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Fourier Transform Spectrometer

FT-IR spectrometers cannot be built as double-beam instruments. Unlike dispersive instruments, FT-IR spectrometers acquire single channel spectra of sample and reference and their ratio is calculated afterwards (Fig. 4.2). Sample and reference may automatically be replaced by a sample slider, or the IR beam may be switched between sample and reference by flip-mirrors. In the case of higher accumulation numbers, the instrument switches repeatedly between sample and reference scan. [Pg.50]

The heart of any FT-IR spectrometer is an interferometer. The Michelson interferometer consists basically of a beamsplitter and two flat mirrors. One of the mirrors is fixed in one interferometer arm, the other mirror is movable in the second interferometer arm. Most common MIR beamsplitters are made of KBr with a multilayer coating. The beamsplitter should have a reflectivity of 50 % and no absorption across its range of use. [Pg.50]

The functionality of a Michelson interferometer is based on a collimated IR beam. The latter is directed to the beamsplitter, which divides the beam into two parts of equal intensity (in the ideal case). The divided beams are reflected, by the fixed and the movable mirrors, back to the beamsplitter, where they recombine [Pg.50]

The mathematical procedure, which is employed to convert the IR interferogram (intensity versus time, also called time domain) to an IR spectrum (intensity versus frequency, also called frequency domain), is called Fourier transformation. Sample and reference interferograms are separately transformed. Afterwards, the ratio of both is automatically calculated and displayed as instrument-independent IR transmission spectrum (Fig. 4.3). [Pg.51]

Traditionally, FT-IR spectrometers used to be divided into two groups, routine and research spectrometers. Both have an affiliated PC for the data processing and handling. Routine spectrometers usually have a resolution limit of ca. 1 cm. Research spectrometers can achieve resolution as high as 0.001 cm . Sources, beamsplitters and detectors are exchangeable in research spectrometers, so one could use these spectrometers from 40000 down to 20 cm (from the UV to far-IR range). In some spectrometers different sources and detectors are installed permanently. They can be switched on or off by means of flip mirrors. Nowadays there are no designated limits between routine and research instraments. [Pg.52]

Fourier analysis permits any continuous curve, such as a complex spectmm of intensity peaks and valleys as a function of wavelength or frequency, to be expressed as a sum of sine or cosine waves varying with time. Conversely, if the data can be acquired as the equivalent sum of these sine and cosine waves, it can be Fourier transformed into the spectrum curve. This requires data acquisition in digital form, substantial computing power, and efficient software algorithms, all now readily available at the level of current generation personal computers. The computerized instmments employing this approach are called FT spectrometers—FTIR, FTNMR, and FTMS instruments, for example. [Pg.109]

It should be noted that FT spectrometers are single-beam instruments. The background must be collected separately from the sample spectrum. The ratio of the two spectra results in a background-corrected spectra, similar to that obtained from a double-beam instrument. While the sample and background spectra are not collected at exactly the same time, because the spectra can be collected rapidly and processed rapidly, background spectra can be collected regularly to avoid the problems encountered with a single-beam dispersive instrument. [Pg.110]

Quantitative Chemical Analysis, 2nd ed. Harper and Row New York, 1968. [Pg.111]

Kerber, J.D. Concepts, Instrumentation and Techniques in Atomic Absorption Spectrophotometry PerkinElmer, Inc. Norwalk, CT, 1993. [Pg.111]

B(u) is a frequency-dependent constant that accounts for instrumental variables such as detector response, the amount of light transmitted or reflected by the beam splitter, and the source intensity [Pg.106]

A commercial high-resolution FTS is depicted in Fig. 4.2. The output of the broadband source is focused on a circular aperture (entrance iris). As in the dispersive set-up, the optical beam is made parallel by a collimating mirror, and it intercepts a beam splitter at a non-normal incidence (usually 45 or 60°). One part of the beam is transmitted towards a fixed plane mirror while the other part towards a plane mirror, which can be translated continuously or in steps at a given distance (scan mirror). The beams reflected back by [Pg.94]

When discussing the methods of measurement of the refractive index, we had mentioned in Chap. 3 the recording of periodic interference fringes in the transmission spectra of dielectric plane parallel samples with a spectral bandwidth smaller than the fringe spacing. This situation is often encountered [Pg.97]

With a high-resolution FTS, it is in principle possible to get an estimation of the true line width by decreasing the spectral resolution 5i s until the observed FWHM stays constant. In the experiments performed with tunable lasers, this condition is generally met. There are also experimental situations where the profile of an absorption or PL spectral feature containing several unresolved individual lines cannot be further resolved by increasing the resolution because of the combination of the intrinsic FWHMs of the components and of their separations. It is possible to artificially decrease the FWHMs of the components in order to determine accurately their positions by a method known as self-deconvolution [19]. [Pg.98]

The uncertainty (or accuracy) on the measured position of an absorption line depends on the noise in the spectrum, but for negligible noise, as a rule of thumb, it can be considered to be ultimately limited to one tenth of the FWHM. [Pg.98]

Copyright 2013 Cengage Learning. AU Rights Reserved. May not be copied, scanned, or duplicated, in whole or in part. [Pg.24]

A third advantage of the Michelson interferometer, the ability to have a very precise wavenumber calibration by comparing wavenumbers of the planetary spectra [Pg.221]

The first to transform an interferogram of an astronomical object was Fellgett (1951, 1958, 1971). In Michelson s time such a transformation would have been time consuming, even for only a few hundred data points. Today, with modem computers and the Cooley-Tukey (1965) algorithm, whichForman (1966) introduced to the practitioners of FTS, transformation of a million data points is not uncommon. [Pg.222]

The Michelson two-beam interferometer records the autocovariance function of the observed radiation, the interferogram, as a function of optical path difference (delay) between both beams. The spectmm is obtained by Fourier analysis of the interferogram. The operation of a Michelson interferometer as an infrared spectrometer is discussed with the help of Fig. 5.8.1. The essential part of the instrument is the beamsplitter, which divides the incoming radiation into two beams of nearly equal intensity. After reflection from the stationary and the movable mirrors, the beams recombine at the beamsplitter. The phase difference between the beams is proportional to their optical path difference, including a phase shift due to the [Pg.222]

In the stepping mode, the signal is integrated at each rest position for a certain time, the dwell time. After that, the Michelson mirror advances to the following position and the next point is recorded. As in the case of an a.c. radiometer an external chopper may be used to modulate the incoming radiation. The stepping technique has been perfected by J. and P. Coimes. [Pg.223]

In the continuous mode the Michelson mirror advances at a constant speed and the signal is sampled at small, equal intervals. At one time the misconception existed that this mode is less efficient than the discrete step mode because the time spent in taking the sample is small in comparison with the time between samples, but [Pg.223]


It is interesting to note that a similar specttum of the 0-0 band of the a-X system, leading to the same value of the absorption intensity, has been obtained using a Fourier transform spectrometer (see Section 3.3.3.2) but with an absorption path, using a multiple reflection cell, of 129 m and half the pressure of gas. [Pg.385]

Fig. 1. Schematic of the optical layout of a Fourier-transform spectrometer. Fig. 1. Schematic of the optical layout of a Fourier-transform spectrometer.
The infrared ellipsometer is a combination of a Fourier-transform spectrometer (FTS) with a photometric ellipsometer. One of the two polarizers (the analyzer) is moved step by step in four or more azimuths, because the spectrum must be constant during the scan of the FTS. From these spectra, the tanf and cosd spectra are calculated. In this instance only A is determined in the range 0-180°, with severely reduced accuracy in the neighborhood of 0° and 180°. This problem can be overcome by using a retarder (compensator) with a phase shift of approximately 90° for a second measurement -cosd and sind are thereby measured independently with the full A information [4.315]. [Pg.269]

Fluorescence emission spectra were recorded with Perkin-Elmer LS Luminescence Spectrometer, whereas IR (transmission and ATR spectra) with Perkin-Elmer 1710 IR Fourier Transform Spectrometer. [Pg.188]

Figure 3.4 shows (i) a line spectrum (one-dimensional dispersive spec-trographic record), (ii) a spectrometric record, (iii) an interferogram obtained by a Fourier transform spectrometer, and (iv, v) two- and three-dimensional double dispersive spectra recorded e.g. by Echelle spectrometers. In principle, all forms may be obtained by OES. [Pg.74]

Free Induction Decay (FID) Interference pattern of decaying cosine waves collected by Fourier Transform spectrometers, stored digitally prior to Fourier Transformation. [Pg.207]

In the mid-IR, routine infrared spectroscopy nowadays almost exclusively uses Fourier-transform (FT) spectrometers. This principle is a standard method in modem analytical chemistry45. Although some efforts have been made to design ultra-compact FT-IR spectrometers for use under real-world conditions, standard systems are still too bulky for many applications. A new approach is the use of micro-fabrication techniques. As an example for this technology, a miniature single-pass Fourier transform spectrometer integrated on a 10 x 5 cm optical bench has been demonstrated to be feasible. Based upon a classical Michelson interferometer design, all... [Pg.142]

Fourier transform spectrometer or double-beam spectrophotometer incorporating prism or grating monochromator, thermal or photon detector, alkali halide cells. [Pg.378]

Fourier transform nuclear magnetic resonance (nmr), 21 278 Fourier transform spectrometers, 19 671 23 137... [Pg.379]

The IR spectra of this new resist films on silicon substrates were measured with a Shimadzu FTIR-4000 Fourier transform spectrometer. The UV spectra of 4,4 -diazidodiphenyl methane in a quartz cell and the films of poly(styrene-co-maleic acid half ester) and the new resist on quartz substrates were measured with a Shimadzu UV-265FS double-beam spectrometer. [Pg.270]

When the development of dedicated i rared spectrometers for surface studies started some ten years ago, some of them were designed as more or less complete ellipsometers, which in principle are insensitive to the ambient gas phase molecules. Fedyk et al. detected CO adsorbed on an evaporated Cu film at 4 torr, while Golden et al. reported work at 100 torr. More recently, Burrows et used a Fourier transform spectrometer and the polarizer approach above to study the reaction-rate oscillations in the oxidation of CO on a large Pt polycrystalline foil at pressures up to one atmosphere. With this rapid FTIR spectrometer they obtained a time resolution of 0.6 s at a sensitivity of 5% of a full CO monolayer. [Pg.39]

M. Kraft, Compact MEMS high-speed Fourier transform spectrometer, 4th International Conference on Vibrational Spectroscopy, Corfu (2007). [Pg.154]

General Procedures - All solvents were evaporated under reduced pressure at 40 C. Infrared (IR) spectra were recorded on a Beckman Aculab spectrometer and " H NMR spectra were recorded at 300 Mhz (Nicolet Fourier Transform Spectrometer). [Pg.149]

NMR and NMR were obtained from a 300 MHz Brucker fourier transform spectrometer. The solutions (20% w/w) were prepared by dissolving the chlorinated rubber (CR) in CDCI3 and QDg for the NMR spectra analysis with tetramethylsilane as an internal standard. [Pg.232]

The proton noise-decoupled 13c-nmr spectra were obtained on a Bruker WH-90 Fourier transform spectrometer operating at 22.63 MHz. The other spectrometer systems used were a Bruker Model HFX-90 and a Varian XL-100. Tetramethylsilane (TMS) was used as internal reference, and all chemical shifts are reported downfield from TMS. Field-frequency stabilization was maintained by deuterium lock on external or internal perdeuterated nitromethane. Quantitative spectral intensities were obtained by gated decoupling and a pulse delay of 10 seconds. Accumulation of 1000 pulses with phase alternating pulse sequence was generally used. For "relative" spectral intensities no pulse delay was used, and accumulation of 200 pulses was found to give adequate signal-to-noise ratios for quantitative data collection. [Pg.237]

Fig. 26 Fourier transform spectrum of v2 of ammonia. Trace (a) is a section of the infrared absorption spectrum of ammonia recorded on a Digilab Fourier transform spectrometer at a nominal resolution of 0.125 cm-1. In this section of the spectrum near 848 cm-1 the sidelobes of the sine response function partially cancel, but the spectrum exhibits negative absorption and some sidelobes. Trace (b) is the same section of the ammonia spectrum using triangular apodiza-tion to produce a sine-squared transfer function. Trace (c) is the deconvolution of the sine-squared data using a Jansson-type weight constraint. Fig. 26 Fourier transform spectrum of v2 of ammonia. Trace (a) is a section of the infrared absorption spectrum of ammonia recorded on a Digilab Fourier transform spectrometer at a nominal resolution of 0.125 cm-1. In this section of the spectrum near 848 cm-1 the sidelobes of the sine response function partially cancel, but the spectrum exhibits negative absorption and some sidelobes. Trace (b) is the same section of the ammonia spectrum using triangular apodiza-tion to produce a sine-squared transfer function. Trace (c) is the deconvolution of the sine-squared data using a Jansson-type weight constraint.
Infrared analyses are conducted on dispersive (scanning) and Fourier transform spectrometers. Non-dispersive industrial infrared analysers are also available. These are used to conduct specialised analyses on predetermined compounds (e.g. gases) and also for process control allowing continuous analysis on production lines. The use of Fourier transform has significantly enhanced the possibilities of conventional infrared by allowing spectral treatment and analysis of microsamples (infrared microanalysis). Although the near infrared does not contain any specific absorption that yields structural information on the compound studied, it is an important method for quantitative applications. One of the key factors in its present use is the sensitivity of the detectors. Use of the far infrared is still confined to the research laboratory. [Pg.161]

Commercial Fourier transform spectrometers operating at moderate resolution (1cm-1) require fractions of seconds to complete a scan of the interferometric mirror (scans may only take tens of milliseconds if only low spectral resolution is required). A new strategy must now be used to study the... [Pg.3]


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