The Hill of Tara in Ireland is a place of great archaeological importance. This region has been occupied by people for more than 4,000 years. Geomagnetic surveys detect subsurface anomalies in the earth's magnetic field. These surveys have led to many significant archaeological discoveries. After collecting data, the next step is to begin a statistical study. The following data measure magnetic susceptibility (centimeter-gram-second ? 10-6) on two of the main grids of the Hill of Tara (Reference: Tara: An Archaeological Survey by Conor Newman, Royal Irish Academy, Dublin).
Grid E: x variable
30.79 12.66 15.99 33.01 37.82 6.37 38.19
29.31 10.81 38.93 15.99 13.77 13.77 27.09
Grid H: y variable
30.68 17.05 56.53 43.84 56.06 13.29 50.89
32.56 36.79 41.02 56.53 30.68 13.76 38.20
(b) Use the results of part (a) to compute the sample mean, variance, and standard deviation for x and for y. (Enter your answers to 2 decimal places.)
the mean for both E and H
s2
S
(c) Compute a 75% Chebyshev interval around the mean for x values and also for y values. (Enter your answers to 2 decimal places.)
x y
Lower Limit
Upper Limit
(b)
Following table shows the calculations:
X | Y | (x-mean)^2 | (y-mean)^2 | |
30.79 | 30.68 | 57.9121 | 39.8161 | |
12.66 | 17.05 | 110.6704 | 397.6036 | |
15.99 | 56.53 | 51.6961 | 381.8116 | |
33.01 | 43.84 | 96.6289 | 46.9225 | |
37.82 | 56.06 | 214.3296 | 363.6649 | |
6.37 | 13.29 | 282.5761 | 561.69 | |
38.19 | 50.89 | 225.3001 | 193.21 | |
29.31 | 32.56 | 37.5769 | 19.6249 | |
10.81 | 36.79 | 153.0169 | 0.04 | |
38.93 | 41.02 | 248.0625 | 16.2409 | |
15.99 | 56.53 | 51.6961 | 381.8116 | |
13.77 | 30.68 | 88.5481 | 39.8161 | |
13.77 | 13.76 | 88.5481 | 539.6329 | |
27.09 | 38.2 | 15.2881 | 1.4641 | |
Total | 324.5 | 517.88 | 1721.85 | 2983.3492 |
Sample size: n=14
Mean:
Standard deviation:
The variance is:
(c)
According to Chebyshev theorem, 75% data values lies within 2 standard deviations of mean.
For x:
Lower limit: 0.16
Upper limit: 46.20
For y:
Lower limit: 6.69
Upper limit: 67.29
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