The amount and rate of soil erosion on hiking trails were monitored around the Susoaidaira area, Daisetsuzan National Park, Hokkaido, which experiences one of the heaviest visitations in mountain national parks of Japan. Method of Cole (1983) was used to understand the changes of the trail surface. Only four sites among nine sites delivered the results for the 10- to 13-year period.
The rates of soil erosion varied from site to site: 193.4 to 1, 402.5cm
2/yr for the period of 10-13 years. Also, the amount and rates varied from year to year even at the same site. These results suggest that short-term monitoring of 1-3 years cannot provide the accurate amount/rate of erosion. Erosion rate derived from short-term monitoring becomes larger when heavy rainstorm comes as the case in 1999. Continuous supply of meltwater of snow in late spring and summer contributes to soil erosion in Daisetsuzan National Park; however, heavy rainfall should be a great contributor to the soil erosion as well.
It is emphasized that mid-term and long-term management of mountain national parks requires understanding of soil erosion derived from long-term monitoring. At the same time, repeat measurement at short intervals should be also placed in the long-term monitoring.
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