7 D6. Geomorphology, Quaternary Geology, and Soils (Posters)
Friday, 20 March 2020
8:00 AM - 12:00 PM
Lake Anne
SUSTAINABILITY ANALYSIS AND SEDIMENTATION IN THE LOWER RESERVOIR ONEONTA, NY; A DRAINED PERSPECTIVE
Paper number: 7-7
Program: Technical Sessions
Time: 8:00 AM – 12:00 PM
Authors
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Keith BrunstadState University of New York - Oneonta, Oneonta, NY
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Les HasbargenState University of New York College at Oneonta, Oneonta, NY
Abstract
Based on several measurements in the down scan sonar profiles, it was determined that the average sediment thickness above a gravel layer is ~ 2 m. In the sonar profile the gravel layer was reflected and interpreted to be indicative of a migrating delta associated with previous draining of the reservoir. Coring operations revealed a max recovery of 101 cm interrupted by the gravel layer. Recovery rates with the Vibracoring were poor with an average recovery rate of 68%. To mitigate this issue a ~ 1.5 m soil profile of the channel banks was collected. Exposed banks along the channel revealed alternating layers of silty clay, mixed organics, and gravel. These observations indicate that sedimentation is driven by spring and fall high precipitation flow events from Oneonta Creek into the Lower Reservoir. Drone imagery captured a month apart was converted into 3D SfM models and was used to create channel profiles to evaluate channel evolution and volume. Calculated total water volume of ~ 46,822.27 m3 for the Lower Reservoir and ~ 1,667,720.1 m3 for Wilber Lake. Approximately ~ 27,213 m3 of sediment has been deposited in the Lower Reservoir from the Oneonta Creek inlet and ~ 101,131.7 m3 of sediment has been deposited in Wilber Lake.
Geological Society of America Abstracts with Programs. Vol. 52, No. 2
doi: 10.1130/abs/2020SE-344995
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