Using the principal component analysis and clustering Forest resources are consistently necessary in the future. It takes much time to produce and breed them. However it is difficult to do due to recent social situation. Considering global environment, forest policy should be considered as a global scale rather than a regional one. At least, the policy needs a national scale concern. In order to support forestry, elementary data are needed. In this study, forest characteristics in Ishigawa-gen province have been analyzed through main component analysis and clustering. The results are shown in fig.5 and fig.6.

현대 산업사회의 큰 문제로 대두되고 있는 도시소각재를 용융시킨 용융슬래그를 출발물질로 하여 부가가치가 높은 P형 제올라이트를 "hydrogelation"법과 "clay conversion"법을 혼합한 새로운 방법에 의해 수열합성하였다. 출발물질은 용융슬래그 이외에 Si 공급원으로 시판되는 규산소다용액을, Al 공급원으로는 Na2O/Al2O3의 비가 약 1.2인 알루민산소다용액을 사용하였다. 80℃의 반응 온도에서 P형 제올라이트의 최적합성조건은 SiO2/Al2O3의 비율 3.2~4.2, H2O/Na2O의 비율 70.7~80.0, 그리고 반응시간이 15시간 이상일 때이었다. P형 제올라이트가 합성되었을 때, 크기가 일정하지 않은 용융슬래그 입자들은 용해되어 사라졌으며, 그 대신 균일한 크기의 P형 제올라이트 결정이 형성되었다. 암모니움 아세테이트법에 의해 측정된 합성 제올라이트의 양이온 교환능은 240cmol/kg 정도이었다.

In case an average accumulation of the investigated area is 200㎥/ha with cutting age of 80 years applied, annual workload will be 77ha and require 5 teams; each team consisting of 5 persons, enabling stabled supply of lumbers of 15,500㎥ every year. If one cutover is less than 2ha with cutting age of 80 years applied, it's possible to protect the peculiar ecology and secure stabled labor, workload and lumbering. It may become model forest out of tropical forest management which is controversial all over the world. Of course this presupposes construction of access roads.

Forest management starts from forest road facility, which is designated as generation source of muddy water in mountain stream during initial stage of establishment. Therefore, this study reviewed the effect of suspended sediment generated in forest road surface on the muddy water in mountain stream with respect to marsh area of forest. As a result, characteristics of outflow of suspended sediment was understood, and it was judged that generation of suspended sediment due to establishment of forest road is diluted by mountain stream this charged from drainage area so as to have small effect on muddy water in total mountain stream.

Suspended sediment outflows mainly by natural situation and artificial action and affects in down-stream. This research studied suspended sediments origination in forests size and mountain stream for natural situation, density for artificial action, and measured the size and possible quantity of suspended sediments origination and studied obstruction method of the generation by artificial action. As the result, I found that the size of generation is about 2～3% of forest size and the forest size which is affecting bare area of valley is about 1～2ha. In addition, possible outflow segments quantity by artificial facilities is assumed to be maximum 200ton/ha and abstract of mountain incline for mountain development needs minimize bare area valley by make right angle with minimum size.