Fourier transform infrared (FTIR) spectroscopy is a widely used analytical technique to identify and quantify samples based on their vibrational spectra; however, obtaining accurate and reproducible data is heavily reliant on the sampling technique used and the sample preparation. The selection of a sampling technique depends on the physical state and chemical properties of the sample while the sample preparation will depend on the choice of sampling technique. Some common sampling techniques for FTIR spectroscopy include transmission, Attenuated Total Reflectance (ATR), diffuse reflectance, and specular reflectance. Transmission is the most straightforward sampling technique for solid, liquid, and gas samples while ATR has become the primary sampling technique for solid and liquid samples due to the lack of sample preparation. Diffuse reflectance is used for powders and highly scattering samples, while specular reflectance is used for highly reflective samples.

Attenuated Total Reflectance (ATR)

Attenuated Total Reflectance (ATR) has become the primary sampling method for FTIR spectroscopy. The major advantage of ATR is the lack of sample preparation for liquid and solid samples. When light reflects off certain materials (diamond, ZnSe, etc.) at a critical angle, the light undergoes total internal reflectance with a small amount of light being absorbed into the sample in contact with the crystal surface (Figure 1). The penetration depth is dependent on the refractive index of both the sample (generally ~1.5 μm) and the crystal itself. Since the refractive index is dependent on wavelength, spectra taken with ATR have slightly different intensity ratios across the spectrum and may need to be corrected to compare to transmission spectra.

Lightpath for an ATR experiment
Figure 1. Lightpath for an ATR experiment

The three most common crystals are diamond, zinc selenide, and germanium, each having advantages and disadvantages. Diamond crystals are rugged, have a penetration depth of 1.5 μm, and a low wavenumber cutoff (200 cm-1), but have poor throughput in the 2,200 cm-1 region. ZnSe has exceptional throughput but a high wavenumber cutoff (650 cm-1). Germanium has a very low penetration depth (0.8 μm) and is useful for highly absorbing substances.

Transmission Techniques

Transmission is the most straightforward technique but requires the most sample preparation. In transmission FTIR spectroscopy, incident light, from an infrared source, passes through a sample and the transmitted light is measured by a detector on the other side of the sample. The transmission spectrum is produced by ratioing the intensity of the incident light (Pin) to the intensity of the transmitted light (Pout): T = Pout / Pin (Figure 2). There are a variety of sampling techniques that can be used to obtain transmission spectra depending on the state of matter of the sample. For solids, the sample can be pressed into a KBr pellet, sandwiched between KBr salt plates, or mixed with a mineral oil to create a mull. For liquids, the sample can be injected into a liquid cell, sandwiched between KBr salt plates, or applied to an IR transparent card. For gases, the sample can be introduced into a gas cell.

Figure 2. Transmission of solids, liquids, and gasses
Figure 2. Transmission of solids, liquids, and gasses

KBr Pellet

The KBr pellet technique is used to measure the transmission of powdered solids. A small amount of powdered sample is mixed with a powdered alkali halide (most commonly potassium bromide, KBr), pressed into a pellet using a pellet die, and placed into a pellet holder. Powdered alkali halides are transparent in the mid-IR (4,000 – 400 cm-1) region and form pellets when subjected to high pressure. A blank KBr pellet, containing no sample, is required to obtain a background spectrum to correct for light scattering losses in the pellet and moisture absorbed by KBr. The main disadvantage of this technique is that KBr is hygroscopic and absorbs moisture from the atmosphere. As a result, this technique is not suitable for measuring samples with absorption bands in the same regions as water. Samples that contain chlorides and hydrochlorides are generally prepared using potassium chloride, KCl, since a halogen exchange reaction occurs between Br and Cl when using KBr.

KBr Plate

The KBr plate technique is used to measure the transmission of powdered solids when simple sample preparation is required, or for measuring highly hygroscopic samples. A powdered sample is sandwiched between two infrared transparent window plates (NaCl, KCl, KBr, KRS-5 CsI, CaF2, Quartz, Polyethylene, etc.) and placed into a demountable cell. One of the most common window plate materials is KBr, which is extremely fragile and hygroscopic. KBr plates should be handled with care to prevent the plate from becoming scratched or chipped, thoroughly cleaned after each use, and properly stored in a desiccator to prevent the plate from absorbing moisture from the atmosphere and becoming cloudy. It should be noted that samples that contain large particles are susceptible to scattering of light, so the measured absorbance may be lower than the true value.

Demountable Cell

Samples that can be formed into thin films with a thickness of 10 μm or less can also be measured. There are various thinning methods that can be used for sample preparation, such as stretching, cutting, and hot pressing. If the sample is soluble in a solvent, the solution can be applied to a KBr plate and evaporating the solvent to form a thin film.

Mineral Oil Mull

Mineral oil mulls are used to measure the transmission of solids that are not suitable for KBr methods, such as samples that absorb moisture during sample preparation (e.g., sugars) and samples that do not dissolve in solvents (e.g., inorganic substances). A powder sample is mixed with a non-volatile mineral oil (most commonly Nujol, a brand of liquid paraffin) to form a paste, which can then be applied to an infrared transparent window plate and placed in a demountable cell to be measured. This technique is not suitable for evaluating bands associated with -CH groups (3,000 – 2,800 cm-1, 1,500 – 1,300 cm-1) because absorption by the liquid paraffin occurs in these regions.

Liquid Cell

Liquid cells are used to measure the transmission of liquids. The sample is sandwiched between two infrared transparent windows (NaCl, KCl, KBr, KRS-5 CsI, CaF2, Quartz, ZnSe, etc.) in either a demountable or sealed liquid cell.

A demountable liquid cell can be used to measure the transmission of non-volatile liquids or a solution of a solid dissolved in a non-volatile solvent. Depending on the peak intensity, the optical pathlength of the demountable liquid cell can be adjusted by adding a spacer. For samples containing water, a KBr window cannot be used. A sealed liquid cell or micro sealed liquid cell can be used to measure the transmission of a volatile liquid or a solution of a solid dissolved in a volatile solvent. Before performing the measurements, it is important to ensure that the solvent itself does not give rise to absorption bands that interfere with those of the target components.

An IR card can also be used to measure the transmission of a solid dissolved in a volatile solvent. The solution is placed on an infrared transparent substrate (NaCl, KBr, KCl, PTFE, Polyethylene, etc.) and allowed to evaporate to form a thin film.

Gas Cell

Gas cells are used to measure the transmission of gases and are often heated to avoid condensation inside the cell. Infrared transparent windows (BaF2, CaF2, NaCl, ZnSe, KBr, SiO2, etc.) seal the gas cell and allow the infrared beam to pass into the gas cell, through the sample, and onto the detector. The pathlength of the gas cell should be adjusted based on the concentration of the gas; a low-concentration gas will require a longer pathlength than a high-concentration gas. The amount of water vapor and carbon dioxide in a gas can be determined if the system is under a full vacuum or a N2 gas purge is performed on the system prior to measurement. One disadvantage of this technique is that gases usually produce sharp absorption peaks, requiring high-resolution instruments to achieve high-quality measurements.

Demountable/Small-Capacity Gas Cell
Demountable/Small-Capacity Gas Cell

Reflectance Techniques

Specular Reflectance

Specular reflectance is useful for analyzing smooth, flat surfaces, such as mirrors. Specular reflection is the reflection of light from a surface where the angle of reflection is equal to the angle of incidence (Figure 5). This technique requires little or no sample preparation.

Specular Reflectance Graphic

RF-81S 10 10° Specular Reflectance Accessory
RF-81S 10 10°
Specular Reflectance Accessory

Sometimes specular reflectance spectra include both the imaginary and real components of the light, giving rise to derivative peaks or other distortions. These distortions make it difficult to search spectral libraries, which are usually collected in transmission. A Kramers-Kronig correction can mathematically eliminate the spectral distortions resulting from specular reflectance measurements and creates a spectrum that looks as if it were collected in transmission (Figure 3).

Figure 3. Kramers–Kronig Correction – Poly(Mthyl Methacrylate) PMMA

Diffuse Reflectance Infrared Fourier Transform Spectroscopy (DRIFTS)

Diffuse Reflectance Infrared Fourier Transform Spectroscopy (DRIFTS) is useful for analyzing rough surface solids and powders. Diffuse reflectance is the reflection of light from a surface where the incident light is scattered at many angles. Incident light is absorbed by each particle in the sample and re-emitted by the combined process of reflection, refraction, and diffraction. The re-emitted light can then be absorbed and re-emitted by other particles in the sample.

Diffuse Reflectance Example in Infrared Fourier Transform Spectroscopy

Samples can be measured as a solid powder (neat), a powder mixed with KBr, or abraded on special abrasive paper. If a sample is too absorbent to be measured neat, it can be mixed with an infrared transparent material, such KBr or KCl, to ensure a deeper penetration of the incident light into the sample, increasing the contribution of the diffuse scattered component and minimizing the contribution of the specular reflection component in the spectrum. The sample should be finely ground and loosely but evenly packed in the sample cup to further increase the penetration depth. Quantitative analysis is possible, but often quite difficult since the particle size, packing, and dilution of the sample must be carefully controlled. A background spectrum must first be collected of the infrared transparent material. To properly compare relative peak intensities from a transmission spectrum, a Kubelka–Munk correction is required (Figure 4).

Figure 4. Kubelka–Munk Correction – Caffeine
Figure 4. Kubelka–Munk Correction – Caffeine

Infrared Reflection–Absorption Spectroscopy (IRRAS) / Reflection–Absorption Infrared Spectroscopy (RAIRS)

Infrared Reflection–Absorption Spectroscopy (IRRAS) or Reflection–Absorption Infrared Spectroscopy (RAIRS) is useful for analyzing thin films on metal substrates with high sensitivity using p-polarized light parallel to the plane of incidence. The electric vectors in the incident and reflected p-polarized light interfere to mutually strengthen and form an electric field of stationary vibration. The interaction of this electric field with a thin film on the metal surface causes an absorption that is stronger than simple transmission measurement, allowing film thickness measurements at the angstrom (Å) level.

Infrared Reflection–Absorption Spectroscopy (IRRAS) /Reflection–Absorption Infrared Spectroscopy (RAIRS)
Infrared Reflection–Absorption Spectroscopy (IRRAS) /
Reflection–Absorption Infrared Spectroscopy (RAIRS)

Despite this, absorption peaks obtained by IRRAS are usually very small, and often require a long accumulation time. In addition, both a reference and a sample substrate must be measured. For these reasons, the spectra can be significantly affected by the absorption of atmospheric H2O and CO2. This technique does not require a KK correction like specular reflectance.

Polarization Modulation–Infrared Reflection–Absorption Spectroscopy (PM–IRRAS)

Polarization Modulation–Infrared Reflection–Absorption Spectroscopy (PM–IRRAS) obtains a measurement of thin films with greater sensitivity than ordinary IRRAS, allowing the process monitoring of the generation of thin films with thicknesses of nanometers or greater on metal substrates in a vacuum chamber.

PM-IRRAS measures the intensity difference in s- and p-polarized light (ΔI = Ip – Is), vertical and parallel to the plane of incidence, respectively, using a Photoelastic Modulator (PEM). The principle of operation of a PEM is based on the photoelastic effect, in which a mechanically stressed optical element exhibits birefringence proportional to the resulting strain. In a PEM, a voltage is applied to the crystal based on the principle of an inverse piezoelectric effect so that the transparent optical element will be distorted as a result. The distortion produces a birefringence of the crystal, and the polarization direction of the light can be modulated by applying a suitable voltage for the wavelength of light used for the measurement.

As s-polarized light does not generate an electric field of stationary vibration, the absorption is much smaller than that of p-polarized light. In PM-IRRAS, the sum of s- and p- polarization signals (Σ I = Ip + Is) is used as a reference, eliminating the requirement to measure a reference substrate. As a result, the effect due to the absorption of atmospheric H2O and CO2 can be greatly decreased. In addition, the results are free from the effect of differences between substrates and the overall measurement time can be shortened. PM-IRRAS measurement allows higher sensitivity by detecting small ΔI signals using a direct lock-in detection by adopting dual modulation spectroscopy of the FTIR interferometer and PEM.

Comparison of IRRAS and PM–IRRAS

Fig. 2 shows the results of a Polymethyl Methacrylate (PMAA) thin film on an Al mirror measured by IRRAS and PM-IRRAS with all other conditions remaining the same. The S/N of spectra obtained using PM-IRRAS are several times better than IRRAS.

Fig. 2. Comparison between IRRAS spectrum and PM-IRRAS spectrum (normalized, offset plotting)

FTIR Microscopy

FTIR spectroscopy is also used in microscopy for microanalysis of the same types of materials that are studied using macro-IR measurement. An FTIR Microscope uses reflection optics to observe and focus infrared light onto samples. ATR, transmission, reflection, and grazing angle objectives are used to transmit and collect infrared energy to a small spot (5 – 50 μm) on the sample of interest. Multiple measurements in selected spots, lines or 3D grids can be used to generate a chemical map. This mapping may be enhanced using imaging analysis, chemometrics, and library searches to automatically identify components and their distribution in a sample.