1. Introduction
Pipelines are commonly used to transport resources such as oil, gas, and water and are frequently buried underground where space is limited [
1,
2]. Nevertheless, these pipelines are prone to various forms of corrosion owing to material properties and surrounding environmental conditions. The primary causes of corrosion in these underground pipelines stem from natural currents, stray currents, and soil conditions [
3,
4]. An analysis of approximately 400 cases involving city gas pipelines revealed that about 35% of accidents were due to natural corrosion. Similarly, a 20-year study by a U.S. Gulf Coast company, assessing around 640 pipeline failures in coastal areas, indicated that 49% of these failures were attributed to corrosion [
5,
6,
7,
8].
To mitigate corrosion, various protective measures, such as selecting appropriate materials, applying coatings to isolate the pipeline from the environment, and employing cathodic protection (CP), are used [
9,
10]. Typically, coatings are applied both internally and externally on pipelines to prevent corrosion. However, external coatings on buried pipelines can deteriorate due to factors such as inadequate surface preparation, changing soil conditions, or damage from nearby construction activities [
11,
12]. When the coating of a buried pipeline is compromised, the exposed metal interacts with the soil, leading to electrochemical reactions that accelerate corrosion [
13,
14,
15,
16,
17]. In critical infrastructures such as power plants, corrosion-induced cracks in pipelines can result in severe economic and environmental consequences. To mitigate these risks, buried pipelines in key facilities are protected with external and internal coatings, along with cathodic protection, which introduces an external current to curb further corrosion. However, if the coating is damaged over time, corrosion and cracking may still occur [
18,
19].
In nuclear power plants, both direct and indirect inspections are periodically conducted on buried pipelines. Given the multitude of buried pipelines in the confined spaces of these facilities, assessments of coating defects are carried out first to determine excavation points. The indirect inspection protocol for buried pipelines typically involves identifying pipeline routes, assessing the status of cathodic protection, and evaluating coating defects. Techniques for locating pipelines include Ground-Penetrating Radar (GPR), which uses electromagnetic waves, and the Alternating Current Voltage Gradient (ACVG) technique, which measures voltage gradients induced by alternating currents [
20]. The GPR is extensively used in sectors such as wastewater management, gas distribution, and telecommunications, proving especially effective in nuclear power plants where pipelines may intersect in vertical, horizontal, and diagonal orientations. The assessment of cathodic protection typically involves the Close-Interval Potential Survey (CIPS) method for measuring pipeline potentials, while the DCVG method is used to detect coating defects in buried pipelines [
21,
22,
23,
24]. It works by applying a direct current to the pipeline and then measuring the voltage difference (potential gradient) on the ground surface. If a defect is present, the current escapes through the exposed area, creating a detectable voltage gradient.
Recently constructed buried pipelines are generally coated with high-performance factory-applied coatings, consisting of three layers: an epoxy layer, a polyethylene adhesive layer, and an outer polyethylene layer [
25,
26]. However, in sections where pipelines are welded onsite (which typically requires the removal of approximately 15 cm of factory coating for welding), a less protective heat-shrink sleeve is applied. Generally, even if defects are present in the factory-applied coating, corrosion is anticipated to be prevented as long as cathodic protection standards are met and there is no further degradation, such as delamination. Yet, heat-shrink sleeves at weld joints tend to sustain more damage or degradation, and frequent pigging has shown these welded sections to be more susceptible to corrosion [
27,
28]. Consequently, weld joints represent high-risk areas for corrosion, making it critical to detect even small micro-defects in these areas to maintain pipeline integrity.
Weld coatings, relatively more vulnerable, pose additional challenges. Heat-shrink sleeves applied to weld joints in trenches experience shear stress from the backfilled soil pressing down on them. Moreover, poor installation quality can lead to stretching, wrinkling, or detachment of the sleeve from the pipeline, especially on the lower portion. This phenomenon is known as coating disbond [
29,
30,
31,
32]. When coating disbond occurs, corrosive electrolytes present in the soil can infiltrate the space between the disbonded coating and the pipeline, coming into direct contact with the weld area.
Under such conditions, the cathodic protection current cannot pass through the highly insulating heat-shrink material and must instead flow through the electrolyte that has entered the gap (a phenomenon known as cathodic shielding). However, the scale of the current entering the gap depends on factors including the size of the disbonded area, the conductivity of the electrolyte under the disbonded coating, and the applied potential. Due to the typically high resistance of this path, the flow of cathodic protection current into the gap is significantly restricted, leading to an inadequate current distribution and continued corrosion. Where coating disbond has occurred, the limited flow of current results in a small potential gradient at the ground surface.
Currently, the primary industry-standard techniques for detecting coating damage in buried pipelines are CIPS and DCVG. However, one substantial limitation of both CIPS and DCVG is their reduced effectiveness in electrically shielded environments caused by coating disbond. This limitation introduces critical uncertainties about whether DCVG can effectively detect such small potential gradients and under what specific conditions these defects can be accurately identified.
This study aims to determine the detectability of both non-shielded and shielded coating defects at rubber-lined weld joints by simulating various conditions to calculate potential distribution and analyzing the shielding effect in coating defect detection using the DCVG method. While this study focuses on DCVG simulation, various detection techniques are commonly used in the field to assess coating defects and cathodic protection status. DCVG (Direct Current Voltage Gradient) is effective in localizing coating disbonds with reasonable surface accuracy, particularly for electrically isolated pipelines. However, it may suffer from signal attenuation in high-resistivity soils or in the presence of shielding. In contrast, current interruption methods provide an overall view of cathodic protection effectiveness through potential decay curves but lack spatial resolution. Electromagnetic sensing techniques are also widely used to detect insulation loss or metallic discontinuities, though they may be less effective for non-metallic coating disbonds.
3. Results and Discussion
DCVG simulation in the non-shielded condition. Figure 2 depicts a model for detecting defects in a non-shielded buried pipe. The model comprised a 30 m long pipe within a homogeneous soil environment. The pipeline’s coating was either missing or damaged at specific spots, exposing the pipeline directly to the external environment. The enlarged view highlights where these coating failures occurred, with defect sizes set at 100 cm
2 and 1 cm
2, leading to direct exposure of the pipeline to the electrolyte.
Figure 3 illustrates the polarization behavior of the pipeline material in deaerated conditions for various soil resistivities (1 kΩ·cm, 10 kΩ·cm, and 19 kΩ·cm). From the polarization curves, electrochemical parameters such as corrosion potential and Tafel constants (Beta A, Beta C) were derived, serving as material data in the simulation. COMSOL Multiphysics
® was used to simulate defect detection in buried pipelines by directly incorporating the data from the polarization curves instead of separately entering the parameters of the material properties derived from the polarization behavior. This method permitted a more accurate depiction of the electrochemical reactions within the electrolyte and improved the simulation’s precision by using an intrinsic analysis to integrate the necessary electrochemical constants with the polarization behavior. This approach allows the same polarization curve data to be reused or updated without the need to manually extract individual parameter values each time, thereby ensuring reproducibility.
Figure 4 illustrates the 3D simulation results for detecting unshielded defects in buried pipelines.
Figure 4a shows the potential distribution within the electrolyte, highlighting the formation of a potential gradient at the defect site.
Figure 4b demonstrates the current distribution within the electrolyte, indicating that the current density is concentrated at the defect location, indicating strong current leakage through the exposed metal surface. This means that the defect acts as an escape point for the cathodic protection current, which creates a voltage signal detectable by surface electrodes. The more concentrated this current, the more detectable the signal.
Figure 5 outlines the computational process used to ascertain the magnitude of the DCVG signal via simulation. The simulation incorporated critical parameters including soil resistivity, defect size, and applied voltage.
Figure 5a illustrates the potential distribution from a lateral view, depicting the pipeline in white, where it is clear that the potential is localized at the exposed defect at the bottom center of the pipeline. From these simulation results, the potential distribution on the ground surface was visualized as depicted in
Figure 5b. Additionally, the ground surface potential along a path parallel to the pipeline is depicted in
Figure 5c, identified as the “on-potential”. The magnitude of the DCVG signal was then determined by calculating the potential difference at various electrode spacings relative to the on-potential. This signal reflected how much current was leaking from the coating defect. Larger defects or lower soil resistivity typically generate stronger signals, which makes defects easier to detect. This approach allows the same polarization curve data to be reused or updated without the need to manually extract individual parameter values each time, thereby ensuring reproducibility.
Based on the simulation results for detecting non-shielded defects in buried pipelines, the DCVG signal can be calculated by determining the potential difference between the survey electrodes using the surface potential (on-potential) gradient induced by the applied voltage. In this study, the resultant DCVG signals calculated using this method are presented in
Figure 6 and
Figure 7.
Figure 6 presents the simulation results for detecting non-shielded defects in buried pipelines under a soil resistivity of 1 kΩ·cm and in the presence of a defect size of 100 cm
2, incorporating the analysis of the detection electrode distance effect. The results showed that the presence of a non-shielded defect led to an increase in the DCVG signal as the applied voltage increased. Additionally, the DCVG signal escalated as the distance between the detection electrodes and the coating defect enlarged.
Similarly,
Figure 7 illustrates the behavior of the DCVG signal under identical conditions to those in
Figure 6, but with a defect size of 1 cm
2. The findings indicated a comparable trend, where the DCVG signal intensified with an increase in the applied voltage. Moreover, as the detection electrode distance increased, the DCVG signal also increased.
These trends are consistent with prior experimental studies, such as Choi et al. (2023) [
37], which also observed that DCVG signals increased with voltage and electrode spacing. This agreement supports the model validity in non-shielded conditions. In contrast, the signal attenuation under shielding is a novel contribution of this study.
These results show that a DCVG signal is significantly reduced in the presence of a shielding layer due to the limited current flow to the defect site. In addition to signal attenuation, shielding can lead to localized electrochemical conditions by restricting the ionic transport and reducing the cathodic protection efficiency at the defect. This may result in an increased corrosion risk despite the absence of detectable signals. Further experimental validation under controlled shielding conditions is planned to examine these electrochemical effects in detail.
Figure 8 presents the simulation results for detecting non-shielded defects in welded pipelines under a soil resistivity of 1 kΩ·cm, illustrating the DCVG signal variations corresponding to the detection electrode distances for different defect sizes.
Figure 8a presents the DCVG signal magnitude for a defect size of 100 cm
2, while
Figure 8b provides the results for a defect size of 1 cm
2.
When the DCVG defect detection threshold was defined as 0.5 mV, it was confirmed that for a defect size of 100 cm
2, defect detection remained effective regardless of the detection electrode distance and the applied voltage. This revealed that for relatively large defects, sufficient signal magnitude is secured under various testing conditions, facilitating defect detection. In contrast, for a defect size of 1 cm
2 and a detection electrode distance of 1 m, detection proved difficult, independent of the applied voltage. This phenomenon is due to the localized nature of the current distribution as the defect size decreases, which subsequently results in a lower potential difference on the ground surface. Moreover, when the detection electrode distance exceeded 3 m, the DCVG signal surpassed the threshold value of 0.5 mV in all applied voltage scenarios. This effect can be interpreted as an increment in signal intensity caused by an expanded distribution of the potential difference across a larger area as the electrode distance increases [
37]. However, employing a large detection electrode distance may introduce practical constraints in field applications, potentially complicating the accurate identification of small defects during actual surveys.
DCVG simulation in the shielded condition. Figure 9 presents the simulation model designed to detect shielded defects in buried pipelines. The model depicts a pipeline with a welded joint at the longitudinal center, where a shielded defect formed due to coating disbond at the weld (
Figure 1). Aside from the defect area, all regions were assumed to be insulated with a protective coating. The defect was modeled as a region where the coating was either detached or wrinkled at the bottom of the pipeline (6 o’clock position) due to shear stress imposed by the surrounding soil or welding quality issues, exposing the pipeline to the electrolyte. The sizes of the exposed defects due to coating disbond were set to both 100 cm
2 and 1 cm
2 in the simulation model, permitting the analysis of these conditions. Additionally, soil resistivities of 1, 10, and 19 kΩ·cm were used to evaluate the detection of shielded defects under diverse soil conditions.
Figure 10 illustrates the 3D simulation results for detecting shielded defects at the pipeline weld.
Figure 10a depicts the potential distribution within the electrolyte, where an increase in potential at the exposed defect area is evident in both the full image on the left and the magnified view on the right.
Figure 10b displays the current density distribution within the electrolyte, indicating that the current density is concentrated at the exposed defect caused by the coating disbond, as visible in both the full and the magnified images.
The DCVG signal was calculated using the method described in
Figure 5, and the results were analyzed to evaluate the effectiveness of the simulations in detecting shielded defects. The DCVG signal was determined by computing the potential difference at the detection electrode distance, utilizing the surface potential (on-potential) gradient induced by the applied voltage. From this, the characteristics of the detection signal were assessed.
Figure 11,
Figure 12 and
Figure 13 present the simulation results when detecting shielded defects under varying soil resistivity conditions, comparing the changes in DCVG signal with variations in detection electrode distance and applied voltage.
Figure 11 illustrates the simulation results when detecting shielded defects in a buried pipeline under a soil resistivity of 1 kΩ·cm and a defect size of 100 cm
2. The analysis indicated that the presence of a shielded defect led to an increase in the applied voltage, which correspondingly increased the DCVG signal. Additionally, as the detection electrode distance increased relative to the coating defect, the DCVG signal also increased.
Figure 12 presents the simulation results for a soil resistivity of 10 kΩ·cm and a defect size of 100 cm
2. The results demonstrate that as the applied voltage increased, the DCVG signal magnitude also increased, and as the detection electrode distance increased, the DCVG signal exhibited an increasing trend.
Figure 13 presents the simulated DCVG response for a defect measuring 100 cm
2 in a high-resistivity environment (19 kΩ·cm). The results indicate that in high-resistivity conditions, the DCVG signal exhibited reduced sensitivity and a diminished variation in magnitude. Despite the reduced sensitivity, the DCVG signal increased consistently with higher applied voltage. Additionally, variations in signal strength became more apparent as the detection electrode distance increased.
Figure 14 presents a graph that displays the variation in DCVG signal magnitude as a function of the applied voltage for a pipeline with an exposed defect size of 100 cm
2. The graph in
Figure 14a corresponds to a soil resistivity of 1 kΩ·cm, that in
Figure 14b to a soil resistivity of 10 kΩ·cm, and that in
Figure 14c to a soil resistivity of 19 kΩ·cm. Additionally, the variations in the DCVG signal due to increasing detection electrode distances were compared.
The analysis was performed by establishing a DCVG defect detection threshold of 0.5 mV. As shown in
Figure 14a (1 kΩ·cm), when the applied voltage was set to 0.3 V, a minimum detection electrode distance of 3 m was required for the signal to surpass the threshold. However, at increased voltages of 0.9 V and 1.5 V, the signal exceeded the threshold at all detection electrode distances, confirming that defect detection was feasible under these conditions. In
Figure 14b (10 kΩ·cm), a detection electrode distance of at least 5 m was necessary when the applied voltage was 0.3 V. As the applied voltage increased to 0.9 V, a minimum distance of 2 m was required to achieve successful detection. At 1.5 V, the signal consistently surpassed the threshold regardless of the detection electrode distance, ensuring reliable defect identification. In
Figure 14c (19 kΩ·cm), the signal did not exceed the threshold at any detection electrode distance when the applied voltage was 0.3 V. However, when the voltage was raised to 0.9 V, a detection electrode distance of at least 4 m was required for the signal to reach the threshold. At an applied voltage of 1.5 V, a minimum distance of 2 m was necessary to achieve a detectable signal.
These findings suggest that as soil resistivity increases, higher applied voltages are required to obtain a detectable signal and the detection electrode distance must be carefully optimized for effective defect detection. In particular, for a soil resistivity of 19 kΩ·cm, maintaining a sufficiently high applied voltage and an appropriately large detection electrode distance is essential to ensure successful DCVG signal identification.
Figure 15,
Figure 16 and
Figure 17 present the simulation results when detecting shielded defects measuring 1 cm
2 under soil resistivity of 1 kΩ·cm, 10 kΩ·cm, and 19 kΩ·cm, respectively. The influence of detection electrode distance and applied voltage on the DCVG signal was analyzed.
Figure 15 illustrates the simulation findings when detecting shielded defects in a buried pipeline with a soil resistivity of 1 kΩ·cm and a defect size of 1 cm
2. The results demonstrate that when a shielded defect was present, an increase in applied voltage led to a corresponding rise in the DCVG signal. Moreover, as the detection electrode distance expanded, the DCVG signal strength also increased.
Figure 16 presents the simulation results for a soil resistivity of 10 kΩ·cm and a defect size of 1 cm
2. The findings indicate that at lower applied voltages, the DCVG signal sensitivity diminished, resulting in a minimal variation in signal magnitude. However, as the applied voltage increased, a substantial rise in the DCVG signal was observed, along with noticeable variations associated with an increasing detection electrode distance.
Figure 17 displays the simulation results for a soil resistivity of 19 kΩ·cm and a defect size of 1 cm
2. The analysis suggested that in high-resistivity environments, the sensitivity of the DCVG signal was significantly reduced. Additionally, at applied voltages below 1.5 V, the signal magnitude remained relatively low, making defect detection more challenging.
Figure 18 illustrates the variation in the DCVG signal as a function of applied voltage for a buried pipeline with a shielded defect of 1 cm
2. The graph in
Figure 18a corresponds to a soil resistivity of 1 kΩ·cm, that in
Figure 18b to a soil resistivity of 10 kΩ·cm, and that in
Figure 18c to a soil resistivity of 19 kΩ·cm. Additionally, the variations in the DCVG signal due to an increasing detection electrode distance were analyzed.
The assessment was carried out by setting the DCVG defect detection threshold at 0.5 mV. In
Figure 18a (1 kΩ·cm), when the applied voltage was 0.3 V, the signal remained below the threshold, irrespective of the detection electrode distance. At an applied voltage of 0.9 V, a detection electrode distance of at least 3 m was necessary for the signal to exceed the threshold. At 1.5 V, the signal exceeded the threshold when the detection electrode distance was at least 2 m. Conversely, under soil resistivity of 10 kΩ·cm (
Figure 18b) and 19 kΩ·cm (
Figure 18c), the DCVG signals did not exceed the threshold at any detection electrode distance, suggesting that detecting defects is impractical under these conditions. The DCVG signal decreased significantly under the shielded conditions, especially when the defect was small, or the soil resistivity was high. These findings suggest that the simulation model can be utilized as a pre-inspection tool for DCVG-based surveys. By analyzing how signal magnitude varies with electrode spacing, applied voltage, and shielding conditions, the results may aid in the optimization of the inspection parameters and help field engineers in interpreting ambiguous signals, especially in high-resistivity soils or partially shielded environments.
Comparison between non-shielded and shielded conditions. Figure 19 presents a comparative analysis of the DCVG signals for non-shielded and shielded defects with a size of 100 cm
2 under a soil resistivity of 1 kΩ·cm. Each graph illustrates the DCVG signal magnitudes based on applied voltage (0.3 V, 0.9 V, 1.5 V) and detection electrode distance (1 m, 3 m, 6 m), allowing for a direct comparison between non-shielded and shielded conditions.
Table 1 shows a comparison of the DCVG signal magnitudes for non-shielded and shielded defects.
Figure 19a shows that under an applied voltage of 0.3 V, the DCVG signal for the non-shielded defect increased with the detection electrode distance, peaking at 7.45 mV at 6 m. In contrast, for the shielded defect, the DCVG signal remained below the detection threshold (0.5 mV) at all distances except for that of 6 m, suggesting that defect detection may be challenging under these conditions. In this study, a detection threshold of 0.5 mV was defined to evaluate defect detectability. This value was determined based on the measurement error of the DCVG instruments under field noise conditions and the results of repeated simulations under the same conditions.
Figure 19b illustrates the DCVG signal behavior under an applied voltage of 0.9 V. For the non-shielded defect, the signal increased with the detection electrode distance, reaching 2.8 mV at 1 m, 7.84 mV at 3 m, and 11.52 mV at 6 m, all of which exceeded the detection threshold, ensuring feasible defect detection. For the shielded defect, the DCVG signal was 0.16 mV at 1 m, remaining below the threshold, but increased to 0.79 mV at 3 m and 1.25 mV at 6 m, surpassing the threshold and allowing for detection.
Figure 19c presents the DCVG signal at an applied voltage of 1.5 V. For the non-shielded defect, the signal magnitude increased consistently with the detection electrode distance, reaching a maximum of 15.58 mV at 6 m, confirming the feasibility of detection under all tested conditions. In the case of the shielded defect, the signal increased to 1.26 mV at 3 m and 1.9 mV at 6 m, exceeding the threshold. However, at 1 m, the signal remained relatively low at 0.24 mV, indicating that detection may be difficult at this distance.
Figure 20 compares the DCVG signals for non-shielded and shielded defects with a size of 1 cm
2 under a soil resistivity of 1 kΩ·cm.
Figure 20a reveals that for the non-shielded defect, the DCVG signal increased with the detection electrode distance, reaching 0.94 mV at 6 m. At 3 m, the signal was 0.59 mV, exceeding the threshold, which supports the feasibility of detection. In contrast, for the shielded defect, the DCVG signal remained below the threshold at all electrode distances, suggesting that detection was unlikely.
Figure 20b illustrates the DCVG signal at an applied voltage of 0.9 V. For the non-shielded defect, the DCVG signal increased with the detection electrode distance, reaching 0.38 mV at 1 m, 0.93 mV at 3 m, and 1.46 mV at 6 m. Detection was feasible at distances of 3 m or more. However, for the shielded defect, the DCVG signal consistently remained below the threshold at all detection electrode distances, making detection challenging.
Figure 20c presents the DCVG signal at an applied voltage of 1.5 V. For the non-shielded defect, the signal increased with the detection electrode distance, reaching 1.98 mV at 6 m, enabling detection at all distances. Conversely, for the shielded defect, the DCVG signal remained below the threshold at all detection electrode distances, with recorded values of 0.11 mV at 1 m, 0.25 mV at 3 m, and 0.34 mV at 6 m, implying that defect detection was difficult.
To further investigate the significant reduction in the DCVG signals for shielded defects compared to non-shielded defects under identical applied voltages, a cross-sectional potential distribution analysis was conducted through simulations, as shown in
Figure 21.
Figure 21 illustrates the simulated cross-sectional potential distribution for shielded and non-shielded coating defects in a buried pipeline.
Figure 21a represents the distribution for a non-shielded defect, while
Figure 21b shows the distribution for a shielded defect. In the case of the non-shielded defect, the potential was widely distributed throughout the surrounding soil (blue regions). Conversely, for the shielded defect, potential variations were confined within the shielded region, with minimal distribution into the surrounding soil.
These results confirmed that in the presence of shielded defects, the non-conductive space created by coating disbond restricts the flow of the survey current, significantly reducing the sensitivity of DCVG signals. This finding suggests that while the DCVG technique is effective for detecting non-shielded defects, its capability may be limited for shielded defects due to weakened detection signals. This trend is consistent with field reports, including that of Choi et al. [
37], where shielding reduced signal detectability despite the presence of active corrosion. Such consistency supports the validity of the simulation model.