Features:
In order to make the asteroid window for primordial black hole masses (∼ 10**17--10**23 g) somewhat intelligible, we consider the masses of asteroids below with the masses of Ceres (NOT shown in Image 2), Vesta, and Itokawa as examples.
For rocky asteroids, the mean density does NOT vary much from 3 g/cm**3. For rocky-icy asteroids with ∼ 50% rock and ∼ 50% water ice by mass, the mean density does NOT vary much from 2 g/cm**3.
The mean diameters and hence the masses of asteroid do vary widely. Table: Asteroid Mass below gives some example asteroid masses from established measurements (the M values) and those calculated from the fiducial value formula (the M_fid values).
We see that the fiducial value formula is better than factor of 2 accurate when compared to the masses of real asteroids. The main reason for the disagreement between the M values and M_fid values is density. Recall, all M_fid values were calculated with the fiducial value ρ = 3 g/cm**3. To explicate:
We also see that our fiducial values for mean diameter and mean density give a fiducial value mass 1.57*10**21 g that is larger than the logarithmic mean mass of the asteroid window for primordial black hole masses (∼ 10**17--10**23 g) which is (17+23)/2 = 20 (i.e., in antilogarithm form mass 10**20 g) by more than 1 dex (i.e., in antilogarithm form by more than a factor of 10).
Aste- Name Year of Mean Mass M Mass M_fid from the fiducial Ratio
roid Discov- Diameter value formula with fiducial Mass_fid
No. ery (km) (g) density ρ = 3 g/cm**3: (g) /Mass
1 Ceres 1801 939.4 9.3835*10**23 1.30*10**24 1.39
4 Vesta 1807 525.4 2.59076*10**23 2.28*10**23 0.879
... M_upper ... 399.3 ... 1.0*10**23
... D = 100 km ... 100.0 ... 1.57*10**21
... M_lower ... 3.993 ... 1.0*10**17
25143 Itokawa 1998 0.330 3.35*10**13 5.64*0**13 1.59
... D = 1 m ... 0.001 ... 1.57*10**7
Notes: