The extremely low sodium vapor pressures which are present in hot quartz furnace tube atmospheres have been measured by atomic absorption spectroscopy. In the system described, sodium vapor pressures are measured between 10 -6 and l0 -9 Torr; however, this range can be extended by simple changes in optics and/or absorption cell length. The data show that the sodium vapor pressure in a new quartz tube changes slowly during heating until the rate of sodium in-diffusing from the hot ceramic liner is balanced by the rate of sodium out-diffusing to the cooler portions of the system. If the design of the furnace tube system is such that the source of the sodium, the furnace liner, is separated by an air space from the inner quartz tube, then the equilibrium sodium vapor pressure inside this tube may be decreased at least tenfold. Foreign gas composition has little effect on the sodium vapor pressure, providing no chemical reactions occur in the system. However, the reaction of hydrogen with the quartz surface results in a marked increase in the sodium vapor pressure. The system described may be easily adapted for determination of other contaminant vapors which could be present in hot quartz furnace tube atmospheres~