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Drainage Design Manual, Hydrology - Flood Control District of ...

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<strong>Drainage</strong> <strong>Design</strong> <strong>Manual</strong> for Maricopa County<br />

<strong>Hydrology</strong>: Application<br />

LL<br />

---------- ca<br />

S 0.5<br />

=<br />

(<br />

------------------------------<br />

4.59) ( 2.30)<br />

= 0.66<br />

255 0.5<br />

b. Select a value for K n<br />

From Appendix D, Section 2 for mountain and foothill watersheds, the Santa Anita<br />

Creek and Medicine Bow River watersheds were found to have similar physical characteristics<br />

to Subbasin S1. The K n values for those watersheds are 0.053 and<br />

0.0534, respectively with lagtimes <strong>of</strong> 1.10 and 0.89 hours, respectively. Comparison<br />

<strong>of</strong> the K n values for these two watersheds to the general values <strong>of</strong> K n for the Phoenix<br />

Mountain S-graph, provided in Table 5.6, indicate that a value for K n <strong>of</strong> 0.053 is appropriate.<br />

K n = 0.053<br />

c. Compute the lag time using Equation (5.11)<br />

The source <strong>of</strong> the K n values for the two similar watersheds is unknown, therefore use<br />

the Corps <strong>of</strong> Engineers version <strong>of</strong> the lag equation.<br />

C = 24K n<br />

= ( 24) ( 0.053) = 1.272<br />

m = 0.38<br />

Lag<br />

<br />

C LL ca m<br />

= ----------<br />

= 1.272( 0.66) 0.38 = 1.09 hours<br />

<br />

S 0.5<br />

The lag <strong>of</strong> 1.09 hours compares favorably to the lag times <strong>of</strong> the similar watersheds<br />

used for the selection <strong>of</strong> K n .<br />

d. Compute Q ult using Equation (5.10)<br />

Q ult = -------------------<br />

645.33A<br />

Δt<br />

Δt = 0.15 lag = ( 0.15) ( 1.09) = 0.164 hours, therefore<br />

use<br />

Δt =<br />

10 minutes<br />

August 15, 2013 9-49

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