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2006-06-12_REVISION - M1982015 (23)
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2006-06-12_REVISION - M1982015 (23)
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Entry Properties
Last modified
6/15/2021 2:56:05 PM
Creation date
11/21/2007 9:36:07 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1982015
IBM Index Class Name
Revision
Doc Date
6/12/2006
Doc Name
CLOMR
From
Carroll & Lange
To
DMG
Type & Sequence
AM1
Media Type
D
Archive
No
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Weld County Public Works <br />Attn: David Bauer, PE <br />• January 30, 2006 <br />J N: 3075 <br />Page 2 <br />Colorado, published in April 1981, contains a table which was also <br />referenced for "Year 2000 Urbanization at Longmont and Lyons." This <br />table lists 100-year peak flows for the St. Vrain River at Idaho Creek <br />(located just upstream of I-25) of 17,070 cfs. On page 38 of this report, <br />there is discussion of the results under section C. Comparison of the Peak <br />Flows for Different Development Conditions. Within this discussion, WRC <br />states, "...[VVje can see that the percentage increase in peak flows <br />resulting from the year 2000 development conditions is minimal. Such <br />increases ranging from none to 1.55% will have a minimal impact on the <br />water surface elevations resulting from the 100-year frequency flood." <br />They continue on to say, "In some cases for the 50-year and 500-year <br />floods, because of flood peak desynchronization, the year 2000 urbanized <br />discharges are slightly lower than those for the existing conditions." The <br />referenced pages of this report are attached. <br />Due to this `minimal difference,' the Army Corp of Engineers Study was <br />used in the CLOMR as this study contained a level of detail not found in <br />any other study including adjusted flow rates at all stations along the St. <br />• Vrain River accounting for the routing effect of a flood in a river, as well as <br />the contributions from smaller tributary streams along the reach of the <br />river. <br />However, Carroll & Lange, Inc. performed an exercise as a check to the <br />sensitivity to the peak discharge on the water surface elevation. In order to <br />obtain an increase of one foot to the 100-year water surface elevation an <br />increase in flow of approximately 6,000 cfs would be needed. This is an <br />increase of approximately 38% to the total peak flow. <br />4. The applicant should verify and demonstrate in the 12/12/05 CLOMR report that <br />the estimated peak flows passing by the proposed development property <br />accurately reflect current conditions. <br />Response: See discussion above. <br />5. The report assumes that the existing berms, that were left by prior gravel and <br />sand mining along the north side of the St. Vrain River channel, will conitnue to <br />exist in their present configuration during the 100-year flood. This assumption <br />may not be justified for un-armored, geotechnically unstable sand and gravel <br />deposits. Additional supporting information is needed to justify this assumption. <br />Response: Concrete debris was placed along the river embankment during <br />the previous mining operation. However, we are currently working with our <br />• geotechnical consultant regarding the stability of the existing river <br />embankment during flood events. Stability recommendations, if any, will <br />
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