This study examines the Symbolic notions of Haein Buddhist Monastery based on the context of Feng-shui. Through the study, it is verified that the geographical features surrounding the Haein Buddhist Monastery are imbued with the basic layout of the monastery and the constitutional elements of the Haein Buddhist Monastery are structured and formed with the architecture and landscape of the monastery. Thus, the study maintains that the siting and the arrangement of the Haein Buddhist Monastery reflect the context of Feng-shui.

기후변화로 인하여 전 세계는 과거에 경험하지 못했던 많은 재산 피해를 받고 있다. 자연재해로 인한 피해를 대비하기 위한 가장 합리적인 방법으로 풍수재담보 보험이 대두되고 있으나 국내의 경우 활성화되지 못하고 있다. 본 논문에서는 풍수재담보 보험의 활성화를 저해하는 요인으로 두 가지를 논의하고자 한다. 첫 번째는 요율제도의 문제점이다. 풍수재담보의 경우, 손해율이 매우 높으며, 이는 풍수재담보를 인수하면 할수록 손해라는 인식이 보험 업계에 퍼지게 된 원인이다. 두 번째는 언더라이팅 자료의 부재를 들 수 있다. 보험인수 결정을 위해서는 고시요율이 풍수재 리스크에 부합하는지를 검토하는 언더라이팅이 필요하다. 하지만 현 보험업계에서 제공받을 수 있는 풍수재담보 언더라이팅 정보는 거의 부재한 상태이며, 이로 인하여 방어적인 인수결정을 하고 있다. 위 두 가지 문제를 해결할 수 있다면 풍수재담보 보험의 활성화가 기대된다. 본 논문에서는 풍수재담보 보험의 활성화를 위해서 현행의 등지요율제도에서 개별 건물의 풍수재 리스크에 부합하는 요율을 책정할 수 있는 개별요율제도 도입의 필요성과 보험업계의 언더라이팅을 지원하는 기관의 필요성에 대해 기술하였다.

To analyze the water characteristics in the dry and wet seasons, the data for temperature, salinity, nutrients and chl-a were used, which were observed in the south coastal area of Korea during April to October 2000. At Yeosu in the south coast of Korea, the higher values of 35.0 psu in salinity were shown in March and April, the lower values of 23.0 psu in salinity were shown in August and September. The annual range of salinity was 12.0 psu. The total amount of precipitation in the wet season (July to October) was occupied 68% (about 846 mm) during 2000. The precipitation of the dry season (November to June) was occupied 32% (about 394 mm) in the year. In the coastal area, the salinity variation is distinct in the period of July to October. Based on this result, we divided the season into two parts: the dry season during April to June and the wet season during July to October. Factor analysis was shown that temperature has strong negative relation and nutrients show positive relations in the dry season by the factor 1, which explains the total variance of 50.6% at the surface water. In the wet season, salinity has negative relation and nutrients show positive relation by the factor 2, which explains the total variance of 33.5%. The bottom layer also showed similar to those of surface water in the results of factor analysis. These mean that nutrients become rich due to the freshwater inflow in the wet season. The low saline water is shown not only in the south coast but also in the overall region in the South Sea of Korea. It is suggested that the South Sea of Korea may call a ROFI (Region of Freshwater Influence) system in summer.