Abstract
There is frequent debate over the long-term stability of calibration specimens. It is an essential component of monitoring, especially for X-ray diffraction equipment used to determine residual stresses. If residual stresses are stable, a second consideration is that the residual stress should not be close to 0 MPa. If such specimens are available for monitoring, it is more sensitive concerning changes. These are key requirements when developing calibration specimens. In this study five specimens were observed, one of them was tested for more than 20 years. The stresses were determined with X-ray diffractometers. In the last four years two different X-ray methods for determination were used. It can be shown that high compressive residual stress does not change in steel if the specimens had no dynamic or static load and were stored under normal laboratory conditions.
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Finding a material in which compressive residual stress is stable
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Showing that the stability of compressive residual stress is over a long term
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The stability of the compressive residual stress is in a great range
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1 Introduction
Compressive residual stress is often built up in the surface layers of a component to enhance its durability because it can delay or suppress the propagation of cracks. Compressive residual stress can be induced using different methods, popular ones being mechanical surface treatments like shot peening or deep rolling [1,2,3]. It has been found that under higher dynamic loads the compressive residual stress reduces. However, the possibility of stress relaxation in components occurring under no load has not been examined often [4], and no studies have reported on the long-term (i.e., over years) stability of compressive residual stress.
Stresses in Almen strips relax within minutes after peening [4]. If after minutes residual stresses are stable it allows calibrating and monitoring X-ray diffractometers, which is very important. The hole-drilling method is traditionally used to determine residual stress. Strain gauges are fixed to the surface and move when drilling into the material commences. From the recorded movement in the strain gauges, the residual stress can be calculated. The disadvantage is that no measurement at the surface is possible, and the strain gauges cannot be used a second time. Before measurements a calibration is not possible using this method. Consequently, X-ray diffraction is becoming the standard method for calibration (see Sect. 4 for a description of this method). Measuring strain by X-ray diffraction is non-destructive at the surface, making it possible to monitor the stability of the equipment and calibrate it with specially designed specimens. This is only possible if the residual stress in the material is stable, but once this condition is met mechanical surface-treated specimens can be easily produced and used.
In this study we aimed to examine the stability of residual stress in steel. The investigation arises from monitoring the X-ray equipment in the accredited laboratory of the Steinbeis-Transfercenter for Spring Technologies, Component Behavior and Process in Germany. All data available the time before 2007 were also involved because the measurement conditions had not changed.
At first in this article the specimens were described to know in which material compressive residual stresses are stable. In the second step the measurement technique will be explained because it is new method for X-ray diffraction. Afterwards the results are shown from 2000 to the present (2020) and the consequences calibration of X-ray diffraction equipment is short discussed.
2 Status of research
The compressive residual stress reduces under a cycle load but after a certain number of cycles it becomes constant. The main variables affecting compressive residual stress are shown and also the limit of residual stresses [5]. In [6] it is reported that a cold-drawn prestressed wire has a significant reduction in the induced compressive residual stresses by cyclic overloading. Depending on the load which was between 0.75 and 1.25 times the yield strength the experiment shows different reduction amounts. The higher the loading the more reduction is achieved up to more than 80%. There are two questions arising from these results, which are still open. Is the residual stress constant over a long time period? Is it independent of the amount of residual stresses in the specimen? To answer this question specimens with strong compressive residual stresses were measured with several different X-ray diffractometers to monitor the development of residual stresses at each specimen. Several diffractometers were used at the same time to detect a shift of one diffractometer.
3 Specimens
3.1 Description of the Specimens
Five different specimens were used in this investigation (Table 1). Specimens 1 and 2 were identical and were named KP1 (calibration probe, in German: Kalibrierprobe 1) and KP2. Figure 1 shows these specimens, and they had the dimensions 60 × 60 × 9 mm. They were made of 50 Cr V 4 (1.8159) steel, with a tensile strength of 1600 MPa after tempering. Subsequently, the specimens were ground to avoid decarburization.
An area of 55 × 55 mm was deep rolled in the shape of a meander to obtain high compressive residual stresses. The area was very smooth at the surface, with a roughness Rz between 5 and 13 μm. The deep rolling parameters were optimized to obtain the maximum compressive residual stress at the surface which was slightly over –900 MPa [7]. The specimens have been in use since 2015, the year of manufacture.
Specimen 3 was called GKN because it was used in a round-robin test in 2008 organized by Mr. Lietzau at GKN Germany [8]. Figure 2 shows this specimen, which has dimensions of 50 × 30 × 10 mm. It is an unalloyed Q&T steel Cf53 (1.1213) which was inductive surface hardened and tempered for 30 min at 180 °C. After this process, the surface area was ground. The residual stress at the surface was approximately –350 MPa. This specimen was manufactured in 2005/2006.
Specimen 4 is referred to as D + N because it is a torsion bar that was produced by Dittmann and Neuhaus in Germany. Its dimensions are 180 mm long × 60 mm diameter (Fig. 3). It is made of steel 56 Ni Cr Mo V 4 (1.7701) with a tensile strength of 2000 MPa and was shot-peened. Its residual stress is about –500 MPa in 100 µm depth. The specimen was manufactured in 2000 and is in use since this time to monitor X-ray diffractometers.
Specimen 5 is known as M13-16. It is similar to Specimen 4, except that it is slightly longer at 200 mm length, and it was manufactured in the beginning of 2016 (Fig. 3). The situation of the residual stress is the same compared to specimen 4.
All data of the specimen are summarized in Table 1:
3.2 Storage of the specimenes
All specimens were stored in the laboratory at temperatures between 10 and 30 °C. The humidity was in the normal range (60—70%). The specimens were stored in a wooden cabinet and there were no additional storage precautions taken. The specimen GKN was lent to the Institute for Metallurgy in Komsomolsk, Siberia, in February and March 2015. This specimen had a higher temperature range.
4 Description of the X-ray diffractometer methods and equipment
Both of the methods to determine residual stresses are based on Bragg ‘s law. The incident X-rays are reflected at different atomic layers lying in the same direction and, if the reflected X-rays have the same phase, constructive interference will appear, and a signal is detected. It is only possible to obtain constructive interference at a special angle ψ (Fig. 4). With some geometrical constraints you get the following formula:
where λ is the wavelength of the X-rays which is known, and d is the spacing of the atomic layers (e.g. [9]).
The change in distance delta d proportional to the macroscopic strain ε. Stress can be calculated using the E-module E and the Poisson’s ratio ν. This means that the residual stress cannot be measured directly and is only determined using calculations.
Every X-ray diffraction gives a fully reflected ring at the angle ψ, which is known as a Debye–Scherrer ring if the material has a polycrystal structure (Fig. 4). Depending on the amount of strain there is, the angle ψ varies and the whole ring is shifted. Now two methods based on the Debye–Scherrer ring are described which were used in practice.
4.1 Cos-α-method
The cos-α-method is new and is not yet very popular. Even so, a brief introduction is provided to it here. There is one incident angle, ψ0 and a whole ring shift is used [10, 11]. Figure 4 illustrates the situation.
The shift’s (see Fig. 5) dependence on the rotating angle α is as follows:
with the shift \(\varepsilon \mathrm{\alpha }1\) of the Debye ring defined in (3):
and \({\sigma }_{x}\) the obtained residual stress in the measurement direction, α the rotation angle of the ring, E the E-Modul, ν Poisson ratio. Ψ is the incidence angle and 2η the angle between the incident and reflected beam. All variables are presented in Fig. 5.
By determining the linear slope (last term in the Eq. (2)), the stress can be calculated.
For this kind of measurement, an X-ray diffractometer (pulstec µ-X360s) operating by means of cos-α-method with an incident angle ψ0 = 35° was used. For steel, Cr-Kα-radiation is in use at nearly all X-ray diffractometers that is also the case of these measurements described here. The setup which was used is shown in Fig. 6. This diffractometer has been in use since 2016.
4.2 Sin2ψ-2θ-method
The sin2ψ-2θ-method detects only a small section of the Debye–Scherrer ring and uses different incident angles ψ (different shifts) to determine the residual stress. Layers with different orientations to the strain are sensitive to different incident angles. The spacing of these layers is proportional to sin2ψ. The formula to calculate stress using this method is as follows.
where ε is the strain, E is the specific diffraction plane elastic modulus and ν is the Poisson’s ratio.
This is the traditional method used to determine residual stress by X-ray diffraction. Good descriptions are found in [12, 13]. For this method, several diffractometers of the type Rigaku Strainflex MFS-2 M were used (Fig. 7). They were manufactured between 1982 and 1988 and maintained by Rigaku based in Japan and later by the lab staff in the same way. A total of five different devices of this type were available during different time periods, because spare parts were not available to repair the old one.
4.3 Comparison of the methods
The relevant measurement parameters of the two methods are summarized in Table 2.
Table 3 shows the existing literature concerning the use of the equivalence of both methods in relation to different materials. The comparison was done in some cases with tensile load stress and in other cases with compressive residual stress. In this case the experiment was performed with compressive residual stresses. Due to this, the measured values from different X-ray diffractometers and methods can be averaged for further investigation.
5 Measurements and results
Formula (2) is simplified. If shear stress exists, it must be eliminated by measuring in the positive ψ and negative ψ-direction [12, 13]. From the two results, the mean is calculated to eliminate the shear stress. Therefore, measurements were made in both directions, and this procedure was carried out for both methods.
The measurement error (standard deviation) of both diffractometers was approximately 30 MPa below the border of ± 400 MPa and for a greater amount 7%. This error is the statistical error of a single measurement. A time grid of a quarter of a year was chosen for the analysis (see Appendix).
All diffractometers which were available were involved to reduce the risk of drift from a single device. The first measurement with one specimen was done in 2000 to monitor a diffractometer. Since 2007 the laboratory is accredited (DIN 17025) which means that the monitoring must be done. in shorter intervals. Over time, more machines were positioned in the lab, while others were taken away if they malfunctioned. Additional specimens were used during this time. If the specimens were measured with different devices, a mean value was calculated (gray fields, see Appendix).
Figure 8 shows the development of the residual stresses of specimens over the investigated period. The x-axis shows the different absolute years in which the measurements were one. The y-axis represents the scale of the obtained residual stresses. Note that it is always compressive stress (negative sign). The specimen D + N was measured for the longest time. Within the errors, the compressive residual stress remains constant. The variation of the single values is caused by the measurement errors (see previous paragraphs). The values are based on the results in the appendix. The single results were connected by a line to see the related points. In the first period the measurement was done occasionally, because the important question of stability arises around 2010 in the scientific community.
Specimens KP1 and KP 2 which had the highest compressive residual stresses were the most sensitive samples concerning a reduction in residual stress. The stress is constant within the errors, and no trend is seen for all specimens. The variations are caused by the measurement errors. E. g. a linear fit taking the values from sample D + N (oldest) gives a slope of m = –1.81 × t (time in absolute years, not the difference of the years), which means there was a calculated slight increase in the compressive residual stress of 36 MPa in 20 years, the lifetime of the sample. Specimen GKN had a slope of m = 2.49, meaning there was a decrease in compressive residual stress of 25 MPa over 10 years (lifetime of the sample). These changes are not significant and within the measurement errors (standard deviation of the Gaussian distribution). The specimens were stored as mentioned above in a normal laboratory environment. As a result, no reduction of compressive residual stresses at different levels can be seen.
The inducing stresses in the specimens creates dislocations with different spacing of the atomic layers in the lattice. This fact can be seen that the reflected beam intensity has a distribution in the reflected angle and is not sharp. The widening of the distribution is an indication of the number of dislocations. The dislocations are created under high selective mechanical pressure (shot peening, deep rolling) which means with a high amount of energy. At high compressive residual stresses at these materials, more dislocation move to the border of a grain and the position are stabilized there [7, 10]. The elimination of these dislocations cannot be done by thermal energy at room temperature.
6 Using specimens for calibration
To change from a monitoring specimen to a calibration specimen, a round-robin test must be done. There is no national or international standard available like with SI units (m, kg, etc.). Specimen KP1 and KP2 were obtained from a large round-robin test that involved 30 laboratories. The test was organized as mentioned above by Mr. Lietzau of GKN, Germany. All laboratories used the sin2ψ-2θ-method because at this time the cos-α-method was not available.
The values of KP1 and KP2 were –934 MPa and –926 MPa, respectively. Both samples had an systematic uncertainty of ± 50 MPa or 5.4%, which are the best value available in public at the moment [14, 19]. Also, all round-robin test results are listed in [14, 19] which was done in public the last 20 years.
7 Conclusion
It was shown that the compressive residual stress in steel induced by mechanical surface treatment does not change over long time periods of more than 20 years if the specimen is stored under normal room conditions. It is unlikely that more extreme storage conditions would impact the compressive residual stress of materials, but it was not tested here.
Such specimens can also be used for long-term monitoring of X-ray diffractometers. If the samples (like KP1 and KP2) are related to a round-robin test it can be used as a calibration sample. Using a high amount of compressive residual stress is possible and this would not be expected to reduce over time.
The compressive residual stresses induced by shot peening and deep rolling affect corrosion positively [20, 21]. Pitting resistance is significant improved by compressive residual stresses [22, 23]. Also, cavitation is delayed [24, 25]. In many cases no dynamic load respectively stress is on a component affected by corrosion. This means, the change of the induced residual stresses is only caused by corrosion or cavitation itself during the operation time. The compressive residual stress can be implemented in such a component long before using it and can be stored over a long time.
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Appendix
Appendix
The numerical data used for the analysis. All values are in MPa. After the numeric year, the quarter (Q) within the year is given See Table 4.
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Mueller, E. The long-term stability of residual stresses in steel. SN Appl. Sci. 3, 877 (2021). https://doi.org/10.1007/s42452-021-04867-z
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DOI: https://doi.org/10.1007/s42452-021-04867-z