어군탐지기를 이용하여 어군의 분포와 그 행동생태를 계측하기 위한 연구의 일환으로 어군의 연직적인 일주회유이동 및 초음파산란강도의 변동특성을 검토하고, 또한 수온의 연직구조와 어군의 연직분포특성과의 관계, 선박의 항주상태에 따른 어군의 행동반응 등을 현장실험을 통하여 검토, 고찰한 결과를 요약하면 다음과 같다. (1) 어군의 공간분포특성은 수온의 연직구조와 밀접한 관계가 있음을 알 수 있었다. (2) 동중국해 중앙부에서 일출 직전까지 수온약층 바로 아래쪽에 군집하고 있던 칼오징어와 전갱이 어군이 일출과 더불어 해저를 향해 급속히 하강하는 일주회유이동이 관찰되었고, 그 하강속도는 0.24m/min이었다. (3) 수온약층이 탁월했던 제주도 서방해역과 대만 북부해역을 대상으로 어군의 연직분포특성과 수온의 연직구조와를 상호 비교 분석한 결과, 표층과 저층의 수온차가 크고, 또 중층에 뚜렷한 수온약층이 형성되어 있는 경우, 전갱이와 칼오징어군은 야간에 수온약층의 바로 아래쪽에 농밀하게 군집하는 특성을 나타내고, 또 표층과 저층의 수온차가 적은 경우에 있어서는 표층까지 완전히 부상하여 군집하는 경향을 나타내었다. (4) 선박을 정선시킬 때, 선저 직하에 분포하는 어족생물이 급히 연직적으로 하향 이동하는 도피행동을 나타내었다. 그러나, 그 후 시간이 경과함에 따라서 다시 원래의 유영층으로 상향이동하는 행동패턴을 나타내었다. 한편, 수온약층을 경계로 하여 상층과 하층에 분포하는 어족생물의 행동패턴에도 차이가 있었는데, 수온약층 아래쪽에 있어서는 어군이 현저한 도피행동을 나타내었지만, 그 위쪽에 있어서는 그러한 징후가 관찰되지 않았다. 이와 같은 현상은 수온약층 아래쪽에는 유영성이 강한 어족생물이, 그 위쪽에는 유영성이 약한 어족생물이 군집하고 있었기 때문이라고 판단된다. 당시 이 해역에서 행한 저층 트롤의 주요 어획물은 물메기, 살오징어, 삼치 등이었다.

The wind pressure distributions were analyzed to provide fundamental criteria for the structural design on the two-span arched house according to the wind directions through the wind tunnel experiment. In order to investigate the wind force distributions, the variation of the wind force coefficients, the mean wind force coefficients, the drag force coefficients and the lift force coefficients were estimated using the experimental data. The results obtained are as follows : 1. The variation of the wind force with wind directions on the side walls was the greatest at the upwind edge of the walls. 2. The maximum negative wind force along the length of the roof appeared at the upwind edge at the wind direction of 60˚. 3. The maximum negative wind force along the width of the roof appeared at the width ratio and wind direction of 0˚ and 0.4 in the first house and 0.6 and 30˚ in the second house, respectively. 4. The mean negative wind force on the side walls of the first house at the wind direction of 0˚ was far greater than that of the second house, and the maximum negative wind force on the roof occurred at the wind direction of 30˚. 5. The maximum lift force appeared on the second house at the wind direction of 30˚, but the lift force on the first house was far greater than that on the second house at the wind direction of 0˚. 6. The parts to be considered for the local wind forces were the edges of the walls, and the edges of the x-direction and the width ratio, 0.4 of the y-direction in the roofs.

전라남도 도라지역에 분포하는 개미의 종류와 그의 종조성을 조사할 목적으로 1986년, 1989년, 1990년, 1991년의 4년간 10개 도서의 31개 지역에서 740 colony를 채집하여 동정 한 결과 4아과 30속 54종이 분포하는 것을 확인하였으며, 그 중에 대흑산도 예리에서 채집한 쌍털비늘개미(신칭)와 소안도 맹선리에서 채집된 조개무늬비늘개미(신청)는 한국산 미기록종인 것으로 사료된다. 10개 도라지역에 분포하는 개미의 종조성이 밝혀졌으며 Nomura-Simpson's Coefficient(NSC) 공식에 의한 종류사도를 분석한 바 전라남도 도라지역의 개미상은 연속적이였다

In this study the presence of pulse in formation of marginal basins through calculation of production rates based on the age of 22 marginal basins distributed in the western Pacific is revealed. The peaks of their productions appear approximately at 0 Ma, 30 Ma and 60 Ma, with the interval of about 30 my. Production peak appears to be the largest near 30 Ma (45 × 10⁴ ㎢). From the fluctuation of production rates, continuous production of marginal basins after 0 Ma (present-day) is inferred, and it is very likely that a production peak which is considerably higher than 30 Ma peak would appear in the future. Such upward inclination of production rates of marginal basins is vividly contrasting to downward decline of those of normal oceans. During the period of declining activities between 10 Ma and 15 Ma no activities of marginal basins are observed. When the marginal basins are classified into back-arc and non back-arc basins on the basis of their evolutionary processes, it is observed that back-arc basins appear to have cyclic production peaks approximately at 0 Ma, 20 Ma and 45 Ma, with the interval of about 20 my. The present-day back-arc basins appear to he most active in their productions. The phenomenon of fluctuations in the quantity of production upto now shows a upward climbing trend. The periods with less activity of back-arc basins appear to have been active in arc volcanism. It is considered that the formation of marginal basins and arc volcanism have been alternately active with time. Non back-arc basins seem to have been formed concentrically at about 25 Ma - 35 Ma and 55 Ma - 80 Ma. In the back-arc basins distributed near northwestern (NW) and southwestern (SW) Pacific around equator, it is revealed that production peak has been moved from SW (55 - 80 Ma) through NW (15 - 55 Ma) to SW (0 - 10 Ma) Pacific in time and space. It is supposed that the periodic formation of marginal basins with time is associated with spatial cycles.

The purpose of this paper is to investigate the relationship between static pressure recovery and velocity distributions in case of swirling flow into a conical diffuser. In this research, velocity distribution is measured by a multi-hole yaw-meter. The following conclusions can be drawn from the experiments. (1) The static pressure recovery depends strongly on the strength of a swirl. (2) A high pressure recovery coefficient is achieved by inserting a solid core into the diffuser center.

초 록 덕유산 지역의 개미의 분포와 개미상을 밝히기 위하여 덕유산 지역을 5개 코스로 나누어 1986년, 1989년, 1991년의 3개년간 16차례에 걸쳐 476 colony를 채집하여 4아과 22속 44종의 분포를 확인하였다. 아과별 종조성은 두마디개미아과가 12속 21종으로 가장 많고 불개미아과가 6속 20종, 침개미아과가 3속 4종, 시베리아개미아과가 1속 1종 이었다. 수직분포의 경향은 고도 500 m에서 전체종의 93%인 41종의 집중 분포하고 있었으며 종별수직분포의 상한계선은 고도 700 m에서 일본침개미와 장구개미를 포함한 5종, 고도 1,000 m에서는 침개미, 호리가슴개미, 나도누은털개미, 스미드개미를 포함하여 10종이 분포하고 있었다.

The wind pressure distributions were analyzed to provide fundamental criteria for the structural design on e single-span arched house according to the wind directions through the wind tunnel experiment. In order to investigate the wind force distributions, the variation of the wind force coefficients, the mean wind force coefficients, the drag force coefficients and the lift force coefficients were estimated by using the experimental data. The results obtained are as follows: 1. When the wind direction was normal to the wall, the maximum positive wind pressure along the height of the wall occurred approximately at two-thirds of the wall height because of the effects of boundary layer flow. 2. When the wind direction was 30˚ to the wall, the maximum positive wind force occurred at the windward edge of the wall. When the wind direction was parallel to the wall, the maximum negative wind force occurred at the windward edge of the wall. 3. The maximum negative wind force along the width of the roof appeared around the width ratio, 0.4, and that along the length of the roof appeared around the length ratio, 0.5. 4. According to the results of the mean wind force coefficients analysis, the maximum negative wind force occurred on the roof at the wind direction of 30˚. 5. The wind forces at the wind direction of 30˚ instead of 0˚ are recommended in the structural design of supports for a house. 6. To prevent partial damage of a house structure by wind forces, the local wind forces should be considered to the structural design of a house.

The Cretaceous granitoids related to base metal mineralization in the studied area consist of hornblende - biotite granite, leucocratic granite and micrographic granite. The major - and trace element data from granitoids, when plotted on the Hacker diagram, average contents of Al₂O₃, CaO, Mg0 and Fe₂O₃ decrease while SiO₂ increases in granitoids from Dolsan toward Namhae and Kwangyang areas. Average content of Rb is higher in Kwangyang area while Ba and Sr decrease in granitoids from Dolsan toward Namhae and Kwangyang, and as shown in triangular diagram of RbBa-Sr, which indicates gradual differentiation of granitic magma from Dolsan toward Namhae and Kwangyang. And, studies of major element variation, calc-alkaline index(61.5) and AFM diagram of granitoids indicates that granitoids have been crystallized from a calc-alkaline magma generated by partial melting of the subducted Pacific Oceanic Crust(or Kula plate) at the compressional plate margin, that is, the volcanic arc. Na₂O/K₂O ratio and magnetic susceptibility of granitoids indicate that they belong to I-type and magnetite series. As shown in atoms against pressure diagram, variation to the number of cations Al^(4+) Al^(6+), (Al+Fe^(3+)^(6+), Si, (Mg+Fe^(2+)), and A-site (Na+K) in amphiboles are shown as functions of estimated crystallization pressure, which the amphibole in granitoids crystallized in the pressure range of 1.8 - 3.0 kbar. According to the two-feldspar geothermometry on granitoids of Kwangyang, Dolsan and Namhae areas, the temperature of cessation of exsolution in perthitic alkali feldspars are 476 - 607℃, 489 - 640℃ and 465 - 629℃, respectively, at assumed pressure of 3 kbar, which may be the result of rapid crystallization in the shallow crustal level(5 - 7.5 ㎞).

The granitic rocks in the southern part of the Kyeongsang basin, Korea, are divided into seven masses based on the petrographical features. They are generally characterized by shallow-depth intrusions. The chemical compositions of amphibole and biotite from the granitic rocks show systematic variations in Fe/(Fe+Mg) ratios as well as Mn and F contents. Hornblende geobarometer indicates low pressure condition (less than 2.3 kbar) at the time of final crystallization of hornblende crystals. The composition of biotite indicates that oxygen fugacity has been almost buffered during crystallization regardless of rock types. The oxygen fugacity is presumably close to the value of Ni-NiO buffer. From the Fe-Ti oxide geothermometry, it seems likely that most of the Fe-Ti oxides have been re-equilibrated during cooling and have suffered oxidation under subsolidus condition.

수평자장을 건 Czochralski(HMCZ) 방법으로 자장강도(B)와 도가니 회전속도(C)가 실리콘 단결정의 산소편석에 미치는 영향에 대하여 연구하였다. B=2, 3, 4kG와 C=4-15rpm에서<100> 방향으로 성장시킨 57mm 직경의 단결정들 내의 산소분포는 대체로 축을 따라서 불균일하였고 톱니모양을 나타내었다. 종래의 CZ 방법과 비교할 때, 이러한 산소분포의 불균일성은 위 강도의 수평자장이 결정성장계면으로의 산소전달에 불안정한 요소로 작용했음을 나타낸다고 볼 수 있다. 반면에 C의 증가는 산소분포의 불균일성의 약화와 산소농도의 전반적인 증가를 유도하였다. 이 결과를 토대로 B=2kG에서 27-36ppma인 산소분포를 가진 단결정이 프로그램된 C에 의해서 얻어졌다. 소자제조공정을 모의한 열처리 과정에서 HMCZ 실리콘의 산소석출은 종래의 CZ 실리콘의 산소석출에 비해서 상대적으로 불균일하였고, as-grown 상태에서의 고르지 못한 HMCZ 실리콘의 산소분포가 주요 원인임이 밝혀졌다.