This study was carried out to investigate the succession patterns of dietary culture and to find out all the educational problems with female college students in both countries as the central figure. The results are as follows. The degree of knowledge acquisition about food of annual custom is 58% in Korea and 72% in Japan. What the rate of knowledge acquisition is high among both countries’ similar food of annual custom are 「Seolnal(Gantan)」, 「Sambok(Doyonohi)」, and 「Chuseok(Tsukimi)」. Cooking experience of festive food is 45% in Korea and 58% in Japan. Among both countries' common festive food what cooking experience is high in Korea are 「Seolnal」 and 「Chuseok」, which are over 97%. In Japan those are 「Gantan」 and 「Tsukimi」, which are over 80%. Regarding learning experience of festive food 「Seolnal」 and 「Gantan」 are beyond 80% and 「Chuseok」 is 88%. In Japan 「Tsukimi」 is 71% and 「Omisoka」 is 85%. The learning sources of food of annual custom are parents and schools in common, and Korea has another learning sources, mass communication. Festive food that is cooked shows much similarity between two countries, but each country has originality. As common food of annual custom 「Seolnal」 has nine kinds of food, 「Sambok」 has three kinds, and 「Chuseok」 has five kinds in Korea In Japan 「Gantan」 has fourteen kinds of food, 「Doyonohi」 has three kinds, and 「Tsukimi」 has five kinds. The successive consciousness about food of annual custom is concentrated on a specific food in Korea. And Japanese consciousness is shown as an expansion-type on diverse food. Korean successive consciousness is 69.4% and Japanese consciousness is 82%. The higher the rate of knowledge acquisition, cooking experience, and learning experience are in both countries, the higher successive consciousness is. So we must note for the importance of home and school’s education.

Fe78B13Si9 비정질 합금의 결정화 거동과 취성 현상을 시차열량기 시험, x-선회절시험 및 투과 전자현미경 관찰을 통해서 조사 연구하였다. 결정화는 두단계의 발열반응으로 진행되었으며, 첫번째 단계에서는 비정질로부터 B.C.C. 구조인 α-(Fe, Si)의 수지상이 생성되었고, 두번째 단계에서는 남아있던 비정질로부터 B.C.T 구조인 Fe2B가 형성되었다. 에닐링 온도에 따른 시편의 파단과 변형율은 비정질 상태인 약 340˚C부터 급긱히 감소하였다.

Temperature depth profiles measured in permafrost and western Utah generally represent anomalous curvatures. The accurate climate change can not be resolved with existing geothermal data, but general magnitude and timing explain the model of global warming. Differences between borehole temperatures observed in different intervals may concur with modeled temperature differences computed from the nearest air temperatures. This agreement indicates that boreholes are recording climate change.

한국 남해역에서 정기적인 해양 관측을 실시하고 있는 국립수산진흥원의 해양관측 정선이 외해쪽에만 치중되어 있어 연안수와 외해수간의 상호관계를 상세히 규명하기 어렵고 또한 해역에 따라서는 정선간의 간격이 커 복잡한 해황을 정확하게 파악하지 못하는 경우도 있다. 따라서 본 연구에서는 1986년 5월 23~25일간 부산수산대학교 실습선 402호를 이용하여 위와 같은 전선대 해역(제주도 동부 해역 부근)에서 자주 발생한다고 알려져 있는 수온역전 현상에 대해 DBT(Digital Momery Bathythermograph)를 사용하여 현장관측을 실시하여 보다 상세한 수온역전 구조와 그 발생 기구를 파악하고 부차적으로 이러한 수온역전 현상이 이 해역에 존재하고 있는 각 수괴들과 어떠한 관계가 있는가를 밝히고자 하였다. 그 결과, 총 67개 정점에서 수온역전이 출현한 정점은 39개이며, 그 출현빈도는 58.20%였다. 한정점에 수온역전 출현빈도는 한 개 층이 9개로서 13.42%, 두 개 층은 14개로서 20.80%, 세 개 층은 16개로서 23.88%로 나타났다. 수온역전은 대체로 수온약층 하의 수심인 40m 이심에서 일어났고 역전 수온 범위는 14~16℃였다. 제주도 동부 해역에서 출현한 수온역전은 고온 고염의 쓰시마난류수가 저온 저염의 한국남안연안수 사이를 침투(intrusion)하여 생기는 수온역전과 저온 저염의 한국남안연안수가 고온 고염의 쓰시마난류수 사이를 침투하여 생기는 수온역전의 두 가지가 있다. 그리고 이러한 수온역전이 전선대에서 빈번히 발생함을 해양 관측을 통하여 구체적으로 밝혔다. 그리고 앞으로도 전선대에서 수온역전의 기구를 규명하여 각 수괴의 존재를 규명하는 문제로 계속적으로 연구해야 될 과제하고 생각한다.

In order to determine the design precipitation, the most probable daily precipitation and annual precipitation at every spot are calculated and iso - precipitation line are drawn. Probability of precipitation and drought phenomena of each gage station are analyzied by the method of frequency analysis from the statistical conceptions. The results summarized in this study are as the follows. 1. Annual mean precipitation in kyungpook area are 1044 mm, about 115 mm less than annual mean precipitation of Korea amounts to l1S9mm, and found to regionally unequal. 2. Monthly mean rainfall of July is 242.2mm, 23.2%, August 174.2mm, 16.7%, June 115mm, 11% and September 114.2mm, 10.9% and Rainfall depth of July-August are more than 40% of annual precipition. This shows notable summer rainy weather by typoon and low pressure storm and seasonal unbalance of water supply. 3. The relation among the maximum precipi.tation per day, per two continuous days and per three contnous days are caculated and the latter is found 31.0% increased rate of the first and the last 48.2% increased rate of first. 4. Probability precipitation in Kyungpook area are shown as 9.0%(5 year), 13.3%(10 year), 17.7%(20 year), 23.1%(50 year), 27.0%(100 year) and 31.1%(200 year) increased rate of each recurrence year compared with observed average annual precipitation. 5. From annual precipitation and maximum daily rainfall data probability of precipitation and precipitation isohyetal line are derived which shown as Table 11 and Fig. 8. 6. Drought days are divided 6 class and analysed results are shown on table 12. Average occurrence time of 10-14 continuous drought days are 2.3 time per year, 15-19 days are 0.9 time per year, 20-24 days are one per six years, 30-34 days are once per nine years and over than 35days are once per 25 years.

1. 반구형 각의 분포 및 집중하중에 의한 좌굴응력 해석은 변형된 각의 형상에 따라 타원체 각의 응력으로 해석함이 타당하다. 2. 일정 한계이상의 형상계수를 갖는 반 구형각에 대하여서는 재료상수를 형상계수의 승수로 고려한 수정된 임계좌굴 하중으로 탄소성 좌굴을 판정함이 더 양호한 결을 준다. 3. 탄소성 좌굴에 있어서 소모된 소성변형 에너지를 계산하기 위하여 항성변형 에너지를 계산하기 위하여 항상선를 따르는 에너지법을 이용하면 양호한 결과를 얻을 수 있다.

Results investigated backwater phenomena at Geumho river basin to get a basic data for Daegu basin area development plan are as the follows. 1. It is a A=0.35 L 1.848 (r = 0.97), the relationship between basin area and river length at Geumho river. 2. Dividing the rainfall of Geumho river basin as two parts, a first half rainfall and a second half rainfall, the amount of a first half rainfall appeared 57.5% comparison with total rainfall. 3. The maximum flood discharge appeared 12 hrs. continuous rainfall rather than 24 hrs. continuous rainfall. 4. Results investigated backwater phenomena from Geumho II bridge to chungchun appeared the rising water level of 69 cm, 55 cm, 44 cm, at section III in the starting point water level of 1.8 m, 2.4 m, 4.0 m respectively. 5. Results investigated backwater phenomena by the flood water level appeared a similar form. There was a average rising water level of 30 cm at section III. At the results of this computation, it was confirmed that section III was affected the highest backwater phenomena among the observed river reaches in Geumho river. In addition, this paper should be given a assistance to decide a economic and safe section in construction of bank of river and estuary barrage.