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Electroanalytical methods
Electroanalytical methods
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Electroanalytical methods are a class of techniques in analytical chemistry which study an analyte by measuring the potential (volts) and/or current (amperes) in an electrochemical cell containing the analyte.[1][2][3][4] These methods can be broken down into several categories depending on which aspects of the cell are controlled and which are measured. The three main categories are potentiometry (the difference in electrode potentials is measured), amperometry (electric current is the analytical signal), coulometry (charge passed during a certain time is recorded).

Potentiometry

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Potentiometry passively measures the potential of a solution between two electrodes, affecting the solution very little in the process. One electrode is called the reference electrode and has a constant potential, while the other one is an indicator electrode whose potential changes with the sample's composition. Therefore, the difference in potential between the two electrodes gives an assessment of the sample's composition. In fact, since the potentiometric measurement is a non-destructive measurement, assuming that the electrode is in equilibrium with the solution, we are measuring the solution's potential. Potentiometry usually uses indicator electrodes made selectively sensitive to the ion of interest, such as fluoride in fluoride selective electrodes, so that the potential solely depends on the activity of this ion of interest. The time that takes the electrode to establish equilibrium with the solution will affect the sensitivity or accuracy of the measurement. In aquatic environments, platinum is often used due to its high electron transfer kinetics,[5] although an electrode made from several metals can be used in order to enhance the electron transfer kinetics.[6] The most common potentiometric electrode is by far the glass-membrane electrode used in a pH meter.

A variant of potentiometry is chronopotentiometry which consists in using a constant current and measurement of potential as a function of time. It has been initiated by Weber.[7]

Amperometry

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Amperometry indicates the whole of electrochemical techniques in which a current is measured as a function of an independent variable that is, typically, time (in a chronoamperometry) or electrode potential (in a voltammetry). Chronoamperometry is the technique in which the current is measured, at a fixed potential, at different times since the start of polarisation. Chronoamperometry is typically carried out in unstirred solution and at the fixed electrode, i.e., under experimental conditions avoiding convection as the mass transfer to the electrode. On the other hand, voltammetry is a subclass of amperometry, in which the current is measured by varying the potential applied to the electrode. According to the waveform that describes the way how the potential is varied as a function of time, the different voltammetric techniques are defined.

Chronoamperometry

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In a chronoamperometry, a sudden step in potential is applied at the working electrode and the current is measured as a function of time.[8] Since this is not an exhaustive method, microelectrodes are used and the amount of time used to perform the experiments is usually very short, typically 20 ms to 1 s, as to not consume the analyte.

Voltammetry

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A voltammetry consists in applying a constant and/or varying potential at an electrode's surface and measuring the resulting current with a three-electrode system. This method can reveal the reduction potential of an analyte and its electrochemical reactivity. This method, in practical terms, is non-destructive since only a very small amount of the analyte is consumed at the two-dimensional surface of the working and auxiliary electrodes. In practice, the analyte solution is usually disposed of since it is difficult to separate the analyte from the bulk electrolyte, and the experiment requires a small amount of analyte. A normal experiment may involve 1–10 mL solution with an analyte concentration between 1 and 10 mmol/L. More advanced voltammetric techniques can work with microliter volumes and down to nanomolar concentrations. Chemically modified electrodes are employed for the analysis of organic and inorganic samples.

Polarography

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Polarography is a subclass of voltammetry that uses a dropping mercury electrode as the working electrode.

Coulometry

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Coulometry uses applied current or potential to convert an analyte from one oxidation state to another completely. In these experiments, the total current passed is measured directly or indirectly to determine the number of electrons passed. Knowing the number of electrons passed can indicate the concentration of the analyte or when the concentration is known, the number of electrons transferred in the redox reaction. Typical forms of coulometry include bulk electrolysis, also known as Potentiostatic coulometry or controlled potential coulometry, as well as a variety of coulometric titrations.

References

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Bibliography

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from Grokipedia
Electroanalytical methods encompass a diverse set of techniques in that investigate chemical analytes by measuring electrical properties, such as potential, current, or charge, within an . These methods rely on the principles of reactions at the interface between an and an solution, where the applied or measured electrical signals correlate directly with the analyte's concentration, behavior, or reaction kinetics. By exploiting heterogeneous processes involving electrodes—typically composed of materials like , glassy carbon, or mercury—and supporting electrolytes, electroanalytical techniques enable precise control over reaction conditions through factors such as electrode surface chemistry and solution composition. The primary categories of electroanalytical methods include potentiometric, voltammetric, coulometric, and amperometric approaches, each distinguished by the electrical parameter emphasized and the mode of operation. Potentiometry measures the potential difference between electrodes at zero current flow, commonly used for ion-selective sensing, such as electrodes or detection of specific cations and anions. , the most versatile group, applies a varying potential while monitoring current, encompassing techniques like (CV) for studying mechanisms, (DPV), and square-wave voltammetry () for enhanced sensitivity in trace analysis. quantifies s by integrating current over time to determine total charge passed during , offering absolute measurements independent of cell constants. maintains a fixed potential to measure steady-state current proportional to , often integrated into flow systems like biosensors. Advanced variants, such as stripping voltammetry or electrochemical impedance spectroscopy, further improve selectivity through preconcentration steps or frequency-domain analysis. Electroanalytical methods are prized for their exceptional sensitivity—often achieving detection limits in the nanomolar range—and versatility across diverse matrices, making them indispensable in fields like for pollutants, pharmaceutical for quantification, and clinical diagnostics for biomarkers such as glucose. Their non-destructive nature for many techniques, combined with the ability to provide mechanistic insights into processes, supports applications in , electrocatalysis, and development. Recent advancements, including electrode modifications with , have expanded their scope to real-time analysis, underscoring their ongoing evolution as robust tools in modern analytical science.

General Principles

Electrochemical Cells and Electrodes

In electroanalytical methods, electrochemical cells serve as the fundamental apparatus for studying processes through controlled interactions between s and an solution. Galvanic cells rely on spontaneous reactions to generate an electrical potential, whereas electrolytic cells apply an external voltage to drive non-spontaneous reactions, with the latter being predominant in techniques requiring precise potential control. The typical setup emphasizes three-electrode configurations to enhance measurement accuracy by isolating the 's response from solution resistance effects. In this system, the is where the target undergoes oxidation or reduction, the maintains a stable potential for comparison, and the counter supplies or accepts electrons to balance the circuit, all immersed in a shared compartment. Early electroanalytical work in the utilized simple two-electrode systems, where the working and counter functions were combined, limiting precision due to uncompensated resistance. The shift to three-electrode systems occurred in the 1940s, driven by Archie Hickling's invention of the potentiostat, which enabled independent control of the potential relative to the reference, significantly improving reproducibility and accuracy in experiments. This configuration remains standard, as it minimizes iR drop—the voltage loss from current flow through the solution—and allows for reliable data in diverse analytical applications. Working electrodes are selected based on the need for inertness to avoid interference with reactions; electrodes, made from polished wire or foil, offer excellent conductivity and a broad potential range in aqueous media. Glassy carbon electrodes, formed by pyrolyzing a precursor into a non-porous, structure, provide chemical stability, low background currents, and resistance to adsorption, making them ideal for organic and biochemical analyses. Mercury-based electrodes, such as the dropping mercury electrode (DME) introduced by Jaroslav Heyrovský for , feature a vertical glass connected to a mercury , where drops form and detach at controlled intervals (typically 3-5 seconds) to renew the surface and suppress polarization effects. Reference electrodes ensure a constant potential benchmark; the (SCE) consists of a containing a mercury pool covered by a paste of mercury and mercurous chloride (Hg/Hg₂Cl₂), filled with saturated solution, and connected to the external medium via a porous ceramic frit or fiber junction to allow ionic contact while preventing contamination. The (Ag/AgCl) electrode comprises a silver wire coated with (often as a paste or sintered layer) immersed in a solution (typically 3 M or saturated), housed in a similar tube with a for isolation. Counter electrodes are usually inert wires or meshes to facilitate efficient current passage without altering the solution composition. Electrolyte solutions are essential for maintaining ionic conductivity and supporting charge transfer; they commonly include supporting electrolytes like (KNO₃), (NaCl), or tetramethylammonium salts at concentrations of 0.1-1 M in aqueous or non-aqueous solvents to reduce ohmic resistance, minimize electrostatic migration of analyte ions, and stabilize the double layer at the electrode interface. The choice of composition depends on the analyte's solubility and the method's requirements, ensuring uniform ion distribution without introducing side reactions.

Electrode Potentials and the Nernst Equation

The equilibrium potential at an electrode-solution interface arises from the balance between oxidation and reduction half-cell reactions, where the electrochemical potential of the oxidized and reduced species is equal. This potential reflects the thermodynamic driving force for the electron transfer process at the interface, governed by the activities of the species involved in the half-reaction. The quantifies this equilibrium potential for a general half-cell reaction of the form Oxidized + ne⁻ ⇌ Reduced. It is derived from the relationship between the change (ΔG) and the cell potential (E), where ΔG = -nFE, combined with the standard expression for ΔG = ΔG° + RT ln Q, leading to -nFE = -nFE° + RT ln Q. Rearranging yields E = E° - (RT/nF) ln Q, where E is the , E° is the , R is the (8.314 J mol⁻¹ K⁻¹), T is the absolute temperature in , n is the number of electrons transferred, F is Faraday's constant (96485 C mol⁻¹), and Q is the defined as the ratio of activities (or concentrations for dilute solutions) of products to reactants. At 25°C (298 K), this simplifies to the logarithmic form E = E° - (0.059/n) log Q, using common logarithms for practical calculations. Standard electrode potentials (E°) are referenced to the (SHE), defined by IUPAC as a in contact with a solution of unit activity H⁺ ions (1 M) and H₂ gas at 1 bar pressure, assigned an E° of 0 V for the 2H⁺ + 2e⁻ ⇌ H₂. For example, the standard reduction potential for the Fe³⁺/Fe²⁺ couple is +0.771 V versus SHE at 25°C and 0, indicating that Fe³⁺ is a stronger oxidant than H⁺ under standard conditions. The is sensitive to changes in solution conditions through the Q term. Concentration influences the potential logarithmically; for the Ag⁺ + e⁻ ⇌ Ag with E° = +0.799 , a tenfold decrease in [Ag⁺] from 1 M to 0.1 M shifts E to +0.740 at 25°C, as log(1/[Ag⁺]) = +1. affects the RT/nF factor, increasing the slope of the logarithmic term and thus amplifying concentration effects; for instance, at 50°C, the becomes approximately 0.070/n instead of 0.059/n. For involving H⁺, such as the / couple Q + 2H⁺ + 2e⁻ ⇌ QH₂ with E° ≈ +0.699 , the potential decreases by 0.059 per unit increase at 25°C, since Q includes [H⁺]², making E = E° - (0.059/2) log([QH₂]/[Q][H⁺]²). In metal ion systems without direct H⁺ involvement, like Cu²⁺/Cu⁺ (E° = +0.153 ), effects are indirect through or , but concentration changes dominate, with E shifting by -0.059 log([Cu⁺]/[Cu²⁺]) at 25°C.

Faradaic and Capacitive Currents

In electroanalytical methods, currents at the electrode-solution interface arise from two primary mechanisms: Faradaic processes involving electron transfer and non-Faradaic processes due to interfacial charging. Faradaic currents result from redox reactions where electrons are transferred between the electrode and solution species, directly linking the current to the rate of chemical transformation according to Faraday's laws. These currents are proportional to the reaction rate, with the magnitude determined by the number of electrons transferred (n), the Faraday constant (F ≈ 96,485 C/mol), and the electrode area (A), such that the rate in mol/s equals i / (n F). The kinetics of Faradaic currents are described by the Butler-Volmer equation, which relates the net current density (i) to the overpotential (η = E - E_eq), where E is the applied potential and E_eq is the equilibrium potential. The equation is: i=i0[exp(αnFηRT)exp((1α)nFηRT)]i = i_0 \left[ \exp\left(\frac{\alpha n F \eta}{RT}\right) - \exp\left(-\frac{(1-\alpha) n F \eta}{RT}\right) \right] Here, i_0 is the exchange current density, α is the transfer coefficient (typically 0.3–0.7), R is the gas constant, and T is the temperature in Kelvin. This form captures both anodic and cathodic contributions, with the exponential terms reflecting activation barriers for oxidation and reduction, respectively. For irreversible processes, large overpotentials make one exponential term negligible, simplifying to the Tafel equation and highlighting kinetic limitations beyond thermodynamic equilibrium. In contrast, capacitive currents, also known as non-Faradaic or charging currents, originate from the accumulation of charge in the electrical double layer at the surface, without net to solution species. This layer behaves like a , with double-layer per unit area typically 10–40 μF/cm² for aqueous solutions (total C = c_dl A), and the current is given by: ic=CdEdti_c = C \frac{dE}{dt} where dE/dt is the rate of change of potential. These currents are particularly prominent during potential transients, such as in voltammetric scans, and model the interface as an where the double-layer is in parallel with Faradaic resistance. Several factors influence the relative contributions of Faradaic and capacitive currents. Capacitive currents scale linearly with scan rate (v = dE/dt), increasing background noise at faster sweeps and potentially obscuring Faradaic signals, whereas reversible Faradaic currents in techniques like exhibit peak currents proportional to v^{1/2} due to control. Irreversibility in Faradaic processes, characterized by slow rates (low i_0 or extreme α), shifts the current-potential response, broadening peaks and reducing sensitivity compared to reversible systems. Electrode surface area and solution resistance also amplify capacitive effects, as larger areas increase C and uncompensated resistance (R_u) lengthens the charging (τ = R_u C). Quantitative separation of these currents is essential for accurate analysis, particularly in where Faradaic peaks overlay a capacitive baseline. One approach involves plotting peak current against scan rate: capacitive components yield a linear relationship through the origin, while Faradaic contributions show linearity with v^{1/2} for diffusion-limited processes, allowing subtraction via baseline correction or regression fitting. In practice, techniques like square-wave voltammetry minimize capacitive interference by sampling differential currents, enhancing Faradaic signal resolution.

Potentiometric Methods

Direct Potentiometry

Direct potentiometry is an electroanalytical technique that quantifies the activity of an ion by measuring the open-circuit potential difference between an ion-selective indicator electrode and a under conditions of zero or negligible current flow. This zero-current method ensures minimal perturbation to the sample, allowing the potential to directly reflect the electrochemical equilibrium at the electrode-solution interface. The measured potential arises from the selective interaction of the target ion with the indicator electrode's sensing element, such as a or , which establishes a phase boundary potential proportional to the ion's activity in solution. The relationship between the measured potential and activity follows a logarithmic response, as described by the , where the changes by approximately 59 mV per decade change in activity for monovalent s at 25°C, known as the Nernstian slope. curves are constructed by plotting the potential against the logarithm of known activities, yielding a linear segment typically spanning several orders of magnitude, from which unknown concentrations can be determined via . This logarithmic dependence arises from the thermodynamic basis of ion partitioning at the interface, enabling sensitive detection down to trace levels in many cases, though the exact slope and linear range depend on the material and solution conditions. A classic example of direct potentiometry is pH measurement using the , where a thin, hydrated silicate glass membrane selectively responds to hydrogen s, generating a potential that varies linearly with over the range of 0 to 14. This electrode, developed in the early and widely adopted for its robustness and accuracy, pairs with a like or Ag/AgCl to form a complete cell for routine laboratory and industrial pH monitoring. Another prominent application is analysis with lanthanum (LaF₃) electrodes, which utilize a single-crystal membrane to detect activities as low as 10⁻⁶ M, as pioneered in the for assessment and dental product evaluation. These solid-state electrodes exhibit near-Nernstian slopes of about -59 mV/decade and high selectivity for F⁻ over common interferents. Selectivity in direct potentiometry is crucial for accurate measurements in complex matrices, where interfering ions can contribute to the measured potential through non-ideal responses described by the Nikolsky-Eisenman equation: E=E0+RTFln(ai+kijaj)E = E^0 + \frac{RT}{F} \ln \left( a_i + \sum k_{ij} a_j \right) Here, EE is the cell potential, E0E^0 is the standard potential, aia_i and aja_j are the activities of the primary ion i and interfering ion j, respectively, kijk_{ij} are selectivity coefficients quantifying the relative response to interferents, and RT/FRT/F is the Nernst factor (approximately 59 mV at 25°C). These coefficients, determined experimentally via methods like the separate solution technique, indicate the electrode's discrimination ability; for instance, a LaF₃ electrode has kF,OH0.05k_{F^-, OH^-} \approx 0.05, meaning hydroxide interference is minimal at neutral pH. Interference effects become pronounced when interferent activities approach or exceed those of the analyte, necessitating ionic strength adjustment or masking agents to maintain accuracy. This equation, rooted in phase boundary potential theory, underpins the design of ion-selective electrodes for multianalyte environments.

Potentiometric Titrations

Potentiometric titrations involve the measurement of the potential difference between an and a as a function of the volume of titrant added to an solution, allowing for the determination of the through changes in . This method relies on the Nernstian response of the indicator electrode to the activity of involved in the reaction. The technique was first introduced in the late , with Robert Behrend performing the initial in 1893 at Ostwald's Institute in , where he titrated mercurous nitrate with halides using a mercury . Early applications focused on reactions, marking the beginning of instrumental endpoint detection in volumetric analysis. Endpoint identification in potentiometric titrations is achieved by analyzing the potential-volume curve, which typically exhibits a gradual change before and after the , with a sharp inflection at the for systems with suitable responses. One widely used approach is the Gran plot method, developed by Gunnar Gran in the early 1950s, which transforms the nonlinear potential data into linear segments by plotting functions proportional to the or titrant concentration against volume. For acid-base titrations, the Gran function before the (e.g., 10^{pH} times volume) extrapolates to zero at the equivalence volume, providing precise determination even in dilute solutions where inflection points are shallow. This method enhances accuracy by avoiding direct reliance on the inflection and is particularly effective for systems with conditional stability constants. Alternative endpoint detection employs first- and second- methods applied to the potential-volume . The first , calculated as the change in potential per unit volume (ΔE/ΔV), plotted against volume, reaches a maximum at the , corresponding to the steepest slope of the curve. The second , the change in the first per unit volume (Δ(ΔE/ΔV)/ΔV), shows a sharp peak or sign change precisely at the , offering higher sensitivity for detecting subtle inflections in weak systems. These techniques are computationally straightforward and improve precision in automated , though they require smooth to minimize noise effects. Potentiometric titrations are classified by reaction type, each exhibiting characteristic potential changes at the due to shifts in the predominant species sensed by the . In acid-base titrations, such as the neutralization of with using a glass , the potential () remains low in the acidic region and jumps abruptly to the basic region at the , reflecting the rapid change from H⁺ dominance to OH⁻ dominance. This jump, often exceeding 6-8 units in strong acid-strong base systems, enables accurate endpoint detection without visual indicators. titrations, exemplified by the determination of with using a silver , show a constant potential before the governed by excess Ag⁺, followed by a sharp decrease after as sparingly soluble AgCl forms, reducing [Ag⁺] dramatically and shifting control to Cl⁻ activity. The potential change can span 100-200 mV or more, depending on . titrations, such as the oxidation of ferrous ion with cerium(IV) using a , exhibit a low potential before the (controlled by Fe²⁺/Fe³⁺ couple) that rises steeply to a high value after, dominated by the Ce³⁺/Ce⁴⁺ couple, with jumps often around 400-600 mV due to differing standard potentials. The primary advantages of potentiometric titrations include the objective determination of the endpoint without reliance on color-changing indicators, making them suitable for , turbid, or opaque solutions where visual methods fail. They also provide high precision and versatility across reaction types, with automation enabling reproducible results in routine analyses. However, limitations arise from the slow response time of electrodes near the , particularly in systems with gradual potential changes, which can prolong titration duration and introduce errors if not equilibrated properly. Additionally, the method requires stable and suitable electrodes responsive to the , limiting applicability in highly irreversible systems.

Amperometric and Voltammetric Methods

Amperometry

is an electroanalytical technique that involves applying a constant potential to a and measuring the resulting current, which is proportional to the concentration of an electroactive diffusing to the surface. At sufficiently positive or negative potentials, the current becomes diffusion-limited, governed by the rate at which the reaches the . In steady-state conditions, such as those achieved with or thin-layer cells, the limiting current ii is described by i=nFADC/δi = n F A D C / \delta, where nn is the number of electrons transferred, FF is the , AA is the area, DD is the coefficient, CC is the concentration, and δ\delta is the diffusion layer thickness. This steady-state current provides a direct measure of concentration, making suitable for quantitative analysis in flowing systems or sensors. Capacitive currents may contribute to the background signal but are typically minimized at longer times. A key variant is chronoamperometry, where a potential step is applied, and the transient current is monitored over time. The current decays as t1/2t^{-1/2} due to the expanding diffusion layer, following the : i(t)=nFACD/πti(t) = n F A C \sqrt{D / \pi t}
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