Errata for SWCE 5/e Updated: 6 May 2011
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Page |
Location |
Existing |
Correct |
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xv |
right column |
National Resource Conservation Service |
Natural Resources Conservation Service |
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16 |
9th line from top |
methemoglobenemia |
methemoglobinemia |
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40 |
Ex. 3.2, line 2 |
Keutucky |
Kentucky |
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40, 41 |
Ex. 3.2, second table, column headings |
I/P loge(loge[I/P]) |
1/P loge(loge[1/P]) |
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43 |
Table 3-1 caption |
Intensity Duration Frequency Table |
Depth Duration Frequency Table |
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44 |
Ex. 3.3, line 1 |
Determine the rainfall intensities |
Determine the rainfall depths |
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49 |
Par. 2, line 4 |
Equation 3.3 |
Equation 3.7 |
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49 |
Ex. 3.7, line 2 |
3.3 |
3.7 |
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54 |
Sec. 4.1, line above Eq. 4.3 |
Rohwer (1931) evaluated the constant C in Equation 4.1 |
Rohwer (1931) evaluated the constant C in Equation 4.2 |
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61 |
First line under Eq 4.10 |
Boltzman |
Boltzmann |
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62 |
First line |
where z in |
where z is |
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64 |
Ex. 4.3, Step (2) |
37.3 |
237.3 |
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65 |
Ex. 4.3, Step (12) |
0.003 cos |
0.033 cos |
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65 |
Ex. 4.3, Step (13) |
41.65 MJ m-2 day-1 |
41.63 MJ m-2 day-1 |
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65 |
Ex. 4.3, Step (14) |
41.65 =31.28 MJ m-2 day-1 |
41.63 =31.27 MJ m-2 day-1 |
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66 |
Ex. 4.3, Step (15) |
5.185 MJ m-2 day-1 |
5.186 MJ m-2 day-1 |
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74 |
Line after Eq. 4.31 |
where ETL in |
where ETL is |
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75 |
Ex. 4.6, Solution |
Calculate ETL from Equation 4-31
The estimated volume of water to be delivered
per irrigation is
Thus the irrigation system should be set to deliver about 1000 L of water every three days. |
Calculate ETL from Equation 4-31
The estimated volume of water to be delivered
per irrigation is
Thus the irrigation system should be set to deliver about 900 L of water every three days. |
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84 |
2nd line after Eq. 5.6 |
T = time (T) |
t = time (T) |
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93 |
Example 5.4, Solution (line 1) |
Weighted CN = 3384/40 |
Weighted CN = 3544/40 |
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101 |
Figure 5-7, table line 8 |
h 20 99 |
h 18 99 |
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101 |
Line under Eq. 5.15 |
ham |
ha-m |
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106 |
Problem 5.10 |
15-mm rainfall |
10-mm rainfall |
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106 |
Problem 5.10 |
6-h, 25-y storm |
6-h, 25-y storm during the dormant season |
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109 |
Figure 6-1b |
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109 |
Figure 6-1c |
P = t + 8d2 / 3t |
P = t + 8d2 / 3t |
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110 |
Above Eq 6.6 |
It disregards elevation potential, since elevation changes are negligible in short reaches of mildly sloped conduits. |
[Delete entire sentence.] |
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119 |
Eq. 6.14 definitions |
R = hydraulic radius (Equation 6.3) |
R = hydraulic radius (Equation 6.2) |
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114 |
Figure 6-5 |
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Insert horizontal rule
under |
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114 |
Below Eq. 6.12 |
where Q is the flow rate (L/T3). |
where Q is the flow rate (L3/T). |
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115 |
Example 6.2, second equation |
= 0.48 m/s |
= 0.48 m3/s |
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117 |
Ex. 6.3, Solution, line 2 |
6-12 and 6-13 |
6.12 and 6.13 |
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125 |
Example 6.5 label |
Example 6.5 |
Example 6.6 |
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133 |
Problem 6.7 |
slope of the channel is 1 percent. |
slope of the channel is 0.08 percent. |
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133 |
Problem 6.7 |
(Insert sentence at the end of the problem.) |
Comment on the practicality of the results. |
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133 |
Problem 6.10 |
Example 6.5 |
Example 6.6 |
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133 |
Problem 6.10, line 2 |
stages of flow as follows: |
stages of flow, yielding the following depth-discharge pairs: |
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133 |
Problem 6.11 |
head of 0.4 m |
head of 0.3 m |
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145 |
Eq. 7.7b |
where θ = field slope angle = tan-1(S) |
where θ = field slope angle = tan-1(s) |
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147 |
Example 7.2, second line |
S = 5 percent |
s = 5 percent |
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147 |
Example 7.2, step 6 |
From Equation 7.8c,
calculate the S-factor: |
From Equation 7.8b,
calculate the S-factor: |
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147 |
Example 7.2, step 7 |
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| 148 | Example 7.3, table line (1) | 19 | 32 |
| 148 | table line (2) | 10 | Satisfactory | 18 | Soil loss too high |
| 148 | table line (3) | 9 | Satisfactory | 15 | Soil loss too high |
| 148 | table line (4) | 15 | 25 |
| 148 | table line (5) | 4.5 | 7.9 |
| 148 | table line (6) | 3.5 | 6.2 |
| 148 | Example 7.3, last paragraph | Note that any practice that includes contouring | Note that any practice that includes terracing |
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157 |
Problem 7.4 |
S = 10 percent |
s = 10 percent |
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158 |
Problem 7.7, second to last line |
density of water is N/m3 |
specific weight of water is N/m3 |
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158 |
Problem 7.8, second line |
Flagstaff,Arizona |
Flagstaff, Arizona |
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158 |
Problem 7.12 |
are collected in 20 seconds. |
are collected in 1 minute. |
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161 |
Last two lines |
… backs- |
… back- |
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166 |
Example 8.1, line 1 |
K = 0.1, 1 = 120 m, S = 8 |
K = 0.1, l = 120 m, s = 8 |
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170 |
Example 8.3, last equation |
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180 |
Table 8-4, Class D |
Bermuda … 0.1 |
Bermuda … 0.06 |
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180 |
Table 8-4, Class E |
0.1 |
0.04 |
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184 |
Last line of top paragraph |
revegeated |
revegetated |
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185 |
Problem 8.4 |
freeboard is |
freeboard is |
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186 |
Problem 8.15 |
[Change the last sentence.] |
Determine the top and bottom widths and design depths for both the 2 and 7 percent sections. |
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192 |
Figure 9-5 Expression for apron length (at top of figure) |
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199 |
Ex 9.2, first equation |
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200 |
Ex 9.4, paragraph 4, line 1 |
58.80 m - 57.73 m = 1.07 m |
58.80 m - 57.76 m = 1.04 m |
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200 |
Ex 9.4, par 4, line 5 |
1.005 m. |
0.975 m. |
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200 |
Ex.9.4, par 4, last line |
0.99 m |
0.97 m |
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200 |
Ex 9.4, par 5, line 1 |
(2’) a = 1.27 m, R = 0.44 m, v = 1.22 m/s, Q = 1.54 m3/s |
(2’) A = 1.22 m, R = 0.43 m, v = 1.21 m/s, Q = 1.47 m3/s |
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200 |
Ex 9.4, par 5, line 2 |
0.076 m, giving a flow
depth of 0.99 m. |
0.074 m, giving a flow depth of 0.97 m. |
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200 |
Ex 9.4, par 5, line 3 |
discharge is 1.54 m3/s |
discharge is 1.47 m3/s |
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200 |
Ex 9.4, par 5, line 5 |
discharge is 1.54 m3/s |
discharge is 1.47 m3/s |
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206 |
Ex. 9.5, Solution, line2 |
= 61.8 m. |
= 68.1 m. |
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215 |
Example 9.8, equation |
11.7 m |
11.5 m |
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222 |
Last line |
absolute viscosity of water (LM-1T-1) |
absolute viscosity of water (ML-1T-1) |
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228 |
Problem 9.14 |
weir coefficient of 3.0 Kc = 1.0 |
weir coefficient of 1.7 Ke = 1.0 |
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238 |
Figure 10-6, for Stream Type A |
ER < 1.4 |
1.4 < ER < 2.2 |
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238 |
Figure 10-6, for Stream Type B |
1.4 > ER < 2.2 |
1.4 < ER < 2.2 |
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276 |
Figure 12-3(c) |
(The fluctuations should be approximately sinusoidal with approximately two peaks per day. The illustration is conceptual rather than precise.) |
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300 |
Equation after 3rd paragraph |
Vg = PEo + QSx + RSy |
Vg = PEo + QSx + RSy 13.4 (add equation number) |
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301 |
Ex. 13.3, Solution step 3 |
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(delete equation number) |
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303 |
Example 13.4, last two lines |
the volume of fills (653 m3). The cut-fill ratio resulting from a lowering of the plane is 1.16. |
the volume of fills (623 m3). The cut-fill ratio resulting from this lowering of the plane is 1.22. |
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312 |
Between Equations 14.5 and 14.6 |
drain flow rate |
drainage rate per unit area |
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312 |
Equation 14.6 |
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312 |
Equation 14.7 |
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314 |
Ex. 14.1, step (2) |
x = … = 0.36 m |
x = … = 0.36 |
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315 |
Step (3) |
… = 1.07 |
… = 1.07 m |
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316 |
Line 1 |
(bo - b) [non-italic right parenthesis] |
(bo - b) |
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320 |
Figure 14-7 |
(10.5 m contour missing) |
(Insert 10.5 contour approx. midway between 10.4 m and 10.6 m contours.) |
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323 |
Paragraph 2, line 2 |
spacing DC |
spacing, DC |
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324 |
Figure 14-10 |
Spacing at 15.6 m |
Spacing at 14.9 m |
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336 |
Example 15.1 |
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336 |
Example 15.1, Columns for Calculated Pe & Actual Pe |
Calculated Pe: 57, 67, 68, 40, 31, 263 Actual Pe: 40, 67, 68, 40, 20, 235 |
Calculated Pe: 48, 55,58,41,13,215 Actual Pe: 40, 55, 58, 41, 13, 207 |
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336 |
Example 15.1, last line |
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337 |
Table 15-2, last line |
(1.19-1.32) |
(1.19-1.44) |
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350 |
Second line of text |
Irrigation should begin July 20 |
Irrigation should begin June 20 |
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366 |
Ex. 16.1, 3rd line |
20(mm/h0.45) t(h)0.45 + 5 (mm/h) t (h) |
20(mm/h0.45) τ(h)0.45 + 5(mm/h) τ(h) |
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379 |
Figure 16-9 |
[Insert label for the x-axis.] |
Discharge (L/s) |
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379 |
Figure 16-9 |
[Insert “L” in gap between arrows above the siphon.] |
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379 |
Figure 16-9 |
[Insert “d” before “= Outside”.] |
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379 |
Figure 16-9 |
[Insert “d” before “= … mm” on each curve.] |
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379 |
Figure 16-9 |
[Insert “L” before “= 2 m” or “= 3 m” on each curve.] |
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382 |
Prob. 16.5, 3rd line |
the elevation of the water surface elevation |
the elevation of the water surface |
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397 |
Table 17-5, bottom of left column |
>130 |
≥130 |
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401 |
First sentence |
Ho in m = |
Hd in m = |
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415 |
Problem 17.7 |
[Insert before the last sentence.] |
The static water level
is |
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428 |
Step (3), line 3 |
Table 15.4 |
Table 15-4 |
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428 |
Step (3), line 4 |
the available water is 12 percent |
the available water is 8 percent |
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428 |
Step (3), line 7 |
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428 |
Step (3), line 8 |
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429 |
Step (12), line 7 |
3.35 L/s |
3.35 L/h |
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429 |
Step (12), last line |
the lateral discharge is 3.35 L/h. |
the average emitter discharge is 3.35 L/h. |
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430 |
Step (16), line 5 |
3.41 |
3.41 L/h |
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446 |
Example 19.2, last two lines |
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449 |
Exp 19.3 Solution |
Perforamnce = |
Performance = |
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456 |
Figure 19-12, Brake Power scale |
0 20 40 60 |
[Delete the 0. Change 20 to 30 and change 60 to 50.] |
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465 |
Equation 20.12 |
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467 |
Equation 20.14 |
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467 |
Step 1 Eq |
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467 |
Step 5 Eq |
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468 |
Step 7 Eq |
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468 |
Step 8 Eq |
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468 |
Step 11 Eq |
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468 |
Step 12 Eq |
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468 |
After Step 12 |
Thus, the estimated soil loss is = 57.9 Mg ha-1y-1. |
Thus, the estimated soil loss is = 80 Mg ha-1y-1. |
[*] The "exp" notation is used here for clarity. The super-superscript characters are difficult to read.