• The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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• v.17 no.1
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• pp.16-24
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• 2012

To study the seasonal pattern of sediment distribution and the transport tendency in Haeundae nearshore area; i) the grain size texture of surface sediment was examined in June, October, and December of 2007, and March and June of 2008, and secondary, ii) the transport tendency was studied by using a two-dimensional sediment transport model of Gao and Collins (1992), and finally, iii) the bathymetric changes were analyzed by using the data collected in February, May, August, and December of 2007 by Haeundae District Office. Spatial distribution of sediment texture, the tendency of sediment transport as well as the bathymetric change showed significant seasonal variations. From June to December of 2007, the eastern part of the Haeundae area, off Dalmaji Hill showed the coarsening of mean grain size with a prominent transport tendency toward the Haeundae beach. On the contrary, the western part of the area, off Dongbaek Island showed a fining trend of mean grain size, and the transport tendency toward the beach was relatively weakened. From December of 2007 to June of 2008, the mean grain size of Mipo Harbor became finer, and the transport tendency toward the central beach decreased. The mean grain size of Dongbaek Island became coarser, while the tendency increased in the direction of the beach. The areas of significant net accumulation and erosion were depicted based on the bathymetric changes between observation periods. During the period of February to May of 2007, net accumulation was observed on the eastern part of the study area, in front of Mipo Harbor. Erosion was generally occurred throughout the area from May to August of 2007. From August to December of 2007, erosion and accumulation was observed off Mipo Harbor and Dongbaek Island, respectively. The change of sediment facies also suggests the accumulation on the eastern coast during the spring, erosion around the entire coast during the summer, and accumulation on the western coast during the winter. The changes in the accumulation and erosion were most apparent during the summer when several typhoons have passed by, while unnoticeable during the spring.

• KSBB Journal
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• v.14 no.3
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• pp.328-336
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• 1999

A green microalga, Chlorella vulgaris UTX 259, was cultivated in a bench-scale raceway pond. During the culture, 15%(v/v) $CO_2$ was supplied and industrial wastewater discharged from a steel-making plant was used as a culture medium. In a small scale culture bottle, the microalga grew up to 1.8 g $dm^{-3}$ of cell concentration and ammonia was completely removed from the wastewater with an yield coefficient of 25.7 g dry cell weight $g^{-1}\;NH_3-N$. During the bottle-culture, microalga was dominant over heterotrophic microorganisms in the culture medium. Therefore, the amount of carbon dioxide fixation could be estimated from the change of dry cell weight. In a semi-continuous operation of raceway pond with intermittent lighting (12 h light and 12 h dark), increase of dilution rate resulted in increase of the ammonia removal rate as well as the $CO_2$ fixation rate but the ammonia removal efficiency decreased. Ammonia was not completely removed from the medium (wastewater) of raceway pond which was operated in a batch mode under a light intensity up to 20 klux. The incomplete removal of ammonia was believed due to insufficient light supply. A mathematical model, capable of predicting experimental data, was developed in order to simulate the performance of the raceway pond under the light intensity of sun during a bright daytime. Simulation results showed that the rates of $CO_2$ fixation and ammonia removal could be enhanced by increasing light intensity. According to the simulation, 80 mg $dm^{-3}$ of ammonia in the medium could be completely removed if the light intensity was over 60 klux with a continuous lighting. Under the optimal operating condition determined by the simulation, the rates of carbon dioxide fixation and ammonia removal in the outdoor operation of raceway pond were estimated as high as $24.7 g m^{-2} day^{-1}$ and $0.52 g NH_3-N m^{-2} day^{-1}$, respectively.

• Journal of Nutrition and Health
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• v.12 no.2
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• pp.1-13
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• 1979

성장발육하는 시기에 영양과 성장하는 아동들의 체위와는 밀접한 관계가 있고 또한 영양부족과 그로 말미암아 자라나는 이학적 소견과도 불가분의 관계가 있기 때문에 그동안 우리나라에서 부분적, 단편적으로 연구 발표된 문헌을 중심으로 그를 검토 고찰하여 보았다. 그 결과를 요약하면 다음과 같다. 우리나라 아동들이 출생후 6개월까지는 주로 모유에 의존하고, 약간이 인공영양에 의존하고 있는데, 이 시기에는 다른 선진제국의 어린이들의 성장발육과의 별 차이가 없었다. 그러나 이유기인 $6{\sim}30$개월 사이에는 우리나라 어머니들의 이유에 대한 지식이 빈약하고 이들 음식물을 그대로 아기들에게 적용하기 힘든 이유등으로 아이들에게 보급해서 주는 음식물이 빈약함으로 말미암아 다른 선진제국 아이들에 비해서 이 시기에 체위가 많이 떨어지고 빈혈현상을 나타내는 것을 볼 수 있다. 이때 고양군에서 농민의 아동들에 대해서 시행한 영양조사 내용을 보면, 전체 칼로리도 부족되고 특히 단백질, 철분, 칼슘, 비타민 A, B복합제가 전반적으로 부족되는 것을 알았다. 이는 어머니들의 육아와 이유식에 대한 지식의 결집도 중요한 역할을 했겠거니와 더욱더 중요한것은 우리나라 어른들의 식습관이, 민족적 전통적으로 짜고, 매웁고, 딱딱해서 이를 아기들에게 그대로 적응해서 먹이기가 힘든 것도 더 중요한 이유가 된다. 어른들을 위한 음식물에도 맵지 않고, 짜지 않으며, 아기들도 즐겨 먹을 수 있는 유동식 혹은 반유동식으로 된 영양가치가 좋은 음식물을 발전시켜 애용하도록 하는 것이 민족적인 긴급한 과제라고 하겠다. 그렇지 않으면 선진제국 모양으로 이유기에 있는 아이들을 위해서 아이들이 즐겨 먹을 수 있는 이유식을 크게 발전시켜서 이유기의 아이들에게 저렴하게 공급할 수 있는 생산공장과 제도의 마련이 긴급하다고 하겠다. 우리 민족의 체위를 향상 시키는데 영양학자와 영양사들에게 기대 하는 바가 크다. 육아하는 어머니의 교육정도와경제적인 면이 아기 체위에 주는 영향에 대한 연구에서는 교육정도가 높고, 경제적으로 좋은 위치에 있는 엄마가, 교육정도가 낮고 경제적으로 가난한 위치에 있는 어머니보다 아이들 체위에 훨씬 좋게 기를 수 있다는 것을 알았다. 특히 이유기에 들어간 6개월 이후에 체위 격차가 심한 것을 볼 때 보충해 주는 음식물의 적절한 보급이 얼마나 필요한가를 말해 주는 것이며 이에는 어머니의 교양과 열의와 경제적 뒷받침이 얼마나 필요하다는 것을 말해주는 것이다. 지역별로 서울에서 부유층 가정과 학교 아동, 농촌 지역 가정과 학교아동, 강원도 산간지역 가정과 학교 아등으로 나누어서 자라나는 아동들의 체위와 이학적 소친을 연구 조사한 바로는 서울 부유층이 제일 좋고 그 다음이 서울 빈한층, 강원도 산간지역 아동의 순으로 좋았으며 농촌지역 아종은 체위가 가장 떨어졌다. 구각증, 구내염등은 강원도 산간지역 아동에 제일 많고, 다음이 농촌지역, 서울 판자촌지역의 순으로 많으며 서울부유충지역이 가장 적어서 이는 산간일수록 또 는 빈한할수록 등물성단백질이 부족되는 것을 말해 주는 것이다. 지역별 혈색소치는 109gm/100ml 이하인 경우가 서울 빈한층가정 아동에 제일 많아서 51.7%나 되며 다음이 산간지역가정, 농촌지역가정의 순으로 많으며 서울부유층가정 아동은 2.2%에 지나지 않는다. 한국아등의 체위와 일본아동의 체위를 비교해 본 바로는 출생 후 약 12개월까지는 별차가 없지만 그후로는 점차로 그 격차가 심해져서 $12{\sim}15$세 사이에 평균체중면에서 5kg정도, 신장면에서 5cm정도의 큰 격차를 나타냈다. 그러나 그후로 성인이 되어감에 따라서 그 격차는 좁아졌다. 이는 일본국이 경제적으로 우리보다 우위에 있음에 따라서 아이들 성장에 필요한 영양분을 적기에 적당하게 공급해 주었기 때문이며 우리는 많은아이들이 가만하기 때문에 그 나이에 맞는 영양분 보급을 적당히 하지 못한 결과로 생각할 수 밖에 없다. 한국 아동의 발육표준치를 1965년초에 측정한 것과 1975년도에 측정한 것을 비교해 본 결과 1975년 치는 1965년도치에 비해 체중과 신장 면에서 상당히 증가하였다. 이는 우리라라 경제상태가 좋아지면서 굶는 아이들이 적어지거나 없어졌을 뿐만 아니라 식품 내용이 개선된 때문으로 해석된다. 따라서 민족의 체위가 개선되고 향상되려면 제일 먼저 해결되어야 할 문제는 국가의 경제력이 향상될뿐만 아니라 빈부의 격차가 적어져서 우리나라에 생을 받은 사람은 누구나 굶는 자가 없이 균형 있는 영양분을 충분히 섭취 할 수 있는기회를 갖도록 되어야 하겠다. 영양학자와 식품관리자들은 우러나라 아이들이 타고난 체위의 잠재성을 충분히 키우기 위해서 어떠한 음식물이 얼마나 필요한지 계산하여 이를 작물로 충분히 충당할 수 있도륵 계획해서 농수산물을 생산하도록 해야겠다. 영양학자들은 우리 민족의 음식물을 개선해서 아기들이 즐겨 먹을 수 있는 어른들의 음식물, 영양식을 발전시켜 이유기에 받는 우리 어린아기들의 수난을 조속히 극복하는 것이 바람직하다. 또한 영양에 대한 교육을 국민학교, 중학교 교과과정에 많이 넣어서 교육하고 영양에 대한 교육과 보급을 조직적으로, 신문, 라디오, 텔레비젼등을 통해서 성인교육을 강화해서 모든 국민들이 적은 돈을 가지고도 보다 나은 영양물을 구해서 섭취할 수 있는 지혜를 가지도록 해야겠다. 국민학교 재학중 및 졸업시기를 전후딘서 체위가 많이 떨어지며 그 영향이 일생동안 간다는 것을 감안할 때 국민학교에서 점심 한끼라도 영양식을 보급해서 우리 국민체위 향상을 위해서 나라에서 직접적으로 공헌하는 바가 있었으면 한다.

• Conservation Science in Museum
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• v.22
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• pp.41-52
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• 2019

Inner walls of the stone chamber of West Ancient Tomb No. 1 and 2 in Neungsan-ri, Buyeo-gun have been inspected for possible trace of murals. Tomb No.1 has a rough surface finish of the stone wall and no traces of murals was observed in any part of the stone walls except the ceiling part of the main chamber. On the ceiling surface, there is black colored area, which showed same visual characteristics for both the surface and interior upon slight scratch of the surface, suggesting that it may not be a painted layer. In addition, this black material is not artificial stuff like black ink but is confirmed as biotite from X-ray diffraction analysis that is one of the constituents of the stone wall. In case of tomb No. 2, white material, that is confirmed as lime(calcite, CaCO3) by X-ray diffraction analysis, was observed on the wall surface of the east, west and north, suggesting possible existence of murals. The lime layers, however, are located mostly on the entrance of east wall of main chamber and the place of passage whereas they are observed only in lower parts on the other walls. It may have been formed by the inflow of soil and lime from the outside as the form of the lime layer in the east wall corresponds to the traces of soil and lime deposited from the thief pit. Furthermore, the filling material found in the gap between the stone slabs of the four directions and the ceiling was confirmed as clay soil, which is different material from the lime present on the stone wall surface. If the lime layer had been artificially constructed for the purpose of creating murals, it would have been more reasonable to use lime as well in the gap between the stone slabs of the four directions and ceiling. In this regard, we conclude that there are no murals in the Tomb No. 2 in the Neungsan-ri.

• The Korean Journal of Quaternary Research
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• v.16 no.1
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• pp.1-16
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• 2002

A total of 4 muddy sediment samples collected from the Central Yellow Sea were analyzed for chemical composition. The results are compared with the previously published Huanghe, Changjiang and Keum River geochemical data in order to understand provenance and sedimentation of fine-grained mud, and the sediment accumulation rates estimated. The sandy sediment facies is distributed in the eastern area, a patch of fine-grained mud exists in the western central prat, and the sandy mud and clay sedimentary facies shot. north to south zonal distribution in the central region. The content of calcium carbonate ranges from 2.8 to 10.5%, and its distributional trends to be more concentrated on the western muddy sediments near toward the China side rather than on the eastern sandy sediments. The accumulation rates obtained using Pb-210 geochronologies for the muddy sediments in the Central Yellow Sea showed ranges from 0.21 to 0.68 cm/yr or 0.176 to 0.714 g/$\textrm{cm}^2$. yr. The sedimentation rate from core CY96010 located in the eastern near side of Shandong Peninsula which is affected by the Huanghe River shows 0.68 cm/yr or 0.714 g/$\textrm{cm}^2$ . yr. The sediment cores CY96008 and CY96002 in the Central Yellow Sea, the estimated of sediment accumulation rates shows 0.21~0.23cm1yr or 0.176~0.220 9/$\textrm{cm}^2$.Vr respectively, which are much lower than above samples. These indicate that the muddy sediments in central area of the Yellow Sea may have received influence of the sediment discharge from the Huanghe River. The concentrations of Ca, Na, Sr, Ho, La, Tb, Ta and Ca/Ti ratio of the muddy sediments in the Central Yellow Sea are higher than those of the Changjiang sediments and lower than those of the Huanghe sediments. However, these element values showed similar concentration patterns than those of the Huanghe sediment. The element contents such as Fe, Ti, Nl, Co, Cr, Cu, Pb, Sc, Ce, Nd, Sm, Eu, Cd and Dy in the study area are higher than those of the Huanghe sediments and lower than the Changjiang River sediments, but these values showed close to resemblance content trends those of the Changjiang sediment. The concentration of Mn, K and Sr in sediments of the study area are similar to those of the Keum River and eastern Yellow Sea sediment. They are rich in Zn, Rb, Cd, U, Cs and Li than those of the other comparison legions. Therefore, the terrigenous materials sources of the muddy sediment in the Central Yellow Sea comes mainly from Huanghe River in the past and present, and also have party derived from the Changjiang and Keum River, while the biological deposit in this area are carried by the Yellow Sea Warm Current.

• The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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• v.20 no.1
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• pp.43-52
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• 2015

The growth and population dynamics of eelgrass (Zostera marina) due to changes in sediment composition were examined in the lower intertidal zone of the Seomjin Estuary, Korea. We surveyed environmental factors such as water temperature, underwater irradiance, main types and organic content of sediment, tidal exposure, and nutrient concentrations in the water column and sediment pore water, in relation to the shoot density, biomass, morphological characteristics, and growth of Z. marina inhabiting lower intertidal zones. The survey was conducted monthly from May to December of 2004 and 2009. The water temperature showed obvious seasonal trends in both study years. Underwater irradiance was significantly higher in 2009 than in 2004. Tidal exposure was not significantly different between 2004 and 2009. The sediment was muddy-sand in 2004 but became sandy and with a significantly lower organic content in 2009. Water column $NH_4{^+}$ concentrations were significantly higher in 2004 than in 2009. Sediment pore water $NO_3{^-}+NO_2{^-}$ concentrations were significantly higher in 2009 than in 2004. Other nutrient concentrations did not differ significantly between 2004 and 2009. Morphological characteristics, including eelgrass length and leaf width were significantly lower in 2009 than in 2004. Eelgrass shoot height, leaf length, and sheath length showed typical seasonal patterns, increasing in early summer and decreasing in autumn, in both years. Vegetative shoot density was not significantly different between 2004 and 2009, while the biomass of individual plant parts and the total biomass were significantly lower in 2009. Eelgrass leaf productivity did not differ between years, but leaf turnover time was significantly shorter in 2009 than in 2004. Eelgrass downsizing and decreased turnover time in 2009 compared to 2004 indicate more effective adaptations to the stress of long-term changes in sediment composition. Overall, results suggest that changes in sediment composition can be a limiting factor for seagrass growth in the intertidal zone.

• Korean Journal of Ecology and Environment
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• v.48 no.4
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• pp.219-228
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• 2015

To secure water resources, dams are normally constructed on the upper - middle part of streams, and it generates physical disturbances such as habitat alteration and stream fragmentation. Such construction can restrict movement of aquatic organisms, especially for freshwater fish which is one of top predator in aquatic ecosystem, and cause genetic fragmentation and community change. In this study, to investigate impact of habitat alteration after dam construction on freshwater fish, we monitored fish community changes, and compared fish fauna between dam reservoir and inflows. Additionally, movement characteristics and habitat boundaries of four species were identified by radio telemetry method. The study was conducted in the Gunwi Dam which was constructed in December 2010. Radio telemetry was applied to Pungtungia herzi, Zacco platypus (living lotic and lentic), Silurus asotus (lentic preferred species) and Zacco koreanus (lotic preferred species). The number of species was remarkably decreased (4 family, 10 species) comparing with before the dam construction (7 family, 15 species). Specifically, Coreoleuciscus splendidus, Niwaella multifasciata, Liobagrus mediadiposalis, Coreoperca herzi and Odontobutis platycephala that inhabit in the lotic environment were not collected in the study area. A total of 8 species were caught in both the dam reservoir and tributaries except 2 species (C. auratus and S. asotus). Sorenson's similarity between the reservoir and its tributaries was high (0.842). All of the radio tagged species stayed in the reservoir except S. asotus which moved to the tributary. These species mainly utilized the shallow littoral zone as a habitat. These results could be useful as a baseline data for efficient management of fishes in lakes.

• Korean Journal of Agricultural and Forest Meteorology
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• v.9 no.1
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• pp.1-16
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• 2007

The use of information on natural resources is indispensable to most agricultural activities to avoid disasters, to improve input efficiency, and to increase lam income. Most information is prepared and managed at a spatial scale called the "Hydrologic Unit" (HU), which means watershed or small river basin, because virtually every environmental problem can be handled best within a single HU. South Korea consists of 840 such watersheds and, while other watershed-specific information is routinely managed by government organizations, there are none responsible for agricultural weather and climate. A joint research team of Kyung Hee University and the Agriculture, forestry and Fisheries Information Service has begun a 4-year project funded by the Ministry of Agriculture and forestry to establish a watershed-specific agricultural weather information service based on "high definition" digital climate maps (HD-DCMs) utilizing the state of the art geospatial climatological technology. For example, a daily minimum temperature model simulating the thermodynamic nature of cold air with the aid of raster GIS and microwave temperature profiling will quantify effects of cold air drainage on local temperature. By using these techniques and 30-year (1971-2000) synoptic observations, gridded climate data including temperature, solar irradiance, and precipitation will be prepared for each watershed at a 30m spacing. Together with the climatological normals, there will be 3-hourly near-real time meterological mapping using the Korea Meteorological Administration's digital forecasting products which are prepared at a 5 km by 5 km resolution. Resulting HD-DCM database and operational technology will be transferred to local governments, and they will be responsible for routine operations and applications in their region. This paper describes the project in detail and demonstrates some of the interim results.

• Korean Journal of Weed Science
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• v.15 no.4
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• pp.289-297
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• 1995

Field experiments were conducted to evaluate the competitive characteristics of weeds with direct-seeded rice. In both dry- and water-seeded rice a weeds) started to grow over the plant height of rice from 45 days after seeding, and there was a great difference in plant height between rice and weeds from 75 days after seeding. Dry weights of weeds drastically increased from 30 days after seeding in both dry- and water-seeded rice, and the increase of dry weight was faster in dry-seeded rice than in water-seeded rice with time. Although weeds competed with rice at earlier growth stages, they did not reduce rice yields and its components until competition period of 75 days after seeding. Required period of weed free at the beginning of the season was 30 to 45 days from seeding in order to avoid any yield loss. The numbers of panicle per plant, spikelets per panicle, grain weight and yield of rice in dry-seeded rice had highly negative correlations with the growth ratios of Echinochloa crus-galli, Ludwigia prostrata, Cyperus difformis, Bidens frondosa, and Cyperus serotinus. In water-seeded rice, the number of plants, panicle per plant, spikelets per panicle and yield had highly negative correlations with growth rate of Echinochloa crus-galli, but the percentage of filled spikelet had negative correlation with Cyperus difformis. Research indicated that in direct-seeded rice weed competition with rice started from 30 days after seeding and significant yield loss by weed competition occurred from 75 days after seeding.

• The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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• v.6 no.3
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• pp.126-134
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• 2001

Several angular sandstone fragments (about 7 cm in longest diameter) occur in two piston cores, obtained from the submarine trough in the northeastern part of Korea Strait. The origin of the sandstone fragments and the paleoenvironment of trough sediment could be suggested from sedimentary facies analysis of cores and identification of ostracod within sandstone fragments. Echo characteristics around two core sites in submarine trough represent the prolonged bottom echoes with diffuse or no subbottom reflectors. The cores consist of a lower bioturbated mud and an upper gravelly sand sediments with sandstone/shell fragments. The bioturbated mud sediments show low water contents (27-44%) and high shear strength (19.2->37 kPa) compared with those of Holocene sediments (60-219% and 1.0-2.7 kPa, respectively) in the inner shelf and continental slope. However, clay contents (48-56%) of the bioturbated mud sediments are similar to those of fluviatile Holocene sediments in the inner shelf. The mean grain size of gravelly sand sediments ranges from 2.3 to 3.0 ${\phi}$ and shows coarsening upward with sandstone/shell fragments. The Holocene palimpsest in the continental shelf are composed of muddy sand sediments or sandy mud sediments (mean grain size: 4.6-7.6 ${\phi}$). Those suggest that two core sediments might be formed from Paleofluvial and paleocoastal deposits during sea-level lowstand. However, sandstone fragments mainly consist of quartz grains and bioclasts, with carbonate matrix, hollow pore, and glauconite. Two extinct ostracod species, Normanicythere sp. and Kotoracythere sp., are recovered in the sand-stone fragments of core EP-7, and they continued to exist from late Pliocene to early Pleistocene in cold water environment of this area. Thus, the sandstone fragments are interpreted to be formed at the paleocoastal environment derived from the Plio-Pleistocene outcrops exposed around the submarine trough during the LGM (Last Glacial Maximum) period.