
Basic Chemometric Techniques in Atomic Spectroscopy: 10
Author(s): Jose Andrade-Garda
- Publisher: Royal Society of Chemistry
- Publication Date: 26 May 2009
- Language: English
- Print length: 300 pages
- ISBN-10: 9780854041596
- ISBN-13: 9780854041596
Book Description
Editorial Reviews
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Basic Chemometric Techniques in Atomic Spectroscopy
By J. M. Andrade-Garda
The Royal Society of Chemistry
Copyright © 2009 Jose Manuel Andrade-Garda
All rights reserved.
ISBN: 978-0-85404-159-6
Contents
Chapter 1 A General Overview of Atomic Spectrometric Techniques Alfredo Sanz-Medel, Rosario Pereiro and José Manuel Costa-Fernández,
Chapter 2 Implementing A Robust Methodology: Experimental Design and Optimization Xavier Tomás Morer, Lucinio González-Sabaté, Laura Fernández-Ruano and María Paz Gómez-Carracedo,
Chapter 3 Ordinary Multiple Linear Regression and Principal Components Regression Joan Ferré-Baldrich and Ricard Boqué-Martí,
Chapter 4 Partial Least-Squares Regression Jose Manuel Andrade-Garda, Ricard Boqué-Martí, Joan Ferré-Baldrich and Alatzne Carlosena-Zubieta,
Chapter 5 Multivariate Regression using Artificial Neural Networks Jose Manuel Andrade-Garda, Alatzne Carlosena-Zubieta, María Paz Gómez-Carracedo and Marcos Gestal-Pose,
CHAPTER 1
A General Overview of Atomic Spectrometric Techniques
ALFREDO SANZ-MEDEL, ROSARIO PEREIRO AND JOSÉ MANUEL COSTA-FERNÁNDEZ
Department of Physical and Analytical Chemistry, University of Oviedo, Oviedo, Spain
1.1 Introduction: Basis of Analytical Atomic Spectrometric Techniques
Analytical atomic spectrometry comprises a considerable number of techniques based on distinct principles, with different performance characteristics and hence with varied application scopes, but in all cases providing elemental chemical information about the composition of samples. Figure 1.1 shows that these techniques can be classified into three main groups according to the type of particle detected: optical spectrometry, where the intensity of either non-absorbed photons (absorption) or emitted photons (emission and fluorescence) is detected as a function of photon energy (in most cases, plotted against wave-length); mass spectrometry (MS), where the number of atomic ions is determined as a function of their mass-to-charge ratio; and electron spectroscopy, where the number of electrons ejected from a given sample is measured according to their kinetic energy, which is directly related to the bonding energy of the corresponding electron in a given atom.
X-ray photoelectron spectroscopy (XPS) and Auger electron spectroscopy (AES) are the two main techniques based on electron spectroscopy. In XPS, a source of photons in the X-ray energy range is used to irradiate the sample. Superficial atoms emit electrons (called photoelectrons) after the direct transfer of energy from the photon to a core-level electron (see Figure 1.2a). Photoelectrons are subsequently separated according to their kinetic energy and counted. The kinetic energy will depend on the energy of the original X-ray photons (the irradiating photon source should be monochromatic) and also on the atomic and, in some cases, the molecular environment from which they come. This, in turn, provides important information about oxidation states and chemical bonds as the stronger the binding to the atom, the lower is the photoelectron kinetic energy.
In an Auger process, the kinetic energy of the emitted electron does not depend on the energy of the excitation source. AES consists of a two-step process: first, the sample is irradiated with an electron beam (or, less commonly, with X-rays), which expels an inner electron (e-1). In a second step, the relaxation of the excited ion takes place through the fall of a more external electron (e-2) to fill the ‘hole’, and then a third electron (e-Auger) uses the energy released in that movement to exit the atom (Figure 1.2b). XPS and AES are considered powerful techniques for surface analysis, with good depth and lateral resolution. However, due to their narrow range of applications in qualitative studies and the scarcity of quantitative analyses, they will not be considered further in this chapter.
The aim of this chapter is, therefore, to introduce briefly the most common quantitative atomic techniques based on both optical and mass spectrometric detection. The main emphasis will be given to conceptual explanations in order to stress the advantages and disadvantages of each technique, the increase in the complexity of the data they generate and how this can be addressed. References to chemometric tools presented in the following chapters will be given.
For these techniques, a dissolved sample is usually employed in the analysis to form a liquid spray which is delivered to an atomiser (e.g. a flame or electrically generated plasma). Concerning optical spectrometry, techniques based on photon absorption, photon emission and fluorescence will be described (Section 1.2), while for mass spectrometry (MS) particular attention will be paid to the use of an inductively coupled plasma (ICP) as the atomisation/ionisation source (Section 1.3). The use of on-line coupled systems to the above liquid analysis techniques such as flow injection manifolds and chromatographic systems will be dealt with in Section 1.4 because they have become commonplace in most laboratories, opening up new opportunities for sample handling and pretreatment and also to obtain element-specific molecular information.
Finally, direct solid analysis by optical and mass spectrometry will be presented in Section 1.5. This alternative is becoming more appealing nowadays and implemented in laboratories because of the many advantages brought about by eliminating the need to dissolve the sample. Techniques based on the use of atomiser/excitation/ionisation sources such as sparks, lasers and glow discharges will be briefly described in that section.
1.2 Atomic Optical Spectrometry
Routine inorganic elemental analysis is carried out nowadays mainly by atomic spectrometric techniques based on the measurement of the energy of photons. The most frequently used photons for analytical atomic spectrometry extend from the ultraviolet (UV: 190–390 nm) to the visible (Vis: 390–750 nm) regions. Here the analyte must be in the form of atoms in the gas phase so that the photons interact easily with valence electrons. It is worth noting that techniques based on the measurement of X-rays emitted after excitation of the sample with X-rays (i.e. X-ray fluorescence, XRF) or with energetic electrons (electron-probe X-ray micro-analysis, EPXMA) yield elemental information directly from solid samples, but they will not be explained here; instead, they will be briefly treated in Section 1.5.
The measurement of analytes in the form of gaseous atoms provides atomic spectra. Such spectra are simpler to interpret than molecular spectra (since atoms cannot rotate or vibrate as molecules do, only electronic transitions can take place when energy is absorbed). Atomic spectra consist of very narrow peaks (e.g. a few picometres bandwidth) providing two types of crucial analytical information: the observed wavelength (or frequency or photon energy), which allows for qualitative analysis, and the measurement of the peak height or area at a given frequency, which provides quantitative information about the particular element sought. The relative simplicity of such atomic spectra and the fairly straightforward qualitative and quantitative information have led to the enormous practical importance of atomic optical spectrometry for inorganic elemental analysis. However, it should be stressed again that to obtain such spectra the analytes must be converted into atoms which will absorb or emit photons of UV–Vis radiation and so an ‘atomiser’, for example a dynamic medium of high temperature where molecules containing the analyte are broken down into individual gaseous atoms, is needed.
1.2.1 Classification of Techniques: Absorption, Emission and Fluorescence
The interaction processes between UV–Vis photons and the outer electrons of the atoms of the analytes can be understood using quantum mechanics theory. In the thermodynamic equilibrium between matter and interacting electromagnetic radiation, according to the radiation laws postulated by Einstein, three basic processes between two stable energy levels 1 and 2 are possible. These processes, which can be defined by their corresponding transition probabilities, are summarised in Figure 1.3.
Spontaneous emission of photons. This process refers to a spontaneous transition of the electron from the excited state 2 to the lower energy state 1 with emission of a photon of frequency v12 = (E2 – E1)/h. This process constitutes the photophysical basis of atomic emission spectrometry, which will be termed here optical emission spectrometry in order to use the acronym OES instead of AES because the latter acronym can be confused with that for Auger electron spectroscopy.
Stimulated absorption of photons. In this case, the electronic transition takes place from state 1 to state 2 in response to the action of an external radiation of the appropriate frequency. Atomic absorption spectrometry (AAS) is based on this process. On the other hand, atomic fluorescence spectrometry (AFS) corresponds to the sequential combination of a stimulated absorption followed by spontaneous emission.
Stimulated emission of photons. This process consists of electronic transitions from the excited energy level to the lower one stimulated by an external radiation of the appropriate frequency (E2 – E1)/h and constitutes the basis of the laser (light amplification by stimulated emission of radiation) phenomenon.
Atomic lines can arise from electronic transitions in neutral atoms or in atomic ions (in general, atomic lines for a given element M are denoted M I, whereas their ionic counterparts are denoted M II). The transitions of outer electrons of an atom may be represented as vertical lines on an ‘energy level’ diagram, where each energy level of the outer electron possesses a given energy and is represented by a horizontal line. For example, Figure 1.4 shows the diagram for the neutral sodium atom (the wavelengths corresponding to the transitions in the diagram are expressed in ångströms, Å). The energy scale is linear in electronvolt (eV) units, assigning a value of zero to the 3s orbital. The scale extends up to about 5.2 eV, which corresponds to the energy necessary to extract the 3s electron and so to produce a sodium ion. All electronic transitions ending on the same energy level are usually called ‘series’, the most likely ones being those ending in the lowest possible energy level (the ground state) of the electron in the atom.
The light coming from such transitions is separated according to its frequency (or its wavelength, λ) and the intensity observed for each frequency measured electronically (e.g. with a photomultiplier tube). Thus, if the observed intensity of the emitted light is plotted against the frequency (or wavelength) of the corresponding transition (line), an ‘atomic emission’ spectrum is obtained (see Figure 1.1). Similarly, an ‘atomic fluorescence’ spectrum would be the plot of the measured intensity (coming from atoms excited by appropriate electro-magnetic radiation) as a function of the frequency of the emitted radiation. Finally, if stimulated absorption of light in response to an electronic transition between a lower and a higher energy level is measured, a plot of ‘percent absorption versus frequency of the light’ can be drawn; such a plot represents an ‘atomic absorption’ spectrum.
The atomic lines in the spectrum appear as vertical lines or ‘peaks’ due to the nature of the transition involved. That is, in molecules an electronic transition is usually accompanied by simultaneous changes in the molecule vibrational and rotational energy levels; sometimes all the three energy types may change simultaneously in an electronic transition in a molecule. The many transition possibilities allowed in this way and the solvent effect derived from the aggregation state of the sample (the ‘excited’ sample is in liquid form) determines that in UV–Vis molecular absorption (or emission) the corresponding ‘peaks’ in the spectrum are widely broadened. Typically, the half-bandwidth of an absorption ‘band’ in such molecular UV–Vis spectra is around 40 nm (or 400 Å), whereas in atomic ‘lines’ the half-bandwidth observed, as a result of pure electronic transitions, is a few hundredths of an ångström (typically 0.03–0.05 Å).
Thus, spectral interferences in atomic spectroscopy are less likely than in molecular spectroscopy analysis. In any case, even the atomic ‘lines’ are not completely ‘monochromatic’ (i.e. only one wavelength per transition). In fact, there are several phenomena which also bring about a certain ‘broadening’. Therefore, any atomic line shows a ‘profile’ (distribution of intensities) as a function of wavelength (or frequency). The analytical selectivity is conditioned by the overall broadening of the lines (particularly the form of the wings of such atomic lines).
The selection of the most appropriate atomic line among all possible transitions for qualitative and quantitative purposes is critical. For most elements, the ‘resonance’ atomic lines (i.e. when the lowest energy level in the corresponding transition is the fundamental or ‘ground state’ level, E0 = 0) are the most sensitive ones in flames and they are used in the majority of flame methods. However, with plasma sources (commonly used in combination with OES), the choice is more difficult because several emission lines from neutral atoms or atomic ions of the same element may appear useful. Often, the expected concentration range will dictate whether to use a neutral atom resonance line, an ion line or a line arising from transitions between excited atomic states. Resonance lines are useful for trace constituents, but they are susceptible to self-absorption of emitted radiation at high concentrations (this effect is due to an excess of analyte atoms in the ground-state level). Lines of lower relative intensities are often used for minor and major constituents. Moreover, the abundance of nearby, potentially interfering lines from other elements, has to be assessed carefully.
1.2.1.1 Atomic Absorption Spectrometry. Principles of Quantitative Analysis
For quantitative purposes in AAS, a magnitude called transmittance (T) which relates, for a given wavelength, the intensity (measured by the detector) of the light source (I0) and the intensity not absorbed which has passed through the atomiser or transmitted light (I) is used:
T = I/I0 (1.1)
The amount of light absorbed is a function of the so-called absorption coefficient (k’) and of the optical pathlength in the atomiser cell (b); k’ depends on the frequency of the selected analytical line and on the concentration of the analyte absorbing atoms. The general absorbance law (Lambert–Beer–Bouguer law) relates transmittance (and so measured intensities I and I0) to k’ and b through the following equation:
T = e-k’b (1.2)
The parameter used in the analytical calibrations by AAS is absorbance (A), which is linearly related to k’ (that is, at a given λ with the atomic concentration of the analyte in the atomiser) and with the length of the optical path:
A = -log T = log 1/T = k’b log e = 0.43k’b (1.3)
For a given set of experimental conditions in an absorption experiment, we obtain
A = constant × b × N0 (1.4)
N0 being the analyte atom density (number of atoms per unit volume) in the ground state in the atomiser. The relationship between the atom concentration per unit volume (N [congruent to] N0) and the concentration of the analyte in the sample, C, is linear under fixed working conditions for a given line of the analyte. Therefore, we can establish a linear relationship between absorbance and C:
A = KbC (1.5)
1.2.1.2 Optical Emission Spectrometry. Principles of Quantitative Analysis
Optical emission spectrometry is one of the oldest physical methods of analysis enabling multielement determinations. In this process, free atoms which are generated by thermal dissociation of the sample material are excited or ionised and excited additionally (several collisions or other processes may be responsible for delivering the required energy). The higher the temperature, the higher is the percentage of excited analyte species (at least, in general) and the higher the emission intensity. The Boltzmann equation relates the temperature (T) with the number of atoms in an energy state E0 and an excited state Eq, provided that the source is in a so-called thermal equilibrium, as
[MATHEMATICAL EXPRESSION NOT REPRODUCIBLE IN ASCII] (1.6)
where n0 is the number of atoms in the energy level E0, n* the number of atoms in an energy state Eq, kB the Boltzmann’s constant, gq and g0 the statistical weights for each energy state (Eq and E0) and T the temperature in Kelvin.
The flames commonly used as atomisers have temperatures in the range 2000–3000 K allowing for the analysis of elements such as Na, K and Cs by OES. The flame temperatures are not high enough to excite many other elements, so other atomisers such as spectroscopic plasmas have to be used.
(Continues…)Excerpted from Basic Chemometric Techniques in Atomic Spectroscopy by J. M. Andrade-Garda. Copyright © 2009 Jose Manuel Andrade-Garda. Excerpted by permission of The Royal Society of Chemistry.
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