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LIBS Spectroscopy: What Laser-Induced Breakdown Spectroscopy Measures and Its Limits

LIBS (laser-induced breakdown spectroscopy) reads elements from a laser-made plasma. How it works, its parts, and a sourced limits checklist.

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LIBS spectroscopy (laser-induced breakdown spectroscopy) identifies the elements in a sample by firing a short laser pulse at it, turning a tiny spot into a hot plasma, and reading the light that plasma emits. It needs essentially no sample preparation and works on solids, liquids and air, but it is less accurate and precise than ICP-MS or XRF.

Short answer

LIBS is a fast, portable atomic emission technique. A laser pulse ablates a microscopic amount of material, the resulting plasma emits light at wavelengths characteristic of the elements present, and a spectrometer records that spectrum. Treat it as a rapid screening and fingerprinting tool, and use ICP-MS or XRF when accuracy and precision matter most.

Definition and scope: one technique, several names

The same method appears in searches and papers as laser-induced breakdown spectroscopy, laser induced breakdown spectroscopy, laser-induced spectroscopy, laser breakdown spectroscopy, or simply LIBS. The differences are hyphenation and abbreviation, not method. The Michigan State University nanotechnology methods page on the Science Education Resource Center (SERC) site describes LIBS as a fast, portable, in situ atomic spectroscopy that can determine the elements in a solid, liquid or air sample, or produce a chemical “fingerprint” of it. Each laser shot leaves a crater of roughly 30 to 400 micrometres across.

How a LIBS measurement works

From laser pulse to spectrum

According to SERC, the laser pulse ablates the sample and forms a plasma hotter than 10,000 K. Excited electrons in the plasma drop back to lower energy levels and emit photons, and the spectrum is recorded across roughly 200 to 1000 nm. The Planetology group at the University of Münster, which operates LIBS systems for geological and planetary samples, gives a plasma temperature of about 10,000 to 20,000 °C and notes that matter can be analysed regardless of its physical state with no or only marginal sample preparation.

Molecules in the plasma emit as well; SERC notes this is exploited in laser-ablation molecular isotopic spectrometry (LAMIS) to obtain isotope ratios.

Instrument parts

  • Laser. SERC reports that the Nd:YAG laser is the most common, at 1064 nm or its harmonics (266 and 213 nm), with pulse widths of 6 to 15 ns and repetition rates from single shots to more than 20 Hz. Double-pulse arrangements increase the signal. The Münster system uses 1 to 250 mJ pulses of 6 to 8 ns.
  • Light collection. A lens and optical fibre collect the emission. Stand-off systems use a telescope from several metres away; NASA Spinoff 2015 describes the ChemCam instrument on the Curiosity rover analysing targets from as far away as 23 feet with a pulse lasting about five-billionths of a second.
  • Spectrograph and detector. SERC describes echelle spectrographs with CCD detectors, with collection starting a few microseconds after the pulse to reduce background light. The Münster system covers 191 to 380 nm and 279 to 900 nm.

LIBS compared with ICP-MS and XRF

The SERC page sets LIBS against ICP-MS and XRF. The table lists only the points that page makes.

Point What SERC states about LIBS
Accuracy and precision Lower than ICP-MS or XRF
Sample preparation Rapid, with essentially no sample preparation
Light elements (H, Li, Be) Highly sensitive
Portability Handheld units about the size of a cordless drill exist

For the ICP side of this choice, see the CASRAI comparison of ICP-MS and ICP-OES and the guide to ICP-MS sample preparation by acid digestion; for another elemental method, see atomic absorption spectroscopy.

Where it matters for labs: a limits checklist

Before relying on LIBS data, check these limits that SERC lists:

  • Shot-to-shot variation. Many spectra are averaged to get a stable result.
  • Accuracy. Accuracy and precision are lower than ICP-MS or XRF.
  • Calibration. Quantification with multivariate methods such as partial least squares regression outperforms single-peak methods, and LIBS calibrations typically require many more standards than other techniques.
  • Instrument dependence. Spectra differ between instruments, so datasets from different instruments generally cannot be combined.

Reported applications include rocks, minerals, soils, food and atmospheric particulates, and fingerprinting tasks such as gem and conflict-mineral provenance, bacterial identification, aggregate properties and detecting heat treatment in metals. The Münster page gives detection limits from ppm to ppt depending on the element. Because the method uses a pulsed laser, instrument use falls under laser safety rules; see the guide to laser safety classes and the explainer on the ANSI Z136.1 laser safety standard.

Common misunderstandings

  • “LIBS and laser-induced spectroscopy are different methods.” They are alternate names for the same technique.
  • “No sample preparation means no sample effects.” Minimal preparation is an advantage, but spectra vary shot to shot and between instruments, which is why averaging and matched calibration standards are needed.
  • “It replaces ICP-MS.” SERC places its accuracy and precision below ICP-MS and XRF, so it complements them.

FAQ

What does LIBS stand for?

Laser-induced breakdown spectroscopy. It is also written laser induced breakdown spectroscopy, and shortened informally to laser breakdown spectroscopy or laser-induced spectroscopy.

Is LIBS destructive?

It removes a small amount of material. SERC reports craters of roughly 30 to 400 micrometres in diameter, and the NASA Spinoff article describes a pinhole-sized analysis area.

What wavelengths does a LIBS spectrum cover?

SERC gives about 200 to 1000 nm. The Münster system covers 191 to 380 nm and 279 to 900 nm with two spectrometers.

Can LIBS analyse samples at a distance?

Yes. Stand-off systems collect light with a telescope from several metres; ChemCam on the Curiosity rover is the example SERC and NASA describe.

Sources

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