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Mt. Usu, in southern Hokkaido, Japan, erupted in March 2000, and in July 2000 a rainfall-induced mudflow occurred on the northern slope of Mt. Konpira, near to the area that was active in the recent eruption. To investigate the effect of this mudflow sediment on gas exchange by tree root systems and tree mortality rates, gas diffusion rates were measured at two study sites at the foot of this slope...
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