Abstract:
An ion trap instrument working at atmospheric pressure, which alleviates requirements of bulky, power consuming vacuum pumps. Traps can accumulate selected ion species, effectively concentrating the analyte of interest and allowing laser spectroscopy to be performed. This lowers the detection threshold of this instrument compared to others and increases the selectivity.

Description:
CROSS-REFERENCE TO RELATED APPLICATION 
       [0001]    This application claims priority to U.S. Provisional Patent Application Ser. No. 61/116,970. 
     
    
     TECHNICAL FIELD 
       [0002]    This application relates in general to ion traps, and in particular, to ion traps operating at atmospheric pressures. 
       BACKGROUND 
       [0003]    Instrumentation for trace compound detection and identification are perpetually pushed for increased sensitivity, lower detection limits, higher resolution and smaller physical size. The most sensitive instruments available include mass spectrometers (MS), which require high vacuum and are bulky with typical volumes on the order of 0.2 m 3 . MS instruments can be either linear quadrupole or quadrupole ion traps. A second type of instrument, but which operates at atmospheric pressure, is the ion mobility spectrometer (IMS). Although the IMS and its closely related cousin, the Differential Mobility Spectrometer (DMS), have demonstrated sub-ppb detection capabilities, resolution between peaks is often poor, and for unknown multi-analyte mixtures, often peaks, and thus species, cannot be resolved. 
     
    
     
       BRIEF DESCRIPTION OF THE DRAWINGS 
         [0004]      FIG. 1  illustrates a schematic of an ion trap, comprising two endcaps ‘a’ and a ring ‘b’ with an electric potential across them, where schematic (1) illustrates positive-biased endcaps and forces on positive ions, while schematic (2) illustrates a reverse bias case; 
           [0005]      FIG. 2  illustrates potential in an ion trap; 
           [0006]      FIG. 3  illustrates a photo-acoustic sensor (PAS) cell; 
           [0007]      FIG. 4  illustrates an ion trap acoustic cell; 
           [0008]      FIG. 5  illustrates a schematic of an embodiment of the present invention; 
           [0009]      FIG. 6  illustrates a schematic of an embodiment of the present invention; 
           [0010]      FIG. 7  illustrates a flow diagram in accordance with an embodiment of the present invention; 
           [0011]      FIG. 8  illustrates a flow diagram in accordance with an embodiment of the present invention; and 
           [0012]      FIG. 9  illustrates a flow diagram in accordance with an embodiment of the present invention. 
       
    
    
     DETAILED DESCRIPTION 
       [0013]    The operating principle for mass spectrometers is to separate species by a mass to charge ratio, m/z, typically by employing an (oscillating) electric quadrupole field, and sometimes in conjunction with applied magnetic fields. The equation of motion for the ion species is: 
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         [0014]    The operating principle for ion mobility spectrometers is separation according to the ion&#39;s drift velocity through the ambient background gas under an applied electric field. The drift velocity is proportional to the electric field according to 
         [0000]        {right arrow over (v)} ( t )=κ( E ) {right arrow over (E)} ( {right arrow over (x)},t ) 
         [0015]    where κ(E) is the ion mobility. Ion mobility κ(E) is often approximated as a constant, but it is actually a power series in even powers of E (so that the drift velocity is an odd power of {right arrow over (E)} hence antisymmetric; when the electric field changes sign the velocity does too, which motion in an isotropic, homogeneous medium should do). Comparing the above two equations, and noting that the velocity is just the first time derivative of the position, the acceleration for an ion in a mass spectrometer is proportional to the electric field, whereas for an ion mobility spectrometer, the velocity is proportional to the electric field. That means the two principles of operation give rise to very different ion motion dynamics. 
         [0016]      FIG. 1  illustrates a schematic of an ion trap. The quadrupole potential in the trap can generically be written 
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         [0017]    And to satisfy Laplace&#39;s equation, the condition 
         [0000]      λ+σγ=1 
         [0018]    follows. For a quadrupole ion trap λ=σ=1, γ=−2. Writing the resulting potential in cylindrical coordinates gives: 
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         [0019]    For an arbitrarily chosen fixed value of Φ(r,z), the relationship between r and z define hyperbola, which are the shape of the ideal endcap and ring electrodes. A plot of the potential is shown in  FIG. 2 ; it is saddle shaped, meaning for a positive ion, the force is radially inward and trapping but axially expelling toward the endcaps, corresponding to schematic ( 2 ) in  FIG. 1 . If the potential is reversed, the corresponding situation is then ( 1 ) of  FIG. 1 . The restoring force increases linearly in both radial and axial coordinates. In operation, the potential Φ 0  is time dependent: 
         [0000]      φ 0 ( t )= U+V  cos(ω t ) 
         [0020]    This oscillating potential alternately produces a trapping then anti-trapping potential in both the radial and axial coordinates. If the frequency ω and potential V are judiciously chosen, the excursion of the ion motion will always be less than the position of the electrodes, making a stable trap. This can be visualized by imagining the potential in  FIG. 2  to rotate about the Phi axis at r=z=0; an ion will be jostled about under the influence of the time varying potential, but on average will experience a central restoring force. The ions can be cooled using momentum dissipation via a 10 mTorr background of helium gas admitted into the trap volume. 
         [0021]    Collisions between ions and helium atoms remove energy from the ions, i.e., energetically cooling and confining them closer to the center of the trap. 
         [0022]    A scan of the m/z ratios of all the different species of ions simultaneously held in the trap is made by sweeping the endcap-ring potential amplitude V and the frequency ω. An alternative process is to excite resonant ions using a small (few hundred millivolts) rf field across the two endcaps. This drives resonant ions into larger amplitude orbits where they are then forced into a detector electrode or channeltron type amplifier for current measurement. 
         [0023]      FIG. 3  illustrates a schematic of a differential ion mobility spectrometer. Trace analytes in a carrier gas, often ambient atmosphere, are flowed from left to right between two parallel plate electrodes. The analyte molecules are ionized by charge exchange with reactive ions generated by radioactive or electric sources. An asymmetric waveform comprising a short duration, large positive potential pulse followed by a long duration, small negative potential pulse moves ions in the zigzag motion indicated in the figure. A net effect is usually to drive the ions into the RF plates. 
         [0024]    By superimposing a small DC electric field across the parallel plates with the use of a compensation voltage Vc, the net trajectory can be made parallel to the plates. Resonant ions then pass through the filter and are detected upon exit by detection electrodes. As the compensation voltage is swept, peaks appear corresponding to different ion species. 
         [0025]    An embodiment of the present invention described herein combines elements of both the mass spectrometer and the ion mobility spectrometer. The ion trajectories in atmosphere indicated in  FIG. 3  are related to ion trajectories in vacuum in a linear ion quadrupole mass spectrometer. A similar principle that allows a linear quadrupole mass spectrometer to become a quadrupole ion trap allows the differential mobility spectrometer to become an atmospheric pressure ion trap. 
         [0026]      FIGS. 5 and 7  illustrate a trap  500  and its operation. Oscillating RF potentials are produced across the endcaps  501 ,  502  and ring electrode  503 ,  504  (see step  704 ). Trace analytes are ionized (step  701 ) via atmospheric pressure chemical ionization as in ion mobility spectrometers. A radioactive source  507  either external to the trap or possibly embedded within an electrode may be used (see step  702 ), or an external soft plasma or field ionization source may be employed. Externally generated ions may be loaded into the trap  500  by flowing them through the trap volume at low flow rates (see step  703 ). Ions slosh back and forth, but not necessarily symmetrically about the trap center. The ion&#39;s velocity is proportional to the instantaneous electric field, not the ion&#39;s acceleration, as is the case in conventional ion traps. Furthermore, the trap  500  may be operated with similar asymmetric waveforms as the differential mobility spectrometer, even including the DC compensation voltage, as directed by the control circuitry  508 . 
         [0027]    Because ion mobility is a function of the electric field strength, and the electric field increases linearly in both the radial and axial directions (but at different rates), ion trajectories are calculated numerically. A Monte Carlo simulation for this trap yields necessary performance characteristics. Once ions are trapped they may be selectively made to have larger excursion from the trap center until they strike a detector (step  710 ); or, laser spectroscopy may be performed for species identification (step  706 ). The detector may be a biased electrode, or a pair of biased electrodes, for sensing ions of + and − charges. Laser spectroscopy essentially recycles each ion&#39;s contribution to the signal so that extremely low concentrations are detectable. Alternatively, the ions may be released into a mass spectrometer (see step  707 ), or an ion mobility spectrometer (step  708 ). The spectrum may be collected and analyzed in step  709 . 
         [0028]    Another embodiment of an ion trap operating at atmospheric pressures uses the trap as an acoustic cell, which measures the concentration and types of ions that are created, which in turn permits a measure of trace chemicals in the atmosphere being probed. 
         [0029]      FIG. 4  illustrates a simplified schematic of a photo-acoustic cell (“PAS”). A gas is enclosed in a cell (not shown), with a cell volume on the order of 1 to 10 cm 3 . A beam of light (e.g., laser light) is passed through the gas in the cell. If the light is absorbed by the gas, the gas will heat up. By modulating the frequency (color) of the light, or by modulating the intensity of the light, a sound wave is created in the cell from the pulses of heat applied to the gas from the light being absorbed. The sound waves are detected by a sound transducer (e.g., microphone). The wavelength of light may be chosen to be sensitive to a particular analyte. The intensity of the sound waves will have some proportion to the concentration of the analyte being detected. In this way, the concentration of specific analytes in a gas is detected. By using several frequencies of light, a plurality of analytes can be detected using one cell. 
         [0030]    A problem with this approach is that the frequency (color) of the light may be hard to achieve except when using broad band light sources. However, in this case, the selectivity of the PAS will be degraded because of the broad spectral band of light used. Some telecom lasers exist in wavelengths useful for some analytes, but other analytes require expensive lasers. It may be preferential to excite the sound waves without using a light source. An ion trap acoustic cell addresses this issue. 
         [0031]    Referring to the schematic illustrated in  FIG. 5 , and the flow diagram of  FIG. 8 , an ion trap acoustic cell (“ITAC”)  500  does not use a light source to excite the sound waves, but uses heat generated by exciting ions in the trap  500  (see steps  801  and  803 ). The ITAC  500  may be configured similar to a standard ion trap. 
         [0032]    The electrodes  501 - 504  may be mounted on stiff, insulating walls  505 . One or more holes (not shown) may be positioned on the cell walls  505  to allow gas to come in and out of the cell  500  (see step  803 ). A hole in one or more electrodes  501 - 504  may be used to position a microphone or sound transducer  506  to monitor for sound waves (see step  808 ). Ni-63 beta sources or other radioactive materials  507  may be placed inside the cell  500  to provide a source of electrons to create ions in the gas (see step  802 ). Other sources of electrons or ions may also be used, such as UV light, corona discharge, dielectric barrier discharge, or insulating barrier discharge. By changing the frequency of the oscillating RF electric potentials on the electrodes and by changing the voltage of the oscillating RF electric fields with control circuitry  508 , specific ions can be trapped (see step  804 ). By modulating the RF on and off at acoustic frequencies (see step  807 ), sound waves are created in the cell  500  (see step  806 ). The intensity of the sound waves is proportional to the concentration of the analyte that is ionized. By sweeping through the parameters of the trapping field, the cell  500  can select which ions are trapped. The Ni-63 beta source  507  may be constantly creating ions. The ion trap  500  improves the sensitivity of acoustic cells since the trap  500  concentrates specific ions while more ions are continuously being made. 
         [0033]    As noted previously, an advantage is that light sources are no longer needed. Selectivity of ions is performed by sweeping the electrical parameters of the trap  500  with the control circuitry  508 . This opens the detection to a broad range of analytes (see step  809 ). 
         [0034]    Referring to  FIGS. 6 and 9 , an alternative embodiment of a PAS  600  is illustrated, which is a combination of RF trapping with light assisted photo-acoustic sensing. Components  601 - 608  operate similarly as components  501 - 508 , and steps  901 - 909  are similar to steps  801 - 809 . In this embodiment, the ions in the trap  600  are selected by tuning the parameters of the ion trap  600  (the RF frequency and amplitude), but the trap  600  may be operated in constant intensity with the light  601  introduced and modulates as in standard photo-acoustic spectroscopy by the control circuitry  608  (see steps  906 - 907 ). This may be referred to as an ion-assisted PAS  600 . An advantage is that it is possible to select different wavelengths to detect the analytes, allowing a lower cost laser  610  to be used for the PAS  600 .