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The Cost of Future Collisions in LEO - Star Technology and Research

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8<br />

are synthesized from the probability-weighted <strong>and</strong> time-averaged streams from all<br />

possible catastrophic collisions. However, we can treat them as physical streams<br />

for the purpose <strong>of</strong> statistical damage calculations.<br />

We will now focus on a very narrow range <strong>of</strong> fragment masses around 1 g<br />

that are believed to be at the “threshold <strong>of</strong> lethality” <strong>in</strong> terms <strong>of</strong> the impacts on<br />

the operational satellites. For short-term projections <strong>in</strong> this range, we will separate<br />

mass <strong>and</strong> altitude distributions by sett<strong>in</strong>g<br />

We will also use cumulative distributions<br />

<strong>and</strong><br />

ρ ki (m, H) = f ki (m) g ki (H). (7)<br />

F ki (m) =<br />

G ki (H) =<br />

∫ ∞<br />

m<br />

∫ ∞<br />

H<br />

f ki (µ) dµ (8)<br />

g ki (h) dh. (9)<br />

Appendix B suggests a simple power law distribution for the number <strong>of</strong> fragments<br />

heavier than m,<br />

F ki (m) = κ ki M k (m c /m) γ , (10)<br />

where m c = 1 g is a characteristic mass, κ ki is the average statistically expected<br />

yield <strong>of</strong> fragments heavier than m c per unit mass <strong>of</strong> the object B k produced <strong>in</strong><br />

a collision with the object B i , M k is the mass <strong>of</strong> the object B k , <strong>and</strong> γ ≈ 0.8.<br />

Based on the data from the Fengyun-1C <strong>and</strong> Cosmos-Iridium events, an estimate<br />

<strong>of</strong> κ ki ≈ 24/kg is derived <strong>in</strong> Appendix B. For each object, the average yield will<br />

depend on its composition <strong>and</strong> design. <strong>The</strong> correspond<strong>in</strong>g distribution density is<br />

f ki (m) = κ ki M k γ m γ c /m γ+1 . (11)<br />

Analysis <strong>in</strong> Appendix C suggests the follow<strong>in</strong>g approximation for the altitude<br />

distribution <strong>of</strong> collision fragments<br />

n(h, h 0 ) = k 0<br />

h s<br />

(<br />

1 + |h − h 0|<br />

h s<br />

) −b<br />

, (12)<br />

where h 0 is the collision altitude, h s is the scale height <strong>of</strong> the distribution, b ≈ 2.37,<br />

<strong>and</strong> k 0 = (b − 1)/2 ≈ 0.69 is a normalization coefficient, such that<br />

∫ ∞<br />

0<br />

n(h, h 0 ) dh = 1.<br />

Characteristic values <strong>of</strong> h s are estimated <strong>in</strong> Appendix C for tracked collision fragments,<br />

however, there is no data on small untracked fragments. It is anticipated

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