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ORIGINAL RESEARCH article

Front. Phys., 03 October 2022
Sec. Optics and Photonics
This article is part of the Research Topic State-of-the-Art Laser Spectroscopy and its Applications : Volume II View all 51 articles

Correcting the light extinction effect of fly ash particles on the measurement of NO by TDLAS

Songjie GuoSongjie Guo1Yan YangYan Yang1Guodong ShaoGuodong Shao1Zhenghui LiZhenghui Li1Wei RenWei Ren2Juehui MoJuehui Mo3Zhimin Lu,Zhimin Lu1,4Shunchun Yao,
Shunchun Yao1,4*
  • 1School of Electric Power Engineering, South China University of Technology, Guangzhou, China
  • 2Department of Mechanical and Automation Engineering, The Chinese University of Hong Kong, Hong Kong, Hong Kong SAR, China
  • 3Cntest Intelligent Scien-tech Co, LTD., Foshan, China
  • 4Guangdong Province Key Laboratory of Efficient and Clean Energy Utilization, Guangzhou, China

The measurement of nitric oxide (NO) concentration in power plant flue gas by tunable diode laser absorption spectroscopy (TDLAS) is susceptible to fly ash particles. The presence of fly ash particles causes laser intensity fluctuations and leads to the second harmonic (2f) signal amplitude changes. In this manuscript, we analyzed the influence of particles on the 2f signal and corrected the measurement error of NO concentration by the wavelength modulation-second harmonic (WMS-2f) technique. Specifically, the 2f signal error caused by quartz sand and fly ash particles were measured, and the exponential function representing the peak-to-peak error of the 2f signal was obtained by fitting. Finally, the peak-to-peak value of the 2f signal and the NO concentration were corrected according to the exponential function. After correction, the NO concentration error under the fly ash influence (the particle size in the range of 10–200 μm and the mass concentration is less than 18.26 g/m3) was no more than 2%. This correction method effectively improves the measurement accuracy of NO concentration by the WMS-2f technique in the fly ash environment.

Introduction

Nitrogen oxide (NOX) is an important air pollutant [1], and its primary source of emissions is coal-fired power plants. The main component of NOx in flue gas is nitric oxide (NO). Various optical techniques have been widely used in gas pollutant monitoring [2, 3]. In daily operation, the continuous emission monitoring system (CEMS) of flue gas is used to online monitor the NO emission concentration. Currently, the in-situ method is one of the primary forms of the CEMS system [4]. This method refers to directly measured in the flue, enables to obtain actual values more easily of flue gas concentrations, and has a short response time [5]. However, the environment in the flue is complex, and the mass concentration of fly ash is relatively high. The extinction effect caused by scattering and absorption by fly ash particles will greatly influence the detection of NO and other components concentration by optical technique [6].

TDLAS is one of the main measurement techniques of NO concentration in flue gas at present [7], including direct absorption spectroscopy (DAS) and wavelength modulation spectroscopy (WMS). DAS is susceptible to interference from low-frequency noise, and its detection sensitivity is limited. WMS can effectively restrain low-frequency noise by superimposing a high-frequency modulation signal on the basic low-frequency scanning signal and demodulating it at high frequency [811]. WMS technique has a high detection sensitivity, which can reach 10−5–10–6. It is widely used for trace gas detection, such as in industrial process control [12], environmental monitoring [13], and pathology diagnosis [14]. The peak value of the second harmonic (2f) signal of demodulated WMS signal corresponds to the central frequency of the gas absorption line, and the 2f signal has a larger amplitude than the higher-order harmonics. Therefore, it is suitable for gas concentration inversion. It was demonstrated that when the absorption is small, the 2f signal amplitude changes approximately linearly with gas concentration at constant laser intensity, absorption path, and modulation parameters [15, 16]. The target gas concentration can be directly calculated by comparison with the 2f signal amplitude of the standard gas. This method is referred to as the wavelength modulation-second harmonic (WMS-2f) technique and was widely implemented in industrial equipment.

However, the stability of laser intensity must be guaranteed to calculate gas concentration using the WMS-2f technique reliably. If the laser intensity fluctuates, the amplitude of demodulated 2f signal accordingly changes. Attenuation of laser intensity by non-gas absorption introduces errors to the calculated values of gas concentration, which limits the application of the WMS-2f technique in environments with drastic laser intensity fluctuation [17]. In particular, the laser intensity is inevitably affected by the extinction effect of fly ash during the in-situ measurements in coal-fired power plants’ flue, which results in small measurement values. Eliminating the influence of fly ash on calculated values of flue gas component concentrations is a difficult problem. Some researchers have proposed using a laser intensity reference signal to eliminate the effect of laser intensity fluctuation. The reference signals can be the filtered laser intensity signal or the first harmonic (1f) signal [18]. Although this method can somewhat eliminate the influence of laser intensity fluctuation, its calculation program is complicated. Moreover, drastic changes in laser intensity and electronic noise in the demodulation process can also result in some errors. Wang et al. discussed the effect of particles on the 2f signal based on the TDLAS technique. They used the transmitted laser intensity to calibrate the 2f signal to solve the problem of particle interference with gas measurements. A concentration of 20% carbon dioxide was measured, and the calibrated 2f peak error was less than 5% [19].

In order to eliminate the particle’s influence on the NO concentration measurement, we analyze the effect of particle mass concentration and particle size on the 2f signal. The law revealed can be used to correct NO concentration errors directly. This method is different from that of measuring laser reference intensity. Direct research on error sources can effectively improve the measurement accuracy of NO concentration in the particulate environment and simplify the computing system. The peak-to-peak error of the 2f signal caused by quartz sand and fly ash was measured in the manuscript. The error was normalized and fitted by the exponential function. Finally, the calculation error of NO concentration was corrected using the error exponential fitting function and the standard gas calibration function.

Correction method

As mentioned above, when measuring NO in the flue gas environment with particles, it is the fundamental guarantee for accurate measurement to determine the extinction effect of particles and correct the measurement signal. The correction flow chart is shown in Figure 1.

FIGURE 1
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FIGURE 1. Correction flow chart of the peak-to-peak value of 2f signal and gas concentration.

As shown in Figure 1, the error exponential fitting function needs to be obtained in advance before correction. In the online measurement, as long as we correct the error of the 2f signal and the gas concentration according to the fitting function. The detailed principle is described as follows.

Due to scattering and absorption of particles, the laser intensity passing through a medium containing particles will attenuate. The attenuation degree is directly related to particles’ mass concentration and particle size. According to the Beer-Lambert law, when a monochromatic parallel light with intensity I0 is incident on a medium containing uniformly distributed particles, the relationship between the transmitted laser intensity I and I0 is as follows [20]:

I=I0exp(τL),(1)

where τ is the medium turbidity. In a simple model, if the scattering medium contains N spherical particles with a diameter D per unit volume, τ can be expressed as follows:

τ=Nakext=π4ND2kext,(2)

where a is the light-facing area of a particle, kext is the extinction coefficient, and kext can be calculated according to the Mie scattering theory [21, 22], kext=2α2n=0(2n+1)(|an|+|bn|), where α=πDλ is called the dimensionless parameter, and an and bn are the Mie coefficients, respectively. Substitution of Eq. 2 into Eq. 1 with subsequent transformation results in the following expression for the difference between the incident laser intensity and the transmitted one:

I0I=I0[1exp(π4ND2kextL)].(3)

For uniform particles of the same size, the relationship between their number concentration N and mass concentration W is expressed as N=6WπρD3, where ρ is the particle density. It can be seen from this expression that at constant values of particle density and average particle size, their mass concentration is proportional to the number concentration. Substituting N into Eq. 3 and normalizing by the incident laser intensity, the following expression for the difference of normalized light intensities to the particle mass concentration was obtained:

1II0=1exp(64ρDkextLW).(4)

The effect of stable and uniformly distributed particles on the scattering and absorption of laser is constant. Therefore, the extinction effect caused by different mass concentrations of particles was measured through experiments and was fitted using Eq. 4. From this, the law describing the dependence of the extinction effect on particle mass concentration can be obtained. This law can be used to correct the measurement error of laser intensity at different mass concentrations of particles.

There are many ways to measure the laser intensity change, including direct and indirect measurements. Although the device for directly measuring the laser intensity is simple, it is necessary to keep the laser power stable, and it is difficult to avoid the interference of low-frequency noise, which will introduce significant errors [23]. TDLAS technique often measures gas concentration by scanning wavelength and also indirectly obtains the change in laser intensity. Noteworthily, correcting laser intensity changes can improve the TDLAS technique accuracy for measuring gas concentrations.

According to the Beer-Lambert law, when a laser beam of frequency ν and intensity I0 passes through a gas sample, the transmitted laser intensity I(ν) can be expressed as follows [24]:

I(ν)=I0exp[S(T)Φ(ν)PXL],(5)

where S(T) is the intensity of the characteristic spectral line of the gas, Φ(ν) is the lineshape function of the absorbed spectral line, which is described here by the Voigt function, P is the total pressure of the gas, X is the volume concentration of the gas to be measured, and L is the transmission distance of laser in the gas medium, respectively. When the central laser frequency ν0 is modulated by a sine wave with an angular frequency ω, the instantaneous laser frequency ν(t) can be expressed as follows [25, 26]:

ν(t)=ν0+dcos(ωt),(6)

where d is the modulation amplitude. Taking into account the characteristics of distributed feedback laser (DFB), it is known that if the laser frequency is modulated, its intensity is modulated as well. The instantaneous laser intensity passing through the gas sample can be expressed by the cosine Fourier series of I(ν0):

I(ν0,t)=n=0An(ν0)cos(nωt),(7)

where An(ν0) are the different harmonic components, which can be measured by a lock-in amplifier:

An(ν0)=2π0πI0(ν0+dcosθ)exp[σ(ν0+dcosθ)XL]cosnθdθ.(8)

Here, θ=ωt, and σ is the light absorption coefficient, respectively. For trace gases σXL1, so Eq. 8 can be approximated as follows:

An(ν0)=2I0XLπ0πσ(ν0+dcosθ)cosnθdθ.(9)

It can be seen from Eq. 9 that each harmonic component is proportional to the gas concentration. In practical measurements, the gas concentration is often calculated using the peak-to-peak value of the 2f signal. At the same time, the 2f peak-to-peak value is proportional to the laser intensity. When the laser intensity decreases by non-gas absorption, the 2f peak-to-peak value also decreases. Eq. 4 can be further expressed as follows:

1VPP(2f)VPP0(2f)=1exp(64ρDkextLW),(10)

where VPP(2f) and VPP0(2f) are the 2f peak-to-peak values in the presence and absence of fly ash, respectively. Under the condition of known mass concentration of fly ash W, the reduction of 2f peak-to-peak value by fly ash extinction is expressed as 1VPP(2f)VPP0(2f). Assuming that the response of the 2f peak-to-peak value to the gas concentration in the absence of fly ash in a particular system is VPP0(2f)=kX+b, the actual gas concentration can be expressed as follows:

X={VPP(2f)+[1VPP(2f)VPP0(2f)]}bk,(11)

where k and b are the slope and the intercept of the linear response function of 2f peak-to-peak value to gas concentration, respectively. Using Eq. 11 to correct the gas concentration can eliminate the measurement error of gas concentration caused by the extinction of fly ash particles.

Experimental setup

In order to verify the feasibility and accuracy of the above correction method, we designed and built an experimental system. Firstly, we selected the absorption line of NO located at 1929.02 cm−1 as the target detection line, corresponding to a wavelength of 5.184 μm. Figure 2 shows the distribution of NO absorption lines between 1.5 and 5.5 μm. It can be seen that the absorption linestrength near 5–5.5 μm for NO is stronger. In particular, there are six very close absorption lines of NO at 5.184 μm, and they work together to produce a larger absorption peak, as shown in the black shaded area in Figure 2B.

FIGURE 2
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FIGURE 2. NO absorption lines distribution between (A) 1.5–5.5 μm. (B) 5.175–5.19 μm (From HITRAN Database).

The main components of the experimental system were the laser, the fly ash unit (as shown in the dashed box), the gas cell, and the signal processing section. A function generator was installed inside the lock-in amplifier (HPLIA, HEALTHY PHOTO), which generated a sawtooth signal with a frequency of 2 Hz and a sine wave signal with a frequency of 6 kHz. These signals were transmitted to the laser controller (HPTCD-Q, HEALTHY PHOTO) and controlled the current of a quantum cascade laser (HPQCL-Q, HEALTHY PHOTO). The modulation voltage was adjusted to keep the modulation coefficient at about 2.2. The QCL central wavelength is 5.184 μm. We used a self-designed fly ash unit system, which included a powder feeder, a fly ash pipe, a powder collector, and a vortex blower. Because the gas cell was closed and the fly ash pipe was open during measurements, it was inconvenient to combine them. Moreover, the effects of gas and fly ash on laser intensity could be considered independent, so we decided to separate them. In the experiment, the laser passed through the fly ash unit first and then through the gas cell. The powder feeder was located above the inlet of the fly ash pipe, so the fly ash reached the inlet of the fly ash pipe by free fall. The outlet of the fly ash pipe was connected to the powder collector and the vortex blower, and the suction force of the latter was used to suck the fly ash into the powder collector. This way, a stable flow fly ash environment was formed inside the fly ash pipe. In order to form a relatively stable gas-solid two-phase flow atmosphere, the fly ash pipe included two parts. The fly ash flowed into the second part of the pipe after being evenly mixed in the first part. In order to ensure the same effect distance between particles and NO on the laser, the length of the second part of the pipe was the same as that of the gas cell, both equal to 0.38 m. The laser beam passed through the second part of the pipe. The measurements were carried out on NO gas in the closed gas cell at the stable pressure of 0.99 atm. The laser beam passed through the gas cell once and entered the photodetector (HPPD-M-A, HEALTHY PHOTO). The laser intensity signal detected by the detector was input to the lock-in amplifier for demodulation to obtain the 2f signal. The latter was recorded and transmitted to the computer by a data acquisition card (USB-6363, NI). The experimental setup is schematically shown in Figure 3.

FIGURE 3
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FIGURE 3. Schema of the experimental setup.

The particle amount was controlled by controlling the vibration frequency of the powder feeder. The particle mass concentration was calculated by measuring their mass per unit of time and the real-time volume of air in the vortex blower. When there were only fly ash particles smaller than 100 μm, agglomeration easily occurred in the powder feeder, and it was difficult to generate a uniform flow of fly ash. The intensity of the laser beam passed through the fly ash pipe considerably fluctuates, causing a measurement error. We first used quartz sand to simulate fly ash. The main component of fly ash is SiO2, which is the same as quartz sand. However, the stacking density of quartz sand particles is slightly higher than that of fly ash, and their agglomeration is not easy to occur. Firstly, the mass concentration of quartz sand was measured and calculated by measuring the particle mass in the powder feeder per unit time (unit: g/h) and the air volume in the fly ash pipe in real-time. The air volume was measured using a gas flow meter installed at the outlet of the vortex blower. The air volume of the vortex blower was about 65 m3/h in these experiments. The mass concentration of particles could be obtained by dividing the particle mass by the air volume. In this experiment, the effects of different mass concentrations of particles on the NO 2f signal were analyzed. A higher volume fraction of NO for the measurement was chosen to ensure that the 2f signal has a high amplitude. Firstly, the gas cell was filled with a gas mixture of NO and N2, the volume fraction of the former being 9.06 × 10–5. After particles flow in the fly ash pipe was stable, the NO 2f signal was recorded, and the experiment was repeated at different particle mass concentrations. Next, the gas cell was flushed with pure N2. Then, five volume fractions of NO, namely 2 × 10–5, 4 × 10–5, 6 × 10–5, 8 × 10–5, and 1 × 10–4, were formulated by NO standard gas of volume fraction 1 × 10–4 in order to quantify and calibrate the errors caused by different mass concentrations of fly ash on the measured values of NO concentration. Two mass flow meters (S48 32/HMT, HORIBA METRON) were used in this process. Finally, these five volume fractions of NO were injected into the gas cell, and their 2f signals were recorded.

Results and discussion

As we known, the fly ash particles produced by coal-fired power plants vary in size and have broad size distributions, usually ranging from several to two hundred microns. In order to study the influence of particle size on the NO 2f signal, we used quartz sand with different particle sizes for experiments. It was found after testing that the quartz sand particles smaller than 54 μm tend to agglomerate. Therefore, three particle sizes were chosen for the experiments, namely 54–76 μm, 97–105 μm, and 105–135 μm.

The measurement results of the NO 2f signal influenced by quartz sand with particle sizes of 54–76 μm are shown in Figure 4. Figure 4A presents the NO 2f signals with the removed background at different mass concentrations of particles. The 2f signal was averaged 10 times, and Figure 5, Figure 8 and Figure 10 were also operated in this way. According to Eq. 10, the 2f peak-to-peak value of NO corresponding to different mass concentrations of quartz sand particles was subtracted from the respective value obtained without quartz sand and normalized to obtain the 2f peak-to-peak error of NO. Figure 4A shows that the 2f peak-to-peak value of NO gradually decreased with the increased mass concentration of quartz sand particles. Then the 2f peak-to-peak error of NO and the mass concentration of quartz sand were fitted by an exponential function in the following form: y=1exp(xt), where y was the 2f peak-to-peak error of NO, and x was the mass concentration of quartz sand, respectively. The fitting result is shown in Figure 4B. The fitting results concluded that the 2f peak-to-peak error of NO and the quartz sand mass concentration had a good exponential correlation with R2 = 0.999. Therefore, this exponential function could be used to correct the 2f peak-to-peak value with subsequent correction of the NO concentration under the condition that the mass concentration of quartz sand particles was known.

FIGURE 4
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FIGURE 4. Effect of quartz sand (54–76 μm) on the NO 2f signal. (A) 2f signal with removed background. (B) Exponential fitting function of 2f peak-to-peak error.

FIGURE 5
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FIGURE 5. Effect of quartz sand on the NO 2f signal. (A) 2f signal with removed background (97–105 μm). (B) Exponential fitting function of 2f peak-to-peak error corresponding to Figure 5A. (C) 2f signal with removed background (105–135 μm). (D) Exponential fitting function of 2f peak-to-peak error corresponding to Figure 5C.

In the same way, quartz sands with particle sizes of 97–105 and 105–135 μm were used for experiments. Obtained results are shown in Figure 5. Similar to the previous case, the 2f peak-to-peak errors of NO were fitted by exponential functions. The values of R2 were 0.999 and 0.998. The obtained results demonstrated that for three different particle sizes, the 2f peak-to-peak error of the NO signal and the quartz sand mass concentration all satisfied a good exponential relationship. The mass concentration of quartz sand particles was calculated by their mass and the air volume of the vortex blower, and there were some differences in the particle amounts between the experiments. Therefore, the quartz sand mass concentrations in the three groups of particle sizes were not exactly the same.

The comparison of the 2f peak-to-peak error exponential fitting functions corresponding to three different sizes of quartz sand particles shown in Figure 4 and Figure 5 demonstrated different t-values for these functions. The t-values gradually increased with particle size, which was consistent with Eq. 10. It indicated that at a constant mass concentration of the same-material particles, the 2f signal error increased with the decrease of average particle size. The reason for this phenomenon was that for the particles with the same mass concentration, under the same action distance with the laser beam, the smaller the particle size, the stronger the extinction effect. Therefore, the laser transmittance and the peak-to-peak value of the 2f signal were also smaller, and the NO concentration error was more significant.

The relationship between the 2f peak-to-peak errors of NO and the mass concentration and particle size of quartz sand could be obtained from the error exponential fitting functions for quartz sand with three different particle sizes results are shown in Figure 6. For quartz sands with three particle sizes, the number of particles obeyed normal size distributions. Therefore, the median values of 65, 101, and 120 μm were taken as the representative ones of the particle size range. It can be seen from Figure 6 that there were some differences in the exponential fitting function of the 2f peak-to-peak error caused by different particle sizes of quartz sand. When the mass concentration of quartz sand was constant, the 2f peak-to-peak error of NO increased rapidly with the decrease of particle size, which is also consistent with Eq. 10.

FIGURE 6
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FIGURE 6. Relationship between the 2f peak-to-peak error of NO and the quartz sand mass concentration and size.

Based on the error exponential fitting function of quartz sand with three particle sizes, the mass concentration of quartz sand was changed to make it different from the value in the error exponential fitting function. The changed mass concentrations are shown in Table 1. The 2f peak-to-peak error caused by them was measured again. The 2f peak-to-peak error was corrected with the error exponential fitting function obtained above, and the correction result is shown in Figure 7. Among them, the black line corresponds to the quartz sand of 54–76 μm, the blue line corresponds to the quartz sand of 97–105μm, and the red line corresponds to the quartz sand of 105–135 μm. The square represents the 2f peak-to-peak error before correction, and the circle represents the corrected value 2f peak-to-peak error. The corrected 2f peak-to-peak errors were all less than 0.8%, indicating that the correction effect was good.

TABLE 1
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TABLE 1. Mass concentration of three particle sizes of quartz sand.

FIGURE 7
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FIGURE 7. 2f peak-to-peak errors and correction results.

To verify the applicability of the above conclusions to fly ash samples, we carried out the same experiments using real flue fly ash produced by a coal-fired power plant. The mass concentration of flue fly ash produced by domestic coal-fired power plants is usually between 10 and 20 g/m3. The size range of fly ash particles used in the experiments was 10–200 μm. Similar to the quartz sand experiments described above, five fly ash mass concentrations were selected. The NO 2f signals corresponding to different mass concentrations were recorded, and the exponential function fitted the 2f peak-to-peak error data of NO. The fitting result shown in Figure 8 reveals the value of R2 equal to 0.995.

FIGURE 8
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FIGURE 8. Effect of fly ash with particle sizes in the range of 10–200 μm on the NO 2f signal. (A) 2f signal with removed background. (B) Exponential fitting function of 2f peak-to-peak error.

The 2f signals of NO were measured for five volume fractions of 2 × 10–5, 4 × 10–5, 6 × 10–5, 8 × 10–5, and 1 × 10–4. The relationship between the 2f peak-to-peak value and the volume fraction of NO was obtained by linear fitting of measurement data, as shown in Figure 9. It can be seen from Figure 9 that the 2f peak-to-peak value and the NO volume fraction satisfied a linear dependence, and the linearity R2 reached 0.999.

FIGURE 9
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FIGURE 9. Relationship between 2f signal and volume fraction of NO.

To verify the accuracy of the determination of NO concentration using the described error correction method, the fly ash mass concentrations different from the five mass concentrations present in Figure 8 were selected. The values of these mass concentrations were 1.87, 3.95, 7.95, 15.8, and 18.26 g/m3. The peak-to-peak value of the NO 2f signal was recorded at each fly ash mass concentration, and the NO concentration was calculated using the calibration function. After that, the NO concentration was corrected by Eq. 11 and using the 2f peak-to-peak error exponential fitting function presented in Figure 8B. The 2f peak-to-peak error and the NO concentration error caused by different mass concentrations of fly ash, together with the corrected results, are shown in Table 2. It can be seen from this table that the NO concentration error reached 54.6% at the fly ash mass concentration of 18.26 g/m3. The maximum error of NO concentration after the correction was less than 2%, which indicated an effective improvement in measurement accuracy.

TABLE 2
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TABLE 2. 2f peak-to-peak error and concentration error of NO before and after correction.

In order to compare with the method of measuring the laser reference intensity, we used a low-pass filter to filter the transmitted laser intensity to obtain the direct current (DC) signal. Then, the 2f/DC signal of NO sample gas with a volume fraction of 9.06 × 10–5 at the effect of fly ash was measured, and the results are shown in Figure 10. It can be seen that the 2f/DC signal peak value of the same NO concentration was still different at the effect of different concentrations of fly ash. The 2f/DC peak error became more significant as the fly ash concentration increased. At the same time, the 2f/DC signals of five groups of standard NO gases with volume fractions of 2 × 10–5, 4 × 10–5, 6 × 10–5, 8 × 10–5, and 1 × 10–4 were measured. The relationship between the peak value of the 2f/DC signal and the gas volume fraction was obtained by linear fitting, and the linearity was good, as shown in Figure 10B.

FIGURE 10
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FIGURE 10. 2f/DC signal of NO (A) Effect of fly ash (10–200 μm) on the 2f/DC signal. (B) Relationship between 2f/DC signal and volume fraction.

The 2f/DC peak error and the NO concentration error caused by different mass concentrations of fly ash are shown in the last two rows of Table 2. The maximum error of the 2f/DC peak value exceeded 4%, and the corresponding NO concentration error was 3.02%. It can be seen that compared with the method of measuring the laser reference intensity, the errors of the two methods were roughly equal when the mass concentration of fly ash was low. But if the mass concentration of fly ash was high, the corrected 2f peak-to-peak error was significantly smaller than the 2f/DC peak error. Therefore, without measuring the laser reference laser intensity, the WMS-2f signal could be directly corrected using the error exponential fitting function presented in the experiment.

Conclusion

In this paper, we analyzed the fly ash influence on the peak-to-peak value of the WMS-2f signal and the NO concentration. The study results are as follows: 1) The peak-to-peak value of the WMS-2f signal satisfied an exponential relationship with the mass concentration of uniformly distributed particles; 2) For the same kind of particles, different particle sizes had different effects on the peak-to-peak value of WMS-2f signal. At constant particle mass concentration, the 2f peak-to-peak error of NO was negatively correlated with the particle size. This conclusion also provided a new idea for obtaining fly ash particle size by optical techniques. The 2f peak-to-peak error and NO concentration error caused by fly ash particles were less than 2% after correction. Therefore, we could measure the exponential relationship between the 2f peak-to-peak error of NO and the fly ash mass concentration in advance. Then, the relationship was input into the calculation program of the gas concentration to introduce necessary corrections and to obtain the actual NO concentration. In conclusion, without measuring the laser reference laser intensity, the WMS-2f signal can be directly corrected by the error exponential fitting function presented in the paper. Such a procedure can effectively eliminate the fly ash influence on the flue gas concentration measurement. Obtained results provide a theoretical basis for fly ash error correction and flue gas concentration inversion in complex working environments.

Data availability statement

The raw data supporting the conclusion of this article will be made available by the authors, without undue reservation.

Author contributions

All authors listed have made a substantial, direct, and intellectual contribution to the work and approved it for publication.

Funding

The study was supported by the National Key R&D Program Intergovernmental International Science and Technology Innovation Cooperation Project (2019YFE0109700), the Science and Technology Project of Guangdong Province (2020A0505140001), the Natural Science Foundation of Guangdong Province-Outstanding Youth Project (2021B1515020071), the Fok Ying Tung Education Foundation 17th Foundation for Young Teachers in Higher Education (171,047), and Innovation and Technology Commission (MHP/049/19), Hong Kong SAR, China.

Conflict of interest

JM is employed by Cntest Intelligent scien-tech Co., LTD.

The remaining authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.

Publisher’s note

All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article, or claim that may be made by its manufacturer, is not guaranteed or endorsed by the publisher.

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Keywords: TDLAS, wavelength modulation, particles, extinction effect, NO concentration, error correction

Citation: Guo S, Yang Y, Shao G, Li Z, Ren W, Mo J, Lu Z and Yao S (2022) Correcting the light extinction effect of fly ash particles on the measurement of NO by TDLAS. Front. Phys. 10:1020376. doi: 10.3389/fphy.2022.1020376

Received: 16 August 2022; Accepted: 31 August 2022;
Published: 03 October 2022.

Edited by:

Yufei Ma, Harbin Institute of Technology, China

Reviewed by:

Zhenzhen Wang, Xi’an Jiaotong University, China
Weiguang Ma, Shanxi University, China

Copyright © 2022 Guo, Yang, Shao, Li, Ren, Mo, Lu and Yao. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

*Correspondence: Shunchun Yao, epscyao@scut.edu.cn

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