ICP-MS Systems and Technologies

An ICP-MS system comprises five basic parts: the sample introduction system, plasma, vacuum interface, ion optics with mass analyzer, and ion detection system (figure 1). The sample introduction system and plasma are operated at atmospheric pressure, whereas the ion optics, mass discrimination, and ion detection areas are operated under high vacuum.

The plasma is a mixture of ions, electrons, and atoms that, at atmospheric pressure, has an extremely high temperature (up to 10,000 K). At these temperatures, most elements easily make the transition from atoms to ions. A very useful characteristic of the argon plasma is that most of the formed ions are single charged positive ions, so mass spectra are relatively simple to generate and interpret.

ICP-MS Instrumentation is varied and the specific design is largely based on the type of applications that the instrument is running. The plasma itself is sustained by a radio frequency (RF) generator, which delivers energy using an induction coil or load coil. Samples are ionized by the plasma and are transferred to the mass analyzer via a vacuum interface. Once separated, ions are detected by the ICP-MS detection system for data analysis by the operator.

The plasma itself generates a magnetic field that directly opposes the RF generator. For a stable plasma, the RF generator and plasma frequencies are synchronized (or ‘matched’) so the magnetic field coming from the plasma has minimal effect and the plasma can be sustained more easily. When samples are introduced, the plasma frequency changes, so the RF generator may become mismatched to the plasma.

Due to this phenomenon, an RF generator must be capable of coping with fluctuations in the plasma by either returning the plasma frequency to the RF generator frequency (performed in frequency-locked generators), or by adjusting the RF generator frequency so that it matches that of the plasma (performed in free-running generators). Free-running RF generators are capable of coping with wider variations in the sample matrix as well, and can therefore sustain the plasma for longer time periods. In so doing, they enable longer analyses because a more robust plasma is possible.

The sample interface is a crucial part of the ICP-MS, comprising a pair of water-cooled cones that allow ions from the sample to enter the high vacuum region.

The sampler cone allows only the central channel of the plasma (where the sample ions are formed) into the intermediate vacuum region. This material also undergoes supersonic expansion so that ions are pulled into the high vacuum region through a skimmer cone, with the aid of a negatively charged extraction lens that is located behind the cone.

Once they pass through the high vacuum region, elemental masses of the sample are separated using a mass analyzer.

There are two types of mass analyzer typically used in ICP-MS, namely quadrupole and magnetic sector. Quadrupole mass analyzers are sequential, so each element is measured in sequence. Magnetic sector analyzers can be either sequential or simultaneous depending on the geometry of the instrument components.

Quadrupole instruments are typically used in routine labs since they are relatively easy to operate and maintain. Magnetic sector instruments are inherently more sensitive than quadrupole instruments because they use higher ion extraction potentials. As a result, they are used in more specialized applications, or when higher sensitivity is needed.

Two of the oppositely placed poles have a positive potential applied to them, and the other two have a negative potential applied. So, the quadrupole actually generates two overlapping electric fields: one in the horizontal plane and the other in the vertical plane.

The DC component of the electric field produces a constant force on the ions while they travel through the quadrupole. Because the ions are positively charged from the plasma, the positive poles repel the ions into the center of the mass analyzer, while the negative poles attract the ions away from the center of the quadrupole.

The AC component counteracts the effect of the DC component depending on the ion’s mass. Because the ions gain energy as they pass through the quadrupole, the degree to which the AC component affects the ion flight path increases along the length of the quadrupole.

Lighter ions are more easily affected by the AC field than heavier ions and they follow the oscillations of the RF driving circuit. Heavier ions are significantly less responsive to the AC field, tending to follow the DC field instead. This means that for the positive pair of poles, lighter ions are pushed out of the quadrupole along its length by oscillations. For the negative pair of poles, the lighter ions are held in the quadrupole by oscillations.

Mass resolution can be controlled by increasing the DC offset of this line, but this does come with an associated loss in sensitivity. Also, the practical resolution limit depends on the overall sensitivity of the instrument. Typically, this is 0.7–0.85u in ‘normal’ resolution. However, in most quadrupole mass spectrometers, resolution can be switched to ‘high’ resolution at 0.3–0.4u. Such a switch helps attenuate very high signals of, for example, matrix components.

Momentum is the product of an ion’s mass and velocity, which is in turn governed by the amount of kinetic energy it contains. Because a plasma produces ions with a wide range of kinetic energies, ions of slightly varying mass could have the same momentum. It is therefore possible for two ions of different mass to have the same radius of curvature through the magnet.

To compensate for this effect, an electric sector analyzer (ESA) is used to separate ions by their kinetic energy. The ESA focuses ions of the same mass yet slightly varying kinetic energies onto the same point in space, so that any remaining ions of slightly varying mass can be rejected from the ion beam.

Correcting ion energies allows the magnetic sector to separate ions into different points in space. Placing separate detectors at these points allows ions to be detected simultaneously, and these so-called ‘multi-collector’ systems are capable of measuring isotope ratios with much greater precision than can be achieved with sequential quadrupole or magnetic sector mass analyzers. In this case, the ESA and magnet are reversed to provide better spatial resolution and stability.

Reducing interferences is a key challenge in ICP-MS, but it can be achieved in several ways. One of the simplest methods is using alternative sample introduction, including aerosol desolvation, to minimize the population of unwanted precursor ions in the plasma itself. This serves to reduce molecular species entering the mass spectrometer. Cold plasma techniques take this effect into account; in plasma generation, the plasma power is reduced, which also reduces the formation of polyatomic species. This method, however, assumes consistent matrix effects; any significant changes in matrix from one sample to the next could have a significant effect on interference generation that cannot be accounted for by internal standardization.

Isobaric interferences can be addressed by measuring another interreference isotope and, after correcting for natural isotope abundance differences, using those counts to estimate the proportion of signal in the analyte channel that is derived from the interference. This can then be subtracted before further data processing to give a more accurate result. This method assumes no isotope fractionation, so it cannot be used for isotope dilution or any method intended for geological process analysis.

The methods mentioned above are not always successful in addressing interferences; therefore, collision reaction cell (CRC) technology has emerged as a comprehensive solution to this issue. In CRC, the cell is a multipole system like the mass analyzer, but only operates with RF voltage. This means it can transmit a range of masses, but each ion mass has an optimum transmission at a different AC voltage.

The CRC can be set to kinetic energy discrimination (KED) mode, which is the most universal mode for interference removal. This mode utilizes helium as the cell gas because it is inert and does not react with the analyte. Helium also has low mass, so it does not degrade signal sensitivity very much.

KED creates a potential energy barrier at the CRC exit using ion lenses. Because the exit of the CRC is more positive than the entrance, this slightly repels ions back into the cell. As the sample ions pass through the CRC, they encounter neutral helium atoms and collide. These collisions slow the ions down, so their kinetic energy is reduced. As the ions progress through the cell and collide with additional upstream helium atoms, their kinetic energy is reduced to the point where the potential energy barrier prevents them from leaving the cell as part of the ion beam, resulting in their ejection from the cell.

Polyatomic ions are larger than sample ions because they are made up of multiple atoms by definition. Because of this, they encounter more collisions than the analyte ions, and so lose energy faster. By altering the amount of helium in the cell, it is possible to reduce the kinetic energy of the polyatomic interferences to the point where they are ejected by the potential energy barrier set up in the cell, but not the analyte ion.