Acta Polytechnica https://doi.org/10.14311/AP.2025.65.0177 Acta Polytechnica 65(2):177–187, 2025 © 2025 The Author(s). Licensed under a CC-BY 4.0 licence Published by the Czech Technical University in Prague PHOTOGRAMMETRIC IMAGE PROCESSING AND COMPARISON OF EXPERIMENTAL RESULT WITH LASER DIFFRACTION AND THE PDA METHOD Adam Huněk∗, Ondřej Bartoš Czech Technical University in Prague, Faculty of mechanical engineering, Department of Energy engineering, Technická 4, 166 07 Prague, Czech Republic ∗ corresponding author: adam.hunek@fs.cvut.cz Abstract. Optical methods have been established as a standard tool for aerosol size measurement. The aim of this paper is to compare the results of two commercial optical instruments based on Phase Doppler Anemometry (PDA) and Laser Diffraction (LD) with an in-house optical photogrammetric measurement method. For the purpose of this comparison, a new in-house image processing procedure was developed with the use of a MATLAB script. The accuracy of the method was tested on several calibration particle samples as well as on PDA and LD commercial instruments. The analysis of the measurements with calibration standard particles was done using the Bias-Variance decomposition method. All three methods were tested on the polydisperse sand particle sample. The results are applicable to determine the benefits and drawbacks of these methods in their application to the broader field of aerosol technology. Keywords: Light scattering, phase Doppler anemometry, photogrammetry, image analysis, Otsu method, automatic thresholding. 1. Introduction For the evaluation of the size distribution of polydis- perse particle systems, certain optical methods have been established as standard diagnostic tools. In many cases of measuring the droplet size, these methods remain the only feasible means [1]. The motivation for this study arose from the analysis of liquid sprays and the study of liquid film breakup in steam tur- bines at transonic flow. In this scenario, droplets form on the trailing edge and are further accelerated to the bulk velocity of the steam flow. The accelerated droplets subsequently hit the rotating blades, caus- ing erosion. The entire process contains the liquid film breakup, formation of droplets, and final flow in the carrier gas; these phenomena can be observed using various optical methods. Photogrammetry (also known as the shadowgraph imaging technique) plays an important role in observing the liquid film breakup and droplet acceleration. Alongside photogrammetry, Phase Doppler Anemometry (PDA) and light diffrac- tion methods are used to measure the final aerosol (wet steam) flow. Moreover, PDA can also be used to measure the velocity at specific positions [2]. Because photogrammetry is applied at the beginning of the droplet formation process (focused on the blade’s trail- ing edge), and the other two optical methods are used when the droplet formation process is complete, it is useful to identify the overlap between these methods. The goal of this paper is to compare all three methods as applied to monodisperse particles of 10, 15, 20, 30, 40, and 80 µm. A new in-house image processing procedure was developed for droplet size evaluation using a photogrammetric method based on the image obtained with a rapid exposure time. The MATLAB development environment was used. For practical ap- plications, a test measurement was performed with a two-phase water nozzle. This nozzle is used in the experiment, where the nozzle generates water droplets, which subsequently saturate the neighbouring air. To set the required condition of the mixture, an exact understanding of the distribution of water droplets from the nozzle is necessary [3]. These results may then be generalised for similar situations, ultimately determining the measurement limitations of all the methods used. For this paper, the experiment was conducted in ambient air and open environment. A similar method for aerosol size evaluation using image analysis was developed by Kashdan et al. [4]. This method is based on the evaluation of the diameter of the object by segmenting it with a specified thresh- old. The experimental setup consisted of a 12-bit CCD camera (PCO Sensicam) with a microscopic optical lens, providing a resolution of 0.7 µm/pixel. Illumination was provided by an infrared diode laser beam, which was diverged at a maximal angle with two prisms, and subsequently diffused with an opal glass lens to ensure even illumination of the photo. This paper focusses primarily on calibrating the depth of field with a Patterson globe and then determining the acceptable depth of field, derived from the linear calibration of the uncertain “halo area”. The sensi- tivity of threshold determination decreases with the diameter of the object. Moreover, as the sensitivity decreases, it is necessary to ensure a sufficient differ- ence between the background and object intensities. 177 https://doi.org/10.14311/AP.2025.65.0177 https://creativecommons.org/licenses/by/4.0/ https://www.cvut.cz/en Adam Huněk, Ondřej Bartoš Acta Polytechnica Subsequently, a measurement was performed on a noz- zle, and the comparison with a PDA measurement showed good agreement. Among the published papers, comparisons of im- age analysis with other optical methods are very rare. Sijs et al. [5] compared laser diffraction, phase Doppler anemometry, and image analysis for several nozzles with an expected droplet diameter range of 150 µm to more than 550 µm. They found that larger droplets cause greater deviations in the evaluation of these methods. However, all methods are reliable for droplets up to approximately 400 µm. The main dis- advantages of each method were identified. While the laser diffraction method is straightforward, it can inac- curately evaluate the increased distribution of smaller droplets as a result of their lower velocity, which leads to an increase in their concentration within the mea- surement volume. This effect has to be taken into account and the measurement has to be performed in a sufficiently large volume to avoid small particles accumulating in the measuring laser beam. Phase Doppler anemometry evaluation can be affected by air bubbles present in the droplets, which can then be falsely evaluated as smaller droplets. Herbst [6] compared the three optical methods for agricultural sprays, with droplet diameters ranging from approx- imately 100 to 500 µm, and found variations in the results of the individual methods that increased with larger droplet sizes. De Cock et al. [7] developed a high-speed imaging method and compared it with phase Doppler anemometry in ISO reference nozzles with droplet diameters ranging from 40 to 1 300 µm. The results, again, demonstrated comparable conclu- sions for smaller droplets, along with variations for larger ones. The imaging method tended to measure a similar Dv50, a larger Dv90, and a smaller Dv10 compared to the PDA. Kashdan et al. [8] developed a digital image analysis technique and compared it to PDA on a pressure-swirl atomiser for fuel droplets with diameters of 5 to 30 µm, finding slight differences in D10 (5 %) and D30 (3 %). The digital image analy- sis technique was able to detect large, non-spherical droplets that the PDA device could not detect. Kash- dan et al. [9] then used the digital image analysis tech- nique in a high-speed two-phase flow, using a pulsed laser for particle illumination with diameters ranging from 10 to 30 µm and velocities of up to 50 m s−1, and compared it with PDA measurements. Both meth- ods were highly compatible for objects larger than 25 µm. In recent years, comparisons of PDA and high- speed camera measurements of droplets from a water nozzle have been published, showing good agreement between the two methods [2]. Most of these published papers focus on distri- butions with droplets greater than 100 µm or those larger than 400 µm, which are often used in agricul- ture. The aim of this paper is to use samples with known monodisperse size distributions to calibrate the developed photogrammetric method and compare Figure 1. The detected object with the intensity values of the pixels at its axis. it to those of PDA (Dantec Dynamics) and Spraytec (Malvern Panalytical Ltd.). Subsequently, all of these methods are compared using non-monodisperse distri- butions for samples with particles ranging from 10 to 150 µm and a two-phase nozzle. This article is the culmination of a long-term research at the Depart- ment of Energy Engineering at CTU Prague on the identification of polydisperse systems. Partial results were recently published, for example, by Hunek [10]. The presented article also provides a complete set of experimental data and their processing. 2. The principle of image analysis methods for aerosol size measurement Most image analysis methods for aerosol size measure- ment rely on capturing images with a short exposure time and a quick flash, typically in the order of mi- croseconds, from a diode or laser, to capture rapidly moving objects. In the resulting greyscale image, the intensity distribution function theoretically has two peaks, representing pixels that clearly belong to the background and the object groups. However, there are many “uncertain” pixels that cannot be clearly determined. The main challenge of image analysis methods is to automatically determine whether these pixels are part of the object or background groups. An example of a detected aerosol is shown in Fig- ure 1. The blue line represents the pixel intensity values along the horizontal axis of the aerosol. There is a well visible transition area between the object and the background (the “halo area”) reported by Kash- dan et al. [4], as well as light reflection at the centre of the aerosol. One possible method to segment these pixels is thresholding such as OTSU segmentation. To eliminate this uncertainty and achieve a reliable measurement method, a calibration is necessary. 178 vol. 65 no. 2/2025 Photogrammetric image processing and comparison of . . . 2.1. OTSU segmentation The photogrammetric method proposed in this paper is based on the OTSU segmentation of the object from the background, as proposed by Otsu [11]. This method can determine the threshold automatically and has the advantage of being fast and straightfor- ward. The OTSU method uses a greyscale image histogram and attempts to find the borderline be- tween the background and object pixels. The max- imum value of between-class variance is used to get the optimal threshold k∗ as described by the following equation: σ2 B (k∗) = max 1≤k