3.1. Analysis of Seasonal Effects on Vertical Track Deflection
This section presents findings from the analysis conducted over a one-year period, spanning July 2017 to July 2018 for the entire track, focusing on the inspection and data gathering activities. Specifically,
Figure 8 illustrates the average track modulus values, depicted graphically for each observed cycle. These results are aligned with the methodology outlined in the preceding sections of the article, ensuring consistency in the data analysis process. This visualization aids in understanding the variability and trends in the track modulus values across different cycles, providing insights into the structural integrity and performance of the tracks under study.
As can be seen from
Figure 8, the overall average modulus is approximately 33 MPa. The distribution of track modulus measurements and its cumulative distribution for all of the measurements is shown below in
Figure 9 for each rail side.
It can be seen from
Figure 9 that the distributions for each rail side are nearly identical as expected. YRel greater than 5.1 mm (corresponding to a modulus of 14 MPa or less) account for approximately 11% of the overall measurements. Thus, if YRel > 5.1 mm is considered soft track, then 11% of the track exhibits soft behavior. This percentage corresponds to almost 100 km of the line. Note that this is based on a 100 m average of YRel values. Local (single or multiple contiguous measurements) exceptions are handled separately.
One of the primary purposes of this study was to evaluate the seasonality effects on track support using deflection data. The track modulus distributions were developed individually for each of these cycles and are shown in
Figure 10.
Figure 10a showed (for the left rail) that the average track modulus value is nearly the same for each cycle, approximately 33 MPa, with a deflection of 3 mm. This is as expected, since seasonal effects will not affect the majority of the track, but only a subset. This is seen on the right side “tail” of the distribution, where cycle January 2018 (wet) extends further to the right. This indicates a certain percentage of modulus values larger than the dry cycles’ values. The seasonal effects can be better visualized in a cumulative distribution plot as shown in
Figure 10b.
Figure 10b shows that for the wet season (cycle Jan. 2018) a larger percentage of higher modulus values exist.
Figure 11 below shows the seasonality effects on track support. It can be seen that all three cycles had approximately 50% of their values near the expected mean of 33 MPa. This indicates they behave the same on average. However, the wet season (January) clearly has more instances of higher YRel values than the dry season results. In particular, nearly 14% of the track has a YRel > 5 mm during the wet season, which correspond to track modulus values of 14 MPa, while only 8.2–11.7% of the track exceeds 5 mm during the dry season. In addition, 3.8% of the track exceeds 7 mm (8 MPa) during the wet season, while during the dry season only 0.5–1.5% of the track exceeds that limit. This macro analysis allows for a global understanding of the seasonal effects.
Based on the results presented in
Figure 11, it is important to note that while there is some rebounding of the track in softer locations after the wet season, there is some permanent degradation. This is identified by the fact that 0.5% of the observations are considered very soft locations (8 MPa) for the first dry season run. These locations increase to 3.8% during the wet season and drop down to 1.5% during the next dry season. Thus, 1% have experienced degradation during the wet season.
In order to get a better understanding of the variability and seasonality effects,
Figure 12 and
Figure 13 present the track modulus variations for 5 km of track from KP 41 to KP 45. The wet season clearly showed seasonality effects by the fact that track modulus decreases in wet weather. While track stiffness decreased during the wet season, data showed that track stiffness increased during the next dry cycle (gray line); see
Figure 13.
To estimate the track modulus values in
Figure 12 and
Figure 13 above, the YRel data were evaluated over a length of 20 m and smoothed using a low-pass filter prior to assessing track modulus using Equation (2). The wet cycle clearly shows the variability, as well as the isolated locations of significant deviation. The pattern of variability is evident in that some locations show similar changes between runs, and softer and stiffer sections of track can easily be seen. In addition, the average track modulus for these three cycles, from km 41 to km 45, was 41.3 MPa in Jul. 2017 (dry), 30.8 MPa in Jan. 2018 (wet), and 39.8 MPa in the next dry cycle (Jul. 2018).
The seasonal effects could also be analyzed by the track geometry defect evaluation during a year before and a year after the stiffness campaigns. The geometry measurements utilized in this analysis comprised gage, alignment, and surface parameters including profile, crosslevel, and warp. A track geometry defect exists when the measured values of track geometry exceed threshold values set based on regulations, in this case FRA [
20]. The threshold value considered a defect is determined by an assigned class of track, where the class is established to limit train speeds according to match the track’s condition. The number of defects in
Figure 14 below is a sum of all class defects. Note that the sections evaluated in this study consisted of Class 3 and 4 tracks.
Figure 14 clearly shows the increase of geometry defects during the wet season, which is related to the variation in track stiffness during this period. This fact is associated with changes in subgrade condition due to the moisture variation and the excess of contamination existing in the ballast of most of the studied track sections. Note that the 2018 dry season shows an increased number of defects with is most likely related to the track degradation.
3.2. Mud Spot Identification
This section of the research is a part of a project to identify track mud spot locations correlating track vertical deflection signatures through MRail data (YRel). The subject focus of this research effort was to classify mud spot conditions with their impact on track maintenance, and more importantly its potential for track safety improvement. Mud spots are a very common problem where water, through capillary action, is “pumped” from the subgrade into the ballast by sleepers that move down under axle loads and then back upwards after the axle has passed over the sleeper. The sleeper acts like a piston pump as the rail elasticity springs the sleeper upward after the axle load passes. The mud mixed in with the ballast causes several problems that increase derailment risk including less stable muddy ballast, significant vertical track deflection, increased rail stresses (and increased risk of a rail break), areas where timber sleepers rot quickly, poor gauge holding stability due to rotting sleepers, poor lateral resistance for track alignment, higher risk of sun kinks from poor lateral resistance, and poor surface.
The biggest problem with mud spots is that there are too many for any railroad to repair 100% of the total. The need is to have a low-cost and fast way to evaluate the severity of each mud spot. Roadmasters inherently know where their mud spots are located and in general perform repetitive maintenance to fix the symptoms and not the root cause of the problem. This maintenance is expensive and requires track time. If the severity for each mud spot were quantified, maintenance could be prioritized. The method to quantify the severity of each mud spot is to analyze the data from the MRail Vertical Track Deflection System as well as other railway track and operating data such as: in site visual inspections, geometry, etc.
Figure 15 shows an exception associated with a spike in YRel used during the development of the model. Investigation of this location revealed this to be an area of fouled ballast. The data from the location presented was extracted for the left rail and a plot of YRel for the surrounding area.
Figure 15 shows a unique YRel signature of the mud spot. The surrounding locations have a mean YRel of 4.3 mm, a peak YRel of 17.8 mm in the center of the mud spot, and an average minimum value of −2.5 mm in the uplift zone. The mud spot YRel map has a length of approximately 5 m in the uplift zone and 4 m at the mean location. Note that this graph depicts the maximum YRel at each measurement location (every meter) as the inspection vehicle moves down the track.
It is important to understand the derivation of YRel and its relationship to deflection. In an ideal situation, i.e., uniform track support, the track will behave as a beam (rail) continuously supported by an elastic foundation (everything below the rail) subjected to sequential point loads (passing wheels) as described in the previous section. The solution for the deflection of a beam continuously supported by an elastic foundation is given by Equation (1). Using linear superposition, the deflection of the rail can be determined for an applied truck load of two wheels. Typical results for the deflection were presented in
Figure 5. It can be seen from this figure that the individual deflection waves from each wheel combine to provide the rail deflection under two adjacent axles on a bogie. This rail deflection shape can be seen at any point along the track and is dependent on the support stiffness and applied load, along with the rail properties.
Figure 5 also showed the projection of the measurement system and graphically how YRel is derived from the actual deflection curve. This can be represented mathematically as follows:
where w(x) = rail deflection at location x. Note that the above is for uniform stiffness, and as mud spots are evaluated, stiffness will have abrupt changes.
Considering the model depicted in
Figure 5, the rail deflection can be modelled using beam on elastic foundation theory, and the modelled YRel value can be calculated from Equation (3) for each measurement location. The rail deflection curves can be converted to YRel plots using the equations presented previously. The YRel map for the mud spot shown is overlaid with a modelled (blue line in
Figure 15) YRel map using BOEF model for a parent track stiffness of 24 MPa and mud spot of 5 m length and mud spot stiffness 3.5 MPa. While not a perfect match to the BOEF model,
Figure 15 shows how the BOEF model closely matches the measured YRel data. It should be noted that the lift regions which flank the peak deflection are not seen in the BOEF model. This is due to the BOEF model’s assumption that the beam is connected to the foundation. This connection drastically minimizes any uplift. In reality, the rail is not fully fixed with the substructure and rail lift is expected.
In order to facilitate production analysis, an algorithm for automatically identifying potential mud spots was develop using signal processing techniques of the YRel signature. After a series of analyses using BoEF to correlate measured YRel data to mud spots, the signature shown in
Figure 15 proves fairly consistent, and depending on mud spot severity, will show changes in length and peak values. Machine learning techniques and other advanced data science techniques can be applied for identifying this signature.
The chosen method for determining a “soft” location was to use fast Fourier transforms (FFTs). The signature shown in
Figure 15 (peak YRel with two uplift values) provides a unique signature that can be evaluated. In order to identify this signal, moving windows of YRel data were transformed into the frequency domain using FFT. Windows were required in order to isolate a specific signal response associated with one mud spot candidate and not the frequency spectrum of the entire dataset. Initial signal analysis was conducted using 130 m windows (to account for uplift zones of 6 m mud spot).
Figure 16a shows an example of a 130 m YRel data window being converted into the frequency domain using an FFT. In the frequency domain, the signal was analyzed to identify the presence of a significant low frequency response. After complete processing, this window was flagged as a potential mud spot candidate. As can be seen, the YRel data show the expected response (large peak flanked by minor uplift deflection signals) and the frequency domain contains a significant low frequency response. This approach allows us to automatically find the location with the associated YRel signature that can be correlated to mud spots. This flagged signature can now be prioritized for severity, as the length and maximum YRel will vary for each mud spot.
This analysis can be applied in real time as well.
Figure 17 shows 500 m of data and identified mud spots (highlighted with red dots).
Note that the YRel signature associated with a mud spot may also be associated with other soft support conditions in track. These may come from consecutive sleepers that are plate-cut or excessively decayed, hanging sleepers, or other localized soft support conditions. Thus, the identification of localized soft support conditions in track is important, whether it be from a mud spot or other cause. In order to limit the analysis to just mud spots, visual inspection and validation of the locations were performed. In addition, the algorithm may not identify newly formed mud spots until they reach peak deflection values that exceed the limits of detection.
Another way to visualize the mud spot location along the track is presented below.
Figure 18 shows the GPS coordinates of identified mud spots in MRS Corridor 1 from June 2017 and February of 2018 (the last measurement in wet season). The figure below clearly shows the evolution of mud spots in this specific corridor by the difference of severity related to the size and the peak of deflection of each mud spot. This location did not receive appropriate substructure maintenance activities during this period of analysis, which facilitated the comparation of seasonal effect and mud spot growth.
Utilizing the FFT approach to identify mud spots, roughly 900 km of MRS vertical deflection data were processed through the steps outlined above. A total of 497 signals were flagged to match the potential signal of a mud spot. Each signal was processed to identify its central deflection zone and total widths as well as its localized mean deflection and its maximum deflection. A histogram of full signal widths is shown in
Figure 19. It can be seen that most signals had a total width of between 9 and 18 m. Full width includes the uplift zones and central deflection zone.
The analyses discussed previously have played a crucial role in prioritizing the maintenance plans for MRS in the years following the project, with a particular focus on preparations for the rainy seasons. The results of the analyses were correlated with other inspection methods to define the most appropriate action plan. Areas with a high concentration of mud spots, covering approximately 34 km (3.8%), with track modulus below 8 MPa, underwent total track renewal and subgrade restoration, as they required drainage and reinforcement interventions. These areas consistently exhibited low support capacity. Additionally, these locations had higher superstructure component degradation, including sleeper replacement and fastener and rail fatigue. Locations with frequent tamping and high geometry degradation, accounting for approximately 10.4% (94 km) of the track, were associated with areas of low support and were designated for the initial phase of the ballast cleaning project. These locations, with a track modulus between 14 MPa and 8 MPa, showed significant variation in support between seasons, as ballast contamination retained water during the rainy period, reducing track modulus and causing geometry degradation.
In addition to areas with low track modulus, locations with high modulus variation over short distances were also evaluated, particularly those at tunnel entrances, bridges, and level crossings. Approximately 100 points required intervention, with 30 needing immediate action due to high dynamic impact. Interventions included bridgehead replacement and complete restoration of level crossings. This plan was based on an integrated analysis of multiple systems. During one of the measurement campaigns, the MRail instrumented train was also equipped with an instrumented wheelset system to correlate measurements. This approach enabled the identification and treatment of the most critical locations for load impact.
These examples illustrate how the strategic approach led to a reduction of more than 50% in the number of defects on the permanent way in the following years. Additionally, it contributed to a notable decrease in the frequency of derailments, with the most recent incident occurring in December 2019.