Ion mobility spectrometers exist based on various principles, optimized for different applications. A review from 2014 lists eight different ion mobility spectrometry concepts.
Drift tube ion mobility spectrometry Drift tube ion mobility spectrometry (DTIMS) measures how long a given ion takes to traverse a given length in a uniform
electric field through a given atmosphere. In specified intervals, a sample of the ions is let into the drift region; the gating mechanism is based on a charged electrode working in a similar way as the
control grid in
triodes works for electrons. For precise control of the ion pulse width admitted to the drift tube, more complex gating systems such as a
Bradbury–Nielsen or a field switching shutter are employed. Once in the drift tube, ions are subjected to a homogeneous electric field ranging from a few volts per centimetre up to many hundreds of volts per centimetre. This electric field then drives the ions through the drift tube where they interact with the neutral drift molecules contained within the system and separate based on the
ion mobility, arriving at the detector for measurement. Ions are recorded at the detector in order from the fastest to the slowest, generating a response signal characteristic for the chemical composition of the measured sample. The ion mobility
K can then be experimentally determined from the drift time
tD of an ion traversing within a homogeneous electric field the potential difference
U in the drift length
L. : K = \frac{L^2}{t_\text{D} U} A drift tube's resolving power
RP can, when diffusion is assumed as the sole contributor to peak broadening, be calculated as : R_\text{P}= \frac{t_\text{D}}{\Delta t_\text{D}}= \sqrt{\frac{LEQ}{16kT\ln2}} where
tD is the ion drift time, Δ
tD is the
full width at half maximum,
L is the tube length,
E is the electric field strength,
Q is the ion charge,
k is the Boltzmann constant, and
T is the drift gas temperature. Ambient pressure methods allow for higher resolving power and greater separation selectivity due to a higher rate of ion-molecule interactions and is typically used for stand-alone devices, as well as for detectors for gas, liquid, and supercriticial fluid chromatography. As shown above, the resolving power depends on the total voltage drop the ion traverses. Using a drift voltage of 25 kV in a 15 cm long atmospheric pressure drift tube, a resolving power above 250 is achievable even for small, single charged ions. This is sufficient to achieve separation of some isotopologues based on their difference in
reduced mass μ.
Low pressure drift tube Reduced pressure drift tubes operate using the same principles as their atmospheric pressure counterparts, but at drift gas pressure of only a few torr. Due to the vastly reduced number of ion-neutral interactions, much longer drift tubes or much faster ion shutters are necessary to achieve the same resolving power. However, the reduced pressure operation offers several advantages. First, it eases interfacing the IMS with mass spectrometry. and re-focussed radially during and after the separation. Third, high values of
E/
N can be achieved, allowing for direct measurement of
K(
E/
N) over a wide range.
Travelling wave Though drift electric fields are normally uniform, non-uniform drift fields can also be used. One example is the travelling wave IMS, which is a low pressure drift tube IMS where the electric field is only applied in a small region of the drift tube. This region then moves along the drift tube, creating a wave pushing the ions towards the detector, removing the need for a high total drift voltage. A direct determination of collision cross sections (CCS) is not possible, using TWIMS. Calibrants can help circumvent this major drawback, however, these should be matched for size, charge and chemical class of the given analyte. An especially noteworthy variant is the "SUPER" IMS, which combines ion trapping by the so-called structures for lossless ion manipulations (SLIM) with several passes through the same drift region to achieve extremely high resolving powers.
Trapped ion mobility spectrometry In trapped ion mobility spectrometry (TIMS), ions are held stationary (or trapped) in a flowing buffer gas by an axial electric field gradient (EFG) profile while the application of radio frequency (rf) potentials results in trapping in the radial dimension. TIMS operates in the pressure range of 2 to 5 hPa and replaces the ion funnel found in the source region of modern mass spectrometers. It can be coupled with nearly any mass analyzer through either the standard mode of operation for beam-type instruments or selective accumulation mode (SA-TIMS) when used with trapping mass spectrometry (MS) instruments. Effectively, the drift cell is prolonged by the ion motion created through the gas flow. Thus, TIMS devices do neither require large size nor high voltage in order to achieve high resolution, for instance achieving over 250 resolving power from a 4.7 cm device through the use of extended separation times. However, the resolving power strongly depends on the ion mobility and decreases for more mobile ions. In addition, TIMS can be capable of higher sensitivity than other ion mobility systems because no grids or shutters exist in the ion path, improving ion transmission both during ion mobility experiments and while operating in a transparent MS only mode.
High-field asymmetric waveform ion mobility spectrometry DMS (
differential mobility spectrometer) or FAIMS (
field asymmetric ion mobility spectrometer) make use of the dependence of the ion mobility
K on the electric field strength
E at high electric fields. Ions are transported through the device by the drift gas flow and subjected to different field strengths in orthogonal direction for different amounts of time. Ions are deflected towards the walls of the analyzer based on the change of their mobility. Thereby only ions with a certain mobility dependence can pass the thus created filter
Differential mobility analyzer A
differential mobility analyzer (
DMA) makes use of a fast gas stream perpendicular to the electric field. Thereby ions of different mobilities undergo different trajectories. This type of IMS corresponds to the
sector instruments in
mass spectrometry. They also work as a scannable filter. Examples include the differential mobility detector first commercialized by
Varian in the CP-4900 MicroGC. Aspiration IMS operates with open-loop circulation of sampled air. Sample flow is passed via ionization chamber and then enters to measurement area where the ions are deflected into one or more measuring electrodes by perpendicular
electric field which can be either static or varying. The output of the sensor is characteristic of the ion mobility distribution and can be used for detection and identification purposes. A DMA can separate charged
aerosol particles or
ions according to their mobility in an
electric field prior to their detection, which can be done with several means, including electrometers or the more sophisticated mass spectrometers. == Drift gas ==