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ORP Sensing Electrode

In document Fossil Plant Cycle Chemistry (Page 97-104)

OXIDATION-REDUCTION POTENTIAL

6.2 Description of Method

6.3.3 ORP Sensing Electrode

Corrosion scientists and electrochemists in the research world typically report ORP values on the SHE scale even though the measurements are rarely actually made using an SHE. In practice, a more robust, more convenient reference electrode is used and the value measured is converted to the SHE scale either by calculation or by adjustment of instrument zero during calibration. In the power industry, however, ORP values are usually reported with respect to the reference

electrode contained in the ORP probe. Such a practice is potentially confusing only because the reference electrode used is not routinely mentioned when reporting the ORP value.

Fortunately, the great majority of ORP probes used in power plants use one type of reference electrode: the Ag/AgCl reference electrode. Also fortunately, the internal electrolyte in the reference electrode, which influences the electrode potential, is typically potassium chloride with a concentration ranging from 3M to a saturated solution. An increase in the chloride

concentration over this range would decrease the reference electrode potential by no more than 11 mV for temperatures in the range 20-30°C (68-86°F) (see Table 6-1). Since errors of 11 mV would be considered small for most practical ORP measurements, knowledge of the precise KCl concentration is usually not an issue at near-ambient temperatures. Corrections for KCl

concentration may be necessary if the ORP is measured at higher temperatures. Nevertheless, confusion has arisen when ORP values measured versus a Ag/AgCl reference electrode are inadvertently compared with others measured versus an SCE or SHE. Consequently, it is recommended that the reference electrode used for the measurement is always mentioned along with the measured ORP values (e.g., ORP = 0.100 V(Ag/AgCl, Sat. KCl)).

Table 6-1

To Convert ORP or ECP Values Measured Using Reference Electrode #1 to Values on Reference Electrode #2 Scale, Add the Indicated Conversion Factor to the Measured Potential [3]

Add the Conversion Factor Below to Convert To Potential (mV) Versus Reference Electrode #2*

To SCE To Ag/AgCl

* Ag/AgCl = silver/silver chloride; SCE = saturated calomel electrode; SHE = standard hydrogen electrode.

Note: the presence of liquid junction potentials may result in the listed conversion factors being in error by 1 or 2 mV.

When reporting and comparing comparing ORP measurements, they should be referred to the same reference electrode scale. As described above, the conversion factors shown in Table 6-1 can be used to convert from one reference electrode scale to another. For instance, an ORP of

+100 mV measured at 25°C (77°F) versus a Ag/AgCl, Sat. KCl reference electrode can be converted to an ORP versus an SHE, by adding 199 mV:

mV

In general, ORP measurements are not subject to solution interferences from color, turbidity, colloidal matter and suspended matter. Deposits on the surface of the metallic portion of the sensing electrode can cause the electrode to be unresponsive or exhibit a memory effect. ORP measurements are temperature sensitive as defined by the Nernst Equation. However, the magnitude of the error is small compared to the variability of the system being measured and automatic temperature compensation is not normally employed.

ORP measurements are also pH dependent as previously discussed. The pH/ millivolts

correlation is approximately 59 mV per standard pH unit at 25°C (77°F). Again it is important to remember that ORP readings are by no means absolute determinations that can be correlated across multiple systems. While a +100mV (Ag/AgCl, 3M KCl) reading may be highly oxidizing in a feedwater system, a cooling tower at lower pH may have very little oxidizing power at this value. For true disinfecting conditions using chlorine, an ORP reading of +400 mV to +600 mV (Ag/AgCl, 3M KCl) may be desired.

6.5 Calibration

The instrument used to measure ORP may be calibrated using standard solutions that have known ORP values. For instance, one possible set of standard ORP reference solutions are based on pH 4 and pH 7 buffer solutions, similar to those used for pH meter calibration. However, for ORP standards, quinhydrone (formulated to provide an equimolar solution of quinone and hydroquinone) is added to the buffer solutions, which forms a reversible oxidation-reduction couple when dissolved in water. Hydrogen ions participate in the reaction between the quinone and hydroquinone, Equation 6-11, creating a pH dependent equilibrium:

C H O + 2H + 2e C H O

When the activity of quinone (aq) is equal to the activity of hydroquinone (aaq), the second term (log a /a ) on the right hand side of Eq. 6-10 drops out so that the electrode potential, E, is hq q dependent only on pH.

The quinhydrone solutions are prepared by dissolving 10 grams of quinhydrone in one liter of pH 4 or pH 7 buffer solution [5]. Quinhydrone is not very soluble, so only a small amount will dissolve in the buffer solution, changing it to an amber color. However, it is important that excess quinhydrone is used so that solid crystals are always present. The quinhydrone powder poses a moderate health risk, causing irritation of the lungs with prolonged exposure to the dust.

The calibration solutions are fairly innocuous unless ingested in large amounts. These hazards are minimized or can be avoided by using safe handling practices. Refer to the relevant MSDS for appropriate information.

For the pH 4 and 7 quinhydrone solutions, ORP values of about 263 mV and 86 mV, respectively, can be expected at 25°C (77°F) when measured against a Ag/AgCl, Sat. KCl reference electrode [2,5,6]. These values are consistent with a change of 59.0 mV per pH unit, which are consistent with the calculated value of 2.303 RT/F (= 59.2 mV at 25°C (77°F)) in Eq.

6-10. ORP values for the standard solutions at other temperatures and for other reference electrodes are provided in ASTM D1498-00 [2] and are reproduced in Table 6-2.

Table 6-2

Expected ORP Values for Reference Quinhydrone Solutions at pH 4 and pH 7 ORP Value (mV)

pH 4 Buffer Solution pH 7 Buffer Solution Reference

* Ag/AgCl = silver/silver chloride (Sat. KCl); SCE = saturated calomel electrode;

SHE = standard hydrogen electrode.

The quinhydrone standards are easily made but they are stable due to reactions with air,

primarily oxygen contamination, for only about eight hours and are not expected to yield highly reproducible ORP values. Nevertheless, ORP values in freshly prepared solutions are expected to be within 10 mV of the values listed in Table 6-2; and an ORP value measured with a probe in one of these standards can usually be considered acceptable if it lies within 30 mV of the listed value. If the electrode does not respond as expected or has a slow response, it should be cleaned and the calibration procedure repeated. Removal of oily or organic deposits can be achieved with a detergent or, if necessary, methanol or isopropyl alcohol. For removal of contaminants or mineral deposits, the electrode should be soaked in 10% nitric acid for 10 minutes.

Alternatively, ASTM D1498-00 suggests the use of warm (70°C) aqua regia for about 1 minute [2]. As a last resort, the platinum surface can be polished with a 600 grit wet-dry emery cloth or a 1-3 micron alumina polishing powder to remove any stubborn coatings or particulates. The electrode will need to soak in purified water for at least 30 minutes after performing any of these cleaning procedures.

A single point calibration (or “standardization”) is often considered adequate. ORP meters, unlike pH meters, do not have “slope calibration” to allow adjustment of the response to a specified change in ORP. Nevertheless, it is usually good practice to verify that the ORP probe (platinum/reference electrode combination) is operating in a predictable fashion by measuring the ORP in a second standard solution. If the electrode potential does not change by the expected amount, the electrode should be cleaned and re-calibrated, as described above.

Other ORP calibration solutions are available based on the ferrous/ferric cyanide or ferrous/ferric sulfate equilibrium reactions, but the quinhydrone standards are more widely used.

6.5.1 Calibration Checks

On-line ORP instruments should be checked periodically to demonstrate calibration stability.

The Line Method [7] is appropriate for verifying instrument stability. Here, a calibrated separate ORP monitor is used to analyze the same sample steam as the installed on-line instrument. The two results are compared to the acceptance criteria (e.g., agree within ± 3 sigma or ± 10%).

Provided the on-line analyzer agrees within the acceptance criteria, the on-line instrument’s calibration is considered to be acceptable. If the results are outside the acceptance criteria the on-line instrument must be recalibrated.

6.6 End User Considerations

Manufacturers of on-line pH monitors typically include the ability to monitor ORP in their instrument design. In fact, the two measurements are closely related and only differ in the design of the sensing electrode and manner in which the mV output signal is manipulated. For the most accurate ORP determinations (±5 mV precision), samples should be maintained at 25 ±1 °C (77

±2 °F) to preclude ion activity discrepancies [2].

ORP sensing probes in power plant feedwater systems do not suffer from foreign material buildup. In cooling water or service water applications, ORP sensing probes are susceptible to foreign material plating the noble metal surface. Some of these applications require almost daily electrode cleaning, stabilization, and calibration verification. Systems are presented by several manufacturers that provide in-situ on-line cleaning of the probe. Calibration is performed with one or more pH buffers to which has been added a quinhydrone compound (see section 6.4).

Most calibrations are only one point (the mV reading of a pH 4 buffer with added quinhydrone) adjustments but making a cross check with a second buffer is advisable. The span value of the output signal is also a user defined variable with many of the instruments. Full scale deflections are possible with as little as 100mV and can be ranged up to 1000mV.

ORP readings are empirical at best but satisfactory for their intended use in fossil feedwater cycles. Absolute values are not transferable from one system to another and may undergo changes with various water quality parameters.

6.7 References

1. Cycle Chemistry Guidelines for Fossil Plants: All-volatile Treatment, Revision 1. EPRI, Palo Alto, CA: 2002. 1004187.

2. ASTM D 1498-00; “Standard Practice for Oxidation-Reduction Potential in Water”. ASTM International West Conshohocken, PA 19426; 2006.

3. Barry Dooley, Digby Macdonald, and Barry C. Syrett, “ORP—The Real Story for Fossil Power Plants”, Power Plant Chemistry, 2003, Volume 5(1).

4. ASTM G5-87, “Standard Reference Method for Making Potentiostatic and Potentiodynamic Anodic Polarization Measurements”, ASTM, Philadelphia, PA. 1987.

5. L. McPherson, Chemical Engineering, p. 143-145, March 1994.

6. S. Filer, A.S. Tenney III, D. Murray and S.J. Shulder, “Power Plant ORP Measurements in High Purity Water”, NUS International Chemistry On-Line Process Instrumentation Seminar, Clearwater Beach, FL. November 1997.

7. ASTM D3864-96(2000), “Standard Guide for Continual On-Line Monitoring Systems for Water Analysis, American Society for Testing & Materials”. American Society for Testing and Materials, Philadelphia, PA.

7

pH

7.1 Purpose and Use

In boiler water, pH is an EPRI Core Monitoring Parameter [1-4]. As such, pH should

continuously be monitored on-line to check the acceptability of the water chemistry, thereby ensuring that corrosion rates are kept at low levels.

In fossil plant steam-water cycles pH may also be monitored for one or more of the following reasons:

• To facilitate the correlation between two or more water chemistry parameter (e.g., pH, conductivity, ammonia correlation).

• To provide a feedback signal for automated process control.

• To warn of in-leakage of contaminants.

• To warn of condensate polisher malfunction.

• To troubleshoot or verify the accuracy of other on-line pH monitors.

• To check the pH of water streams not routinely monitored continuously by on-line monitors.

The data generated by continuous on-line monitoring of pH is used by plant chemistry and operations personnel. The goal for plant personnel is to maintain pH within prescribed limits.

The pH method and instrument described below is substantially different from the pH method and instrument used for environmental or other high ionic strength solutions. Although the technical understanding for the measurement of pH is essentially the same, other considerations for these high ionic strength samples are significantly different. For a discussion on

environmental pH analysis refer to APHA Standard Methods for Examination of Water and Wastewater, Part 4500-H+ [5].

7.2 Description

The term pH is a measure of the acidity (or alkalinity) of an aqueous fluid. The factor that most influences the level of acidity is the activity of the hydrogen (H+) ions in the fluid. By definition, pH is the logarithm of the reciprocal of the H+ activity:

H

In weak solutions typical for power plant on-line instrumentation applications, H+ activity is approximately equal to H+ concentration in moles/liter. The pH is obtained by measuring the potential difference between a pH-sensitive electrode and a reference electrode, both of which are immersed in the solution of interest.

Measurement of pH is accomplished by means of an electrode that develops an electrochemical potential directly related to the H+ activity of the solution in which the electrode is immersed.

The purpose of the pH-sensing electrode is to provide a varying electrochemical signal corresponding to the H+ ion concentration in the solution being tested.

Although it is not feasible to measure the electrochemical potential directly, it is possible to measure differences in potential with a voltmeter or electrometer. Consequently, a reference electrode is needed in addition to the pH-sensitive electrode to complete the circuit. The purpose of the reference electrode is to provide a constant electrochemical reference potential (a baseline) against which the potential of the pH-sensing electrode can be compared. The reference electrode potential is not affected by H+ ion concentration.

Therefore, when pH instrumentation measures the potential difference between the pH-sensitive electrode and the reference electrode, the potential difference can be directly related to the H+ ion activity at the pH electrode surface.

Instrument manufacturers supply the pH electrodes and reference electrodes separately or in a single combined unit. For low-conductivity pH applications separate electrodes provide some technical advantages discussed below. For routine pH applications combination electrodes are adequate.

7.3 Technical Considerations

Water samples taken from the steam/water cycle typically have low ionic strength (i.e., 0.1 to 100 µS/cm), leading to several analytical challenges. These challenges can be overcome provided appropriate pH sensing and reference electrodes are selected; appropriate temperature compensation is applied; interfering ions are minimized; interfering stray current is minimized;

and, appropriate calibration and calibration checks are performed. Without appropriate

consideration of these factors it is not unusual for the pH electrode response to be slow, “noisy”, and non-reproducible under such circumstances.

In document Fossil Plant Cycle Chemistry (Page 97-104)