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The observed results of the hydrophone and sediment trap pit showed that the detectable grain diameter lower limit by hydrophone is about 2 mm, and the volume of sediment measured by the hydrophone is about 2% to 50% of the actual flowing down sediment volume that deposited in trap pit [1], and the ratio depends on the flood conditions such as the season, water depth and so on (Table 1, Fig. 5). Fig. 2 Observation equipment installed in Omukawa River 50th groundsel Fig. 3 Observation data from hydrophone, turbidimeter and water level gauge Kamanashigawa River Omukawa River Installation of observation equipment Sedimentation pit Suspended load meter Water gauge / turbidimeter Hydrophone Bed load sampler Portable observation equipment Current meter Water gauge / turbidimeter Suspended load sampling pipe 50th Groundsel, Omukawa River 2014/4/1 2014/12/1 2015/1/31 2017/4/1 1.0E-07 1.0E-06 1.0E-05 1.0E-04 1.0E-03 1.0E-020 50 100 150 200 250 2014/7 2014/10 2015/1 2015/4 2015/7 2015/10 2016/1 2016/4 2016/7 2016/10 2017/1 2017/4 2017/7 2017/10 1.0E-08 1.0E-06 1.0E-04 1.0E-02 1.0E+00 1.0E+020 50 100 150 200 250 2014/7 2014/10 2015/1 2015/4 2015/7 2015/10 2016/1 2016/4 2016/7 2016/10 2017/1 2017/4 2017/7 2017/10 0.0 1.0 2.0 3.0 4.0 5.00 50 100 150 200 250 2014/7 2014/10 2015/1 2015/4 2015/7 2015/10 2016/1 2016/4 2016/7 2016/10 2017/1 2017/4 2017/7 2017/10 1 2 3 4 5 6 7 8 ※ ①~⑧shows the period of SAR image data at Table 2 Rain fall:Hakushu observation station 364
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Book of Full Papers Symposium Hydro Engineering
Title
Book of Full Papers
Subtitle
Symposium Hydro Engineering
Author
Gerald Zenz
Publisher
Verlag der Technischen Universität Graz
Location
Graz
Date
2018
Language
English
License
CC BY-NC-ND 4.0
ISBN
978-3-85125-620-8
Size
20.9 x 29.6 cm
Pages
2724
Keywords
Hydro, Engineering, Climate Changes
Categories
International
Naturwissenschaften Physik
Technik
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