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A fundamental negative result is then proved: no general self-stabilizing algorithm exists for distributed defeat status computation, indicating that self-stabilizing algorithms for this problem can be defined only under specific conditions.
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The numerical computation indicates that the method is efficient.
The computation indicates that the RSM is superior to the other turbulence models in capturing the swirl flow effect in comparison with measurements.
The result of theoretical computation indicates that all coordinate bonds are basically intermediate and covalent dominant interactions in complex 1, and complex 1 has the high thermal stability, which coincides with the result of thermogravimetric analysis (TGA) of complex 1.
Equations showing the dependence of the limiting activity coefficient on the virial coefficient values (B11, B12, and B22) used in their computation indicate that the influence may be considerable for derivatives numerically larger than about 4 × 10−5 mol cm−3.
The results of numerical computation indicate that the maximum or minimum sensitivity of a cladding mode coupled with PCF-LPG is predetermined by its dispersion, which is also influenced by the PCF structure geometry.
Thermodynamics computation indicated that some of this high fluoride groundwater is supersaturated with respect to fluorite, fluorapatite and hydroxyl-apatite (Singaraja et al. 2012; Chidambaram et al. 2012; Li et al. 2015).
(3) Region except near the center, polar axis and equatorial plane of the EarthThe simulated computation indicates that the errors ΔB and Δh are correlated with the distance between the point P and the center of the Earth, which are shown in Tables 7 and 8, taking the case that B = 11°, L = 45° for example.
Region except near the center, polar axis and equatorial plane of the EarthThe simulated computation indicates that the errors ΔB and Δh are correlated with the distance between the point P and the center of the Earth, which are shown in Tables 7 and 8, taking the case that B = 11°, L = 45° for example.
(2) Region of the equatorial plane of the EarthThe simulated computation indicates that the error ΔB is always zero, and the errors Δh are correlated to the distance between the point P and the center of the Earth, which is shown in Table 6.
(1) Region of the polar axis of the EarthThe simulated computation indicates that the error ΔB is always zero, and the errors Δh are correlated with the distance S between the point P and the center of the Earth, which is shown in Table 5.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com