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Table 1 Root mean square (rms) of temperature differences in the bottom 200 km (ΔTbot) of the models

From: Influence of composition-dependent thermal conductivity on the long-term evolution of primordial reservoirs in Earth's lower mantle

HDprim

KDprim

 

rms ΔTbot (K)

 
  

Global

Positive

Negative

1

1

507.3

526.1

485.4

1

0.74

498.7

469.0

524.9

1

0.50

491.0

485.9

491.9

10

1

600.3

673.6

530.0

10

0.74

591.2

706.4

491.7

10

0.50

623.7

742.7

517.3