High Kinetic Energy Ion Mobility Spectrometry (HiKE-IMS)
is a versatile
technique for the detection of gaseous target molecules that is particularly
useful in complex chemical environments, while the instrumental effort
is low. Operating HiKE-IMS at reduced pressures from 10 to 60 mbar
results in fewer ion-neutral collisions than at ambient pressure,
reducing chemical cross-sensitivities and eliminating the need for
a preceding separation dimension, e.g., by gas chromatography. In
addition, HiKE-IMS allows operation over a wide range of reduced electric
field strengths E/N up to 120 Td,
allowing separation of ions by low-field ion mobility and exploiting
the field dependence of ion mobility, potentially allowing separation
of ion species at high E/N despite
similar low-field ion mobilities. Given these advantages, HiKE-IMS
can be a useful tool for trace gas analysis such as triacetone triperoxide
(TATP) detection. In this study, we employed HiKE-IMS to detect TATP.
We explore the ionization of TATP and the field-dependent ion mobilities,
providing a database of the ion mobilities depending on E/N. Confirming the literature results, ionization
of TATP by proton transfer with H3O+ in HiKE-IMS
generates fragments, but using NH4
+ as the primary
reactant ion leads to the TATP·NH4
+ adduct.
This adduct fragments at high E/N, which could provide additional information for reliable detection
of TATP. Thus, operating HiKE-IMS at variable E/N in the drift region generates a unique fingerprint of
TATP made of all ion species related to TATP and their ion mobilities
depending on E/N, potentially reducing
the rate of false positives.