• 대한토목학회논문집
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• 제1권1호
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• pp.1-8
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• 1981

하구(河口)는 해수(海水)와 담수(淡水)가 만나는 아주 복잡(複雜)한 지점(地點)으로 하구(河口)에서의 염도분포(鹽度分布)에 대한 수리학적(水理學的)인 일반적(一般的)인 해석(解析)은 대단히 어렵기 때문에 본(本) 연구(硏究)에서는 현지관측(現地觀測)을 통(通)하여 염도(鹽度)의 분포특성(分布特性)을 알기 위하여 조차(潮差)가 큰 군산(群山) 외항(外港)부근의 3지점(地點)에서 조석일주기(潮汐一週期)동안 1~1.5시간 간격으로 연속적(連續的)으로 현지관측(現地觀測)을 실시하였으며 분석결과(分析結果) 다음과 같은 몇가지 결론(結論)을 얻었다. 1. 염도(鹽度)와 전기전도도와의 비(比)가 0.5~1.0 사이에 대부분(大部分)이 산만하게 분포(分布)되어 있음이 재확인(再確認)되었다. 2. 염도(鹽度)는 만조시(滿潮時)에 가장 크고 만조(滿潮)에서 간조(干潮)로 됨에 따라 점점 작아져서 간조후(干潮後) 0~2시간(時間) 사이에 가장 작았다. 3. 금강하구(錦江河口)의 밀도류(密度流)는 대체로 강혼합형(强混合型)이었고 유량(流量)이 클 때는 완혼합형(緩混合型)이었다. 4. 연직염도분포(鉛直鹽度分布)에 파고(波高)의 영향은 별(別)로 없었다. 5. 최대연직염도차(最大鉛直鹽度差)는 대체로 10g/l 이하(以下)였으며 최소치(最少値)가 나타나는 시기(時期)는 대조시(大潮時)에는 간조후(干潮後) 0~2시간후(時間後)였고 소조시(小潮時)에는 만조후(滿潮後) 2~3시간(時間) 후(後)에 나타났다.

• Ocean and Polar Research
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• 제37권2호
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• pp.127-140
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• 2015

A continuous series of 60 snow samples was collected at a 2.5-cm interval from a 1.5-m snow pit at a site on the Styx Glacier Plateau in Victoria Land, Antarctica, during the 2011/2012 austral summer season. Various chemical components (${\delta}D$, ${\delta}^{18}O$, $Na^+$, $K^+$, $Mg^{2+}$, $Ca^{2+}$, $Cl^-$, $SO_4{^2-}$, $NO_3{^-}$, $F^-$, $CH_3SO_3{^-}$, $CH_3CO_2{^-}$ and $HCO_2{^-}$) were determined to understand the highly resolved seasonal variations of these species in the coastal atmosphere near the Antarctic Jang Bogo station. Based on vertical profiles of ${\delta}^{18}O$, $NO_3{^-}$and MSA, which showed prominent seasonal changes in concentrations, the snow samples were dated to cover the time period from 2009 austral winter to 2012 austral summer with a mean accumulation rate of $226kgH_2Om^{-2}yr^{-1}$. Our snow profiles show pronounced seasonal variations for all the measured chemical species with a different pattern between different species. The distinctive feature of the occurrence patterns of the seasonal variations is clearly linked to changes in the relative strength of contributions from various natural sources (sea salt spray, volcanoes, crust-derived dust, and marine biogenic activities) during different short-term periods. The results allow us to understand the transport pathways and input mechanisms for each species and provide valuable information that will be useful for investigating long-term (decades to century scale periods) climate and environmental changes that can be deduced from an ice core to be retrieved from the Styx Glacier Plateau in the near future.

• 한국대기환경학회지
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• 제25권4호
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• pp.275-288
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• 2009

The Korean government strengthened the environmental polices to manage and enhance Metropolitan Area air quality, and also has enforced "Special Act on Seoul Metropolitan Air Quality Improvement (SASMAQI)" issued in Dec. 2004. Recently government expanded the Seoul Metropolitan Air Quality Management District (SMAQMD) to the outskirts satellite cities of Seoul area through the "Revised Law Draft of SASMAQI". The SMAQMD has been alloted the allowable emission loads to the local governments on the basis of the carrying $PM_{10}$ capacity. However, in order to establish the effective air quality control strategy for $PM_{10}$, it is necessary to understand the corresponding sources which have a potential to directly impact ambient $PM_{10}$ concentration. To deal with the situations, many receptor methodologies have been developed to identify the origins of pollutants and to determine the contributions of sources of interests. The objective of this study was to extensively identify $PM_{10}$ sources and to estimate their contributions at the metropolitan area. $PM_{10}$ samples were simultaneously collected at the 3 semi-industrialized local cities in the Seoul metropolitan area such as Hwasung-si, Paju-si, and Icheon-si sites from April 15 to May 31, 2007. The samples collected on the teflon membrane filter by one $PM_{10}$ cyclone sampler were analyzed for trace metals and soluble ions and samples on the quartz fiber filter by another sampler were analyzed for OC and EC. Source apportionment study was then performed by using a positive matrix factorization (PMF) receptor model. A total of 6 sources were identified and their contributions were estimated in each monitoring site. Contribution results on Hwasung, Paju, and Icheon sites were as follows: 33%, 27%, and 27% from soil source, 26%, 26%, and 21% from secondary aerosol source, 11%, 11%, and 12% from biomass burning, 12%, 6%, and 5% from sea salt, 7%, 15%, and 19% from industrial related source, and finally 11%, 15%, and 16% from mobile and oil complex source, respectively. This study provides information on the major sources affecting air quality in the receptor sites and thus it will help to manage the ambient air quality in the metropolitan area by establishing reasonable control strategies, especially for the anthropogenic emission sources.

• Asian Journal of Atmospheric Environment
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• 제6권4호
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• pp.281-287
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• 2012

Aerosol concentrations at the CC-Lag site in the Teshio Experimental Forest increased from winter to spring and sometimes showed extremely high values associated with Kosa and/or forest-fire events. The range and mean of the mass concentrations of aerosol chemical species were as follows: total particulate mass, 1.2-29, 5.0; elemental carbon, 0.061-2.2, 0.43; organic carbon, 0.059-3.5, 0.79; and sulfate, 0.12-6.2, 1.8 ${\mu}g/m^3$. The total masses of the deposited particles on hybrid larch and on bamboo leaves were approximately 35 and 30 ${\mu}g/cm^2$, respectively. The amounts of soil particles on the leaves were 6 ${\mu}g/cm^2$ for the upper part of hybrid larch, 2 ${\mu}g/cm^2$ for the lower part of hybrid larch, and 1 ${\mu}g/cm^2$ for Sasa bamboo leaves. The amounts of deposited black carbon were 2.3 ${\mu}g/cm^2$ for the upper part of hybrid larch, 0.6 ${\mu}g/cm^2$ for the lower part of hybrid larch, and 0.2 ${\mu}g/cm^2$ for Sasa bamboo leaves. Half of the total deposited particular mass was attached on the hybrid larch; however, most of the total deposited mass was adhered on the Sasa bamboo leaves. Regardless of the species, there tend to be more deposited particles on the leaves in the upper part than in the lower part, with only a few meters height difference. Comparing the composition of the deposited particles to that of the atmospheric aerosols without any size cut, the fractions of water-soluble material sulfate and sea salt in the deposited aerosols were about one tenth and one hundredth lower than that in the aerosols, respectively. On the basis of the measured concentration and the deposited amount on leaves, the deposition velocity of black carbon was estimated to be approximately 0.5 cm/s.

• Journal of Advanced Marine Engineering and Technology
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• 제41권3호
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• pp.197-201
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• 2017

대부분의 어선에서는 포획된 어류를 관리하고 저장하기 위해 얼음 냉각 시스템을 사용한다. 그러나 얼음 냉각 시스템은 작동 시간의 제한뿐만 아니라 적절한 온도와 염분 농도를 유지하는 것이 어려운 단점이 있다. 본 연구의 목적은 어류 운반선의 어창에 적정한 해수온도 유지를 위한 해수 냉각 시스템용 만액식 증발 열전달 특성을 파악하는데 있다. 실험은 냉매의 해수 온도, 유량 및 포화 온도의 변화를 주며 열전달 특성을 파악하였다. 동일 열유속에서 Aluminium-Brass tube가 Copper-Nickel tube 보다 외측 열전달계수가 약 10% 큰 것으로 확인할 수 있었으며, 이를 통해 해수용 열교환기의 전열관으로 Aluminium-Brass를 적용하는 것이 열전달 측면에서 효과적일 것을 확인할 수 있었다. 만액식 단관 열전달계수와 18 kW급 만액식 해수냉각시스템의 총괄열전달계수의 비교를 통해 동일 조건에서는 25%정도 단관의 열전달계수가 큰 값을 나타내었으며, 이러한 결과는 만액식 관군 열교환기의 설계를 위한 중요한 자료가 되리라 판단된다.

• 미생물학회지
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• 제46권4호
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• pp.366-374
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• 2010

비배양에 근거한 16S rDNA-DGGE fingerprinting 방법을 적용하여 공생세균 군집구조를 조사하였다. Zobell 배지와 천일염 배지를 사용하여 총 164균주를 선별하였다. 이들 균주로 부터 증폭한 16S rDNA를 제한효소 HaeIII와 MspI을 사용하여 절단한 후 각각의 다른 RFLP 패턴으로 구분하였다. RFLP패턴으로부터 유래한 16S rDNA의 염기서열 분석 결과, 알려진 염기서열들과 95% 이상의 유사도를 나타내었으며 Proteobacteria (Alphaproteobacteria, Gammaproteobacteria), Actinobacteria, Firmicutes, Bacteroidetes의 4개의 문이 나타났으며 우점 군집은 Alphaproteobacteria였다. 해면에서 분리한 total gDNA로 부터 증폭한 16S rDNA의 DGGE 분석 결과 5개의 DGGE band가 확인 되었고, 각각의 band의 염기서열 분석 결과 알려진 염기서열들과 96% 이상의 유사도를 나타내었으며 band로부터 밝혀진 모든 서열들은 배양되지 않은 세균 클론들과 높은 상동성을 나타내었다. DGGE에 의한 공생세균 군집은 Proteobacteria (Alphaproteobacteria, Gammaproteobacteria), Actinobacteria, Spirochetes, Chloroflexi로 4개의 문(phylum)으로 나타났다. Spirastrella abata의 공생세균 군집에 대한 RFLP와 DGGE 적용 결과, Alphaproteobacteria, Gammaproteobacteria, Actinobacteria의 공통 세균 그룹이 발견되었으나 전체적인 공생세균 군집구조는 분석 방법에 따른 차이를 나타내었다.

• 한국대기환경학회지
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• 제20권3호
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• pp.381-396
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• 2004

In order to understand the precipitation acidity and chemical composition of ion species in Iksan area as well as to know the difference of chemical characteristics in precipitation samples from the viewpoint of precipitation sampling method, precipitation samples were collected by wet-only automatic precipitation sampler and bulk manual precipitation sampler in Iksan, from March 2003 to August 2003. The mean pH of precipitation was 5.0. There was a little significant difference in the mean value of pH between automatic and manual sampler. However, pH values of some precipitation samples were lower in automatic sampler than in manual sampler, especially in case of precipitation samples with small rainfall for March 2003. The mean concentrations of each ions in precipitation were generally a little higher in precipitation samples collected by the manual sampler than in those collected by the automatic sampler because of accumulation of dry deposition on the surface of glass funnel installed at the manual sampler during the sampling period or no rainfall. Dominant species determining the acidity of precipitation, were N $H_4$$^{[-10]}$ and nss-C $a^{2+}$ for cations and nss-S $O_4$$^{2-}$ and N $O_3$$^{[-10]}$ for anions. The mean concentration of N $H_4$$^{+}$ and nss-C $a^{2+}$ were 31 $\mu$eq/L and 9 $\mu$eq/L for the automatic sampler and 40 ueq/L and 16 ueq/L for the manual sampler, respectively. In addition, nss-S $O_4$$^{2-}$ and N $O_3$$^{[-10]}$ were 27 $\mu$eq/L and 13 $\mu$eq/L for the automatic sampler and 32 $\mu$eq/L and 17 $\mu$eq/L for the manual sampler, respectively. Although the concentrations of the acidifying ions of nss-S $O_4$$^{2-}$ and N $O_3$$^{[-10]}$ were about 3 times higher than those for foreign pristine sites, precipitation acidity were estimated to be natural due to the neutralization reaction of the alkaline species of N $H_4$$^{+}$ and nss-C $a^{2+}$ with its higher concentrations. Considering the ratios of nss-S $O_4$$^{2-}$/N $O_4$$^{[-10]}$ nss-S $O_4$$^{2-}$, it was found that ammonium sulphate was dominant in Iksan precipitation. The major non-sea salt ions were maximum concentrations for March, but decreased with increasing of precipitation amount.on amount.

• 미생물학회지
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• 제51권1호
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• pp.86-95
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• 2015

독도의 해안에 군락을 이룬 해안식물 근권에서 호염성 및 염내성을 가지는 세균의 분리를 위해 3종의 해안식물의 군락을 선정한 후 각 식물의 군집 하부에서 토양시료를 채취하였다. 시료는 marine broth 한천배지를 이용하여 형태학적인 구분을 통해 순수분리 되었다. 분리된 161개 세균들을 NaCl 9.0% 농도로 조정된 배지에서 생존하는 26개 균주를 선발하여 genomic DNA를 얻은 후, 16S rRNA gene sequence를 증폭하여 부분동정 하였다. 이들의 유연관계 확인을 위해 계통수를 작성한 결과, 이들은 각각 Firmicutes (30.8%), Gamma proteobacteria (53.8%), Bacteroidetes (7.7%), Alpha proteobacteria (7.7%), Actinobacteria (7.7%)에 속하였으며, 이는 기존의 독도 토양 및 해수 미생물상 연구와 특징적 차이를 보인다. 또한, 분리된 세균의 종 조성도 기존 독도 토양 및 해양연구와 유의적으로 상이함을 보였다. 이에 더하여 선발된 26개 균주들 중에서 4균주가 12.0% 이상의 염농도에서 생장하였으며, 이들 중에서 3개 균주가 15.0% 이상의 염농도에서 생장하여 극호염성의 특성을 나타내었으며, 광범위한 염분농도에서도 생장하는 특성을 보였다. 이들은 해안식물 근권에서 독도 특유의 고염분 및 염분변화라는 환경적 스트레스를 극복하며 해안식물과 어떠한 상호작용을 하는 것으로 생각된다.

• 한국구조물진단유지관리공학회 논문집
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• 제21권6호
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• pp.83-90
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• 2017

원전콘크리트는 두꺼운 벽체를 가진 매스콘크리트 구조이며 시공초기에 건조수축 및 수화열에 따른 균열이 발생하기 쉽다. 또한 냉각수를 항상 필요로 하므로 해안가에 위치하는데, 균열이 발생한 콘크리트에서는 염화물 이온의 유입으로 인해 철근 부식이 빠르게 발생한다. 본 연구에서는 6000 psi 급 고강도 원전콘크리트 배합을 이용하여 재령 및 균열에 따른 확산계수의 변화를 분석하였다. 이를 위해 재령 56일, 180일, 365일 동안 양생된 콘크리트에 균열폭을 0.0~1.4 mm까지 유도하였으며 정상상태의 촉진 확산실험을 수행하였다. 균열폭의 증가에 따라 확산계수는 최대 2.7~3.1배로 증가하였으며, 재령의 증가에 따른 확산계수의 저감성이 크게 평가되었다. 또한 180일 동안 비말대에 노출된 균열부 콘크리트에 대하여 겉보기 확산계수 및 표면염화물량을 평가하였으며, 촉진 실험결과와 비교를 수행하였다.

• 한국식품조리과학회지
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• 제23권5호
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• pp.731-748
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• 2007

In this study, we investigated e kinds and names of side dishes along with their recipes and ingredients occuring in Korean cookbooks published before the 17th century. The side dishes were classified 79 kinds of Guk, 23 kinds of Jjim and Seon, 15 kinds of Gui, 3 kinds of Jeon, 7 kinds of Nureumi, 3 kinds of Bokkeum, 30 kinds of Chae, 11 kinds of Hoe, 7 kinds of Jwaban, 6 kinds of Mareunchan, 12 kinds of Pyeonyuk and 5 kinds of Jeonyak, Jokpyeon and Sundae. The earliest records were found on Guk, Jjim, Jwaban, Po and Pyeonyuk Gui, Namul and Hoe were recorded after the 1500's and Nureumi, Jeon, Jeonyak, Jokpyeon and Sundae were developed relatively late in the late 17th century. As to the kinds of side dishes, Guk was the most common. Guks cooked before the 17th century used different recipes and more types of ingredients than today, including some that are not used today. For Jjim, various seasonings were added to main ingredients such as poultry, meat, seafood and vegetable. Most of the records found for Jjim used chicken as the main ingredient. Gui was recorded as Jeok or Gui and there weren't many ingredients for Gui before the 17th century. Gui was usually seasoned with salt or soy bean sauce and broiled after applying oil. Vegetables were broiled after a applying flour-based sauce. The Jeon cooked at that time was different from the one that is cooked today in that cow organs or sparrows were soaked in oily soy bean sauce before being stewed. Nureumi, which was popular in the 17th century, but rarely made today, was a recipe consisting of adding a flour or starch-based sauce to stewed or broiled main ingredients. Chae was a side dish prepared with edible plants, tree sprouts or leaves. Chaes like Donga and Doraji were colored with Mandrami or Muroo. Hoe was a boiled Hoe and served after boiling seafood. Jwaban was cooked by applying oil to and then broiling sparrows, dudeok, and mushrooms that had been seasoned and dried. For dried Chans, beef or fish was thin-sliced, seasoned and dried or sea tangle was broiled with pine nuts juice. There are some recipes from the 17th century whose names are gone or the recipes or ingredients have changed. Thus we must to try to rebuild three recipes and develop recipes using our own foods of today.