Table 3
Initial porosity φ0, initial thermal conductivity
k0, average final porosity
, initial planetesimal radius
R0, final planetesimal radius
Rf, thickness of the porous layer
Dp, central maximum temperature
Tmax, and central pressure
Pc at
.
SCP | ORP | RHP | BCCP | |||
φ 0 | % | 47.64 | 39.54 | 25.95 | 31.98 | |
k 0 | W m-1 K-1 | 0.088 | 0.14 | 0.32 | 0.22 | |
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Screep |
![]() |
% | 31.91 | 32.64 | 25.81 | 30.55 |
R 0 | km | 6.20 | 5.91 | 5.53 | 5.69 | |
R f | km | 5.68 | 5.70 | 5.52 | 5.65 | |
D p | km | 2.08 | 3.25 | 5.52 | 5.65 | |
T max | K | 934 | 905 | 808 | 869 | |
P c | MPa | 0.021 | 0.025 | 0.033 | 0.029 | |
I T | K | 762−925 | 750−905 | 740 − | 745 − | |
t comp | Ma | 0.44 | 0.53 | 1.07 | 1.51 | |
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Spar |
![]() |
% | 16.83 | 19.10 | 21.21 | 20.89 |
R 0 | km | 6.20 | 5.91 | 5.53 | 5.69 | |
R f | km | 5.32 | 5.37 | 5.41 | 5.41 | |
D p | km | 1.15 | 1.59 | 3.42 | 2.30 | |
T max | K | 734 | 727 | 706 | 717 | |
P c | MPa | 0.021 | 0.025 | 0.033 | 0.029 | |
I T | K | 650−700 | 650−700 | 650−700 | 650−700 | |
t comp | Ma | 0.08 | 0.08 | 0.15 | 0.10 | |
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Bcreep |
![]() |
% | 25.16 | 21.15 | 15.96 | 17.72 |
R 0 | km | 62.04 | 59.13 | 55.27 | 56.85 | |
R f | km | 55.07 | 54.12 | 52.98 | 53.36 | |
D p | km | 22.07 | 23.70 | 25.50 | 20.30 | |
T max | K | 739 | 739 | 738 | 739 | |
P c | MPa | 2.1 | 2.5 | 3.3 | 2.9 | |
I T | K | 662−739 | 655−739 | 645−738 | 650−738 | |
t comp | Ma | 9.67 | 7.89 | 6.12 | 5.28 | |
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Bpar |
![]() |
% | 9.07 | 9.19 | 8.68 | 9.06 |
R 0 | km | 62.04 | 59.13 | 55.27 | 56.85 | |
R f | km | 51.61 | 51.63 | 51.54 | 51.61 | |
D p | km | 5.50 | 6.60 | 9.50 | 8.00 | |
T max | K | 736 | 735 | 734 | 735 | |
P c | MPa | 2.1 | 2.5 | 3.3 | 2.9 | |
I T | K | 650−700 | 650−700 | 650−700 | 650−700 | |
t comp | Ma | 0.86 | 0.86 | 0.86 | 0.86 |
Notes. The lower value of the temperature interval IT defines the temperature at which the central porosity changed by 1% of φ0 and the upper value defines the temperature at which φ = 10-5 was reached. The compaction time tcomp is the time between the onset and the end of porosity loss in the centre. Considered are bodies with terminal radii of 5 km (Screep, Spar) and 50 km (Bcreep, Bpar). Thereby, compaction is modelled either via creep (Screep, Bcreep) or as a T-dependent process only (Spar, Bpar). For each case four packings are considered with the corresponding initial porosity and radius, as well as the corresponding computation of the effective stress.
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