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Manual recorded precipitation is used as reference to calculate deviation for automatic recording.
The measured data was used to calculate deviation in molar refractivity, ΔR, excess molar volume, VmE, deviation in viscosity, ∆ η, and Excess Gibb's free energy of activation of viscous flow, ∆ G⁎E.
Since dominant markers cannot be used to calculate deviation from the Hardy-Weinberg equilibrium directly, two complementary statistical methods, which do not rely on these assumptions, were used and showed similar values for EcoRI/MspI data.
The genotype distributions for each study were used to calculate deviation from Hardy Weinberg equilibrium (HWE) using a χ test, and those studies which did show evidence of deviation were excluded in a sensitivity analysis.
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Uncertainty analysis entailed calculating deviations in the measurements.
To this end we calculated deviations from expected as the difference between observed frequencies and expected frequencies.
For each trait, we achieved this by first calculating deviations of each individual from its family mean and randomly permuting these deviations within each family.
7. Calculate standard deviation of sample IF using a t-test.
We used the least-square estimation to calculate the deviation.
To calculate the deviation, it is necessary to first define the 'model'model
It is possible to calculate the deviation without constructing a tree.
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