RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 20, ES5007, doi:10.2205/2020ES000740, 2020
| $q_b^\circ$, mW/m$^2$ | $T_\circ$, K | $T_s^\circ$, K | $\Psi_2$ | $\displaystyle{ {c- c_m}\over c_m}$ | $ \displaystyle{ {a- \hat{a}}\over \hat{a}}$ |
| Case I | |||||
| a)#x81;051 | 5648 | 5486 | 0.015 | 0.07 | -0.04 |
| b)#x81;041 | 5889 | 5670 | 0.0006 | -0.006 | -0.15 |
| Case II | |||||
| a)#x81;050 | 5933 | 5692 | 0.007 | 0.07 | -0.05 |
| b)#x81;042 | 5784 | 5572 | $5\, 10^{-5}$ | $5\, 10^{-4}$ | -0.26 |
| Case III | |||||
| a)#x81;051 | 6008 | 5681 | 0.0003 | -0.003 | -0.04 |
| b)#x81;041 | 5383 | 5184 | $3\, 10^{-5}$ | $3\, 10^{-4}$ | -0.4 |
Citation: Reshetnyak M. Yu. (2020), Inverse problem for the Earth's core evolution model, Russ. J. Earth Sci., 20, ES5007, doi:10.2205/2020ES000740.
Copyright 2020 by the Geophysical Center RAS.