The Hill of Tara in Ireland is a place of great archaeologic
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 Compute sigma x, sigma x^2, sigma y, sigma y^2. Use the results of part (a) to compute the sample mean, variance, and standard deviation for x and for y. Compute a 75% Chebyshev interval around the mean for x values and also for y values. Use the intervals to compare the magnetic susceptibility on the two grids. Higher numbers indicate higher magnetic susceptibiity. However, extreme values, high or low, could mean an anomaly and possiible archaeological treasure. Grid H shows a wider 25% range of values. Grid E shows a wider 75% range of values. Grid E shows a wider 25% range of values. Grid H shows wider 75% range of values. Compute the sample coefficient of variation for each grid.
Solution
d) Coefficint of variation
CV=sd(x)/mean(x) *100
CV=53.95%
CV for Y =49.63%
| X | Y | XY | X^2 | Y^2 | |
| 21.57 | 56.06 | 1209.214 | 465.2649 | 3142.724 | |
| 10.81 | 29.27 | 316.4087 | 116.8561 | 856.7329 | |
| 8.96 | 38.67 | 346.4832 | 80.2816 | 1495.369 | |
| 27.09 | 13.76 | 372.7584 | 733.8681 | 189.3376 | |
| 24.13 | 20.34 | 490.8042 | 582.2569 | 413.7156 | |
| 36.19 | 53.24 | 1926.756 | 1309.716 | 2834.498 | |
| 10.81 | 25.98 | 280.8438 | 116.8561 | 674.9604 | |
| 10.44 | 12.35 | 128.934 | 108.9936 | 152.5225 | |
| 6.37 | 42.43 | 270.2791 | 40.5769 | 1800.305 | |
| 24.5 | 44.31 | 1085.595 | 600.25 | 1963.376 | |
| 16.73 | 39.61 | 662.6753 | 279.8929 | 1568.952 | |
| 7.48 | 14.23 | 106.4404 | 55.9504 | 202.4929 | |
| 28.94 | 17.05 | 493.427 | 837.5236 | 290.7025 | |
| 35.6 | 18.93 | 673.908 | 1267.36 | 358.3449 | |
| sum | 269.62 | 426.23 | 8364.527 | 6595.647 | 15944.03 |
| means | 19.25857 | 30.445 | 597.4662 | 471.1177 | 1138.859 |
| variance | 107.9347 | 228.2662 | 251709.3 | 192214.4 | 1016963 |
| standard | 10.38916 | 15.10848 | 501.7064 | 438.4226 | 1008.446 |
