Knowing
accurate saturated vapor pressures of explosives at ambient
conditions is imperative to provide realistic boundaries on available
vapor for ultra-trace detection. In quantifying vapor content emanating
from low-volatility explosives, we observed discrepancies between
the quantity of explosive expected based on literature vapor pressure
values and the amount detected near ambient temperatures. Most vapor
pressure measurements for low-volatility explosives, such as RDX (1,3,5-trinitro-1,3,5-triazinane)
and HMX (1,3,5,7-tetranitro-1,3,5,7-tetrazocane), have been made at
temperatures far exceeding 25 °C and linear extrapolation of
these higher temperature trends appears to underestimate vapor pressures
near room temperature. Our goal was to measure vapor pressures as
a function of temperature closer to ambient conditions. We used saturated
RDX and HMX vapor sources at controlled temperatures to produce vapors
that were then collected and analyzed via atmospheric flow tube-mass
spectrometry (AFT-MS). The parts-per-quadrillion (ppqv)
sensitivity of AFT-MS enabled measurement of RDX vapor pressures at
temperatures as low as 7 °C and HMX vapor pressures at temperatures
as low as 40 °C for the first time. Furthermore, these vapor
pressures were corroborated with analysis of vapor generated by nebulizing
low concentration solutions of RDX and HMX. We report updated vapor
pressure values for both RDX and HMX. Based on our measurements, the
vapor pressure of RDX at 25 °C is 3 ± 1 × 10–11 atm (i.e., 30 parts per trillion by volume, pptv), the
vapor pressure of HMX is 1.0 ± 0.6 × 10–14 atm (10 ppqv) at 40 °C and, with extrapolation,
HMX has a vapor pressure of 1.0 ± 0.6 × 10–15 atm (1.0 ppqv) at 25 °C.