• Title/Summary/Keyword: 표층

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Analysis of Surface Current Measurement Based on X-band Radar Image (X-밴드 레이더 이미지 기반 표층해류 계측 분석)

  • Na-Yun Kang;Yu-Kyung Lee;Young-Jun Yang
    • Proceedings of the Korean Institute of Navigation and Port Research Conference
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    • 2022.11a
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    • pp.323-324
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    • 2022
  • This paper explains the comparison results of surface current measurement using X-band Radar image through analysis. Measurements were carried out from February 2022 using the X-band Radar for marin ships installed at Sokcho Beach. Based on the Korea Hydrographic and Oceanographic Agency ocean observation buoys, the accuracy of surface current(current speed) measurement was verified through comparison and analysis of measurement data.

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Introduction of Surface Current Measurement Based on X-band Radar (X-밴드 레이더 기반 표층해류 계측 기법 소개)

  • Na-Yun Kang;Jose Carlos Nieto-Borge;Young-Jun Yang
    • Proceedings of the Korean Institute of Navigation and Port Research Conference
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    • 2022.06a
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    • pp.424-425
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    • 2022
  • This paper introduces X-band radar-based surface current measurement technique. A marine X-band radar used for navigation was installed at Sokcho Beach to collect surface current data in real time. Based on this, in order to verify the accuracy of the measurement of surface current (Current speed), the Korea Hydrographic and Oceanographic Agency Marine observation buoy compared it with the data. Data collected from January 2022 were compared and as a result the possibility of surface current(Current speed) measurement using radar confirmed.

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Distributions of $^{226}Ra$\;and\;^{228}Ra$in the Surface Waters of East Sea of Korea (한국 동해 표층수중 $^{226}Ra$$^{228}Ra$의 농도분포)

  • YANG Han-Soeb;KWON Yeoung-Ann;KIM Gue-Buem;KIM Seong-Soo
    • Korean Journal of Fisheries and Aquatic Sciences
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    • v.25 no.5
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    • pp.399-405
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    • 1992
  • Using $MnO_2-coated$ fiber extraction and gamma counting techniques, we measured the distributions of $^{226}Ra$\;and\;^{228}Ra$ in the surface waters at 14 stations of East Sea of Korea in September, 1988. The concentrations of $^{226}Ra$\;and\;^{228}Ra$ in the surface waters ranged $70-110\;dpm/10^3l$ and 102=232 $dpm/10^3l$, respectively. In general, the concentrations of Ra isotopes were shown higher in the coastal and southern stations than those in the outer and northern stations in our observed area. Also, the concentrations of Ra isotopes in the study area were significantly higher than values in the other area of the East Sea and Kuroshio surface water, but much lower than the concentrations in the surface water of Yellow Sea reported previously. There was an inverse relationship between the $^{226}Ra/^{228}Ra$ ratio and salinity in the surface waters of Kuroshio, Yellow Sea and East Sea of Korea. This indicates that the continental shelf waters such as Yellow Sea and East China Sea are main source of Ra isotopes in surface waters of the East Sea of Korea.

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Change of Organic Rice Yield as Affected by Surface and Broadcast Fertilizer Applications (유기질비료의 표층 및 전층시비에 따른 벼 수량 변화)

  • Kim, Hyun-Woo;Choi, Hyun-Sug;Kim, Byeong-Ho;Kim, Hong-Jae;Choi, Kyeong-Ju;Chung, Doug-Young;Lee, Youn;Park, Kwang-Lai;Jung, Seok-Kyu
    • Korean Journal of Organic Agriculture
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    • v.20 no.1
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    • pp.81-89
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    • 2012
  • This study was investigated to evaluate the effects of fertilizer application of surface and broadcast for rice culture on the soil chemical, physical, and microbial properties as well as growth and yield of rice. The application was made with 'Dongjin 1' rice at Jeollanam-do Agricultural Research & Extension Services from 2008 to 2010. Soil organic matter and cation concentrations were increased by surface and broadcast applications, respectively. Plots treated by surface application tended to be higher seasonal N-mineralization rate in the organic fertilizer and seasonal soil organic matter than those of broadcast application. Soil physical properties seemed to be improved by the broadcast application, and soil microbial properties were increased by the surface application. Surface application increased 5% of rice yield compared to that of broadcast.

Seasonal Variation of Surface Sediments in the Kwangseungri Beach, Gochanggun, Korea (고창군 광승리 해빈 표층 퇴적물의 계절 변화)

  • So, Kwang-Suk;Ryang, Woo-Hun;Choi, Sin-Lee;Kwon, Yi-Kyun
    • Journal of the Korean earth science society
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    • v.33 no.6
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    • pp.497-509
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    • 2012
  • The Gochanggun Kwangseungri macro-tide open-coast beach, located in the southwestern coast of Korea, was investigated in terms of the seasonal variations of surface sediment facies and sedimentary environment. Surface sediments of 45 sites in four seasons (May 2006 - February 2007) were sampled along three survey lines (15 sites in each survey line). The surface sediments of the Kwangseungri Beach are mainly composed of fine-grained sands, and its mean grain size is the coarsest in winter. Mud facies partly exists in summer, whereas it is nearly absent in winter. The spatial distribution of surface sediments shows a coast-parallel band of fine and medium sands during spring, fall, and winter. In the northern part, the study area is dominated by fine sands during summer, whereas by coarse sands during winter. These results can be interpreted that tide is more effective than wave on the surface sediment distribution of the Kwangseungri Beach during the summer season.

Water Column Structure and Dispersal Pattern of Suspended Particulate Matter (SPM) in a floating ice-dominated fjord, Marian Cove, Antarctica during Austral Summer (유빙이 점유한 남극 마리안 소만의 하계기간 수층 구조와 부유물질 분산)

  • Yoo, Kyu-Cheul;Yoon, Hoo-Il;Kang, Cheon-Yun;Kim, Boo-Keun;Oh, Jae-Kyung
    • The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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    • v.5 no.4
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    • pp.295-304
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    • 2000
  • Vertical measurement of CTDT at about 30 min intervals and spatial surface temperature, salinity, and concentration of suspended particulate matters were conducted to elucidate the character of water column and the dispersal pattern in a floating ice-dominated fjord, Marian Cove, West Antarctica. Marian Cove showed two distinct water layers in terms of turbidity; 1) cold, fresh, and turbid surface plume in the upper 2 m,2) warm, saline, and relatively clean Maxwell Bay inflow between 15-45 m in water depth. Thermal melting of Maxwell Bay inflow and tidewater glacier/floating ices developed the surface mixed layer and the activity of floating ices cause Maxwell Bay inflow to be unstable. Due to the unstable water column, the development of Maxwell Bay inflow and subsequent surface plume are not influenced by tidal frequency. Coastal current generated by strong northwesterly wind may extend warm, saline, and turbid surface plume into the central part of the cove along the northern coast via the western coast of Weaver Peninsula. Terrigenous sediments of meltwaters from the glaciated ice cliffs near the corner of tidewater glacier and some coasts enter into the cove and their dispersion depends upon the hydrographic regimes (tide, wind, wave etc.). At the period of spring tide, the strong wind stress with the northwesterly wind direction reserve suspended sediment-fed surface plume and so allow the possibility of deposition of terrigenous sediments within the basin of cove.

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Seasonal Variability of Thermal Structure and Heat Flux in the Juam Reservoir (주암호의 계절별 수온 구조와 열수지 변화)

  • Sun, Youn-Jong;Cho, Cheol;Kim, Byong-Chun;Huh, In-Aa;Yoon, Jun-Heon;Chang, Nam-Ik;Cha, Sung-Sik;Cho, Yang-Ki
    • Korean Journal of Ecology and Environment
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    • v.36 no.3 s.104
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    • pp.277-285
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    • 2003
  • Temperature profiles were observed to understand seasonal variation of thermal structures in the Juam reservoir from March 2000 to May 2001. Heat flux which affects thermal structures was calculated by observed water temperature and meteorological data. Temperature became homogeneous vertically by convection due to the surface cooling in winter. Maximum heat loss through the surface (109.45W/$m^2$) occurred in December. There was a horizontal gradient of water temperature in winter. The temperature was $3^{\circ}C$ at upstream and $5^{\circ}C$ near the dam. The surface temperature increased by the increase of solar radiation in spring and summer. Maximum heat gained through the surface was 101.95 W/$m^2$ in July. Maximum surface temperature was $29^{\circ}C$ in August, whereas the bottom water was $7^{\circ}C.$ Surface mixed layer became thicker and its temperature decreased by surface heat loss in fall and winter.

Effect of the Coated Urea Fertilizer in the Poorly Drained Coarse Textured Paddy Soils (배수 불량한 사질답에서 피복요소비료의 효율적 이용연구)

  • Kwon, Hye-Young;Park, Chang-Young;Lee, Jae-Saeng;Jeon, Won-Tai;Park, Ki-Do;Choi, Jyung
    • Korean Journal of Soil Science and Fertilizer
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    • v.34 no.2
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    • pp.105-109
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    • 2001
  • Poorly drained coarse textured paddy soils has harmful substances(e.g. $Fe^{2+}$, $H_2S$, organic acid etc.) due to reduction condition, and lower soil temperature during early stage of rice crop. The roots of the rice plant usually were distributed in the surface layer, and prone to lodged. To solve the problems, the study was carried out in the typical poorly drained, sandy loam textured paddy soils during 1997-1998. Coated urea and urea fertilizers were applied on the surface and whole layer mixed respectively. Yield of the surface fertilization of coated urea had increasing tendency but not significant. Advantages of this experiment was saving of about 30% of nitrogen fertilizer and top dressing labour, which would reduce possibility of water pollution.

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The Effect of Anticyclonic Eddy on Nutrients and Chlorophyll During Spring and Summer in the Ulleung Basin, East Sea (동해 울릉분지에서 봄과 여름동안 시계방향 와류가 영양염과 엽록소에 미치는 영향)

  • Kim, Dong-Seon;Kim, Kyung-Hee;Shim, Jeong-Hee;Yoo, Sin-Jae
    • The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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    • v.12 no.4
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    • pp.280-286
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    • 2007
  • In order to find out the effects of the anticyclonic eddy on the distribution of nutrients and chlorophyll concentrations in the Ulleung Basin during spring and summer, we measured temperature, salinity, nutrients, and chlorophyll from the surface to 200 m water depth at five stations in July 2005 and April 2006. In spring, surface mixed layer was very deep inside the eddy, about 200 m, but it was relatively shallow outside the eddy, about $20{\sim}60$ m. Inside of the eddy, nutrients in the surface waters were sufficient by supply from the deep layer, whereas outside of the eddy, they were fairly depleted due to the stratification in the surface layer. In spring, chlorophyll concentrations were relatively low inside of the eddy due to the deeper surface mixed layer compared with the euphotic depth, and the depth-integrated chlorophyll concentrations outside of the eddy were twice as much as those inside of the eddy. In summer, nutrients in the surface waters were completely depleted at all stations due to the well stratification in the surface layer. The typical distribution pattern of subsurface chlorophyll maximum was observed at all stations, and the depth-integrated chlorophyll concentrations inside of the eddy were almost twice as much as those outside of the eddy. The anticyclonic eddy appearing in the Ulleung Basin every year significantly affects the phytoplankton biomass, with the opposing effects in spring and summer; in spring, the anticyclonic eddy suppresses phytoplankton growth, but in summer, it enhances the phytoplankton biomass.

A Study on Applicability of Soil Strength for Surface Treatment (표층처리를 위한 현장의 강도적용에 관한 연구)

  • Yang, Tae-Seon;Kim, Byeong-Ho
    • Journal of the Korean Geosynthetics Society
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    • v.4 no.3
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    • pp.45-52
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    • 2005
  • Most marine structures are constructed on very soft soil, soil improvements are needed for the area of road, buildings. In this paper, some considerations of several case studies on soil placement method after geotextile placement, known as surface treatment, are done. Considerations of strength applicability on the advanced construction method of sand and soil placement are proposed in this paper. Typical tensile strength of geotextile used in the surface soil stabilization method is 15t/m, and thickness of sand and soil placement between 1.6m and 3.1m. Undrained shear strength of soft clay layer ranges $0.2{\sim}1.2t/m^2$. In order to minimize the difficulties which include soil disturbance, soft soil gush and overturn of vertical drain installation rig more studies are needed.

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