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Title: Three-dimensional simulation of flow, salinity, sediment, and radionuclide movements in the Hudson River estuary

Conference ·
OSTI ID:5267553

The three-dimensional, finite difference model, FLESCOT simulates time-varying movements of flow, turbulent kinetic energy, salinity, water temperature, sediment, and contaminants in estuarine, coastal, and ocean waters. The model was applied to a 106-km (66-mi) reach of the Hudson River estuary in New York between Chelsea and the mouth of the river. It predicted the time-varying, three-dimensional distributions of tidal flow, salinity, three separate groups of sediments (i.e., sand, silt, and clay), and a radionuclide (/sup 137/Cs) in both dissolved and particulate (those sorbed by sediments) forms for over 40 days. The model also calculated riverbed elevation changes caused by sediment deposition and bed erosion, bed sediment size distribution and armoring, and distributions of the particulate /sup 137/Cs sorbed by sand, silt, and clay in the bed.

Research Organization:
Pacific Northwest Labs., Richland, WA (USA)
DOE Contract Number:
AC06-76RL01830
OSTI ID:
5267553
Report Number(s):
PNL-SA-12778; CONF-8508103-2; ON: TI85018225
Resource Relation:
Conference: Conference on hydraulics and hydrology in the small computer age, Orlando, FL, USA, 13 Aug 1985
Country of Publication:
United States
Language:
English