Observational evidence for the accretion of low-metallicity gas onto the Milky Way; metallicity, physical conditions and distance limit for HVC complex C
B. P. Wakker, J. C. Howk, B. D. Savage, S. L. Tufte, R. J. Reynolds, H. van Woerden, U. J. Schwarz, R. F. Peletier
Abstract
We present observations of the (field of the) Seyfert galaxy Mark290, which probes the high-velocity cloud (HVC) complex C, one of the largest HVCs. We find that this object has a metallicity of 0.094pm0.020(+0.022-0.019) times solar. We determine a lower limit to its distance of 5 kpc (z>3.5 kpc). If the gas is in thermal equilibrium with a hot halo, then it is also likely that D<30 kpc, putting the HVC in the Galactic Halo, as was the case for HVC complex~A (for which z=2.5--7 kpc). We find that, on this sightline, H+ represents 23pm10% of the hydrogen in the HVC. The total gaseous mass is 2x106 (D/5 kpc)2 Msun and, depending on whether the space velocity is completely radial or vertical, the HVC represents a downward mass flux of ~0.036-0.083 (D/5 kpc) Msun/yr, or 2.9--6.7x10-3 (D/5 kpc)-1 Msun/yr/kpc2. The low metallicity and large mass suggest that complex C is unlikely to be part of a Galactic Fountain, but rather represents accreting low-metallicity material. It may be a present-day analogue of the damped Ly-alpha absorbers seen in QSO spectra. Our abundance result provides the first direct observational evidence for the infall of low-metallicity gas on the Milky Way, required in models of galactic chemical evolution. It remains to be seen whether ultimately complex C is a remnant of the formation of the Milky Way (Oort 1970), a gas cloud orbiting the Galaxy (Kerr & Sullivan 1969), a Local Group object (Verschuur 1969, Blitz et al. 1996), the result of tidal interactions between the Magellanic System and the Galaxy >3 Gyr ago (an "Old Magellanic Stream"; Toomre, quoted in Kerr & Sullivan 1969), or was formed when hot, ionized intergalactic gas was compressed by the motion of the Milky Way (Silk et al. 1987).
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