Borderline Aggregation Kinetics in ``Dry'' and ``Wet'' Environments
Paul. L. Krapivsky (CIMS, NYU), Sidney Redner (BU)

TL;DR
This paper analyzes the kinetics of aggregation processes influenced by evaporation and condensation, revealing critical behaviors, scaling laws, and exact solutions for different growth rates and environmental conditions.
Contribution
It provides a comprehensive analysis of aggregation-evaporation and aggregation-condensation kinetics, including exact solutions and asymptotic behaviors for various growth models.
Findings
Critical evaporation rate leads to a $k^{-5/2}$ mass distribution.
Typical cluster mass grows as $t^{2/3}$ at critical evaporation.
Scaling laws depend on the cluster growth rate $L_k$, with different growth behaviors.
Abstract
We investigate the kinetics of constant-kernel aggregation which is augmented by either: (a) evaporation of monomers from finite-mass clusters, or (b) continuous cluster growth -- \ie, condensation. The rate equations for these two processes are analyzed using both exact and asymptotic methods. In aggregation-evaporation, if the evaporation is mass conserving, \ie, the monomers which evaporate remain in the system and continue to be reactive, the competition between evaporation and aggregation leads to several asymptotic outcomes. For weak evaporation, the kinetics is similar to that of aggregation with no evaporation, while equilibrium is quickly reached in the opposite case. At a critical evaporation rate, the cluster mass distribution decays as , where is the mass, while the typical cluster mass grows with time as . In aggregation-condensation, we consider the…
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