Write the distributed fragment power-law size distribution as . A spherical fragment has mass . Since this population contains one half of the target mass,and henceThe distributed fragments have total geometric cross-sectionThe single fragment containing the other half of the mass has diameter and cross-section . Therefore the exact result within the model isFor and , area is dominated by the smallest distributed fragments while mass is dominated by the largest, so normally the first term is negligible and
The half-target mass assigned to equal fragments containsfragments. Their total geometric cross-section is consequentlyIgnoring the negligible single largest fragment in ,For example, if , this ratio is and is large for a broad size range. This reflects the inverse-size cross-section per unit mass of equal-density spherical fragments: concentrating the mass at small creates more area.
Let the belt contain bodies. Its total mass fixesFor equal mass density, an impactor of diameter supplies specific impact energyThus catastrophic disruption requires , whereThe impactor number density per diameter is . Neglecting gravitational focusing, the geometric collision cross-section is , so the exact catastrophic planetesimal collision rate in this model isEquivalently, with ,If , the steep distribution makes impactors just above dominate and their collision cross-section is approximately . HenceThis approximation also assumes a common and size-independent catastrophic disruption threshold .
A collision producing cross-section has target diameterby part (ii). The production rate of clumps above is the number of targets in each size interval times their per-target catastrophic rate. Therefore, with ,Using the small-impactor approximation from part (iii) givesWhen , this reduces toAssigning each event to its much larger target avoids double-counting collisions in this approximation.
For the Dohnanyi collisional cascade exponent and ,Substitution in part (iv) yieldsThusThe dependence is the pair-collision scaling. Longer-lived clumps are more numerous, stronger bodies disrupt less often, and smaller fragments put more geometric cross-section into each event. At fixed total mass, increasing lowers the normalization of the power-law size distribution and therefore lowers the event rate.
The impact gives fragments a spread of orbital energy and specific angular momentum. Their resulting spread of mean motion lets Keplerian shear stretch a compact dust clump into an arc and then a ring, while the spread of orbital frequencies causes phase mixing. Size-dependent radiation-pressure coefficients immediately place small grains on different eccentric or even radiation-pressure blowout orbits; Poynting–Robertson drag and stellar-wind drag then alter their orbits on longer timescales. Further collisions grind or disperse the clump, and planetary perturbations can accelerate mixing.
These processes depend strongly on . Small grains have larger radiation-force-to-gravity ratios and generally shorter collisional or drag lifetimes, while larger fragments remain closer to the parent orbit but can preserve a velocity-dispersion-driven clump for longer. The lifetime also depends on collision location, ejection velocities, optical depth, and orbital radius. A universal fixed is therefore a useful population-model approximation, not a literal property of every collision; a size- and event-dependent lifetime distribution is more realistic.
Articles by others on the same topic
There are currently no matching articles.