EP53B-1012
Measurement of Channel Morphology in a Headwater Stream using Low-Altitude Photography and a 3D Model Software

Friday, 18 December 2015
Poster Hall (Moscone South)
Keisuke Nidaira1, Marino Hiraoka1, Takashi Gomi1 and Yoshimi Uchiyama2, (1)Tokyo University of Agriculture and Technology, Tokyo, Japan, (2)Kanagawa Prefecture, Atsugi, Japan
Abstract:
We developed a method for measuring detail channel morphology using a low elevation photographic scanning. This study was conducted in a 36-m step-pool channel segment in a headwater stream of Ooborazawa watershed located in 20 km south of Tokyo. The channels were covered by Boenninghausenia japonica and Oplismenus undulatifolius var. undulatifolius. Therefore, topographic measurement in high altitude (up to 5 m) using a drone is not applicable. D50 and D90 of channel substrates were 4 cm and 21 cm, respectively. A plastic case that equipped with two digital cameras (RICOH CX5) is mounted at the top of 2.2 m of a glass fiber pole. Photos were taken every 5 seconds from 1.8 m above ground surface. Eleven ground control points (GCP) were installed and measured coordinates. We developed digital 3D topographic model using PhotoScan Pro edition version 1.0.0 and the developed 1 cm contour map using ArcGIS version 10.2. Furthermore, we measured the number, height, and length of steps for examining the accuracy of data. Resolution of obtained topographic model was from 9 to 11 mm per pixel. 1 cm of particle was identified using photo was 1 cm. Estimated step height was agreed to the measured step height in the field. We detected maximum channel scour from October to December, 2014 with (146.5 mm/day for maximum daily rain) occurred at pools with 13cm changes , while 5 to 10 cm of changes in sediment deposition occurred from Mya to June, 2015 with 78.5 mm/day of maximum daily rain. Disposition of sediment was concentration within the sequences of step structures. Our method allows us for understanding detail sediment movement and resultant localized channel changes in steep channels.