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If not, we divide the area of the Sink into i parts equally.
The output of the inversion of Eq. (7) is the real J r and imaginary J i parts of a line current J above the Earth.
(2.14)We denote a partition say π of n by π = ( a 1 α 1 ⋯ a r α r ) when there is α i parts of size a i ; ( i = 1, 2, …, r ).
The energy of each state s is defined to be E s =−RTlog(p s )-RTlog, and we make the assumption that E s can be linearly decomposed into i parts such that E s =∑ i −RTlog(p s i )−RTlog (Clote and Backofen, 2000).
After that, select an i parts and click Add to shape > expand.
Figure 3a c show the variation of dielectric constant (ε R), dielectric loss (ε I), real (M R) and imaginary (M I) parts of electrical modulus as a function of temperature.
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