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The drift cells collect the ionisation produced by charged particles, thus allowing the tracks to be reconstructed.
Within the 18 drift chambers are a total of 35,148 individually instrumented hexagonal drift cells.
The tracking detector is made up of four modules each containing about 500 drift cells containing a gaseous mix of helium, ethanol and argon.
It is possible to couple two drift cells and to do IMS experiments [ 50– 50].
However, traps that operate at lower pressure (mTorr) are often coupled to drift cells operating at higher pressures (e.g., a few torr).
The ion drift technique has origins in early parallel-plate drift cells which were used extensively during the early development of the field.
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Each drift cell has a central 40 micron wire surrounded by twelve 50 micron wires made of stainless steel.
The basic idea behind TIMS is the reversal of the classic drift cell analyzer.
The periodic-focusing DC ion guide (PDC IG) drift cell provides increased ion transmission with minimal loss in resolution.
Heating the drift cell to ∼450 K caused dissociation of the (2M + 2H 2+ ion into two (M + H)+ units on the 1 ms experimental time scale.
The ion pulses are injected into a six-ring drift cell filled with helium where ions having different electronic configurations can separate because they have different ion mobilities.
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