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Boggs Mountain Demonstration State Forest Draft ... - Cal Fire

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<strong>Boggs</strong> <strong>Mountain</strong> <strong>Demonstration</strong> <strong>State</strong> <strong>Forest</strong> <strong>Draft</strong> Management Plan, June 2008<br />

Culvert Sizing Procedure for the 100-Year Storm<br />

The Rational Method of estimating flood discharge from small watersheds was used to determine<br />

the proper size diameter culvert for the drainages on <strong>Boggs</strong> <strong>Mountain</strong> <strong>Demonstration</strong> <strong>State</strong><br />

<strong>Forest</strong>. To calculate the size of culvert which would handle the 100-year storm flood flow, the<br />

volume of runoff which would occur at each stream crossing must first be estimated. The<br />

Rational Method is based on the equation: Q=CIA<br />

Where: Q= peak runoff at crossing (in cfs)<br />

C= runoff coefficient (percent runoff)<br />

I= uniform rate of rainfall intensity (inches/hour)<br />

A= drainage area (in acres)<br />

Information needed:<br />

A= area of watershed (acres)<br />

H= elevation difference between highest point in watershed and the crossing point (ft)<br />

L= length of channel in miles from the head of the watershed to the crossing point<br />

I= uniform rate of rainfall intensity. Obtained from precipitation frequency-duration data for<br />

local rain gages .<br />

C= runoff coefficient from table created by Rantz (1971)<br />

When selecting an “I” value, one must consider the travel time for the runoff to reach the crossing<br />

(Tc), and the precipitation conditions for the particular watershed. Time of concentration can be<br />

calculated using the formula: Tc=[11.9L 3 /H] 0.385<br />

Where: Tc= time of concentration (in hours)<br />

Once the time of concentration has been determined, then that value is used to determine which<br />

rainfall duration to use. For all of the calculations, a 10 minute duration was used. The runoff value<br />

for a 10-minute duration of a 100-year flood flow was obtained from rainfall depth duration frequency<br />

table for Clear Lake Highlands (.31), and then multiplied by six to get the hourly value (1.86). The<br />

runoff coefficient (C) used for all of the drainages at <strong>Boggs</strong> was 0.4. This is representative of<br />

woodland with a shallow impeding horizon.<br />

Once the volume of runoff was estimated for each of the crossings, the Culvert Capacity<br />

Nomograph was used to determine the needed culvert size that will accommodate the 100-year<br />

flood flow. The culvert entrance type for all of the crossings is Type 1, with a headwall. The<br />

headwater depth in diameters was calculated by dividing the distance from the road grade to the<br />

bottom of the culvert by the culvert size in feet. By drawing a line from the headwater depth (in<br />

diameters) through the discharge values (in cfs), one will be able to determine the needed culvert<br />

size (in inches).<br />

Lower Mill Creek:<br />

The crossing at Lower Mill Creek has two 30-inch “shotgun” culverts mounted in concrete<br />

measuring 4’ from the base of the culvert to the headwall, and 7’ to the road grade. The<br />

headwater depth is 2.8 culvert-diameters.<br />

A=152 acres L=3200 feet (.67 miles) H=680 feet<br />

Tc= [11.9(.67) 3 /680] .385 = .133 hours (7.96 minutes)<br />

82

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