• Title/Summary/Keyword: Low water depth

검색결과 678건 처리시간 0.03초

Reflection and Dissipation Characteristics of Non-overtopping Quarter Circle Breakwater with Low-mound Rubble Base

  • Balakrishna, K;Hegde, Arkal Vittal;Binumol, S
    • Journal of Advanced Research in Ocean Engineering
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    • 제1권1호
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    • pp.44-54
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    • 2015
  • Breakwaters are the coastal structures constructed either perpendicular (shore connected) or parallel (detached) to the coast. The main function of breakwater is to create a tranquil medium on its leeside by reflecting the waves and also dissipating the wave energy arriving from seaside, resulting in ease of manoeuvrability to boats or ships to their berthing places. Different types of breakwaters are being used at present, such as rubble mound breakwater, vertical wall type breakwater and composite breakwater. The objective of this paper is to investigate reflection coefficients (Kr) and dissipation (loss) coefficients (Kl) for physical models of Quarter circle caisson breakwater of three different radii of 0.550 m, 0.575 m and 0.600 m with S/D ratio of 2.5 (S=spacing between perforations, D=diameter of perforations). The models were tested in the monochromatic wave flume of the department, for different incident wave heights (Hi), Wave periods (T) and water depths (d). It was observed that reflection coefficient increased with increase in the wave steepness (Hi/gT2) and decreased with increase in depth parameter (d/gT2) and hs/d (Height of structure including rubble base/depth of water). The loss coefficient decreased with increase in the wave steepness and increased with increase in depth parameter and hs/d.

도시 소하천 합류부 수심변화에 대한 실험연구 (Experimental Study on the Depth-Variations of Confluence Area in Small Urban Channel)

  • 심기오;이길춘
    • 물과 미래
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    • 제28권3호
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    • pp.197-204
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    • 1995
  • 인구의 도시집중으로 인하여 유역의 유출용적이 증대하며 이로 인한 합류부의 수위상승으로 내수배제가 불가능하게 되어 침수피해가 발생하고 있다. 본 실험연구에서는 소유역 하천에서 우수거의 합류로 인한 본류하천의 흐름변화를 실험하였으며, 하천의 수위상승을 소하천(본류)의 유량과 경사, 우수거(지류)의 유량과 경사 및 합류각에 따른 본류의 수위상승을 분석하였다. 실험결과 본류하천의 경사에 대해서는 경사가 급할수록 수심비가 증대하는 것으로 나타났으며, 본류의 유량은 적을수록, 지류의 유량은 많을 수록 수심비는 크게 나타났다. 합류각에 대해서는 합류각이 작을수록 수심비가 작은값을 나타내고 있다. 이와 같이 도시 소하천의 합류시 수심비의 상승영향을 보면 합류각, 지류유량 및 본류유량 등의 순으로 상승영향이 밀접하게 나타났다.

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Effects of Lower Dietary Lysine and Energy Content on Carcass Characteristics and Meat Quality in Growing-finishing Pigs

  • Zhang, Jinxiao;Yin, Jingdong;Zhou, Xuan;Li, Fengna;Ni, Jianjun;Dong, Bing
    • Asian-Australasian Journal of Animal Sciences
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    • 제21권12호
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    • pp.1785-1793
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    • 2008
  • Fifty-four PIC barrows were used to evaluate the effects of lower dietary lysine content and energy level on carcass characteristics and meat quality in slaughter pigs. Pigs were allotted to one of three treatments by body weight with six replicate pens in each treatment. The dietary treatments for body weights of 20-50 kg, 50-80 kg and 80-90 kg were as follows, respectively: control diet (digestible energy 14.22 MJ/kg, lysine/DE 0.67 g/MJ, 0.53 g/MJ and 0.42 g/MJ); a low lysine group (digestible energy 14.22 MJ/kg, lysine/DE 0.49, 0.38 and 0.30 g/MJ); and a low lysine-low energy group or low nutrient group (digestible energy 13.11 MJ/kg, lysine/DE 0.49, 0.38 and 0.30 g/MJ). The daily weight gain, daily feed intake and feed efficiency were calculated in the overall growth period (nearly 12 weeks). Meanwhile, carcass characteristics and meat quality were evaluated at 60 and 90 kg body weight respectively. During the overall growth trial, lowering dietary lysine and nutrient level both decreased weight gain (p<0.05) and feed efficiency (p<0.01). At 60 kg body weight, decreasing dietary lysine and nutrient level noticeably decreased dressing percentage (p<0.01) and back fat depth at last rib of PIC pigs (p<0.01), but enhanced marbling scores (p<0.10), intramuscular fat content (p<0.10) and water loss rate (p<0.01) of the longissimus dorsi muscle. At 90 kg body weight, lean percentage (p<0.01) was evidently reduced by both lowering lysine content and nutrient level in the diet. However, the shoulder back fat depth (p<0.05) and marbling scores of the loin eye muscle (p<0.05) were increased; Lowering dietary nutrient level could improve back fat depth of 10th rib (p<0.01) and last rib (p<0.01), intramuscular fat content (p<0.10), redness (p<0.01) and water loss rate of the loin eye muscle (p<0.05), but decrease loin area (p<0.05). Finally, when comparing the 60 kg and 90 kg slaughter weights, it was found that the shoulder back fat depth (p<0.01, p<0.10), 6th-7th rib (p<0.01, p<0.01), 10th-rib (p<0.01, p<0.01) and last rib back fat depth (p<0.01, p<0.01) of the low lysine and low nutrient group were all obviously increased comparing with the control group. Taken together, the results showed that decreasing dietary lysine content and nutrient level increased intramuscular fat content and water loss rate of longissimus dorsi muscle; On the other hand, both lowering dietary lysine and nutrient level markedly compensated to increase back fat deposition in the later finishing period (body weight from 60 to 90 kg) in contrast to the control group.

춘계 베링해 알류산 해분의 해양환경 특성 (Characteristics of the Oceanographic Environment in the Aleutian Basin of the Bering Sea during Spring)

  • 최석관;오택윤
    • 한국수산과학회지
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    • 제46권2호
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    • pp.201-215
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    • 2013
  • The characteristics of the oceanographic environment in the Aleutian Basin of the Bering Sea during spring in 1996, 1997, and 1999 were clarified. An investigation of the water properties revealed five basic layers in the Bering Sea during spring: (1) a surface layer of warm and low-salinity water induced by solar heating, (2) a subsurface layer of cold and low-salinity water propagated slowly by heat from the surface layer, (3) a thermocline layer where salinity was constant but temperature sharply decreased, (4) a temperature inversion layer, and (5) a deep layer with a gradual decrease in temperature and increase in salinity toward the bottom. The ranges of water temperature and salinity were $1.8-5.5^{\circ}C$ and 31.81-34.08 in 1996, $1.5-7.2^{\circ}C$ and 31.9-34.06 in 1997, and $0.5-5.6^{\circ}C$ and 32.0-34.11 in 1999, respectively. The water temperature of the surface layer was approximately $1.6^{\circ}C$ higher in 1997 than in 1996 and 1999. The lowest temperature at a depth of 100-150 m was about $1^{\circ}C$ lower in 1999 than in 1996 and 1997. Nutrient levels (nitrate, phosphate, and silicate) contributing to the control of the growth of phytoplankton were higher in the Aleutian Basin than in the eastern continental shelf and Bogoslof Island area. This was closely associated with the phytoplankton distribution. Nutrient concentrations were lowest at a depth of 25 m. The high primary production at that depth was confirmed from the vertical distribution of chlorophyll a. Chlorophyll a levels were above $4.0{\mu}L^{-1}$ in some areas in 1996 and 1999, but below $2.0{\mu}L^{-1}$ in most areas in 1997. Zooplankton density was about three times higher in 1999 than in 1997.

Field Measurements of Wave Directionality in Water of Finite Depth

  • Memos, Constantine;Ziros, Athanassios
    • Ocean and Polar Research
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    • 제25권4호
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    • pp.437-446
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    • 2003
  • Field measurements of directional waves were carried out during the summer of 2002 at two coastal sites in water of finite depth. A couple of general purpose instruments were used employing acoustic Doppler technology. The aim of the study was to investigate the spatial behavior of the directional movement of waves as they come ashore. In total,74 tests were carried out during which sea states of low to moderate intensity were recorded. A great number of these runs displayed bimodal characteristics of the spreading function at high frequencies. It was found that in general, the frequency-integrated directional width tends to broaden as the water shoals and when refraction effects are negligible. This is attributed to wave-wave interactions that become pronounced in shallow water. The same directional width showed, also, a tendency to increase with increasing peak frequency of the sea state spectrum. The behavior of the kurtosis of the spreading function was also examined. It was found that for higher frequencies this index tends to increase in wave spectra above a certain sea severity threshold.

초고압수에 의한 화강석절삭에 대한 연구 (A study on the slot cutting in granite by high speed water jet)

  • 선우춘;최병희
    • 터널과지하공간
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    • 제4권2호
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    • pp.92-101
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    • 1994
  • Water jet has been employed in extraacton of minerals for many years but the applications of low pressure jent s ar emodfined to some fields. With increasing strength of equipment it is possible to consider the use of high speed water jets for cutting hard rock. The high speed water jet technology is applied to various engineering fiels such as precessing rocks, quarrying rocks, mechanical fracturing as wel as rock excavation under the sea. For slot cutting in rocks with high speed water jets it is necessary to establish the empirical formula for estiamation of the cutting depth. The cutting depth is influenced by cutting parameters such as driving pressure, traverse speed, standoff distance, and shape and diameter of nozzel. Tests were carried out with a variety of cutting parameters on three types of granite. Nozzle pressures ranged from 1,200 to 2,800 bar, traverse speeds from 0.45 to 10.38 cm/min, standoff distances from 4.5 to 13.5 mm, and three types of nozzle diameter were used.

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A Derivation of Aerosol Optical Depth Estimates from Direct Normal Irradiance Measurements

  • Yun Gon Lee;Chang Ki Kim
    • 신재생에너지
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    • 제20권1호
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    • pp.79-87
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    • 2024
  • This study introduces a method for estimating Aerosol Optical Depth (AOD) using Broadband Aerosol Optical Depth (BAOD) derived from direct normal irradiance and meteorological factors observed between 2016 and 2017. Through correlation analyses between BAOD and atmospheric components such as Rayleigh scattering, water vapor, and tropospheric nitrogen dioxide, significant relationships were identified, enabling accurate AOD estimation. The methodology demonstrated high correlation coefficients and low Root Mean Square Errors (RMSE) compared to actual AOD500 measurements, indicating that the attenuation effects of water vapor and the direct impact of tropospheric nitrogen dioxide concentration are crucial for precise aerosol optical depth estimation. The application of BAOD for estimating AOD500 across various time scales-hourly, daily, and monthly-showed the approach's robustness in understanding aerosol distributions and their optical properties, with a high coefficient of determination (0.96) for monthly average AOD500 estimates. This study simplifies the aerosol monitoring process and enhances the accuracy and reliability of AOD estimations, offering valuable insights into aerosol research and its implications for climate modeling and air quality assessment. The findings underscore the viability of using BAOD as a surrogate for direct AOD500 measurements, presenting a promising avenue for more accessible and accurate aerosol monitoring practices, crucial for improving our understanding of aerosol dynamics and their environmental impacts.

홍제천 정비를 위한 하천유지유량 확보 및 수질개선 방안 연구 (Study on the Management of Minimum Low Flow and Water Quality of Hongjechun)

  • 황병기;호종광;오경석
    • 환경영향평가
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    • 제14권1호
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    • pp.37-46
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    • 2005
  • In this study, field surveys were performed for 12 stations in main stream of Hongjechun and 3 stations in 2 tributaries, respectively, in order to find out dried reaches of the stream, and to examine the water quality of the stream, and to suggest methods to improve the stream concerned into eco-stream. In the results of water quality in stream, however distinct difference for seasonal variation of the water quality was not found, the water quality of winter was relatively better than that of other seasons. Annual mean concentration of BOD was 6.5mg/L in the upper reach, 11.8mg/L in the middle reach, 15.3mg/L in the lower reach of main stream, and total mean was 12.5mg/L, while the BOD concentration was 3.6mg/L in the upper reach, and was 9.6mg/L in the low reach of Gukichun, the tributary. Based on flow examination, the level of water depth was so low and the flow can not be traveled downstream in the reach between ST-9 and ST-10 for low water season, whereas it was observed that the flow was traveling except the dry season even the water level was lower than that of adjacent stations.

Application of Percentile Rainfall Event for Analysis of Infiltration Facilities used by Prior Consultation for LID (Low Impact Development)

  • Kwon, Kyung-Ho;Song, Hye-Jin
    • KIEAE Journal
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    • 제15권5호
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    • pp.5-12
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    • 2015
  • Purpose: Retention and infiltration of small and frequently-occurring rainfall by LID facilities account for a large proportion of the annual precipitation volume. Based on 4 standard facilities such as Porous Pavement, Infiltration Trench, Cylindrical Infiltration Well, Rectangular Infiltration Well by Seoul Metropolitan Handbook of the Prior Consultation for LID. The total retention volume of each facility was calculated according to the type and size. The Purpose of this study is to find out the quantitative relationship between Percentile Rainfall Event and Design Volume of Infiltration Facilities. Methode: For the estimation of Percentile Rainfall Event, Daily Precipitation of Seoul from 2005 to 2014 was sorted ascending and the distribution of percentile was estimated by PERCENTILE spreadsheet function. The managed Rainfall Depth and Percentile of each facility was calculated at the several sizes. In response to the rainwater charge volume of 5.5mm/hr by the Category "Private large site", the 3 types of facilities were planned for example. The calculated Rainfall Depth and Percentile were 54.4mm and 90% by the use of developed Calculation-Module based on the Spreadsheet program. Result: With this Module the existing Designed Infiltration volume which was introduced from Japan was simply converted to the Percentile-Rainfall-Event used in USA.

수심에 따른 득량만 키조개 어장의 환경특성 (Environmental Characteristics According to the Depth in Deukryang Bay , Culturing Ground of Pen Shell ( Atrina Pectinata ))

  • 최용규
    • 수산해양기술연구
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    • 제31권2호
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    • pp.127-141
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    • 1995
  • 득량만의 키조개 어장의 해양 환경을 알아보기 위하여 1994년 7월 12일(대조기)과 19일(소조기)에 걸쳐 득량만의 수형 분포 특성을 조사하였다. 득량만은 관측 기간중에 대조기와 소조기에 따른 빛의 연직감쇠계수(k)가 0.6인 곳을 경계로 하여 3개 해역으로 구분될 수 있었다. 조석 주기에 따른 k가 0.6인 등치선의 변화는 대조기에는 약 10m인 등수심선, 소조기에는 약 5m인 등수심선과 유사하게 분포하였다. 따라서 득량만의 수심 약 5~10m인 해역은 조석 주기에 따라서 수형의 특성이 뚜렷하게 바뀌는 수역이라고 할 수 있다. 즉, 수심 약 5~10m인 만 중앙 해역은 T-S diagram에서 대조기때는 수심이 얕은 해역의 수형군에 가까이 분포하고, 소조기때에는 수심이 깊은 수형군에 가까이 분포하였다. 그리고 성층 정도를 나타내는 변수인 log 하(10)(H/U 상(3))의 값은 수심 5m와 10인 등수심선에서 약 2.1~2.2의 값을 나타내었다. 특히, 본 연구 기간인 1994년 7월 동안은 혹서와 갈수로 인하여 예년치보다도 기온은 약 2$^{\circ}C$이상 높았으며, 강수량은 예년치보다도 훨씬 낮은 음의 값을 나타내었다. 이러한 영향으로 인하여 득량만의 수괴의 밀도는 관측 기간동안 주로 수온에 의해서 결정되고 있었다. 앞으로는 기상 자료 및 득량만에서의 과거 누년자료를 분석하여, 이상(abnormal) 고수온년에 대한 만내의 물리적인 변동, 조류와 해저 지형에 기인한 내부파의 형성이나 연속 관측에 의한 급조등에 관한 연구도 필요하리라 생각된다.

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