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Last modified
1/26/2010 10:08:58 AM
Creation date
10/5/2006 4:14:29 AM
Metadata
Fields
Template:
Floodplain Documents
County
Douglas
Community
Douglas County
Basin
South Platte
Title
South Platte River Post Wildfire Floodplain Study, Hayman Burn Area, Douglas County
Date
11/24/2004
Prepared For
CWCB and Douglas County Public Works
Prepared By
Anderson Consulting Engineers
Floodplain - Doc Type
Floodplain Report/Masterplan
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<br />I <br />I <br />I <br />I <br /> <br />approximate-level hydraulic study of the Somh Plane River shortly after the Hayman Fire. <br />FinalJ).. in the 3-mile reach from dO\l,llstream of Trumbull to upstream of Deckers. main channel <br />data was derived from the existing USGSIFIS hydraulic model. Unfortunately, information <br />regarding cross section location and configuration from the USGSIFIS model was not available <br />at the time locations for new surveyed cross sections ".;ere being identified. Based on the <br />assumption that the USGSIFIS model would be adequate for the purposes of the current study. <br />no additional information was gathered in this reach. with the exception of the three bridges and <br />their associated cross sections. Consequently, the relatively large cross section spacing that is <br />apparent in several instances in the USGSIFIS model continues to be reflected in the current <br />hydraulic model. The data sources used for each cross section are identified in Table 4.3. <br />For the cross sections where the main channel was defined using the data contained in the <br />USGSIFIS model. one of two vertical adjustments were made in the preparation of the current <br />hydraulic model. The USGSIFIS model was prepared based on the !\GVD 1929 vertical datum. <br />In order to convert main channel elevations to the NA VD 1988 vertical datum. all ground <br />elevations were adjusted vertically by +3.67 feet. This is the conversion between NGVD and <br />NA VD at Deckers. as determined by the \..idely recognized CorpsCon software. After making <br />this vertical adjustment. it was found that six of the USGSIFIS cross sections appeared to be <br />significantly lower than expected based on field observations. After the datum adjustment. these <br />six cross sections still indicated the presence of relatively deep holes along the river. These <br />holes were shown to be on the order of at least several feet. causing pools covering as much as <br />one.quarter river mile. Field observations indicated a generally much smoother. monotonic bed <br />profile. where pools of this size were not apparent. Consequently. additional vertical <br />adjustments were made to theses sections by fitting them to the stream profile generated by <br />adjacent cross sections. A brief summary of the adjustments made to the USGSIFIS cross <br />sections is pro\'ided in Table 4.3. Detailed documentation of these cross sectional adjustments is <br />included in Appendix E.I. <br /> <br />I <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />I <br />I <br />I <br /> <br />'*..4 Road CrossingslBridges <br /> <br />I <br />I <br /> <br />A total of 11 bridges were identified within the study reach: one in the lower detailed <br />reach. seven in the upper detailed reach. and three in the approximate reach. The geometry of <br />each of the eight bridges within the two detailed study reaches was confirmed by observations <br />and/or measurements taken during the field reconnaissance efforts completed for this study. <br />However. in the course of evaluating the existing parameters for the three bridges in the <br />USGS/FIS model. it was clear that elevation data contained in the USGSfFIS model for the three <br />bridges was not consistent \\ith recent bridge survey data. field observations and LiDAR <br /> <br />I <br />I <br /> <br />COCWCB03_South PhUlcJcpon_Joc <br /> <br />13 <br /> <br />A,dutsO, eo"AhhG bGi'Hm.. he. <br />
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