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FLOOD10391 (2)
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Last modified
11/23/2009 12:41:10 PM
Creation date
7/25/2007 12:47:51 PM
Metadata
Fields
Template:
Floodplain Documents
County
Boulder
Community
Boulder
Stream Name
South Boulder Creek
Title
Proposal, South Boulder Creek Floodplain Study Hydrology and Hydraulic Analyses, RFP No 17-2003
Date
3/14/2003
Prepared For
Boulder Department of Public Works Utilities Division
Prepared By
Ayres Associates
Floodplain - Doc Type
Floodplain Report/Masterplan
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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />AYRES <br />ASSOCGAYES <br /> <br />Finite Element vs. Finite Difference Models <br /> <br />Ayres Associates has experience in several 2-dimensional models, including the Corps <br />of Engineers RMA-2 model, the Federal Highway Administration FESWMS model and <br />the proprietary FLO-2D model. Each of these models has specific strengths and <br />weaknesses. Therefore, we select the most appropriate model based on the physical <br />conditions of the project and the needs of the client. The first two models are finite <br />element (FE) models and the third is a finite difference (FD) model. <br /> <br />The two FE models are well suited for detailed hydraulic and hydrodynamic modeling <br />but can be very challenging to apply to some conditions. RMA-2 is not recommended <br />for this project because it cannot accurately simulate areas with near-critical and <br />supercritical flow. Given the steep grade of the main channel, side channels and <br />floodplain areas, near-critical flow is expected and RMA-2 would probably not maintain <br />numerical stability. FESWMS can accurately simulate sub- and supercritical flow <br />conditions and would be our recommendation if a steady state model would be <br />required by the City of Boulder. We do not recommended FESWMS for this project <br />because we expect significant numerical instability problems for dynamic flow <br />simulation as areas of the model wet during the rising limb of the hydrograph and dry <br />as the hydrograph recedes. Large areas of wetting and drying expected for South <br />Boulder Creek would be a significant technical obstacle for either FESWMS or RMA-2. <br />The two FE models are also less suitable when the main channel is very small, as is <br />the case at South Boulder Creek. <br /> <br />FLO-2D is the most appropriate model for this project. Although the finite difference <br />(FD) approach has some limitations related to the level of detail that can be achieved, <br />this model should be numerically stable and accurate for South Boulder Creek <br />conditions. In FLO-2D, a uniform grid is required for the entire model, so some.small <br />topographic variation could be obscured depending on the grid size selected. The FD <br />approach in FLO-2D uses slightly simplified equations of motion, but is more <br />numerically stable and, therefore, much better for this project. FLO-2D includes <br />overland flow, channel flow, structures, levees, and embankments, and can include <br />rainfall, infiltration, and sediment transport if necessary. FLO-2D includes good flow <br />visualization, and Ayres Associates has experience with importing FLO-2D output into <br />the Microstation CADD program for additional floodplain delineation and enhanced <br />graphical output. Ayres Associates has extensive experience in post-processing 2- <br />dimensional model output for additional analysis and flow visualization purposes. This <br />experience will be applied to FLO-2D results by importing the results into the graphical <br />environment used for finite element modeling. Therefore, this project will have the <br />numerical advantages of finite difference modeling combined with the flow visualization <br />advantages associated with finite element modeling. <br /> <br />Topographic Mapping for Hydraulic Analysis <br /> <br />We recommend that new topographic mapping be developed for hydraulic modeling <br />and floodplain delineation. The new topographic mapping should be at least to a 2-ft <br />contour interval and preferably to a 1-ft contour interval to very accurately identify split <br />flow paths and other topographic features. Direct survey of the South Boulder Creek <br />channel, ditches, other channels, roadways, and levees should also be conducted for <br />model development. The first step in developing the FLO-2D model will be developing <br />a HEC-RAS low-flow model of the South Boulder Creek channel. A FLO-2D model <br /> <br />22 <br />
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