FOREST DISTURBANCE BY THE 1926 MUDFLOW AND REVEGETATION PROCESSES AT MT.TOKACHI VOLCANO

Research Project

Project/Area Number	03660145
Research Category	Grant-in-Aid for General Scientific Research (C)
Allocation Type	Single-year Grants
Research Field	林学
Research Institution	HOKKAIDO UNIVERSITY
Principal Investigator	YAJIMA Takashi HOKKAIDO UNIV., FAC.OF AGR., ASSOCIATE PROF., 農学部, 助教授 (90142702)
Co-Investigator(Kenkyū-buntansha)	NAKAMURA Futoshi HOKKAIDO UNIV., FAC.OF AGR., ASSOCIATE PROF., 農学部, 助教授 (90172436) SHIMIZU Osamu HOKKAIDO UNIV., FAC.OF AGR., INSTRUCTOR, 農学部, 助手 (20178966) SHIBUYA Masato HOKKAIDO UNIV., FAC.OF AGR., INSTRUCTOR, 農学部, 助手 (10226194)
Project Period (FY)	1991 – 1992
Project Status	Completed (Fiscal Year 1992)
Budget Amount *help	¥2,200,000 (Direct Cost: ¥2,200,000) Fiscal Year 1992: ¥900,000 (Direct Cost: ¥900,000) Fiscal Year 1991: ¥1,300,000 (Direct Cost: ¥1,300,000)
Keywords	Revegetation / Mudflow / Disturbance / Picea glehnii / Soil analysis / 泥流流下状況 / 立地
Research Abstract	The 1926 mudflow at Mt.Tokachi Volcano created a vast, bare land mass with heterogeneous and edaphic conditions. Forests were regenerated mainly by seedings supplied from remaining vagetation islands and surrounding areas. Vagetative regrowth was possible in downstream and boundary areas of the mudflow where forests suffered light damage. Revegetated forests display a mosaic structure, consisting of small or large elongated patches. Atands can be classified by dominant soecies, such as Picea glehnii, P.jezoensis, Abies sachalinensis, and betula spp. Pure Betula stands are found at the boundary areas of the mudflow where fine sediment was deposited. Picea glehnii stands were established in the central areas of bounder-rich soil deposits. Dwarf bamboo(Sasa spp.) dominated the floor of Betula stands, and it is likely that its rapid recovery playd an important role in forming Betula stands. Soil analysis clearly indicated the strong linkage between edaphic conditions and stand types. We concluded that differences in atand structures of revegetated forests could be attributed the heterogeneous site conditions created by the mudflow.