Spectroscopy is the study of how matter interacts with electromagnetic radiation across wavelengths from radio waves to gamma rays. Instead of forming a conventional image, spectroscopic methods separate radiation by wavelength or frequency to produce a spectrum: a record of intensity versus wavelength. That spectrum encodes information about the identity of atoms, ions and molecules, their energy levels and transitions, as well as macroscopic properties such as temperature, pressure and velocity. Instruments used for these tasks are commonly called spectrometers or spectrographs; for basic introductions to the nature of electromagnetic radiation see light and electromagnetic waves.

Basic principles

At the quantum level, electrons and molecular vibrations occupy discrete energy states. Transitions between these states absorb or emit photons with energies equal to differences between levels, producing characteristic spectral lines or bands. Selection rules, line strengths and molecular structure determine which transitions are allowed and how intense they are. Continuous spectra may arise from hot dense sources, while line spectra appear from tenuous gases. Wavelength shifts produced by motion (Doppler effect) and cosmological expansion alter observed positions of features and are key diagnostics in astronomy; see practical notes at observational techniques.

Instrumentation and measurement

Spectroscopic setups include dispersive elements (prisms, gratings), interferometers, monochromators and detectors tuned to particular ranges. Calibration using known reference lines, correction for instrumental response and subtraction of background signals are routine. Resolution, sensitivity and signal-to-noise ratio determine the smallest features that can be reliably measured. Modern instruments couple optics with electronics and software for data acquisition, reduction and visualization; technical guides are available at instrumentation guides.

Major techniques

  • Absorption and emission (UV–visible): identify elements and electronic transitions; used in chemistry and astronomy. Further reading: UV–Vis resources.
  • Infrared (IR) and Raman: probe molecular vibrations and chemical bonds; widely used in organic analysis and materials science. Practical summaries at IR and Raman summaries.
  • Nuclear magnetic resonance (NMR): exploits nuclear spin transitions in magnetic fields to determine molecular structure and dynamics; see NMR overviews.
  • X‑ray spectroscopy (XPS, XAS): examines core electrons and local chemical environment, valuable in surface and solid‑state chemistry; technical notes at X‑ray technique overviews.
  • Laser and time‑resolved spectroscopy: enable high sensitivity and study of ultrafast processes; experimental approaches are summarized at laser spectroscopies.

Spectral shapes and physical effects

Line profiles reflect natural broadening, thermal (Doppler) broadening, collisional broadening and instrumental effects. Isotopic shifts, hyperfine structure and Zeeman splitting in magnetic fields give additional diagnostic detail. Quantitative analysis uses models of line formation and radiative transfer in optically thick or thin media. For applied examples and case studies consult application notes.

Applications

Spectroscopy is foundational across sciences: in chemistry for identifying functional groups and concentrations; in astrophysics for determining composition, temperatures and velocities of stars and galaxies; in environmental monitoring for measuring pollutants; in medicine for diagnostic imaging and metabolic studies; and in industry for quality control and process monitoring. Combined approaches such as hyperspectral imaging merge spatial and spectral information for remote sensing and material identification.

History, limitations and future directions

From early observations of spectral lines in sunlight and heated gases to modern lasers and detectors, spectroscopy has evolved with advances in optics and electronics. Limitations include overlapping features in complex mixtures, sensitivity thresholds and interpretation ambiguities; these are being addressed by higher resolution instruments, time‑resolved methods and computational analysis including machine learning. For deeper technical and historical context see additional resources at further reading.