We used the absolute values of NSBP instead of nocturnal BP fall to divide the subgroups in tertiles because the first variable has a minor coefficient of variation (data not published).
The uniformity of the flow distributions can be improved about 10 60% by fitting orifice rings or tube protrution with a range of the minor loss coefficients: 0.5 3.
When various frequencies microwaves were input, the tunability resulted in a minor reflection coefficient of 0.05.
The predictions of the proposed slip flow model on both the pressure recovery and minor loss coefficient are found in good agreement with the corresponding data in the literature.
The static pressure recovery and the minor loss coefficient through an axis-symmetric, circular cross-section, sudden-expansion fitting of a horizontal pneumatic conveying line with air solid particle flow are analytically studied.
However, batch-to-batch differences are considered to be minor: the coefficient of variation (inter-assay) as determined with two kit control samples was minimal (5.9% at the level of 20.3 nmol/L and 5.4% at the level of 77.4 nmol/l), no significant between-day drift, time shifts, or other trends were observed and the percentage of variance attributable to batch-to-batch differences was 4.5%.
Adversely, larger E j denotes a lower degree of variation of the ratings, the less information over attribute j, and minor objective significance coefficient ( {w}_j^o ) (Hafezalkotob and Hafezalkotob 2016b).
In this dendrogram, the 44 C. alismatifolia samples appeared to form three main clusters and five minor clusters at coefficient level 5.6: cluster I included three non-irradiated members and cluster II included 10 Gy irradiated individual plants of all four varieties and 20 Gy irradiated samples of Doi Tung 554 and Kimono Pink varieties except KP20-4 (no flowering).
The minor importance of these coefficients can be attributed to the fact that these coefficients will be multiplied by the absolute electro-osmotic permeability parameter, which is on the order of 10−9 m2/(V s).
For the ocean bottom observatories, we finally obtain similar coefficients and minor differences in G for 1-D and 3-D modellings.
