• Title/Summary/Keyword: Warm Water Spreading

Search Result 7, Processing Time 0.022 seconds

A Study on the Thermal Fields Control using a Floating-type Current Control Structure (부유식 해수유동제어구조물의 유동제어 특성에 대한 연구)

  • Boo, Sung-Youn
    • Journal of Ocean Engineering and Technology
    • /
    • v.13 no.2 s.32
    • /
    • pp.147-158
    • /
    • 1999
  • Warm or waste water discharged from offshore-based facilities often causes environmental polution as it is transported to coastal area due to tidal actions. In this research a floating-type current control structure is introduced in order to reduce the pollutant spreading in the coastal area. Effectivenss of the structure is investigated through the numerical experiment which is based on a 3-D finite difference multi-level scheme. The warm-water spreading in the bay is reduced when the draft of the structure increases and its optimum draft is found to be between 0.25h and 0.65h, where h is the water depth. The proposed structure is also tested in the Gohyun Bay and it ts proven to be applied to controllling pollutant spreading if its draft is properly chosen.

  • PDF

The Fluctuation Characteristics of the Water Mass and the Current Structure of the Southeastern Region of The East Sea

  • Cho, Kyu-Dae;Lee, Chung-Il
    • Proceedings of the Korean Society of Fisheries Technology Conference
    • /
    • 2000.05a
    • /
    • pp.181-182
    • /
    • 2000
  • Due to the instability of the EKWC, the oceanic conditions in the East Sea are affected by the fluctuations of the moving paths of the TWC, polar fronts, and warm eddies. In particular, warm eddies play an important role in spreading the surface water of the East Sea from its southern coastal region to its interior region (Isoda, 1994). However, the fluctuation characteristics of the meandering TWC and the warm eddies in the East Sea are not yet known due to the instability of the TWC. Hideaki(1999) showed that the moving paths and features of the TWC in the coastal regions of Japan were not constant. (omitted)

  • PDF

Plywood Properties by PEG Treatment Conditions on Veneer (단판(單板)의 PEG 처리조건(處理條件)에 따른 합판(合板)의 성질(性質))

  • Suh, Jin-Suk;Doh, Geum-Hyun
    • Journal of the Korean Wood Science and Technology
    • /
    • v.17 no.2
    • /
    • pp.20-25
    • /
    • 1989
  • This study was carried out in order to investigate the treatment effect of PEG soln which is a common dimensional stabilizer to green log. sawing panel etc, on bonding product including plywood widely-used in secondary processing unit. The 30% concentration of aqueous PEG soln. with molecular weight of 400, 1.000 and 4,000 were prepared respectively, and also dipping the veneer in the PEG soln. spreading the PEG soln. on veneer and mixing the PEG soln. in the adhesive were allowed. Then the ratio of PEG impregnation on veneer, the adhesive strength of plywood were epitomized as follows: The ratio of impregnation by PEG 4,000 at dipping condition was highest. while that by PEG 400 at same condition was lowest. However, the effect of PEG molecular weight on the ratio of impregnation at spreading condition did not occur. 2. The adhesive strength was great in the order of 4,000>400>1,000 in molecular weight of PEG at dipping and spreading conditions. In case of mixing the PEG soln. in the adhesive, the adhesive strength was great in the order of 400>1,000>4,000 in molecular weight of PEG. Throughout three treatment conditions, PEG 400 was relatively favourable with about 10kg/$cm^2$ dry strength. 3. The adhesive strength was great 10 the order of spreading >dipping >mixing condition. 4. Although adhesive strength with the 30% concentration of aqueous PEG soln. was decreased by 35% and over, compared to control (non-treatment) adhesive strength, all types of PEG treatment except mixing the PEG soln. in the adhesive exceeded the standard dry strength for common use panel. 7.5kg/$cm^2$. 5. In warm water-proof test, the adhesive strengths by all PEG treatment conditions were less than the standard wet strength, 7.5kg cot, and also delamination of glue line occured mostly in mixing in the PEG soln. in the adhesive condition.

  • PDF

A Study on Syndromes of Oryeongsan(五岺散證) (오령산증(五岺散證)에 대한 연구(硏究))

  • Bang, Jung-Kyun
    • Journal of Korean Medical classics
    • /
    • v.20 no.1
    • /
    • pp.151-164
    • /
    • 2007
  • In "Sanghanlon(傷寒論)", there are several articles to explain about Oryeongsan's syndrome. Most important articles of them are No. 72 and No. 75. Oryeongsan is explained by many doctors as a prescription to control exterior and interior, because they considered that symptoms of 72 and 75 articles were caused by exterior and interior's syndrome. Accordingly, they explained that RAMULUS CINNAMOMI(桂枝) and warm water remove exterior pathogens, and PORIA(茯笭) and others remove interior fluid retention. But considering the origin of a fluid retention, RAMULUS CINNAMOMI's effects are rather activating Yang(通陽) and warming Yang(溫陽) than removing exterior pathogens. The fluid retention is cauesd by insufficiency of Yang energy, because body fluid's spreading depends on Ynag energy. RAMULUS CINNAMOMI's effects of activating Yang and warming Yang improve the fluid retention and spread body fluid to the whole body. Some doctors use CORTEX CINNAMOMI(肉桂) instead of RAMULUS CINNAMOMI, because CORTEX CINNAMOMI's effects of activating Yang and warming Yang are better than RAMULUS CINNAMOMI's. There are many opinions about what is the main symptom of Oryeongsan's syndrome, but the difficulty in urination is understood by most doctors as the main symptom of Oryeongsan's syndrome. From the viewpoint of that, they understand that Oryeongsan's main effect is the induce diuresis. But the induce diuresis does not only mean a urination. The induce diuresis must be understood as the removing fluid retention by sweat and urine through the spreading body fluid.

  • PDF

Effect of Length of Outfall Structure on Reattachment of Thermal Discharge (온수방류의 귀환에 방류구 길이의 영향)

  • Yoon, Tae-Hoon;Yook, Woon-Soo;Yi, Yong-Kon
    • Water for future
    • /
    • v.27 no.3
    • /
    • pp.123-134
    • /
    • 1994
  • The reattachment of buoyant effluent to shore in a crossflow is investigated experimentally. The effluent is produced by discharging warm water through projecting side channel into a confined cross-flow of the same depth. In the projecting effluent, the size of recirculating region, which is formed by defleted thermal plume on the lee of the effluent, tends to increase, but the maximum temperature decreases in the direction of the crossflow and it has more even transverse spreading compared to non-projecting type. The heat flux across the crossflow is found to be independant of the projected length of the side channel under relatively low buoyancy flux on the contrary to high buoyancy flux. The reattachment of the effluent can be specified by both velocity ratio and densimetric Froude number, whereas only the velocity ratio is governing factor to the reattachment of the effluent in the case of non-projecting type.

  • PDF

Relationship between Sea Surface Temperature derived from NOAA Satellites and Cochlodinium polykrikoides Red Tide occurrence in Korean Coastal Waters (NOAA 위성자료에 의한 해수표면 수온분포와 Cochlodinium polykrikoides 적조 발생의 상관성)

  • Suh, Young-Sang;Kim, Jeong-Hee;Kim, Hak-Gyoon
    • Journal of Environmental Science International
    • /
    • v.9 no.3
    • /
    • pp.215-221
    • /
    • 2000
  • The relationship between the distribution of sea surface temperature(SST) and dinoflagellate(Cochlodinium polykrikoides) bloom areas were studied. The SST data were derived from the infrared channels of AVHRR(Advanced Very High Resolution Radiometer) sensor on NOAA(National Oceanic and Atmospheric Administration) 12 and 14 satellites during 1995-1998. The initial water temperature at C. polykrikoides bloom was about 21${\circ}C$ at the coastal areas of the South Sea and along the shore of the East Sea of Korea during the summer season of 1995. The northern limit of red tides was coincident with that of 21${\circ}C$ isothermal line in the East Sea. The red tides that initially bloomed at the coast of Pohang on September 21, 1995 moved to the coast of Uljin on September 26, 1995. The skipped appearance of the red tides in the areas between Pohang and Uljin was due to the East Korean Warm Current, which was moving offshore from Pohang to approach to Uljin. The cold water which was formed by tidal front in the western coast of the South Sea and by upwelling water from deep layer in the southeastern coast of the Korean peninsula played a role in blocking the spreading of red tides during summer season in 1997 and 1998. In conclusion, the distribution of red tides appeared to be dependent on the initial water temperature at red tides bloom. The SST at the red tides varied from 21${\circ}C$ to 25${\circ}C$; 21${\circ}C$, 23${\circ}C$, 24 and 24-25${\circ}C$ in 1995, 1996, 1997 and 1998, respectively.

  • PDF

Structure of Upwelling off the Southease Coast of Korea (夏秀 韓國 南東海岸의 湧昇의 構造)

  • Lee, Jae-Chul;Na, Jung-Yul
    • 한국해양학회지
    • /
    • v.20 no.3
    • /
    • pp.6-19
    • /
    • 1985
  • Hydrographic data and daily time series of longshore wind, sea level and sea surface temperature were used in order to explain why the upwelling effect in SST is especially prominent near Ulgi-Gampo although the sea level records along the whole southeast coast show a nearly uniform upwelling-downwelling response to wind. Regional difference in intensity of the wind-induced upwelling represented by the SST decrease is attributed to the combined influence of two factors; one is the baroclinic tilting of isotherms due to the East Korea Warm Current (EKWC) near the Ulgi-Gampo coast, the other is the topographic effects around the southeast coast. Baroclinic tilting effect of EKWC which is generally strongest near the coast of Ulgi to Gampo results in both of the shoaling of cold water and the westward trapping of the coldest bottom water over the shallower shelf rather than the deepest troough region off that coast regardless of the season. Therefore, becacse of the cold water ready for upwelling at the subsurface layer, SST responds very rapidly to the upwelling-favorable winds of summer only off the Ulgi-Gampo coast. Spreading isobaths from Pusan to Gempo can reinforce the upwelling of the cold bottom water and its westward trapping.

  • PDF