The mainly purpose of this research was to investigate tendency of changes regarding the recipe of Naengmyeon (Korean cold noodles) based on water. In order to conduct of this research, we analyze the recipe data published in Korea from 1800's to 1980's. A method of mainly study was conducted by content analysis and literature review. The documents of recipe used research were 42 literatures (euigwae, recipe book, magazines, and dictionaries). In addition, the recipes of Naengmyeon based on water were total method of 84. The results of an analysis of recipe data published in the last 200 years showed 3 different types of the recipe of Naengmyeon based on water; 1) Naengmyeon based on water of Kimchi juice type 2) Naengmyeon based on water of (meat) broth type 3) Naengmyeon based on water of mixed (Kimchi juice+broth) type.

본 연구는 장기 해양관측(1966-1995)자료, 위성관측자료 및 수치모델기법을 이용하여 한국 남서해역에서 하계에 형성되는 조석전선괴 저수온역의 시공간적 변화를 파악하였다. 한국 남서 연안해역에서는 6월과 8월에 대흑산도~진도간 해역의 표면에서 주변 해역보다 2~3℃ 낮은 저수온역이 분포하면서 조석전선역이 형성됨을 확인할 수 있었다. 수온수평경도가 0.3℃/km 이상인 조석전선은 성층계수 2.0~2.5 범위이며, 0.03℃/km 이상인 저수온역은 성층계수 2.5~3.0의 범위와 일치하였다. 소조시에서 대조시까지 조석주기가 변하는 동안 조석전선의 위치변동은 전선은 25~75km, 저수온역의 범위는 60~90km로 조류의 세기에 정비례하여 이동 범위가 커지는 것으로 나타났다. 또한, 남서쪽 외해역으로 저수온역이 확장되는 원인은 진도 남서쪽으로 향하는 10cm/s 이상의 강한 조석잔차류에 의한 것으로 판단된다.

자생나리 종자의 발아율은 20-25oC에서 높았다. 이 온도에서의 솔나리, 땅나리, 털중나리와 하늘나리의 발 아율은 거의 100%, 참나리와 중나리는 각각 88.0%와 73.0%였다. 반면 말나리, 섬말나리와 하늘말나리의 발 아율은 34.0-54.0%로 낮았다. 발아는 대부분 15oC에서 지연되어 발아율이 높은 종일수록 발아소요일수가 단 축되었다. 발아와 일장과는 대체로 무관하였으나 장일 하에서 하늘나리는 촉진된 반면, 말나리와 섬말나리는 억제되었다. 발아속도도 일장효과가 적었으나 중나리는 일장이 길수록 촉진되었고, 섬말나리는 지연되는 경향 이었다. PGRs 온탕처리의 효과를 보면, 땅나리, 솔나리, 털중나리, 참나리와 하늘나리의 발아율은 무처리와 차 이가 없었다. 그러나 중나리는 BA에 의해 발아율이 향상 되었다. 중나리와 참나리는 습윤냉장 기간이 길어짐에 따라 발아율이 향상된 반면, 말나리와 섬말나리는 저하 되었다. 발아소요일수는 습윤냉장 기간이 길어질수록 종에 관계없이 단축되었다. 건조저장시의 발아율은 실 온보다는 저온저장구에서, 방치구보다는 데시케이터 저 장구에서 높아, 4oC 데시케이터 저장구에서 발아율이 가장 높았다. 하늘나리는 실온에서 장시간 방치시 발아 율이 급격히 떨어졌으나, 중나리는 데시케이터 사용만 으로도 발아율이 장기간 유지되었다.

Some biological activities such as an electron donating capacity, the contents of total polyphenol compounds and flavonoids, fibrinolytic activity and α-glucosidase inhibitory activity have been detected in hot water extracts of Ligularia fischeri and Angelica gigas Nakai. To increase the usefulness of the functional ingredients for prevention and improvement of some metabolic disorders, ethanol-treated hot water extracts of Angelica gigas Nakai were prepared. A hot water extract of Ligularia fischeri has 92% of electron donating capacity, 39.4 mg/g of total polyphenol compounds, 24.8 mg/g of flavonoids and 29.8% of α-glucosidase inhibitory activity, but no fibrinolytic activity. A hot water extract of Angelica gigas Nakai has 94.7% of electron donating capacity, 5.8 mg/g of total polyphenol compounds, 2.6 mg/g of flavonoids, 0.48 plasmin units of fibrinolytic activity and no α-glucosidase inhibitory activity. However, with partial purification using cold ethanol treatment, the α-glucosidase inhibitory activity of Angelica gigas Nakai was increased to 70.5%. Thus, we expected a more useful effect with the use of the addition of a cold ethanol-treated Angelica gigas Nakai extract. The L, b values of cold buckwheat noodles using a mixture of 0~3% of Ligularia fischeri powder and 0.5% of an ethanol-treated hot water extract of Angelica gigas Nakai were decreased with the addition of an increasing amount of Ligularia fischeri powder. Among the mechanical qualities, only adhesiveness was significantly higher in 3% Ligularia fischeri noodles. From sensory evaluation data, it was determined that these two functional ingredients did not ruin the color, texture, and overall acceptance of the cold buckwheat noodles. A higher amount of the extracts improved the quality of the product with little added cost.

여름철 팽이버섯 병재배시 톱밥배지에서 발생하는 균사생장 억제증상의 원인을 구명하고 그 경감대책을 확립하기 위하여 톱밥배지 배합시 물온도를 24℃(상온수)와 6℃(저온수)로 하고, 배지제조후 살균전 경과시간을 0, 3, 6, 9시간으로 달리하여 팽이버섯의 재배시험을 수행하였다. 배지제조 후 살균전 시간이 경과함에 따라 배지온도가 상승하고, pH는 6.5에서 5.2∼5.6으로 낮아지는 경향이었다. 이때 톱밥배지 내에서 세균밀도가 증가하였으며, 물온도 24℃에서는 6℃보다 6시간 이후의 세균밀도가 1.9∼4.1배 높았다. 톱밥배지에서 분리한 세균과 대치배양시 팽이버섯균의 생장이 억제되었다. 또한 배지제조후 살균전 시간이 경과함에 따라 배지내의 전질소 함량이 감소하였으며 유리당의 함량도 종류에 따라서 증가 또는 감소하였다. 배지배합시 24℃물 처리구는 6℃물 처리구에 비하여 팽이버섯 병재배사에서 균배양기간 및 버섯발생기간이 각각 1∼2일 지연되는 경향이었으며, 자실체 수량도 저온수 처리구에서 안정적이었다. 그리고 9시간 경과한 배지에서는 균사생장이 정지되었다. 배지제조후 경과시간에 따라 팽이버섯 발생기간은 1∼3일이 지연이 되었으며, 자실체수량은 6시간이 경과된 배지에서 7∼12% 감소하는 경향이었다. 본 시험은 여름철 고온기의 팽이버섯 재배시 배지제조에 6℃이하의 저온수를 사용하여 배지내 미생물 증식을 억제시키고, 입병작업을 마치는 즉시 고압살균 함으로써 배지의 성분을 안정화시켜 버섯의 안정생산에 기여할 것으로 기대된다.

가압 경수로형 원전에 사용되는 Alloy 600 증기발생기 전열관재료의 입계응력부식균열 거동에 미치는 냉간변형의 영향을 1차 냉각수 모사조건에서 정속인장시험방법으로 조사하였다. 인장 냉간변형은 응력부식균열을 크게 가속화 시키지는 않았으며 변형량이 25%이상인 경우에는 응력부식균열이 발생하지 않았다. 이 현상은 냉간 변형량 및 형태에 따른 미소변형 및 응력의 불균질성에 영향을 받는 것으로 사려되며 응력의 크기는 직접적인 영향을 주지 않는 것으로 보인다. 국부적인 큰 응력구배가 존재하는 경우 균열의생성 및 성장이 현저히 가속화되었는데 이는 원전 1차측 응력부식균열 기구가 응력구배에 의존하는 과정과 연관되어 있다는 증거이다. Hump 시편을 이용한 정속인장시험방법은 짧은 실험기간내에 원전 1차측 응력부식균열 특성을 평가할 수 있는 방법이었다.

This paper, examines the relationship between water temperatures and fishing conditions of common squid by the squid angling fishery from June to September in 1993-1995. The condition of the common squid fishing largely depended on the fluctuation of water temperature in the coastal area of Gampo. Monthly mean water temperatures during June m September in 1993 and 1994 were relatively higher than those in 1995 in Gampo area. But the values between July and August in 1995 were about 5℃ lower than those in 1993 and 1995. Coefficients of variation (CV) of water temperature showed the lowest value during July ~ September in 1993, however, the highest value was observed in July and August in 1994. Catch per unit effort (CPUE ; kg/angling) showed a peak with 73.7kg in 1993 when the CV was low. On the other hand, the lowest CPUE of 39.6kg was observed in 1994 when the CV was high. It was concluded that the high stability of water temperatures and the weak strength of cold water have caused the good fishing conditions of common squid.

In 1996, a cold-water damage occured in the paddy field at the downstream of the Umoon dam. To study the cause and the preventive measures of the cold-water damage a field study was performed during the growing season of 1997. Field measurements such as water temperatures at reservoir, irrigation canal and in the paddy field were made. As a result, there was no cold-water damage due to the right irrigation water management practice in 1997. The cold-water damage is possible to happen, however, and the preventive measures were provided.

Based on a precise analysis of the long-term(1971-1984) hydrographic and wintertime air temperature data gathered in the middle and southern yellow Sea, and together with other supplimentary data from Gteratures, water characteristics of the Yellow Sea Bottom Cold Water(YSBCW) and its southward extension are reexamined ; the influence of the wintertime air temperature on the YSBCW temperature and on its spatial distribution also discussed. It was found that the hitherto defined water characteristics (T, S) of the YSBCW restrict especially the upper limit of salinity to too lower values compared to the real situation, so they are not adequate to describe the spatial distribution of the water and its southward extension phenomenon. From the present study, the southward extention of the YSBCW through the cold water through west off Chejudo from spring to summer is found highly possible ; it is strongest is April and it can be detected until August. In consequence of such a southward advection of the bottom cold water, the water temperature at 50m depth in the cold water through west off Chejudo shows its lowest values in April, with a mean temperature increase by 0.4℃ only from April to August(compared to 4℃ increase near the axis of the Yellow Sea embayment). The frequently observed cold water mass from the west to the southwest(near 32°N, 126°E)off the island during spring and summer is connected with and influenced profoundly by the bottom cold water from the southern Yellow Sea, showing almost same water. characteristics as those of the latter ; it preserves quite well its wintertime water characteristics until summer. Therefore it seems to be quite reasonable to include this cold water mass(found west to southwest off Chejudo) in the definition of the YSBCW. Here, we have suggested a new definition of the YSBCW : T$lt;12℃, 32.2$lt;S$lt;33.5‰ With this new definition, the spatial distribution of the YSBCW from the offshore of the Shandong peninsula to the southwestern area off Chejudo as well as its southward extension from spring to summer can be adequately described. The wintertime air temperature is one of the most important meteorological factors, controlling the summertime water temperature of the YSBCW and its spatial distribution. In other words, the bottom cold water formed during a severe cold winter exhibits in summer lower temperatures and also wider spatial distribution toward the coasts and to the south than that formed during a mild winter.

Dynamical conditions for the fronts around the Yellow Sea Cold Water Mass, were investigated by means of the oceanographical data and simple numerical experiment. The coastal front developed along the coast inside the Yellow Sea and distinguished the Yellow Sea Cold Water Mass from the coastal water is attributed to the predominant tidal mixing near the coast. On the other hand the southern part of the front of the cold water mass would be explained a a part of the extention of a western boundary current which flows into the Cheju Channel.

동지나해.황해의 최근 10개년간(1970~1979) 안강망에 의한 참조기.강달이 어획자료를 이용하여 어획량.어장의 경년변동과 저층수온과의 관계를 조사하였다. 그 결과, 1970~1976년간의 어획량은 수온보다 2~3년 늦은 위상(Time lag)을 가지고 변화하였다. 1970~1973년은 감소, 1974년 초~1975년 말은 급격한 증가, 그리고 그 후 1976년 말까지는 평형상태이었다. 그러나 1976년 이후에는 어획노력량의 증가로 인하여 이러한 위상을 가지는 경형은 명확하지 않았다. 또한, 수온이 평년 보다 낮았던 저수온 년인 1977년의 어장분포는 수온이 높았던 고수온 년인 1972년보다 남쪽으로 치우쳐 있는 경향을 보였다

동계(冬季) 황해(黃海)에서 1961년(年)부터 1974년(年)까지 (1966년제외(年除外) 13년간(年間)의 열수지(熱收支)를 산출(算出)하고 이 기간(期間)동안 하계동지나해(夏季東支那海)에서의 황해(黃海) 냉수(冷水) 세력(勢力)과의 관계(關係)를 분석(分析)한 결과(結果)를 요약(要約)하면 다음과 같다. (1) 황해상(黃海上)의 일사량(日射量)은 동계중(冬季中) 12(月)이 가장 낮아 약 160~190ly/day이고, 1월(月)과 2월(月)로 갈수록 점차 증가(增加)하여 2월(月)에는 250~260ly/day로서 12월(月)에 비(比)하여 79~90ly/day가 컸다. 동계(冬季) 일사량(日射量)의 년별변화량(年別變化量)은 약 50 ly/day 이하(以下)인 것으로 나타났다. (2) 해면(海面)에서의 장파복사량(長波輻射量)이 유효일사량 보다 12월(月)에는 30~70ly/day, 1월(月)에는 27~46ly/day 정도 크게 나타났으나, 2월(月)에는 반대(反對)로 20~30ly/day 정도 작게 나타났다. (3) 일사량(日射量)에서 해면반사량(海面反射量)과 해면복사량(海面輻射量)을 뺀 값은 100 ly/day 이하(以下)이고, 12월(月)과 1월(月)에는 (-), 2월(月)에는 (+)로 나타나며, 3개월간(個月間)의 평균(平均)은 약 -20 ly/day정도이다. (4) 현열방출량(顯熱放出量)과 증발열량(蒸發熱量)을 합한 값은 1963년(年) 1월(月)이 최고(最高)였고 (882 ly/day), 1961년(年) 2월(月)이 최저(最低)였다.(471 ly/day). (5) 동계(冬季) 황해(黃海)에서 잃어버린 총열량(總熱量)은 1962년(年)이 평균(平均) 588 ly/day로서 최저(最低)이며, 1968년(年)에 716 ly/로서 최고(最高)였다. (6) 1971년(年) 8월(月)에 황해(黃海)와 동지나해(東支那海)의 표층수(表層水)는 여러 종류로 분류(分類)되나, 30m 이심(以深)에서는 수온(水溫)이 6.4˚~13.2℃, 염분(鹽分)이 33.17%˚ 이상(以上)으로서 다같이 저온(低溫)의 성질(性質)을 띠고 있다. (7) 평균(平均) 수온분포도(水溫分布圖)에서 단위면적당(單位面積當) 적산수온(積算水溫)을 냉수지수(冷水指數) 50m층(層)의 지수(指數)를 수평지수(水平指數), 32˚N의 20m 이심층(以深層)의 지수(指數)를 수직지수(垂直指數)라 하면, 1962년(年)의 경우 수평지수(水平指數)가 1.86, 수직지수(垂直指數)가 3.18로서 냉수지수(冷水指數)가 5.04였고, 1968년(年)의 경우에는 냉수지수(冷水指數)가 -3.21였다. (8) 냉수지수(冷水指數)에서 11월하순(月下旬)의 황해(黃海)의 수온(水溫)의 표준편차(標準偏差)를 뺀 값 C-T'w와 동계열수지(冬季熱收支)와의 관계(關係)는 C-Tw'=32.06-0.049QT이고, 그상 상관계수(相關係數)는 0.94이다. 또 수평지수(水平指數)에서 초기조건(初期條件)을 뺀값 Ch-T'w/2, 수직지수(垂直指數)에서 초기조건(初期條件)을 뺀 값 Cv-T'w/2와 열수지(熱收支)와의 관계(關係)는 Ch-T'w/2=12.20-0.019QT Cv-T'w/2=18.07-0.027QT이고, 그 상관계수(相關係數)는 각각(各各) 0.90 및 0.97이다. 이 결과(結果)로서 동계(冬季) 황해(黃海)에서의 열수지(熱收支)와의 하계(夏季) 동지나해(東支那海)의 황해(黃海) 냉수세력(冷水勢力)과의 상관계수(相關係數)가 높음이 밝혀졌으므로, 동계열수지(冬季熱收支)를 계산(計算)하고, 11월(月) 하순(下旬)의 황해수온(黃海水溫)만 알면 하계(夏季) 황해(黃海)의 냉수세력(冷水勢力)을 예측(豫測)할 수 있어 어장(漁場) 선정에 많은 도움이 되리라고 생각된다.

Background : Upon harvest in the summer, seeds of Panax ginseng are unmatured and need further maturation, dehiscence and cold-stratification, for germination. For the cold-stratification, the seeds should be stored in the cold temperature for 90-100 days, however no further description about the storage condition have been described even though there have been many problems in emergence rate and quality of ginseng in the spring-sowed filed. Methods and Results : Thus here we tested 3 different storage temperature(2℃, -2℃, and – 20℃) in combination of 4 different seed water content(59%, 54%, 31%, and 7%) as cold-stratification condition. After 100 days of storage, seeds were placed on the filter paper after watering with distilled water in the petri dish and incubated at 10℃. Fifty percent of seeds stored at 2℃ with 59% water content had already germinated even in the storage room before germination test. Seeds with 59% and 54% water content stored at 2℃ and –2℃ germinated in a similar rate, but emergence of above ground part was higher in the seeds with 54% water content. Seeds with 31% and 7% water content stored at 2℃ and –2℃ showed low germination rate, because of fail in stratification or death. Seeds stored at –20℃ scored even lower germination rate and fail in emergence of above ground part. Conclusion : Seed water content and temperature during the cold-stratification period of ginseng seeds affected on the seed viability and germination rate, thus control of seed water content and storage temperature might improve the emergence rate of spring-sowed ginseng filed.

In this study, Analyzed characteristic about permeability cold-mixed recycled asphalt concrete using waste asphalt concrete and MMA. As a result, porosity was 20.4%, Water permeability coefficient was 0.94cm/sec and Skid Resistance test was 50BPN

This work investigates the relationship between the sea breeze circulation and ozone concentrations during cold water events in the southeastern coastal area of the Korean Peninsula, where coastal upwelling frequently occur. This analysis was performed based on the classification of two categories, such as cold water and non-cold water events, over the period of 2000-2009. The low air temperature (0.5℃), low SST (5℃) and the wind direction(southerly) are the features of the cold water events in the Southeastern coastal area. Moreover, ozone concentrations in the cases of the sea breeze circulation and cold water events were significantly lower (below 30 ppb) than those (70∼100 ppb) in the non-clod water events, because of the low air temperature (10∼20℃) and high wind speed (3∼5 m/s) around the southeastern coastal area.

The data of temperature, chlorophyll a, phytoplankton and NOAA/AVHRR satellite data were analyzed about 7 stations around Wando Island area on August 30, 2005. The sea water temperature range was from 15.19℃ to 24.97℃, and there was a cold water mass from the station 1 to 5 around the outside of Chungsando Island, the water temperature was lower at the bottom than surface. The salinity was 32.41～34.03, DO was 7.40～9.14 mg/L, but the concentration of chlorophyll a was 1ug/L higher at the bottom than surface. Total phytoplankton appeared from the whole stations were 47 genus, 80 species and diatoms were dominant. A lot of dinoflagellates Ceratium furca and diatoms Thalassithrix spp. mostly appeared in the cold water mass were turned up from the station 1 to 5. 4 groups of phytoplankton clusters were shown in the surface, and 3 groups of phytoplankton clusters were shown at the bottom according to the water temperature. On the ground of the result analyzed with NOAA/AVHRR satellite data, the SST around Wando Island was 22～25℃, it was formed by thermohaline front latitudinally.