Sample
|
a
Beta/gamma
|
b
Uranium mgkg
-1
|
c
U238/U235
|
---|
Soil 1 | 150 | 0.857, 0.685, 1.033 | 129 |
Soil 2 | 120 | 0.164, 0.231, 0.252 | 132 |
Soil 3 | 160 | 0.688, 0.759, 0.637 | 129 |
Soil 4 | 190 | 0.725, 0.603, 0.867 | 130 |
Soil 5 | 220 | 0.119, 0.738, 0.907 | 118 |
Soil 6 | 130 | 1.44, 1.51, 1.51 | 129 |
BP Horizon Oil | Â | 0.070, 0.073, 0.073 | 138 |
Sediment R. Euphrates | Â | 1.05 mgkg-1 | NA |
Well water |  | 2.72 μgL-1 | NA |
River water |  | 2.24 μgL-1 | NA |
Tap water |  | 2.28 μgL-1 | NA |
- Three separate aliquots were taken from each soil sample and results are shown. Limit of Detection was 0.002 mgkg-1. As a check on the ion exchange method, the Uranium atom ratio from the deep oil from the BP Horizon Macondo oil spill was run with the Fallujah soil samples.
- a nGyh-1; b mean of three runs is tabulated for each of three aliquots; LOD, U-235 = 0.0007; c Natural ratio is 137.88; these measurements are derived from counts using the ion-exchange extracted Uranium solutions. 95% CI limits for Natural Uranium Ratio are 132.1 < Ratio < 144.1, Values below 132.1 are thus enriched, above 144.1 depleted with p < 0.05. NA = not assessed.