본 연구에서는 경위의 TM-1A와 GPS(모델명: 4000SSI, GPS 45 Garmin corporation)를 활용하여 공주대학교 천문대의 위치를 결정하였다. 경위의를 이용한 관측에서는 2개의 별(α Aur, α Boo)을 선정하여 남중시각과 남중고도를 측정한 다음위도와 경도를 얻어내었다. 또 GPS를 이용한 관측에서는 6개의 GPS 위성에서 보낸 자료를 수신하여 위도와 경도를 측정하였다. 공주대학교 천문대의 위치는 경도 127˚8'33'.16 , 위도 36˚ 28'14'.20로 결정되었다.

The Kongju basin of Cretaceous sedimentary rocks, which is located in the area between Ogcheon fold belt and Gyeonggi massif, is developed by the strike-slip fault and shows elongated rhombic shape trending roughly NE and SW with about 4㎞ in width and 25㎞ in length. Two stripes of ductile shear zone are traced in basement rocks along the boundary of basin. The shear sense of ductile shear zone is suggested to be sinistral. The Cretaceous sedimentary rocks within the Kongju Basin also exhibit deformed state in terms of developments of en-echelon arrayed folds, faults and various kinds of joint systems. The majority of joints is occupied by the fractures whose strikes are approximately normal to the directions of en-echelon arrayed fold axes. The shortening(α^(-1)) of fold system is most pronounced at the central part of the basin and gradually decreases toward both ends of the basin. Both of the strikes of fold axial planes and the azimuths of fold axes change discontinuously to form sigmoidal style of en-echelon arrayed folds. The en-echelon arrayed folds, all plunged towards SW direction, indicate that upper layers of the sedimentary rocks are more distributed in the SW area of the basin than in its NE area. The gravity anomaly around the Kongju basin shows 12∼17 mgal in the outer metamorphic zone and 8∼10 mgal in the basin; and its minimum value occurs in NE-SW direction along the western boundary of the sedimentary basin. The electric resistivity study on both boundaries of the basin shows 200∼300Ω-m in the boundary zone, 500∼600Ω-m in sedimentary rocks, and 1000Ω-m or more in the granite-gneiss region. These values indicate that the east boundary be gentle slope and the west one be steep fracture zone. 'These patterns of geophysical data implicates that the Kongju sedimentary basin should be dipping down to the west.

Around Umsong-Jeungpyeong, the Cretaceous sedimentary basin is located along NNE direction which can be associated with Kongju basin. These basins are studied in terms of field geology, stratigraphy, paleontology, geological structure and geophysical prospecting. Chopyung Groups were deposited in the Cretaceous period : Baegyari Formation conformably over Chopyung Formtion in fault-generated tan and river basin with lake characteristics in the central part. The fossils found for the first time in this study area are Onychiopsis elongata and Euestheria, and they suggest the Chopyung Groups may be identified with the Naktong Subgroups of Kyungsang Basin. After depositon of Chopyung Groups, igneous activity became vigorous : granite intrusion in westside, andesite and basalt in east fault line and tuffaceous deposits. The gravity survey shows high Bouguer anomaly over andesites and metamorphic rocks, and low in granite area. The mean depth of density discontinuity boundary seems to be 1200∼1400m. The electric resistivity survey suggests that the cast boundary of the basin be a vertical fault.

한국의 〈바리공주의 전설〉은 스토리와 캐릭터 창작에서 「바리데기」 저승신화를 대부분 수용하면서 레이스형 시나리오 구조를 지니고 있다. 〈바리공주의 전설1: 지옥의 탄생수〉에 이 어, 〈바리공주의 전설2: 왕의 부활〉을 출시했다. 일본에서 〈페르소나4〉는 현대사회를 무대 로 하여 「이자나기·이자나미」 저승신화를 변용하고 있다. 기존의 페르소나 시리즈의 스토리와 요소들을 포함시켜 ‘이식작(移植作)’과 ‘외전(外典)’ 방법을 통해 여러 장르의 게임을 개발했다. 이는 연속적인 부가 트랜스미디어 콘텐츠를 개발하는데 성공한 사례라고 하겠다. 게임 콘텐츠 를 더 풍부하게 개발하여 부가가치를 높일 수 있는 방안을 다양하게 모색해가야 할 것이다.

20세기 60연대 미국에서는 여러 가지 기세 드높은 운동이 폭발하였다. 여권운동이 그 중의 중요한 하나이며 그 시대의 대표적인 운동이다. 이번의 여권운동과 민권운동, 청년 반란운동 등 유명한 운동 이 지금도 미국 사회에 영향을 미치고 있다. 여권 운동의 발전에 따라 여권주의사상이 영화 작품에도 들어가고 있다. 디즈니가 애니메이션의 선두 주자로써 그 혁신적인 이념을 이용하여 시대의 특징과 요구에 부합한 공주 캐릭터를 하나하나 만든다. 디즈니 애니메이션에서 총 20명의 공주가 나오고 그 중 중요한 10명 이 아래와 같다. 모험심이 강하고 세상에서 가장 아름다운 노래를 부르는 인어공주 아리엘. 순수 황 실 혈통에 순결하고 아름다운 백설공주. 지성과 총명함을 가진 우아한 벨공주. 온유하고 유머감각이 있는 선량한 신데렐라. 꿈을 좋아하고 단순한 오로라공주. 똑똑하고 독립적이고 호기심 많은 쟈스민 공주. 몽상적이고 효성스러운 뮬란. 사랑으로 생명을 감화하고 자기희생 정신 있는 포카혼타스. 용감 하고 아름다운 꿈을 가지고 있는 티아나공주. 아름답고 세상에 가장 긴 머리카락을 가지고 있는 라푼 젤공주. 본문은 디즈니가 각 시기의 작품 예를 들어서 《백설공주》, 《인어공주》, 《겨울왕국》 세 작품 중 《백설공주》에는 여성의식이 거의 없다. 《인어공주》중에는 여성의식의 맹아가 나타난다. 마지 막으로 《겨울왕국》에서는 여성주의의 새로운 단계가 이루어진다. 이 과정에서 디즈니의 작품에 여 성에 대한 인정이 계속 진화하고 있다. 여성지위의 승인은 남성의 부속적인 승인에서 자기 승인으로 변환한 과정이 나타난다. 디즈니사가 어떻게 시대 특징을 따라 여성 캐릭터를 만들고 사상성과 예술 성 양 측면의 성공을 달성한지를 알아보고자 한다.

The purpose of this study is to approach for the flow analysis of changing central-place functions and basic demands between the central city and the small town. Under the rural society progressed, this study examines how the small town changes in the relation to the central city. The subject of study is based on changes in demand for retail and hospitality. The small town is providing basic demands and urban services primary for the rural in the settlement system. Because of the rural depopulation and the aging of society, Retail and hospitality in the rural is reducing of the facility followed. But the majority of related researches are stocks approach. These studies are useful to find out the characteristic of small town, but is difficult to consider the influence of the central city. In this situation after this study using the function index is set up a concept model, it examines for the basis of changes in demand for the small town. The result of the analysis is that the changes of retail and hospitality are more severe in the more small town than in the central city. Whereas the small town with a population decline is consistent with the reduced number of branches, Population growth in the central city is reduced to the number of the Number of branches. The central-place function has been strengthened in the central city. While the younger generation, recreation, etc. related retail are disappearing rapidly, the mainstream of small town is grocery, home improvement, restaurants.

수질 인자들은 다양하고 관계가 복잡하여 수질 변화를 예측하는데 많은 어려움이 있다. 따라서 입력과 출력이 비교적 용이하고 비선형 예측에 적합한 신경망 모형을 이용하여 금강유역 공주지점의 DO, BOD, TN에 대한 월수질 예측을 수행하고 ARIMA 모형과 비교하여 적용 가능성을 검토하였다. 사용된 신경망 모형은 학습을 위해 BP(Back Propagation) 알고리즘을 적용하였으며 학습을 향상시키기 위한 모멘트-적응학습율(Moment-Adaptive

The transfer function was introduced to establish the prediction method for the DO concentration at the intaking point of Kongju Water Works System. In the most cases we analyze a single time series without explicitly using information contained in the related time series. In many forecasting situations, other events will systematically influence the series to be forecasted(the dependent variables), and therefore, there is need to go beyond a univariate forecasting model. Thus, we must build a forecasting model that incorporates more than one time series and introduces explicitly the dynamic characteristics of the system. Such a model is called a multiple time series model or transfer function model. The purpose of this study is to develop the stochastic stream water quality model for the intaking station of Kongju city waterworks in Keum river system. The performance of the multiplicative ARIMA model and the transfer function noise model were examined through comparisons between the historical and generated monthly dissolved oxygen series. The result reveal that the transfer function noise model lead to the improved accuracy.

Serpentinite of the Yesan-Gongju-Cheongyang area has been formed by serpentinization of ultramafic rocks. The ultramafic rock might be composed mainly of oilvine with minor pyroxene and amphibole. Olivine has a considerably restricted chemical compositional ranging from Fo90 to Fo93. Fresh serpentinite containing large amount of oilvine is usually massive in occurrence and dark green to black in color. Serpentine minerals occur not only as major mineral of serpentinite, but also as remnants in the talc ore which was formed from serpentinite. XRD study indicates that antigorie is the most abundant serpentine mineral of the serpentinite. Serpentinite consisting of antigorite usually shows non-pseudomorphic texture, whereas that consisting of lizardite shows pseudomorphic texture. Antigorite is found along the margins or fractures of olivine grains resulting in the formation of network of magnetite which was formed at the time of serpentinization. Lizardite, subordinate constituent mineral of serpentinite, frequently shows pseudomorphic mesh-texture after olivine. The chemical differences between antigorite and lizardite/chrysotile are small, so both minerals are not easily discernible with the electron microprobe. Antigorite occuers as elongate blades, flakes, or plates forming interpenetrating texture to obliterate previous textures. SEM study also shows that most serpentine minerals occur in platy or tabular form rather than in asbestiform. Fractures formed after main serpentinization are observed within the pseudomorphic central olivine grain. Careful observation of the serpentine pseudomorphs gives a great deal of data on the pre-serpentinization nature of the serpentine pseudomorphs gives a great deal of data on the pre-serpentinization nature of the ultramafic rocks. It is inferred that the serpentinization took place after the emplacement of ultramafic body into the relatively wet environment ceased and the cooling intrusive body crossed into the stability field of serpentine. It is inferred that the final pervasive serpentinization took place over a long time, by hydrothermal water supplied through the fracture system produced during emplacement of ultramafic rock.

The talc of the Daeheung, Pyeongan, and Cheongdang (Shinyang) talc deposits in the Yesan-Gongju-Cheongyang area is a hydrothermal alteration product of serpentinite originated from ultramafic rocks. The mineral assemblages in alteration zones are: serpentine, serpentine-talc, talc, talc-chlorite, talc-phlogopite-chlorite, and talc-tremolite-chlorite. Chemical distributions in both the Al2O3-FeO-MgO system and the immobile elements suggest that the serpentine-talc and talc rocks are the reaction product of ultramafic rocks and silicic hydrothermal solution without addition of other granitic components, whereas chlorite-, phlogopite-, and tremolite-bearing rocks are the metasomatic alteration product of serpentinite by hydrothermal solution affected by granitic gneiss. Discontinuities in the immobile element ratios of mineral assemblages are due to changes in their mineralogy. The relative contents of Al2O3, TiO2, Zr in the talc-phlogopite-chlorite and talc-tremolite-chlorite rocks increase irregularly with increasing phlogopite, tremolite, and/or chlorite contents in contrast to other ore types. But the relative contents of Cr, Ni, and Co are uniform in all the mineral assemblages. Chemistry of each mineral assemblage formed by steatitization of serpentinite suggests that Cr, Co, Ni, MgO, and Fe2O3 are relatively immobile during the alteration, whereas SiO2, Al2O3, CaO, and K2O are highly increased. The contents of chlorite, phlogopite, and tremolite in each mineral assemblage might be controlled by addition of Al2O3, K2O, and CaO, respectively. The high contents of other elements than immobile elements in the altered rocks as compared with unaltered rocks indicate that a large amount of elements were introduced from hydrothermal solution up to about 8∼41% in total mass showing maximum value in the talc-phlogopite-chlorite rock.