• Journal of Nutrition and Health
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• 제57권3호
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• pp.349-364
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• 2024

본 연구는 AHP를 적용하여 영양교사 및 영양사의 학교급식 식단 작성 시 고려 요인들의 상대적 중요도를 학교급별로 비교함으로써 효율적인 학교급식 식단 구성 방안에 대한 기초자료를 제공하고자 하였다. 모집단인 전국 유·초·중·고·특수학교 20,548개교를 대상으로 표본을 추출하여 총 395부 중 166부를 회수하였고, SPSS 통계 프로그램을 이용하여 CR이 0.2 이하인 응답에 대해 분석을 진행하였다. AHP를 이용하여 학교급식 식단 구성의 각 분야별 상대적 중요도를 분석한 결과 조리 인력 및 시설, 기호도, 영양의 균형, 조리 과정, 식재료 순으로 높게 나타났으며, 각 분야의 가장 중요한 하위 영역은 조리종사자의 숙련도, 급식대상자의 기호도, 영양소 섭취 기준, 위생, 식품비 예산이었으며, 이는 각 학교급에서 가장 높은 비율을 차지하였다. 더불어 급식 대상자의 기호도, 영양소 섭취 기준, 식품비 예산은 식단 작성 시 어려운 점의 상위 3가지 항목과도 일치해 식단 작성 시 반영이 어려울수록 상대적 중요도가 높게 나타남을 확인할 수 있었다. 본 연구는 향후 학교급식 식단 구성 및 관리 업무 효율 증대에 기여하며 정책 운영 방향 설정을 위한 기초자료로 활용될 수 있을 것으로 판단된다.

• 자원환경지질
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• 제2권4호
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• pp.73-90
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• 1969

The area studied is a southwestern part of Okcheon geosynclinal zone which streches diagonally across the Korean peninsula in the mid-central parts of South Korea, and is bounded by Charyeong mountain chains in the north and by Sobaek mountain chains in the south. The general trend of the zone is of NE-SW direction known as Sinian direction. Okcheon system of pre-Cambrian age occupies southwestern portion of Okcheon geosynclinal zone, and Choseon and Pyeongan systems of Cambrian to Triassic age in northeastern portion of the zone. It was defined by the writer that the former was called "Okcheon Paleogeosynclinal zone" and the latter "Okcheon Neogeosynclinal zone," although T. Kobayashi named them "Metamorphosed Okcheon zone" and "Non-metamorphosed Okcheon zone" respectively and thought that sedimentary formations in both zones were same in origin and of Paleozonic age, and C.M. Son also described that Okchon system was of post-Choseon (Ordovician) and pre-Kyeongsang (Cretaceous) in age. According to the present study two zones are separated by great fault so that the geology in both zones is not only entirely different in origin and age, but also their geolosical structures are discontinuous. Stratigraphy and structure of Okcheon system are clearly established and defined by the writer and its age is definitely pre-Cambrian. It is clarified by present study that the meta-sediments in and at vicinity of Charyeong mountain chains are correlated to Weonnam series of pre-Cambrian age which occupies and continues from northeast to southwest in and at south of Sobaek mountain chains, and both metasediments constitute basement of Okcheon system. Pyeongan, Daedong and Kyeongsang systems were deposited in few narrow intermontain basins in Okcheon paleogeosynclinal zone after it was emerged at the end of Carboniferous period. Granites of Jurassic and Cretaceous ages and volcanics of Cretaceous age are cropped out in the zone. Jurassic granite is aligned generally with the trend of Okcheon geosynclinal zone, whereas Cretaceous granite lacks of trend in distribution. Many isoclinal folds and thrust faults caused by Taebo orogeny at the end of Jurassic period are also parallel with Sinian directieon and dip steeply to northwest. Charyeong, Noryeong, Sobaek, and Deogyu mountain chains are located in areas of anticlinorium, and Kyongsang system in narrow synclinal zones. Folds in Okcheon neogeosynclinal zone are generally of N 70-80W direction but deviate to Sinian direction at the western parts of the zone. This phenomena is interpreted by the fact that the folds were originated by Songrim disturbance at the end of Triassic period and later partly modified by Taebo orogeny. Thrust faults of Taebo orogeny coentinue from Okcheon paleogeosynclinal zone into neogeosynclinal zone, forming imbricated structure as previously described. Strike-slip faults perpendicular to Sinian direction and shear faults diagonally across it by 55 degrees also prevail in neogeosynclinal zone. It is concluded from viewpoints on geology and geological structure that l)Okchon geosyncline had changed its location and affected by numerous disturbances through geologic time, and 2)mountain chains in the area such as Charyeong, Noryeong, Sobaek, and Deogyu were originated as folded mountains. Differing from others, however, Sobaek range was probably formed at the time of Songrim disturbance and modified later by Taebo orogeny. It is cut by Danyang-Jeomchon fault at the vicinity of Joryeong near Munkyeong village and does not continue to southwest beyond the fault, whereas southwestern portion of erstwhile Sobaek range continues to Taebaek rangd northeastward from Deogyusan passing through Sangju, Yecheon, and Andong. From these evidences, the writer has newly defined the erstwhile Sobaek range in such a way that Sobaek range is restricted only to northeastern portion and Deogyu range is named for the southwestern portion of previous Bobaek range.