31. Class
Freq. Cum. freq.
Cum. rel. freq.
2 2
.050 14
16 .400
11 27
.675 8
35 .875
4 39
.975 39
.975 1
40 1.000
33. a.
640.5, 582.5
b.
610.5, 582.5
c.
591.2
d.
593.71
35. a.
, ,
. Deletion of the largest observation 18.0 causes and to be a bit smaller
than . b.
By at most 4.0
c.
No; multiply the values of and by the conversion factor 12.2.
37. 39. a.
b.
.383
41. a.
.7
b.
Also .7
c.
13
43. 45. a.
; the deviations are
b.
.482, .694
c.
.482
d.
.482
47.
. The magnitude of s indicates a sub- stantial amount of variation about the center a “representa-
tive” deviation of roughly 25.
49. a.
56.80, 197.8040
b.
.5016, .708
51. a.
1264.766, 35.564
b.
.351, .593
53. a.
Bal: 1.121, 1.050, .536 Gr: 1.244, 1.100, .448
b.
Typical ratios are quite similar for the two types. There is somewhat more variability in the Bal sample, due primarily
to the two outliers one mild, one extreme. For Bal, there is substantial symmetry in the middle 50 but positive skew-
ness overall. For Gr, there is substantial positive skew in the middle 50 and mild positive skewness overall.
55. a.
33
b.
No
c.
Slight positive skewness in the middle half, but rather symmetric overall. The extent of variability appears sub-
stantial. d.
At most 32
57. a.
Yes. 125.8 is an extreme outlier and 250.2 is a mild outlier.
b.
In addition to the presence of outliers, there is positive skewness both in the middle 50 of the data and, excepting
the outliers, overall. Except for the two outliers, there appears to be a relatively small amount of variability in the data.
59. a.
ED: .4, .10, 2.75, 2.65; Non-Ed: 1.60, .30, 7.90, 7.60
b.
ED: 8.9 and 9.2 are mild outliers, and 11.7 and 21.0 are extreme outliers.
x 5 116.2, s 5 25.75
.82, .32, 2.98, 2.38, .22 x 5
115.58 x
| 5 68.0, x
tr20
5 66.2, x
tr30
5 67.5
x 5 1.0297, x| 5 1.009
x
tr10
5 11.46
x |
x x
x
tr
x |
x
tr12.5
5 12.40
x | 5 12.50
x 5 12.55
24–,28 20–,24
16–,20 12–,16
8–,12 4–,8
0–,4 There are not outliers in the non-ED sample.
c.
Four outliers for ED, none for non-ED. Substantial posi- tive skewness in both samples; less variability in ED
smaller f
s
, and non-ED observations tend to be somewhat larger than ED observations.
61.
Outliers, both mild and extreme, only at 6
A
.
M
. Distributions at other times are quite symmetric. Variability increases
somewhat until 2
P
.
M
. and then decreases slightly, and the same is true of “typical” gasoline-vapor coefficient values.
63.
, , . A histogram consisting of 8 classes
starting at 52, each of width 4, is bimodal but close to uni- modal with a positive skew. A boxplot shows no outliers,
there is a very mild negative skew in the middle 50, and the upper whisker is much longer than the lower whisker.
b.
.9231, .9053
c.
.48
67. a.
Female values are typically somewhat smaller than male values, and show somewhat more variability. An M boxplot
shows negative skew whereas an F boxplot shows positive skew.
b.
69. a. b.
189.14, 1.87
71. a.
The mean, median, and trimmed mean are virtually iden- tical, suggesting a substantial amount of symmetry in the
data; the fact that the quartiles are roughly the same distance from the median and that the smallest and largest observa-
tions are roughly equidistant from the center provides addi- tional support for symmetry. The standard deviation is quite
small relative to the mean and median. b.
See the comments of a. In addition, using as a yardstick, the two largest and three smallest observations
are mild outliers.
73.
small amount of variabil- ity, slight bit of skewness
75. a.
The “five-number summaries” , the two fourths, and the smallest and largest observations are identical and there
are no outliers, so the three individual boxplots are identical. b.
Differences in variability, nature of gaps, and existence of clusters for the three samples.
c.
No. Detail is lost.
77. c.
Representative depths are quite similar for the four types of soils—between 1.5 and 2. Data from the C and CL soils shows
much more variability than for the other two types. The box- plots for the first three types show substantial positive skew-
ness both in the middle 50 and overall. The boxplot for the SYCL soil shows negative skewness in the middle 50 and
mild positive skewness overall. Finally, there are multiple out- liers for the first three types of soils, including extreme outliers.
79. a. c.
12.53, .532 x
n1 1
5 nx
n
1 x
n1 1
n 1 1 x
| x 5
.9255, s 5 .0809, x| 5 .93, 1.5Q3 2 Q1
y 5 ax 1 b , s
y 2
5 a
2
s
x 2
F: x
tr10
5 3.24 M:
x
tr10
5 3.652 3.65
F: x 5
3.28, x| 5 3.15, s 5 .478, f
s
5 .50
M: x 5
3.64, x| 5 3.70, s 5 .269, f
s
5 .40
4
th
5 70.4, f
s
5 12.6
upper lower 4
th
5 57.8
x 5 64.89, x| 5 64.70, s 5 7.803
Copyright 2010 Cengage Learning. All Rights Reserved. May not be copied, scanned, or duplicated, in whole or in part. Due to electronic rights, some third party content may be suppressed from the eBook andor eChapters. Editorial review has deemed that any suppressed content does not materially affect the overall learning experience. Cengage Learning reserves the right to remove additional content at any time if subsequent rights restrictions require it.
81.
A substantial positive skew assuming unimodality
83. a.
All points fall on a 45° line. Points fall below a 45° line.
b.
Points fall well below a 45° line, indicating a substantial positive skew.
Chapter 2
1. a.
{1324, 3124, 1342, 3142, 1423, 1432, 4123, 4132, 2314, 2341, 3214, 3241, 2413, 2431, 4213, 4231}
b. c.
d. {1324, 1342, 1423, 1432, 2314, 2341, 3214,
3241, 2413, 2431, 4213, 4231}, contains no outcomes A and B are disjoint,
{3124, 3142, 4123, 4132, 2314, 2341, 3214, 3241, 2413, 2431, 4213, 4231}
3. a. b.
c. d.
,
5. a.
{1, 1, 1, 1, 1, 2, 1, 1, 3, 1, 2, 1, 1, 2, 2, 1, 2, 3, 1, 3, 1, 1, 3, 2, 1, 3, 3, 2, 1, 1, 2, 1, 2, 2, 1, 3, 2, 2, 1,
2, 2, 2, 2, 2, 3, 2, 3, 1, 2, 3, 2, 2, 3, 3, 3, 1, 1, 3, 1, 2, 3, 1, 3, 3, 2, 1, 3, 2, 2, 3, 2, 3, 3, 3, 1, 3, 3, 2, 3, 3, 3}
b.
{1, 1, 1, 2, 2, 2, 3, 3, 3}
c.
{1, 2, 3, 1, 3, 2, 2, 1, 3, 2, 3, 1, 3, 1, 2, 3, 2, 1}
d.
{1, 1, 1, 1, 1, 3, 1, 3, 1, 1, 3, 3, 3, 1, 1, 3, 1, 3, 3, 3, 1, 3, 3, 3}
7. a.
There are 35 outcomes in .
b.
{AABABAB, AABAABB, AAABBAB, AAABABB, AAAABBB
}
11. a.
.07
b.
.30
c.
.57
13. a.
.36
b.
.64
c.
.53
d.
.47
e.
.17
f.
.75
15. a.
.572
b.
.879
17. a.
There are statistical software packages other than SPSS and SAS.
b.
.70
c.
.80
d.
.20
19. a.
.8841
b.
.0435
21. a.
.10
b.
.18, .19
c.
.41
d.
.59
e.
.31
f.
.69 S
S 5 B
¨ C 5 5SSF, SFS, SSS6 5 C,
B ´ C 5
5SSF, SFS, FSS, SSS6 5 B, A
¨ C 5 5SSF, SFS6,
A ´ C 5
5SSF, SFS, FSS, SSS6, C
r
5 5FFF, FSF, FFS, FSS, SFF6
C 5 5SFS, SSF, SSS6
B 5 5SSF, SFS, FSS, SSS6
A 5 5SSF, SFS, FSS6
A
r
5 A
¨ B A
´ B 5 B 5
52314, 2341, 3214, 3241, 2413, 2431, 4213, 42316 A 5
51324, 1342, 1423, 14326 S 5
23. a.
.067
b.
.400
c.
.933
d.
.533
25. a.
.85
b.
.15
c.
.22
d.
.35
27. a.
.1
b.
.7
c.
.6
29. a.
676; 1296
b.
17,576; 46,656
c.
456,976; 1,679,616
d.
.942
31. a.
243
b.
3645 days roughly 10 yr
33. a.
1,816,214,400
b. 659,067,881,572,000 c. 9,072,000
35. a.
38,760, .0048
b.
.0054
c.
.9946
d.
.2885
37. a.
60
b.
10
c.
.0456
39. a.
.0839
b.
.24975
41. a.
10,000
b.
.9876
c.
.0333
d.
.0337
43.
.000394, .00394, .00001539
45. a.
.447, .500, .200
b.
.400, .447
c.
.211
47. a.
.50
b.
.50
c.
.625
d.
.375
e.
.769
49. a.
.34, .40
b.
.588
c.
.50
51. a.
.436,
b.
.581
53.
.083
55.
.236
59. a.
.21
b.
.455
c.
.264, .462, .274
61. a.
.578, .278, .144
b.
0, .457, .543
63. b.
.54
c.
.68
d.
.74
e.
.7941
65.
.087, .652, .261
67.
.000329; very uneasy.
69. a.
.126
b.
.05
c.
.1125
d.
.2725
e.
.5325
f.
.2113
71. a.
.300
b.
.820
c.
.146
75.
.401, .722
77. a.
.06235
b.
.00421
79.
.0059
Copyright 2010 Cengage Learning. All Rights Reserved. May not be copied, scanned, or duplicated, in whole or in part. Due to electronic rights, some third party content may be suppressed from the eBook andor eChapters. Editorial review has deemed that any suppressed content does not materially affect the overall learning experience. Cengage Learning reserves the right to remove additional content at any time if subsequent rights restrictions require it.