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Anomalies in total force values of the geomagnetic field (F a ) corresponding to crustal magnetizations (J i ) are approximately expressed by the following formula, which is equivalent to equation (5) in Yamazaki (2009): (3) where l i denotes the direction cosines of the ambient geomagnetic field and H represents the Curie point depth.
Assuming that all sequencing error rates e i are approximately equal (a valid assumption if all pools are sequenced using the same sequencing platform), the reads with the alternate allele should be more or less randomly distributed across the k pools.
where MIN D,E) is the smaller of D and E. In conclusion, the variation rates for a, e, and i are approximately given by Equations (33) to (35) for i≤H/2a, Equations (36) to (38) for the intermediate inclination (H/2a<i≤2H/a), Equations (30) to (32) for i>2H/a.
An implication of these observations is that the CH bonds of rings A and C in I are approximately perpendicular to each other.
Contrary to what occurs with the somatic chromosomes, the meiotic chromosomes of coffee (C. arabica) at the pachytene stage of prophase I are approximately 30 times greater in length than their corresponding somatic chromosomes.
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As can be seen, in the sampled range, K i is approximately linear in [glc].
For a completely localized wave function Ψ k (i) is approximately δ k i →P≈1 while for a typical delocalized wave function on D atoms, Ψ k (i) is approximately 1 D, and then P≈D.
From the best fit by Equation 1, it is obtained that the Q i is approximately 0.986 eV.
The capacity of a MIMO link l in state i is approximately given as [43], {R_{i}^{l}}=i cdot log_{2}left(1+frac{bar{rho}^{l}}{i}right) (4).
In a weighted correlation network, the propensity p i of node i is approximately |kME i | β.
The statistic (1) for each marker i is approximately normally distributed with variance 1 and mean non-centrality parameter.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com