LIDAR ASSESSMENT OF SEDIMENT TRANSPORT RELATED TO THE REMOVAL OF MARMOT DAM, SANDY RIVER, OREGON
The LiDAR imagery includes two data sets acquired before the dam removal and two afterward. Esri ArcMap 10 was used to process the LiDAR-derived DEMs to determine changes in surface elevation between successive images. The data resolution allowed for creation of 3-meter DEMs. Differencing two DEMs resulted in a new raster showing the locations of erosion and deposition for that period of time. A gain in elevation represents deposition of sediment while a loss represents erosion. The locations, vertical elevations, and horizontal dimensions of sediment bars were measured for each year to calculate the change in the volume of stored. Each DEM was differenced from the previous year in order to show the sequential change in sediment distribution. The net erosion and net deposition were determined for each successive pair of LiDAR acquisitions to determine the cumulative volume of mobilized sediment and the spatial distribution of erosion and deposition. These observations will be used to determine whether the previously unaccounted sediment can be located, as well as any systematic patterns in sediment redistribution over the 4-year period.