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Some aspects of the Isaacs principle of transition and his main equation for differential games are considered to demonstrate that those equations contain some implicit assumptions, and are valid under certain contiguity condition which is defined and analyzed for differential games.
In Section 3, the main equation for the boundary value problem (1 - 3) is derived.
The integral equation (11) is called the main equation for the boundary value problem (1 - 3).
The evidence shows that these instruments were not jointly significant in the main equation for migration flows at the conventional significance levels.
After evaluating the effect of each factor, the equations will be integrated so that the main equation for modeling the relation between weather and reliability will be extracted.
This moment condition implies that the value of the τth conditional quantile of ln(w) − XβSP is zero, an equality that is the main equation for identification.
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The main equations for blood flow calculation are as follows: (1) Q v = π R 4 Δ P v 8 μ Δ l, Q t = 2 π R · Δ l · L p P v − P i − σ T π v − π i, Q = Q v − Q t, where Q is the flow rate of each vessel segment, which amounts to zero at each node of the vessel network due to the assumption of flux conservation and incompressible flow.
For spatial data over time, our main equation of interest (expressed in differences for spatial unit s between period t and t-1, denoted by the difference operator Δ) relates the crime rate to the immigrant/population ratio as: Δ Crime Population st = β 1 Δ Immigrants Population st + β 2 Δ X st + T t + ϵ st (1).
First, we estimate our main equation separately for men and women.
The main equations used for calculations are listed in Table 2.
Further, using the solution of the main equation, we provide an algorithm for solving the inverse problem.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com