This study was investigated to viscosity, color, chemical properties, and lipid and fatty acid composition for examination of physical and chemical characteristics of sesame oils. Yield of sesame oil was higher in Ansan sesame than that of Chinese and Dambaek sesame. Viscosity of sesame oils was higher than that of shame oils from Dambaek and Chinese sesame, but turbidity and sedimentation rate were higher in Dambaek's sesame oil than those of Ansan's and Chinese sesame oils. In the acid value, saponification value and iodine value of sesame oils, and chemical characteristics of Dambaek's sesame oil were better than those of the others. The neutral, glycolipid and phosholipid contents of sesame oils were 91.1∼92.1, 2.5∼3.5 and 5.5∼6.4%, respectively. The major fatty acids of sesame oils were oleic, linoleic palmitic and stearic acid. The content of oleic acid was higher in Dambaek's and Ansan's sesame oil than that of Chinese sesame oil, and the content of linoleic acid was higher in Chinese sesame oil than the others. The fatty acid composition of neutral lipid, glycolipid and phospholipid were similar to those of total lipid. The ratio of unsaturated fatty acid and saturated fatty acid was higher in Korean sesame oils than those in Chinese sesame oil. The mineral(Mg, Cu, Fe, In, Al, Mn) content of Korean sesame oils was higher than that of Chinese sesame oil. and heavy metals(Cu, Ag, Pb, Cd, As) were not detected.

밀의 경ㆍ연질성 구분을 효과적으로 수행할 수 있는 새로운 방법을 모색하기 위해 주상분석법을 이용한 측정법과 기존의 몇 가지 측정방법의 정확도 및 상관관계를 상호 비교 분석한 결과를 요약하면 다음과 같다. 주상분석법을 이용하여 측정한 곡립의 초자질율은 경도계 및 NIRS에 의한 방법과 고도로 유의적인 상관이 인정되었으며 곡립의 단백질 함량과도 분석방법간에 고도로 유의한 상관이 인정되었다. 주상분석법을 이용한 초자질율의 측정은 반복간의 오차가 적고, 측정된 결과가 기존의 경도측정 방법과 상관이 매우 높아 새로운 연경질성의 구분기준으로 사용할 수 있었으며, 곡립의 연경질성 분석후 곡립의 발아력이 상실되지 않으므로 밀의 용도별 고품질 육종효율 증진을 위한 초기 선발방법으로 사용이 가능할 것으로 사료되었다.

본 연구에서는 수자원 관리와 저수지의 최적 운영에 영향을 미치는 위험의 수준을 결정하고 위험의 특징을 규명하기 위하여 위험도 평가시 평가기준이 될 수 있는 신뢰도, 복원도, 취약도 등의 지표를 수학적으로 정의하였다. 그리고 저수지 시스템의 기능 수행 능력을 평가하기 위해서 추계학적 모의 발생기법을 통하여 모의 발생된 월 유입량 자료를 이용하여 대청 다목적댐을 대상으로 저수지 물수지 분석을 실시하였다. 분석 결과를 토대로 저수지 시스템의 기능 수행 능력을

본 연구에서는 낙동강유역 진동, 현풍, 왜관 지점의 연평균 유량자료에 대하여 다변량 추계학적 모형올 적용하여 가뭄특성을 해석하였다. 추계학적 모형으로는 다변량 자기회귀 (MAR) 모형과 다변량 contemporaneous 자기회귀 (MCAR) 모형올 사용하였으며, 잔차계열의 왜곡도 검사, 계열상관도(correlogram) 등의 적합도 검정을 통하여 MCAR(1) 모형과 MAR(1) 모형올 적정 모형으로 선정하였다. 또한 MCAR(1) 모형과 MAR(1)

This experiment carried out to find the storage life according to the kinds of packaging material. Sheridan(Grape) which was fumigated SO2 were wrapped with polyethylenes(Bio-PE and PE) and stored at under 90% RH modified condition. The resorts were summarized as follow. Natural weight loss was increased according to the storage time during the 135days storage that was only 1.0-1.7% in sealing section while 10% in non-sealing section. Abonrmal fruits were increased as the storage time was increased and it was 6.6-6.7% in sealing section while 100% in non-sealing during the 135days storage. Quality of appearance and taste are better in sealing section than non-sealing section and it was good in Bio-PE sealing section between packaging materials. Moistrue content was de creased as the storage range was increased and the decreasing rate of that during the storage was 4.9-5.2% in sealing section between treatments. During the storage range increased, the soluble solid degree was increased in non-sealing section but decreased in sealing section.

The precious serpentine, referring to a rare and highly valuable gem variety of serpentine group minerals, is found to occur in serpentinite from Booyo Gren Jade Mine which is located in Oesan-myun, Booyo-gun of Chungchungnam-do. Geommological properties of the precious serpentine have been investigated by use of polarizing microscope, specific gravity balance, refractometer, hardness pencils, X-ray diffractometer, XRF, ICP-MS analyser, and infrared absorption spectroscope.The precious serpentine from Booyo is colored deep green with oily luster and semi-transparent. It is highly tough and Mohs's scale of hardness is measured to be 5-6. Specific gravity is determined to be 2.67, and a single refractive index ND=1.56 is observed by a spot method, using sodium light source. X-ray powder diffraction data is represented by the reflection lines at 7.40(100), 4.64(25), 3.68(68), 2.757(69), 2.530(49), 2.549(32), and 1.710(21a), which compares very well with that of antigorite of serpentine group minerals. The major chemical compositions of the precious serpentine group minerals. The major chemical compositions of the precious serpentine are SiO2 42.49%, MgO 39.08%, Fe2O3 3.85%, and H2O 11.87%. Besides, trace elements such as Cr(2188), Ni(1110ppm), Co(58ppm), and Ta (108ppm) are relatively spectrum shows peaks at 3670, 1190, 1070, 980 and 610cm-1. Strong absorption at 3670cm-1 is due to OH stretching, and 1190, 1070 and 980cm-1 due to SiO stretching. The absorption 610cm-1 is formed by alteration of pre-existing ultramafic rock, namely peridotite, with an introduction of fluid with very little content of CO2, under 400℃ environment. Magnetite inclusions, finely disseminated in the precious serpentine, may be a result of Fe precipitation, during serpentinization of olivine-bearing country rock.