The protein cloud-point temperature (TCloud) is a known representative of protein–protein interaction strength and provides valuable information during the development and characterization of protein-based products, such as biopharmaceutics. A high-throughput low volume TCloud detection method was introduced in preceding work, where it was concluded that the extracted value is an apparent TCloud (TCloud,app). As an understanding of the apparent nature is imperative to facilitate inter-study data comparability, the current work was performed to systematically evaluate the influence of 3 image analysis strategies and 2 experimental parameters (sample volume and cooling rate) on TCloud,app detection of lysozyme. Different image analysis strategies showed that TCloud,app is detectable by means of total pixel intensity difference and the total number of white pixels, but the latter is also able to extract the ice nucleation temperature. Experimental parameter variation showed a TCloud,app depression for increasing cooling rates (0.1–0.5 °C/min), and larger sample volumes (5–24 μL). Exploratory thermographic data indicated this resulted from a temperature discrepancy between the measured temperature by the cryogenic device and the actual sample temperature. Literature validation confirmed that the discrepancy does not affect the relative inter-study comparability of the samples, regardless of the image analysis strategy or experimental parameters. Additionally, high measurement precision was demonstrated, as TCloud,app changes were detectable down to a sample volume of only 5 μL and for 0.1 °C/min cooling rate increments. This work explains the apparent nature of the TCloud detection method, showcases its detection precision, and broadens the applicability of the experimental setup.
Quantification of protein–protein interactions can be used to assess the colloidal stability of biopharmaceutical formulations  or to identify environmental conditions which induce desired phase transitions for separation techniques  and 3-D structure determination of proteins . One of the empirical parameters to quantify protein–protein interactions is the protein cloud-point temperature (TCloud) . This temperature represents the point at which a protein solution displays liquid–liquid phase separation (LLPS). The temperature at which LLPS is detected is mainly determined by protein–protein interaction strength, where higher TCloud values are found for strong attractive forces and low TCloud values for weaker attractive forces . The accompanying increase in solution turbidity when LLPS occurs is a characteristic that is often exploited for TCloud measurements by means of spectroscopic methods [6, 7], light scattering detection [5, 8,9,10,11,12,13], or imaging and microscopy [14,15,16,17,18].
Preceding work presented a novel experimental setup to detect TCloud in a high-throughput manner (60 samples per experiment) using a low sample volume (24 μL) . To cover a wide range of protein–protein interaction strengths, the experimental setup included a cryogenic device. This allowed for TCloud detection at sub-zero temperatures in addition to above zero temperatures. Despite the confirmed robustness of the developed method, a comparison with literature data obtained with light scattering showed that only an apparent TCloud (TCloud,app) is detectable with the developed experimental setup, as normalized values showed similar trends but the absolute TCloud values were different. Thus, the results obtained with the developed method were found to be robust and precise, but the apparent nature of TCloud rendered the absolute values meaningless for inter-study comparison.
To ensure the usability of historic and future TCloud data across the field to further elucidate protein phase behavior, it is of importance to understand TCloud,app and how the employed experimental setup influences its apparentness. Previously proposed sources that cause TCloud,app were the differences in cooling rate, sample volume, and the employed detection approach. Due to the limited information available in the literature to fully evaluate the influence of these experimental parameters on TCloud detection with any experimental setup, a conclusive reason for the observed apparentness is lacking. The work presented in this study aims to identify the source of the observed TCloud,app.
The combination of a cryogenic device and an automatic image acquisition system allows for monitoring the protein solution behavior at sub-zero degrees Celsius, which was applied for the quantification of (weakly) attractive protein–protein interactions, represented by sub-zero TCloud values. Various image processing strategies are available to highlight image objects or image characteristics for image analysis purposes, such as segmentation, defocusing, and smoothing . Work reported by other research groups that employ visible light-based methodologies to determine TCloud extract the mean gray level (MGL) , light intensity , or manually determine clouding by means of microscopy [15, 16]. The methodology developed in our lab employs the total intensity difference (TID) of images, where each image is compared to the starting image to detect change over time . The current work investigates the effects of different visible light image analysis strategies and determines whether differences in absolute TCloud,app values occur as a result of the analysis strategies. In addition, other temperature points of interest may arise when protein solutions are cooled to sub-zero temperatures, such as the solution freeze point, the solution thaw point, or the solutions’ ice nucleation temperature. Knowledge and understanding of these temperature points can be applied in protein formulation research, as it aids the design of optimal storage procedures for frozen or freeze-dried products [20,21,22,23]. Such temperature points may already be present in the captured image-based data but currently applied image analysis strategies are not able to extract this information.
In the scope of this research, three image analysis strategies were used to investigate the effects on TCloud,app determination and to explore a broader application of the developed experimental setup. This included two previously reported image analysis strategies for TCloud detection, namely MGL  and TID . As the camera used in this work captures color images, the mean red, blue, and green color pixel values were explored in addition to the gray color level. The third image analysis strategy was based on binarized images, where images are processed to solely contain black and white pixels using different threshold values.
The experimental parameters which were investigated during this study are the cooling rate and sample volume. The cooling rate was varied between 0.1 °C/min and 0.5 °C/min, with increments of 0.1 °C/min, where 0.1 °C/min is the slowest cooling rate of the employed cryogenic device as well as the smallest step size. This relatively narrow range was selected to investigate whether small cooling rate increments already affect the TCloud,app absolute value and, in parallel, to provide information on the detection sensitivity of the experimental setup. In addition, a maximum of 0.5 °C/min was chosen, as faster cooling rates may lead to deviating temperatures between the set and measured temperature during the course of an experiment. The sample volume was varied between 5 μL and 24 μL, where 24 μL was the original sample volume described in the preceding work. A reduction in sample volume was preferred to capture not only the effects of sample volume changes but also to further miniaturize the experimental setup, which is a beneficial characteristic for high-throughput screening applications due to reduced material usage.
To summarize, the work presented in this study includes the investigation of three different image analysis strategies and two experimental parameters. It was aimed to understand the source of TCloud,app and explore the information content of the generated data beyond TCloud detection.
Materials and methods
A 0.6 molar sodium phosphate buffer at 8 different pH values (5.8, 6.0, 6.3, 6.5, 6.8, 7.2, 7.4, and 7.8) was employed. The buffer components were sodium di-hydrogen phosphate (monohydrate; Merck KGaA, Darmstadt, Germany) and di-sodium hydrogen phosphate (anhydrous; VWR, Radnor, PA, USA). After preparation, and after two weeks of storage, the buffer solutions were filtered over a 0.2 µm Supor®-200 filter (Pall Corporations, Port Washington, NY, USA). This buffer system was chosen to use literature data provided by Taratuta et al.  as a validation set. The pH value was set with a five-point calibrated pH meter (HI-3220, Hanna® Instruments, Woonsocket, RI, USA), which was equipped with a SenTix® 62 pH electrode (Xylem Inc., White Plains, NY, USA). The pH value of all buffers was checked throughout the study and was maintained within ± 0.05 pH unit of the desired pH values.
Protein solution preparation
A 90 g/L hen-egg white lysozyme (Hampton Research, Aliso Viejo, CA, USA) solution was prepared on the day of experimentation. The required amount of protein was dissolved in the respective buffer. The solution was run over a 0.2 µm Supor® polyethersulfone (PES) pre-syringe filter (Pall Corporations, Port Washington, NY, USA). The protein stock concentration was measured with a NanoDrop™ 2000c UV–Vis spectrophotometer (Thermo Fischer Scientific, Waltham, MA, USA), using an extinction coefficient of 22 Lg−1 cm−1. To remain within the detection range of the spectrophotometer, 1:10 dilutions were prepared for concentration measurements. All prepared protein solutions were used within 7 h and stored at room temperature until use.
Cloud-point temperature measurements
The protein cloud-point temperature was determined using the setup as described by Klijn et al. . This setup employs a cryogenic device (EF600M 105, Grant Instruments, Cambridgeshire, UK) and a GoPro Hero4 camera (GoPro Inc., San Mateo, CA, USA) for image acquisition. The following GoPro settings were used to minimize image fluctuations: ProTune white balance was set to 4000 K, ISO limits were set to 200 (minimum and maximum), and EV Comp was set to − 2.0. For varying cooling rates, the number of seconds per image was adjusted to match the images per degrees Celsius as closely as possible. This was done to keep the temperature sampling rate comparable between different cooling rates. In addition, this reduces the amount of data for slower cooling rates as these experiments run for a longer period of time. For example, an experiment running from 15 to − 40 °C with a cooling rate of 0.1 °C/min results in 3300 images for a 10 s per image setting, which translate to an image every 0.02 °C. A 0.5 °C/min cooling rate results in 660 images for a similar setup, which is 0.08 °C per image. By adjusting the frame rate to 30 s per image for a 0.1 °C/min cooling rate, one obtains 1100 images, which translates to 0.05 °C per image. Thus, the temperature sampling rate is more comparable and the amount of data is decreased. However, the employed GoPro Hero4 solely allows a setting of 1, 5, 10, 20, 30, or 60 s per image, which is why an exact temperature sampling match could not be realized. The employed seconds per image for a cooling rate of 0.1 °C/min, 0.2 °C/min, 0.3 °C/min, 0.4 °C/min, and 0.5 °C/min, were 30, 10, 10, 10, and 10, respectively. This translates to an image every 0.05 °C, 0.03 °C, 0.05 °C, 0.07 °C, and 0.08 °C, respectively.
During TCloud,app measurements, the temperature was set to decrease from 15 °C to − 40 °C. An overview of the employed parameters per experiment can be found in Table 1. After a holding time of 1 min at − 40 °C, a heating rate of 3 °C/min was used to return to a temperature of 20 °C. Heating was not monitored as it was shown in previous work that TCloud,app detection with the employed setup is more reliable during cooling than during heating . All samples were prepared in 96-well crystallization plates (MRC Under Oil 96 Well, SWISSCI AG, Neuheim, CH) and sealed with Duck® Brand HD Clear sealing tape (ShurTech® Brands, LC., Avon, OH, USA) prior to measurements to prevent evaporation. All samples were measured as six technical replicates, with which the median (as a measure of central tendency) and median absolute deviation (as measure of spread) of TCloud,app were calculated. Calculation of the median and median absolute deviation TCloud,app was performed after outlier detection. A data point was considered an outlier based on Tukey’s fences , employing a whisker length of 0.75 times the interquartile range. For comparison to literature data, the median protein cloud-point temperatures were normalized by means of min–max normalization.
All data processing was established in the MATLAB programming environment (version R2018b, The MathWorks Inc., Natick, MA, USA). Data smoothing was performed with a moving mean window of 5% of the total number of data points. Due to insufficient data quality, the experiment with a cooling rate of 0.3 °C/min and a sample volume of 24 µL was smoothed with a moving mean window of 2.5%. Different image analysis strategies were applied to this work. The image analysis strategy referred to as total intensity difference (TID), indicates that image analysis was performed as described in Klijn et al. . In addition to TID, two other strategies were employed, namely the mean color level and the total white pixel count, which will be explained in the following sections.
Mean color levels
The mean color value was defined as the mean pixel value of the cropped well image. This value was extracted for each color (red, green, and blue) from the raw color image and the gray image (obtained with the MATLAB function rgb2gray). This was done to evaluate the applicability of the image analysis approach presented in other work, where the mean gray value of images was used to detect TCloud.
Total white pixel count
To obtain the number of white pixels in an image, each cropped well image was transformed into a binary image from which the total sum of white pixels was calculated. Conversion of a raw color image to a binary image requires the definition of a white level. The white level determines which pixels will become white in the binary image, thereby influencing the total white pixel count. Five different white levels were investigated, three arbitrarily predefined levels (0.50, 0.75, and 0.85) and two data-dependent levels that were set per microtiter plate well image. The two data-dependent levels included (1) a white level calculated with MATLAB function graythres (employing Otsu’s method to find the optimal separation value ) based on the first image of each well (t0) and (2) a white level set to the mean intensity of the gray image of the first image of each well (t0). Thus, the data-dependent white levels are defined for each well customarily, while the predefined arbitrary levels are set for all wells equally. Two variables were extracted from the obtained data, namely TCloud,app and the ice nucleation temperature (TNuc). TCloud,app was defined as the minimum number of total white pixels, which is comparable to the TID definition, and TNuc was defined as the maximum gradient where the total white pixel count increased.
A UV-Star® µClear® half-area 96-well plate (Greiner Bio-One, Kremsmünster, AU) was used to perform a single run on the cryogenic device which was monitored with a thermographic camera (FLIR Ax5, FLIR Systems, Wilsonville, OR, USA). A framerate of 25 frames per second was used and temperature data were extracted with the software FLIR Tools (FLIR Systems, Wilsonville, OR, USA). The measurement was conducted with demineralized water (50 µL) and the plate was sealed with Duck® Brand HD Clear sealing tape. The temperature gradient was set to run from 20 to − 20 °C, with a holding time of 2 min every 5 °C. The thermographic camera was not calibrated or optimized for the atmospheric settings. Therefore, only the relative temperature change from the starting point (t0) was determined. This allowed for the comparison of the thermographic data with temperature data extracted from the cryogenic device software.
Results and discussion
Image analysis strategies
To evaluate the influence of different image analysis strategies on TCloud,app detection, three image analysis strategies were performed using the same data set. The image analysis strategies include the TID, the total number of white pixels (TWP), and the evaluation of the mean gray, red, blue, and green level (MGL, MRL, MBL, and MGrL, respectively). Figure 1 shows exemplary data for TID, TWP (using a white level of 0.50), and MGL using data of three samples, namely at pH 5.8, pH 6.8, and pH 7.8 with a sample volume of 20 µL and a cooling rate of 0.5 °C/min. Here, the left y axis indicates the respective variable and the right axis indicates the measured temperature by the cryogenic device during the measurement.
Total intensity difference (TID)
The TID was extensively discussed in previous work  and will therefore be only briefly described here. The TID is a measure of dissimilarity between two images, which increases when a solution moves from transparent to turbid. The relatively sharp increase in TID observed in Fig. 1a as the temperature decreases was identified as the TCloud,app. More specifically, TCloud,app was defined as the temperature at which the sharp increase flattened, which represents the point at which solution clouding is concluded. This was observed in the data shown in Fig. 1a at approximately t = 2600 s for the sample with pH value 7.8 (black), at t = 3200 s for pH 6.8 (brown), and at t = 4200 for pH 5.8 (yellow).
Total number of white pixels (TWP)
The TWP analysis requires a definition of the white level to separate black and white pixels in each image. In this work, five different white level definitions were evaluated, namely 0.50, 0.75, 0.85, and two data-dependent levels (MATLAB function graythres value and mean gray intensity based on the first cropped well image). Figure 1b only shows three exemplary results for data obtained with the 0.50 white level, as this level was found to include two distinct signal changes and the results obtained with other white levels did not result in any significant signal changes or any additional information. Data for the exemplary samples obtained with the other white levels can be found in the Supplementary Material, Figure S1. In addition, to visualize the lack of information available in the images obtained by the other white levels, exemplary images at 15 °C, TCloud,app, and − 40 °C can be found in the Supplementary Material in Figure S2.
The first significant signal change in Fig. 1b, represented by a decrease in TWP, corresponds to the increase in TID data seen in Fig. 1a at approximately t = 2600, 3200, and 4200 s for pH 7.8, 6.8, and 5.8, respectively (indicated by the vertical line in the corresponding color). This means that TCloud,app is also detected by means of counting white pixels in a binary image. Upon visual inspection of images, it was found that the TWP decrease is caused by a decrease in light reflection by the sample as the sample becomes turbid. In addition to the decrease in TWP at TCloud,app, a distinct increase in TWP is seen at a later time point, as the temperature further decreases. Here, a sharp increase in TWP is observed at around t = 5000 for all pH values. Based on data obtained for demineralized water samples included in each data series, the observed TWP increase was attributed to the ice nucleation temperature (TNuc) of the supercooled samples. The average TNuc of these water samples was − 30.8 ± 2.2 °C (see Supplementary Material, Table S1). The average TNuc is in line with literature values of supercooled water droplets, where TNuc values down to -32 °C were reported for droplets with a diameter of 1000 µm . For reference, the sample volume employed in this work would roughly translate to a droplet diameter of 2000–5000 μm, assuming a perfect sphere. Even though a TNuc was identifiable with TWP data using a 0.50 white level, a trend for TNuc values was not found among the measured protein samples (see Supplementary Material, Fig. S3). Thus, it is concluded that the sample volume and cooling rate applied in this study do not affect TNuc using the current setup. Notably, TNuc of a sample containing protein, or solely the buffer solution (blank), was identified by means of a TWP increase, while water samples showed a decrease in white pixels upon freezing. An example of these opposite trends can be found in the Supplementary Material, Fig. S4. Visual image inspection showed that the TWP increase for protein samples was due to the formation of white-colored ice, while water samples showed gray ice formation, a color comparable to the turbidity seen during protein solution clouding.
Mean color levels
Mean color levels were included in this study, as work by Pincemaille et al. applied extracted MGL to determine TCloud. Figure 1c shows exemplary MGL data over the course of a measurement with the setup developed in our lab. The vertical dashed lines in Fig. 1c show the position of TCloud,app as detected in Fig. 1a. The corresponding observed signal changes in Fig. 1c are a slight increase in MGL for pH 7.8 (black) and two slight minima for pH 5.8 (yellow) and pH 6.8 (brown). These inconsistent changes in MGL have an absolute value of approximately 1–10 (depending on the pH value), while Pincemaille et al. reported absolute changes of the MGL with a value of 100. Thus, in contrast to the results presented by Pincemaille et al., the MGL data obtained in this work did not contain enough discriminatory information for the extraction of a consistent signal change that corresponded to TCloud,app. All other mean color levels (red, green, and blue) also did not contain discriminatory information. Examples for the red, blue, and green mean color level can be found in the Supplementary Material, Figure S5. Exemplary images for each color level at 15 °C, TCloud,app, and − 40 °C can be found in the Supplementary Material as well, in Figure S2. The inability to transfer the MGL image analysis protocol as described by Pincemaille et al. to another camera-based setup illustrates a potential general hardware dependency of image analysis strategies to detect TCloud.
The TCloud,app results obtained with TID and TWP image analysis were compared to each other to quantify their similarity in absolute TCloud,app values. Figure 2 shows TCloud,app values determined with the TID image analysis strategy (x axis), and with the TWP image analysis strategy (y axis) for all cooling rates, sample volumes, and pH values. All TCloud,app values obtained with the TWP image analysis strategy can be found in the Supplementary Material, Table S3. The total root-mean-squared error (RMSE) of 6.4 °C, the average RMSE of 0.7 °C, and the R2 of 0.998 indicate there is a relatively small difference between the two image analysis strategies for TCloud,app detection. One-way ANOVA analysis resulted in an F value of 0.07 and a p value of 0.80, reflecting an insignificant difference between TCloud,app values obtained with the TID and TWP image analysis strategies (see Supplementary Fig. S6). Nevertheless, considering that MGL was not readily transferable between different setups, a collaborative initiative to evaluate the performance of multiple image analysis strategies in combination with different camera-based experimental setups would be of interest to promote the development of robust and transferable image analytical approaches to facilitate relatively simple and high-throughput TCloud detection.
In addition to several image analysis strategies, two experimental parameters were varied in this work, namely the cooling rate and sample volume. The cooling rate was varied as previous work showed TCloud,app depression for increasing cooling rate (an increase from 0.5 °C/min to 2.5 °C/min and 10 °C/min ). In this work, it was investigated for which cooling rate increment the decrease in TCloud,app could already be detected. The limit and effect of sample volume reduction were investigated as previous work proposed sample volume as a possible factor influencing absolute TCloud,app values. In addition, sample volume reduction allows for evaluating the miniaturization potential, which benefits high-throughput screenings due to a reduced material requirement. The results for both experimental parameters are presented in Fig. 3.
Figure 3a shows the median TCloud,app per pH value for different cooling rates (0.1–0.5 °C/min). All median TCloud,app values can be found in the Supplementary Material, in Table S4. The last data point (pH 7.8) in the 0.2 °C/min cooling rate data series (dark brown) is considered an outlier. This was attributed to a sample preparation error, as a comparable TCloud,app value was found for the data point at pH 6.5 in the same data series. Disregarding this outlier, the results presented in Fig. 3a show that a cooling rate change between 0.1 °C/min and 0.5 °C/min resulted in a consistent decrease of TCloud,app for faster cooling rates. To quantify this observed TCloud,app decrease in Fig. 3a, the average TCloud,app difference between each data point per cooling rate was calculated with respect to the data obtained with a cooling rate of 0.1 °C/min. These average temperature differences are depicted in Fig. 3b, where the error bars indicate the standard deviation of TCloud,app differences obtained with all pH values per data series. Figure 3b indicates that a cooling rate increase from 0.1 °C/min to 0.3 °C/min already results in a reduction of TCloud,app by 0.9 ± 0.8 °C. Overall, an absolute average TCloud,app decrease up to 3.2 ± 0.7 °C was found for increasing the cooling rate from 0.1 °C/min to 0.5 °C/min, respectively. One-way ANOVA analysis resulted in an F value of 1.33 an p value of 0.27 upon analyzing the data obtained with a cooling rate of 0.1 °C/min and 0.5 °C/min (see Supplementary Fig. S6). This was considered a significant change as it reflects a greater difference in variance compared to the variance obtained between the image analysis strategies (F value of 0.07 and p value of 0.80) and the high precision of the TCloud,app data (MAD of 0.3 °C for all 40 data points).
The resulting median TCloud,app values for sample volumes varying from 5 to 24 μL are presented in Fig. 3c. Here, it is shown that smaller sample volumes led to higher TCloud,app values. The effect of higher TCloud,app values for lower sample volumes was found to be consistent for all pH values. Similar to the cooling rate experiment, the average TCloud,app difference for each sample volume data series was calculated, with respect to the lowest sample volume (5 μL). These differences are depicted in Fig. 3d. A decrease in the TCloud,app value was already detectable for the first sample volume increase from 5 to 10 µL, represented by an average TCloud,app difference of 1.6 ± 1.0 °C. The largest difference was seen between a sample volume of 5 µL and 24 µL, with an average absolute TCloud,app difference of 5.5 ± 1.4 °C. The difference in TCloud,app between a sample volume of 5 μL and 24 μL was considered significant based on ANOVA results, showing a F value of 3.33 and p value of 0.09 (see Supplementary Material S6). Despite the TCloud,app differences based on sample volume, a detection limit was not reached. Thus, this experiment demonstrated that even a sample volume of as low as 5 μL can be used with the employed experimental setup for a reliable and accurate TCloud,app detection.
TCloud,app values obtained for all cooling rates, and sample volumes were validated by means of comparison to literature data from Taratuta et al. . The RMSE was used to quantify the relative difference between the TCloud,app obtained in each data series, employing both TWP and TID, and literature TCloud data, where low RMSE values indicate a high similarity. The resulting RMSE values for varying cooling rates and sample volumes are presented in Fig. 4a, b, respectively.
With the exception of the data obtained with a cooling rate of 0.2 °C/min, all RMSE values are below 0.08. This is considered a low RMSE value, as all data are normalized between 0 and 1. The high RMSE for 0.2 °C/min is due to the outlier at pH 7.8, as discussed in Sect. 3.2.1. The relatively low RMSE between each data series and literature data confirms that all tested cooling rates, sample volumes, and image analysis strategies result in a similar data variance as a function of the sample pH value. Based on this data, it was concluded that the investigated variables are not the direct source of the apparent nature of TCloud,app.
The cooling rate and sample volume experiments showed a TCloud,app depression for faster cooling rates, and higher sample volumes, respectively. Our preceding study speculated that this could be caused by camera-related insensitivity or a difference between the temperature measured by the device and the actual sample temperature . The camera-related insensitivity can no longer be considered a source, as not only the cooling rate but also a sample volume increase resulted in a TCloud,app depression. If camera-related insensitivity occurred, then lower sample volumes would be more difficult to measure with an insensitive detection, and therefore would lead to lower TCloud.app values. As this was not observed, the TCloud,app depression is attributed to the difference between the measured temperature by the cryogenic device and the actual sample temperature during the measurement. To gain insight into the temperature deviations, an exploratory measurement with demineralized water samples was performed, where the visible light camera was substituted with a thermographic camera. It should be noted that using a thermographic camera brings its own technical challenges, as calibration is required for thermographic imaging, measurements are sensitive to atmospheric factors, and new data analytical infrastructure is necessary [27, 28]. Although we are aware of these issues regarding thermographic imaging, optimization of the thermographic setup, and the subsequent data analytical workflow is considered outside the scope of this study. This exploratory experiment was solely used to confirm the existence of a temperature deviation.
The thermographic results are shown in Fig. 5. A snapshot of the thermographic measurement in Fig. 5a indicates three locations for which temperature data was extracted, namely the metal adapter (Metal, cross), the microtiter plate (Plate, plus), and a demineralized water sample (Sample, circle). In Fig. 5b, the relative temperature decrease (right y axis) for these points are plotted over the course of the experiment, alongside temperature data obtained from the cryogenic device, namely the set temperature in the software (Target) and the temperature measured during the experiment (Device). The measurement ran from 20 °C to − 20 °C, with a cooling/heating rate of 1 °C/min and a 2-min holding time every 5 °C. These holding steps were included to determine whether this would benefit temperature control.
The relative temperature decrease was the metric of choice for comparison, as the thermal camera settings were not optimized. Here, the temperatures are relative to the starting temperature of the respective measurement source. To highlight the temperature difference, the left y axis in Fig. 5b indicates the difference between the relative sample temperature (green solid line) and the relative device temperature (black solid line). Over the course of the measurement, the sample temperature deviates from the device temperature up to nearly 7 °C after approximately 3250 s (approximately 54 min). The subsequent steep increase in sample temperature (approximately at t = 3200 s and a temperature of − 31 °C) is the latent heat of fusion, which is a result of ice nucleation in the supercooled water sample. This confirms the occurrence of TNuc during experimental runs with the employed setup, as was seen in Sect. 3.1.2 for TWP image analysis strategy results.
In addition to the deviation between the sample temperature and the device temperature, a temperature deviation was seen for the metal adapter and the microtiter plate when compared to the device temperature. This indicates that the multi-layered setup as well as the samples are sources of the observed temperature discrepancy. Based on the thermographic results, it can no longer be assumed that the measured temperature by the cryogenic device is equal to the actual sample temperature. Thus, the systematic discrepancy between the measured device temperature and the actual sample temperature is the source of the apparent nature of the detected TCloud. The thermographic data shows that a 2-min holding time every 5 °C was not long enough to reach a temperature equilibrium between the device, adapter, plate, and sample for a 24 μL sample volume. Previous studies in literature do not always report on the sample volume and/or the corresponding equilibrium time, but values were found to range from 2 to approximately 30 min for a sample volume of 60–300 μL [6, 17]. Thus, it is recommended that the equilibrium time should be determined separately for different sample volumes, cooling rates, and employed cryogenic device setups. Alternatively, one could determine a TCloud,app correction factor with thermographic sample temperature data, so that one still benefits from high-throughput, low volume, and fast TCloud measurements without time-consuming intermediate equilibrium steps.
This work was performed to investigate the source of TCloud,app values of lysozyme obtained by means of a cryogenic device in combination with an automated image acquisition system to facilitate a broader understanding of experimental and data evaluation influences and to enable inter-study data comparability. For this, three image analysis strategies, five cooling rates (0.1–0.5 °C/min), and five sample volumes (5, 10, 15, 20, and 24 µL) were investigated in particular. The investigation of different image analysis strategies showed that extraction of the total white pixel count resulted in additional information compared to the previously used total intensity difference, as the total white pixel count is able to detect TCloud,app and TNuc. Faster cooling rates showed a decrease in TCloud,app, with an average absolute difference of 0.1 ± 0.4 °C up to 3.2 ± 0.7 °C. A similar trend was seen for increasing the sample volume from 5 μL to 24 μL, where the average absolute difference in TCloud,app ranged from 1.6 ± 1.0 °C to 5.5 ± 1.4 °C. The observed TCloud,app was affected by the investigated experimental variables due to a discrepancy between the measured device temperature and the actual sample temperature, which was confirmed based on a thermographic measurement. Despite sample temperature discrepancy, the precision of the employed experimental setup was shown by the ability to detect differences in TCloud,app values induced by small cooling rate increments (0.1 °C/min). Moreover, the sample volume was reduced by 80% from 24 µL down to 5 µL, which still yielded reliable results. This demonstrates that the employed experimental setup is not only capable of precise measurements, but that it is also highly sensitive. Overall, the presented work identified the source TCloud,app as well as the influence of the sample volume and cooling rate in this regard, while simultaneously miniaturizing the setup and indicating a potential application expansion of the employed experimental setup by means of a different image analysis strategy.
Agrawal NJ, Kumar S, Wang X, Helk B, Singh SK, Trout BL (2011) Aggregation in protein-based biotherapeutics: computational studies and tools to identify aggregation-prone regions. J Pharm Sci 100:5081–5095. https://doi.org/10.1002/jps
Huettmann H, Zich S, Berkemeyer M, Buchinger W (2015) Design of industrial crystallization of interferon gamma: phase diagrams and solubility curves. Chem Eng Sci 126:341–348. https://doi.org/10.1016/j.ces.2014.12.018
Calero G, Cohen AE, Luft JR, Newman J, Snell EH (2014) Identifying, studying, and making good use of macromolecular crystals. Acta Crystallogr Sect F Struct Biol Commun 70:993–1008. https://doi.org/10.1107/S2053230X14016574
Petsev DN, Wu X, Galkin O, Vekilov PG (2003) Thermodynamic functions of concentrated protein solutions from phase equilibria. J Phys Chem B 107:3921–3926. https://doi.org/10.1021/jp0278317
Broide ML, Tominc TM, Saxowsky MD (1996) Using phase transitions to investigate the effect of salts on protein interactions. Phys Rev E Stat Phys Plasm Fluids Related Interdiscip Top 53:6325–6335. https://doi.org/10.1103/PhysRevE.53.6325
Raut AS, Kalonia DS (2016) Effect of excipients on liquid-liquid phase separation and aggregation in dual variable domain immunoglobulin protein solutions. Mol Pharm 13:774–783. https://doi.org/10.1021/acs.molpharmaceut.5b00668
Boire A, Menut P, Morel MH, Sanchez C (2013) Phase behaviour of a wheat protein isolate. Soft Matter 9:11417–11426. https://doi.org/10.1039/c3sm51489g
Ishimoto C, Tanaka T (1977) Critical behavior of a binary mixture of protein and salt water. Phys Rev Lett 39:8–11. https://doi.org/10.1103/PhysRevLett.39.474
Asherie N (2004) Protein crystallization and phase diagrams. Methods 34:266–272. https://doi.org/10.1016/j.ymeth.2004.03.028
Liu C, Asherie N, Lomakin A, Pande J, Ogun O, Benedek GB (1996) Phase separation in aqueous solutions of lens gamma-crystallins: special role of gamma s. Proc Natl Acad Sci USA 93:377–382. https://doi.org/10.1073/pnas.93.1.377
Grigsby JJ, Blanch HW, Prausnitz JM (2001) Cloud-point temperatures for lysozyme in electrolyte solutions: Effect of salt type, salt concentration and pH. Biophys Chem 91:231–243. https://doi.org/10.1016/S0301-4622(01)00173-9
Muschol M, Rosenberger F (1997) Liquid-liquid phase separation in supersaturated lysozyme solutions and associated precipitate formation/crystallization. J Chem Phys 107:1953–1962. https://doi.org/10.1063/1.474547
Taratuta VG, Holschbach A, Thurston GM, Blankschtein D, Benedek GB (1990) Liquid-liquid phase separation of aqueous lysozyme solutions: effects of pH and salt identity. J Phys Chem 94:2140–2144. https://doi.org/10.1021/j100368a074
Park EJ, Bae YC (2004) Cloud-point temperatures of lysozyme in electrolyte solutions by thermooptical analysis technique. Biophys Chem 109:169–188. https://doi.org/10.1016/j.bpc.2003.11.001
Bloustine J, Virmani T, Thurston GM, Fraden S (2006) Light scattering and phase behavior of lysozyme-poly (ethylene glycol) mixtures. Phys Rev Lett 96:1–4. https://doi.org/10.1103/PhysRevLett.96.087803
Galkin O, Vekilov PG (2000) Control of protein crystal nucleation around the metastable liquid-liquid phase boundary. Proc Natl Acad Sci 97:6277–6281. https://doi.org/10.1073/pnas.110000497
Pincemaille J, Banc A, Chauveau E, Fromental JM, Ramos L, Morel MH et al (2018) Methods for screening cloud point temperatures. Food Biophys 13:422–431. https://doi.org/10.1007/s11483-018-9548-1
Klijn ME, Wöll AK, Hubbuch J (2020) Apparent protein cloud point temperature determination using a low volume high-throughput cryogenic device in combination with automated imaging. Bioprocess Biosyst Eng 43:439–456. https://doi.org/10.1007/s00449-019-02239-x
Young I, Gerbrands J, Van Vliet L (2006) Fundamentals of image-processing. vol. 72. Delft, The Netherlands: Delft University of Technology. https://doi.org/10.2493/jjspe.72.583
Singh SK, Nema S (2010) Freezing and thawing of protein solutions. In: Jameel F, Hershenson S, (eds) Formulation and process development strategies for manufacturing biopharmaceuticals. John Wiley & Sons, Inc., Hoboken, p. 625–75. https://doi.org/10.1002/9780470595886.ch26.
Fang R, Bogner RH, Nail SL, Pikal MJ (2020) Stability of freeze-dried protein formulations: contributions of ice nucleation temperature and residence time in the freeze-concentrate. J Pharm Sci. https://doi.org/10.1016/j.xphs.2020.02.014
Geidobler R, Winter G (2013) Controlled ice nucleation in the field of freeze-drying: fundamentals and technology review. Eur J Pharm Biopharm 85:214–222. https://doi.org/10.1016/j.ejpb.2013.04.014
Searles JA, Carpenter JF, Randolph TW (2001) The ice nucleation temperature determines the primary drying rate of lyophilization for samples frozen on a temperature-controlled shelf. J Pharm Sci 90:860–871. https://doi.org/10.1002/jps.1039
Tukey J (1977) Exploratory data analysis. Addison-Wesley, Reading
Otsu N (1979) A threshold selection method from gray-level histograms. IEEE Trans Syst Man Cybern 9:62–66. https://doi.org/10.1109/TSMC.1979.4310076
Dorsch R, Hacker P (1950) Photomicrographic investigation of spontaneous freezing temperatures of supercooled water droplets.
Vollmer M, Möllmann K-P (2010) Fundamentals of infrared thermal imaging. In: Vollmer M, Mollman K-P (eds) Infrared thermal imaging. Wiley-VCH Verlag GmbH & Co. KGaA, Weinheim, p. 1–72. https://doi.org/10.1002/9783527630868.ch1.
Teena M, Manickavasagan A (2014) Thermal infrared imaging. In: Manickavasagan A, Jayasuriya H (eds) Imaging with electromagnetic spectrum. Springer, Berlin Heidelberg, Heidelberg, pp 147–73. https://doi.org/10.1007/978-3-642-54888-8.
The authors would like to thank Anna Wöll and Dennis Weber for the scientific discussions during the project. This research did not receive any specific grant from funding agencies in the public, commercial, or not-for-profit sectors.
Open Access funding enabled and organized by Projekt DEAL.
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Klijn, M.E., Hubbuch, J. Influence of image analysis strategy, cooling rate, and sample volume on apparent protein cloud-point temperature determination. Bioprocess Biosyst Eng 44, 525–536 (2021). https://doi.org/10.1007/s00449-020-02465-8
- Protein stability
- Colloidal stability
- Nucleation temperature
- High-throughput screening
- Liquid–liquid phase separation