겨울철에 한우의 추위 스트레스를 경감하기 위하여 개방한우사의 북측 면에 윈치커튼 을 설치하여 차가운 북서풍 또는 북풍을 막아주고 있으나 윈치커튼의 최소 개방 면적 기 준이 마련되지 않은 실정이다. 따라서 본 연구는 한우의 추위 스트레스를 경감하기 위한 북측 윈치커튼의 최소 개방 면적 기준을 마련하기 위하여 수행되었다. 우리나라의 겨울 철 평균 풍속이 2 m/s 정도 되기 때문에 표준 개방한우사를 대상으로 1, 2 및 3 m/s의 풍속을 기준으로 북측 윈치커튼의 최소 개방 면적을 결정하고자 computational fluid dynamics(CFD) 시뮬레이션을 실시하였다. CFD 시뮬레이션 결과에 의하면, 폭이 30 m 인 표준 개방한우사의 경우 북측 윈치커튼의 최소 개방 면적은 10∼15 cm로 나타났다.

The federal government has been implemented several housing policies attempting to improve living quality at Eup-Myun area(rural area), but those were mostly fund supports to reconstruct or repair houses. Existing minimum housing standard is focused on urban apartments and indoor space, but the houses of Eup-Myun area are scattered and are different from urban's house space. Therefore, this study focused on these area, and intended to propose suitable minimum housing standard for Eup-Myun area. Based on literature reviews about housing standard of England, U.S., Japan and South Korea, questionnaire survey was given to 50 experts divided into 2 groups, professors of architecture and researchers on rural environment. This study proposed the direction of new minimum housing standard of Eup-Myun area, it could be added to 2 household composition, be divided into 2 groups, agricultural and non-agricultural residents into facility guideline, be added to outdoor facilities, for example warehouse and open yard, and finally be inserted water quality into environment standard. The results of this study provide insightful strategies for rural housing standard.

The size of minimum order stream has a very sensitive effect on runoff analysis model using the divergence characteristic of stream. Therefore, in this study, the threshold area of minimum order stream has been examined the change characteristic of topographical parameters. The subject basin of the research was the upper basin of the Kumho water gage station which is located in the middle of the Kumho river. The 1:25,000 numerical geography which was constructed 10×10m mesh was used. The range of investigation of topographical parameters are number of stream order, length, area, slope, basin relief, sinuosity ratio, drainage density and total stream length etc. It was found from the result of analysis that the threshold value of minimum order stream has a very big effect on topographical parameters of basin. It was found that the threshold area of minimum order stream revealed under 0.10km2. Furthermore, the parameters showed a serious change except for over 0.10km2.