Fig. 5
M(R) dependence for the exact solution of the TOV equations obtained using a unified EOS and the approximate approach for the DH EOS. Different values of ncc are used (from left to right; 0.16, 0.13, 0.11, 0.09, 0.077 fm-3, see Table 1 for details). The value ncc = 0.077 fm-3 corresponds to the “real” crust-core boundary for the DH model. The solid blue curves show the M(Rcore) relation, the dashed red curves show the M(R) approximation based on Eqs. (11), (12), and the black curve shows the exact solution of the TOV equation.
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