INHOMOGENEOUS CHEMICAL EVOLUTION OF THE GALACTIC DISK

We present analytical models for inhomogeneous chemical evolution (ICE) of systems in which the star formation history resembles a series of bursts, localized in space and/or time, with intermittent periods of remixing. The additional parameter of this model is the metallicity increment of bursting subsystems, but this parameter is constrained by the spread in the age-metallicity relation. We apply this model to the solar annulus in the Galactic disk and show that ICE models yield an improved fit to the observed shape of the stellar abundance distribution function (ADF). The G-dwarf problem can be alleviated with ICE models, but infall of metal poor ps and/or some preenrichment of the disk during the epoch of protogalactic evolution is still required to explain the paucity of low-metallicity dwarfs. ICE models also suggest an explanation of the reduced frequency of metal-rich G-dwarfs relative to the predictions of the simple model. It does not seem likely that chemical evolution of the solar annulus proceeded in a medium that was well-mixed at all times. So, while the simple model may be used to describe the evolution of bulk abundances in a well-mixed system, we promote the use of simple ICE models to describe the evolution of systems that locally undergo enhanced star-forming bursts, but in which the resulting chemical enrichments are only slowly remixed and homogenized within the global system.