Table 1.
Parameters of the three polytropes employed for the EOSs of Model1 and Model2 (indices correspond to the number of the polytrope).
| Par. | Model1 | Model2 |
|---|---|---|
| γ1 | 3.20 | 2.50 |
| γ2 | 2.83 | 3.22 |
| γ3 | 2.50 | 3.00 |
| nb,12 | 0.21 | 0.24 |
| nb,23 | 0.70 | 0.50 |
| mb,1 | 1.017982 | 1.016573 |
| mb,2 | 1.014858 | 1.021916 |
| mb,3 | 0.977851 | 1.015670 |
| κ1 | 0.006646 | 0.006646 |
| κ2 | 0.008745 | 0.003538 |
| κ3 | 0.016621 | 0.005042 |
Notes. γ is the index of polytrope, nb is baryon density, where change of the polytrope occurred, κ is the pressure coefficient and mb the baryon mass at the point where the crust joins with the first polytrope (mb,1) or where two polytropes join (mb,2 and mb,3). Other parameters were calculated from the conditions of mechanical and chemical equilibrium.
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