Homework 3 answers Note: These answers do not strictly display significant figures. 7 7.25 A nonhomogeneous watershed has the following distribution of landcover: Fraction 0.25 0.30 0.20 0.10 0.15 Landcover Cultivated land Forest Pasture Open space Open space Soil Group C D C B C Slope (%) 2.3 2.2 1.9 1.8 2.1 Runoff Coefficient from Table 7.9 0.19 0.16 0.24 0.08 0.17 (Note: I added the last column.) Estimate the runoff coefficient for use in predicting a 10-yr peak discharge. Cw W C W i i i 0.25 * 0.19 0.30 * 0.16 0.20 * 0.24 0.10 * 0.08 0.15 * 0.17 0.177 0.25 0.30 0.20 0.10 0.15 7.27 Using the Rational Method, estimate the 10-yr peak discharge from a 35-acre watershed using the IDF curve shown in Figure 4.4. Assume light industrial development with the principal flowpath being paved surfaces including gutter flow. The principal flowpath has a length of 1,800 ft and a slope of 2%. Table 7.10 gives a recommend runoff coefficient of 0.65 for light industrial areas. Table 3.14 gives k = 9.1 for a paved surface, thus velocity is: v kS 0.5 9.1 * 0.02 0.5 1.28 ft / s tc L v60 1,800 ft 23 min ft s 1.28 * 60 s min For a duration of 23 minutes and a return period of 10 years, Fig. 4.4 gives intensity of 4 inches per hour. So: q p CiA 0.65 * 4 * 35 91 ft 3 / s Alternatively, Kirpich’s formula gives tc=11 min. Using that duration, i=6 in/hr, so qp=137 ft3/s. It is also reasonable to say that k = 42. Then v = 6 ft/s and tc=5 minutes. For this short duration, i=7.9 in/hr, so qp = 180 ft3/s. Homework 3 Answers, Page 2 of 3 7.43 Compute the weighted runoff curve number for the following conditions and use it to compute the depth of runoff (in.) for a storm depth of 4.5 in. Area Fraction Land Use/Condition 0.30 Lawns, open space/fair 0.25 Residential/0.5-acre lots 0.45 Woods/good Soil CN from Group Table 3.18 C 79 D 85 C 70 (Note: Last column added.) CN av W CN W i i i 0.30 * 79 0.25 * 85 0.45 * 70 76.45 0.30 0.25 0.45 1000 1000 10 10 3.08in; I A 0.2 * S 0.2 * 3.08 in 0.62 in CN 76.45 P I A 2 4.5 0.622 2.17 in Q P I A S 4.5 0.62 3.08 S 7.45 Compute the curve number for a 20-acre drainage area that has the following characteristics. Compute the depth of runoff (in.) for a storm of 5 in. Compute the runoff using both a weighted CN approach and a weighted Q approach Area (acres) Imperviousness % Soil Group CNp from p. 165 for use in Eq’n 3.50 4 6 7 3 24 18 60 75 B C B C 61 74 61 74 CN w CN p 1 f f 98 69.88 78.32 83.2 92 S (in.) Q (in.) 4.31 2.77 2.02 0.87 2.03 2.74 3.19 4.09 For the weighted CN approach: CN av W CN W i i i 0.2 * 69.88 0.3 * 78.32 0.35 * 83.2 0.15 * 92 80.39 0.1 0.3 0.35 0.15 1000 1000 10 10 2.44 in CN 80.39 2 2 P 0.2 S 5 0.2 * 2.44 Q 2.93 in P 0.8S 5 0.8 * 2.44 S For the weighted Q approach: Qav W Q W i i i 0.2 * 2.03 0.3 * 2.74 0.35 * 3.19 0.15 * 4.09 2.96 in 0.1 0.3 0.35 0.15 Homework 3 Answers, Page 3 of 3 7.49 Assuming C soil and the watershed conditions of Problem 7.27, estimate the peak discharge with the SCS Graphical Method. To get qu, we need tc and IA/P. We will assume Type II rainfall since the IDF curve is for Baltimore. (See Fig. 4.14 on p. 213.) To keep things simple, let’s use the same tc we found in 7.27, 23 minutes is 0.38 hours. Table 3.18 gives 91 for the CN for industrial districts on C soil. From Figure 4.4, a 24-hour, 10-yr storm has an intensity of 0.21 in/hr, thus a total storm depth of 5.04 inches. So: 1000 1000 10 10 0.99 in; I A 0.2 * S 0.2 * 0.99 in 0.20 in CN 91 IA 0. 2 0.04 Use 0.1 P 5.04 S From Figure 7.9c, qu is about 610 ft3/(s·mi2·in). Pe is obtained as: Pe 2 P 0.2S P 0.8S 2 5.04 0.2 * 0.99 5.04 0.8 * 0.99 4.02 in Area is 35 acres, which need to be converted to square miles. Since we don’t know of any ponds or swamps within the watershed, we’ll use FP=1. Then: q p qu APe F 610 ft 3 1mi 2 ft 3 * 35 ac * * 4 . 02 in * 1 134 640ac s s mi 2 in Alternatively, using tc = 11 min ≈ 0.2 hours, qu = 810 ft3/(s·mi2·in). So qp = 178 ft3/s. Using tc = 5 minutes ≈ 0.1 hr gives qu off the top of the chart, about 1020 ft3/(s·mi2·in). So qp = 224 ft3/s