity distribution in the isopycnal layer of $27.14{\sim}27.26$ with acceleration potential on 27.22 up surface also showed clearly that the low salinity water flowed from the coastal area and intruded into the Ulleung Basin. This implies that the ESIW flows ken the north to the south along the east coasts of Korea and spreads into the Ulleung Basin in summer.