Abstract. Compaction is the process by which snow densifies, storing water in alpine regions and transforming snow into ice on the surface of glaciers. Despite its importance in determining snow-water equivalent and glacier-induced sea level rise, we still lack a complete understanding of the physical mechanisms underlying snow compaction. In essence, compaction is a rheological process, where the rheology evolves with depth due to variation in temperature, pressure, humidity, meltwater. The rheology of snow compaction can be determined in a few ways, for example, through empirical investigations (e.g. Herron & Langway,1980 J. Glaciol.), by microstructural considerations (e.g. Alley, 1987 J. Phys.), or by measuring the rheology directly, which is the approach we take here. Using a ``French-press'' compression stage, Wang and Baker (2013, J. Geophys. Res.) compressed numerous snow samples of different densities. Here we derive a mixture theory for compaction and air flow through the porous snow to compare against these experimental data. We find that a plastic compaction law explains experimental results. Taking standard forms for the permeability and effective pressure as functions of the porosity, we show that this compaction mode persists for a range of densities and overburden loads. These findings suggest that measuring compaction in the lab is a promising direction for determining the rheology of snow though its many stages of densification.