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Last modified
1/26/2010 10:06:54 AM
Creation date
10/5/2006 3:57:33 AM
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Template:
Floodplain Documents
County
Boulder
Basin
South Platte
Title
Analysis of a High Hazard Flood Zone
Date
10/1/1987
Prepared For
Boulder
Prepared By
David Love & 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 />The weights (W) of individuals considered in this analysis varied from 30 pounds to 240 <br />pounds. This range is based on observation of weight data obtained through various agencies <br />(Reference 1 and 2). <br /> <br />Buoyancy forces (B) are based upon the weight of water displaced by the design monolith at a <br />given depth (d). <br /> <br />B = (Thickness) x (Face) x (d) x oywater <br /> <br />This force is a product of the volume of the individual below depth "d", and the specific weight of <br />water (y), which is approximately 62.4 pounds per cubic foot (pel) under a wide range of <br />conditions. Note that the design monolith volume was varied according to the individual's weight <br />as discussed later in this analysis. <br /> <br />The dynamic force (P) of the water is based upon its velocity component normal to the face of <br />the monolith, a coefficient of drag representing losses due to friction and loss of momentum, and <br />the density of water. <br /> <br />P = (Cd) x (p) x (V212) x (An) x (SI) <br /> <br />The coefficient of drag (Cd) is a function of shape <br />and /low regime. Values of Cd were obtained from the <br />"Colorado Floodproofing Manual" (Reference 3) and <br />represent losses induced by drag on rectangular objects. <br />The density of water (p) is approximately 1.94 slugs per <br />cubic foot (scl) for purposes of this study. The velocity <br />(V) component contributing to this force represents the <br />average velocity parallel to /low in the vicinity of the <br />monolith. This is actually the resultant of the theoretical <br />velocity distribution, which varies from a minimum value <br />at ground level (GL) to a maximum value near the water <br />surface (Figure 2). The resultant velocity actually acts <br />Figure 3 through a point slightly below half the depth of /low <br />(Reference 4), but for the purpose of this analysis it will <br />be assumed to act through the midpoint of the depth (Figure 4), which is a conservative <br />approximation. The area nonnalto /low (An) was again varied according to weight. A safety factor <br />(SI) was used to conservatively reflect the degree of uncertainty in the assumptions on which this <br />equation is based. Note that this factor of safety is applied in both the slippage and the toppling <br />moment analysis. <br /> <br />Forces due to friction (Ff), acting in the opposite direction of the applied dynamic water <br />force, are a product of the resultant weight of the monolith [the weight (W) of the individual minus <br />the buoyancy force (E)], and an assumed coefficient of friction (~). <br /> <br /> <br />Ff= ij!) x (W - B) <br /> <br />The static coefficient of friction (for bodies at rest) is normally about 0.7 for dry surfaces such as <br />concrete and asphalt paving. For the purposes of this analysis, ~ was varied from a low value of <br />0.3 for slippery surfaces to 0.7 as an upper limit. <br /> <br />-6- <br />
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