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Figure 1:
Ratio of the radiation pressure force to the gravitational
force vs. grain size for different grain materials and porosities, P,
calculated for an A5V (![]() ![]() ![]() ![]() |
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Figure 2:
Nominal case. Color-coded maps (log-scale) of the
vertical optical thickness of avalanche grains,
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Figure 3: Time evolution of the cross-sectional area amplification factor (the ratio of the total cross-sectional area of the avalanche grains within 500 AU to its initial value at t=0). Initial increase is due to dust production by outflowing planetesimal debris colliding with the disc material. When the grain removal (due to star radiation pressure) rate exceeds the grain production, the value of F drops (see text for more details). |
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Figure 4:
Ratio of the total number of grains produced by the avalanche
by the time t,
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Figure 5:
Maximum amplification factor as a function of the
minimum size assumed for the initial planetesimal debris. The power-law index for the size
distribution is equal to its nominal value
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Figure 6:
Dependence of the maximum amplification factor on the power-law index of the initial size-frequency distribution of the planetesimal debris (Eq. (8)),
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Figure 7: Dependence of the maximum amplification factor on the location of the primary planetesimal breakup. |
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Figure 8:
Radial velocities vs. distance from the star for grains with
different ![]() ![]() |
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Figure 9:
Dependence of the maximum amplification factor on the minimum
size for debris produced in avalanche collisions
(Eq. (12) with
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Figure 10: Dependence of the maximum amplification factor on the value q1 in Eq. (12) for collisionally produced grains (q2=1.83). |
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Figure 11: Maximum amplification factor as a function of porosity for pure silicate grains. The value of the threshold energy, Q*, is assumed to be the same as in the nominal case. |
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Figure 12: Maximum amplification factor vs. value of the threshold energy, Q*. Values for s0=1 cm grains are denoted on the axis. For the other sizes the threshold energy is given by Eq. (11). |
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Figure 13:
Different test radial distributions for
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Figure 14:
Maximum amplification factor as a function of ![]() |
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Figure 15: Top panel: face-on case: color-coded map of the ratio between the geometric surface densities of the avalanche grains and that of the "field'' population for the nominal case. Bottom panels: edge-on case: midplane fluxes (arbitrary units) for the nominal case at avalanche maximum, edge-on orientation. The 2 solid lines indicates the total midplane fluxes ("field''+avalanche) for each side of the disc (differences between the 2 sides are so small here that the 2 lines are almost indistinguishable). The dashed lines show the midplane fluxes for just the avalanche particles. Plot a) corresponds to the forward scattering function and b) to the isotropic case. |
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Figure 16:
Same as Fig. 15, but
for collisionally weaker grains
with
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Figure 17: Same as Fig. 15, but for the case of a disc 5 times more massive than in the nominal case. |
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Figure 18: Same as Fig. 15, but for a vertically thinner disc, described by Eq. (19). The total mass of the disc is the same as in the nominal case, but the asymmetries become prominent. |
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Figure B.1: The total number of SPs as a function of time for a typical nominal case run. |