Accuracy of consequence assessments could be improved by accounting for the leak path deposition of aerosol in the source term. Recent experimental measurements from Sandia (2018) provided evidence of partial microchannel plugging due to particulate deposition. This filtration effect is relevant to the source term assessments and it is not unreasonable to anticipate that aerosol deposition in more realistic geometries could even lead to complete plugging of the leak path. This report summarizes current progress (as of end of Q3 FY 2020) on the development of a phenomenological model of aerosol transport, deposition, and plugging through microchannels. The purpose is to introduce a generic, reliable numerical model for the prediction of aerosol transport, deposition, and plugging in leak paths while accounting for potential plugging formation. This report includes (1) an overview of recent additions and improvements on the recently developed numerical model to analyze the various deposition processes in leak paths, to provide quantitative estimates of penetration factors, and to gain an understanding of the variables that affect them and (2) a summary of recent benchmarking results of the model's validity with recent experimental measurements from Sandia.It is found that aerosol deposition on canister walls would occur from a cloud with homogeneous distribution due to thermal flow convection and is only possible when the particles penetrate into the stagnant boundary layer in contact with the walls. Typically, larger particles (>1 μm) are removed by gravitation deposition whereas smaller particles (<0.1 μm) deposit due to diffusive deposition. A temperature difference of 0.01 o C in a canister with an effective wall length of four meters is capable of keeping an aerosol cloud consisting of particles smaller than 20 μm homogenously distributed inside the canister. This is a direct consequence of the large difference between convective flow velocity, in the order of 10-20 cm/s or higher, and particle's settling velocity which is several orders of magnitude lower (~10 -3 cm/s).Further, it is shown that within enclosure volumes within range of typical canisters, a homogeneously distributed monodisperse aerosol will decay exponentially due to gravitational settling with a decay constant for particles of 1 μm aerodynamic diameter is 0.02 hr -1 and a half-life of 34.6 hrs. For 0.1 μm aerodynamic diameter the decay constant is 0.002 hr -1 with a half-life of 346 hrs. Similarly, for 10 μm aerodynamic diameter, the decay constant is 0.2 hr -1 with a half-life of 3.46 hrs. Coagulation and diffusive deposition are expected to decrease these times even further.