The recycling cell formation problem means that disposal products are classified into recycling part families using group technology in their end of life phase. Disposal products have the uncertainties of product status by usage influences. Recycling cells are formed considering design, process and usage attributes. In this paper, a novel approach to the design of cellular recycling system is proposed, which deals with the recycling cell formation and assignment of identical products concurrently. Fuzzy clustering algorithm and Fuzzy-ART neural network are applied to describe the states of disposal product with the membership functions and to make recycling cell formation. This approach leads to recycling and reuse of the materials, components, and subassemblies and can evaluate the value at each cell of disposal products. Application examples are illustrated by disposal refrigerators, compared fuzzy clustering with Fuzzy-ART neural network performance in cell formation.

최근 유럽연합에서는 동물실험을 통하여 검증된 성분을 함유하고 있는 화장품에 대하여 판매를 금지할 것을 선언하였다. 그리하여 동물실험을 대체할 동물실험 대체모델의 개발이 필요해졌다. 인공피부는 화장품, 의약품 및 의료 기기의 안전 테스트에 있어서 아주 중요한 시스템이다. 본 연구에서는 기저막과 표피를 가지고 있는 최적의 인공피부를 만들기 위한 시도를 하였다. 이러한 목적으로 중간엽줄기세표(MSCs, mesenchymal stem cells)와 지방전구세포를 진피 세포인 섬유모세포와 혼합하여 진피대체물을 만들었다. 기저막과 표피의 형성은 면역조직화학 염색(immunohistochemical stains)을 통하여 확인하였다. 여러 가지 모델 중에서, 중간엽줄기세포를 혼합한 모델에서 표피의 두께가 제일 두꺼웠으며 또한 PCNA와 involucrin의 분포가 실제 사람피부와 비슷하였다. 결론적으로, 본 연구의 결과는 진피대체물에 중간엽줄기세포를 혼합한 인공피부가 동물실험 대체모델로 개발될 수 있다는 점을 제시한다.

The formation mechanism of the snow cells of the Yellow Sea associated with snowfall over the southwestern part of Korea on 4 February, 2004 has been investigated using special upper-air sounding and radar data obtained for the KEOP (Korea Enhanced Observing Period) Intensive Observing Period (IOP). Results show that the types of snow cells for the selected period are classified into L(Longitudinal)-mode, Low-level convergence, and T(Transverse)-mode with their evolution from L-mode to T-mode. In particular, the existence of low-level warm and humid layer associated with temporally southwesterly inflow for about 4 hours provides a favorable condition in forming the T-mode snow cells. The vertical depth of the T-mode snow cells is deeper than that of L-mode ones due to the southeastward penetration of cold and dry air into relatively warm and humid air. In addition, it is found that wind shear vector between 1000 hPa and 600 hPa is one of the factors which control the orientation of snow cells in formation embedded into the snowbands for the both modes.