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Last modified
7/14/2009 5:02:36 PM
Creation date
5/22/2009 12:56:40 PM
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Template:
UCREFRP
UCREFRP Catalog Number
9593
Author
Tetra Tech Inc.
Title
Concept Development Report Hartland Diversion Dam Fish Passage Structure Delta, Colorado.
USFW Year
2000.
USFW - Doc Type
Grand Junction, CO.
Copyright Material
NO
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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 />calibration of the model. Cross section 1900 is the most upstream section located <br />approximately % miles upstream of the diversion structure. The most downstream cross <br />section is 100 and is located 2 % miles below the diversion structure. In addition to the cross <br />section surveys, Reclamation prepared a detailed topographic survey at the Hartland headgate <br />and dam structure. <br />The hydraulic analysis for the development of the alternatives is based on the <br />assumption that the water levels are controlled by the top of the dam and the rock cribbing <br />along the dam does not have a permeability that results in a significant flow capacity. <br />5.1 Model Calibration, hydraulic parameters <br />Manning's n values (roughness coefficient) are estimated from inspection of the <br />channel. The n values within the channel banks are further refined by calibration of the HEC- <br />RAS model based on surveyed water surface elevations. Surveyed water surface elevations <br />are utilized as the downstream boundary conditions and for comparison with the calibration <br />model. Flows utilized in the calibration run are from the USGS gage information at Delta <br />recorded at the time of the water surface elevation surveys. For n-values above the banks, <br />where surveys and calibration runs are not possible, values from the Delta County FIS are <br />used. The flow change option within the HEC-RAS steady flow data editor is used to model a <br />flow intake of 60 cfs at the Hartland headgate. The inline weir editor within HEC-RAS is used <br />to model the diversion as a weir using a weir coefficient of 2.64. <br />Manning's n values in the model are shown in Table 5.1. These selected n values are <br />within the range of values used by FEMA for the hydraulic analysis of the Gunnison River for <br />preparation of the Delta County FIS. The FEMA values are included in Table 5.1 for <br />comparison purposes. A typical coefficient of contraction of 0.1 and coefficient of expansion of <br />0.3 is also used in the HEC-RAS model. The calibration run and results are presented in <br />Appendix C. <br /> <br />20 <br />
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