Differences in amounts of pools and riffles between upper and lower reaches of a fully sedimented dam in a mountain gravel-bed river

To understand the extent of changes in the habitat structure of macroinvertebrates due to channel degradation, the amount of pools and riffles and bed materials were determined in upper and lower reaches of a fully sedimented dam in a mountain gravel-bed river. Pools occurred more frequently and individual pools were longer in the lower reach than in the upper reaches; the total length of pools in the former was four times than in the latter. In contrast, individual riffles in the upper reaches were longer than and the total length double that in the lower reach. The main bed materials in the upper reaches were moderate-sized cobbles and boulders (diameter 10–40 cm), which generated moderately steep and long riffles. In the lower reach, these materials were scarce and the main bed materials were large boulders (>50 cm) and bedrock, which generated steep and short riffles; finer materials (