6.5 Cable Fault Locating
Key Takeaways
Cable fault locating is a two-stage process: prelocation narrows the fault to a distance along the cable, then pinpointing finds it within a few feet at the surface.
A low-voltage TDR finds opens, splices, and low-resistance faults, but a high-resistance fault is invisible to it until a surge creates a temporary arc.
Arc reflection combines a surge generator with a TDR so the momentary arc appears as a low-impedance reflection on the trace, which is the standard method for high-resistance faults.
Distance from a TDR trace depends on the cable's velocity of propagation, so using the wrong VOP scales every measured distance by the same error.
Sheath and jacket faults are located with a DC voltage applied to the sheath and an A-frame earth-gradient receiver, not with a TDR.
Why Fault Locating Is Its Own Skill
A megger tells you a cable is bad. It does not tell you where. On a 2,400 ft medium-voltage feeder in duct bank, the difference between knowing the fault is at 340 ft and not knowing is the difference between one excavation and twelve. The Level 2 DCO lists cable fault locating as an explicit knowledge item under Cables, and the exam tests method selection rather than instrument operation.
The workflow is always the same four steps:
- Isolate, verify dead, and ground both ends. Discharge the cable and keep it grounded until you are ready to test.
- Characterize the fault — is it open, low resistance, high resistance, or a sheath fault? An insulation resistance test and a continuity check answer this in two minutes.
- Prelocate — find the distance to the fault from one end.
- Pinpoint — walk the route and find the fault at the surface within a few feet.
Step 2: Characterizing the Fault
| Test result | Fault type | Prelocation method that works |
|---|---|---|
| Conductor continuity open | Open circuit / broken conductor | TDR (low voltage) |
| Very low IR, low resistance to ground or between phases | Low-resistance (bolted) fault | TDR, or resistance bridge |
| IR low but not zero, or IR normal until voltage is applied | High-resistance / flashover fault | Arc reflection, surge pulse reflection, or decay |
| Conductor good, jacket/sheath resistance to earth low | Sheath or jacket fault | DC voltage plus A-frame earth gradient |
The distinction the exam cares about: a high-resistance fault is invisible to a low-voltage TDR. The fault only conducts when enough voltage is applied to break down the gap, so a 20 V TDR pulse passes straight by it and reflects off the far end. Technicians who do not understand this conclude the cable is healthy.
Prelocation Methods
Time Domain Reflectometry (TDR)
A TDR launches a low-voltage pulse down the cable and displays the reflections. Impedance changes send energy back:
- An open reflects a positive (upward) pulse.
- A short or low-resistance fault reflects a negative (downward) pulse.
- Splices, joints, and taps produce small reflections that are useful landmarks — comparing an as-found trace against a commissioning baseline trace is the fastest way to spot what changed.
Distance comes from the round-trip time and the cable's velocity of propagation (VOP), usually expressed as a fraction of the speed of light or as a velocity factor. Because the pulse travels out and back:
distance = (velocity x round-trip time) / 2
VOP is a property of the insulation. Typical XLPE and EPR power cable runs near 0.5 to 0.56 of the speed of light; paper-insulated lead-covered cable is lower. If you enter the wrong VOP, every distance the instrument reports is wrong by the same percentage. Setting VOP for XLPE and testing a PILC cable can put you 15% off — 60 feet on a 400 ft run. Where a cable of known length is available, calibrate by shooting the open far end and adjusting VOP until the trace reads the true length.
Arc Reflection (ARM)
The workhorse for high-resistance faults. A surge generator (thumper) and a TDR are connected through a filter. The surge breaks down the fault into a temporary arc; the arc is a near short circuit; the TDR — triggered during the arc — sees a clear negative reflection at the fault. The filter protects the TDR from the surge energy. Its advantage over plain thumping is that you get a distance before you start walking, and you can compare the pre-arc and during-arc traces overlaid, which makes the fault unmistakable.
Surge Pulse Reflection (ICE / Impulse Current)
Used when the fault will not hold an arc long enough for arc reflection, or where the fault is at very high resistance. A high-energy surge is applied and the current transient is captured; the fault distance is read from the period of the traveling-wave oscillation. It is more interpretive than arc reflection but works on faults that ARM cannot capture.
Decay (Voltage Decay) Method
For flashover faults that only break down above a voltage the surge generator cannot sustain — typical of faults in joints on long cables with high capacitance. The cable is charged with a DC source until the fault flashes over; the resulting traveling wave is captured and the distance derived from its period. Used with a hipot rather than a thumper.
Bridge Methods (Murray and Wheatstone Loop)
The oldest prelocation technique. The faulted conductor is looped at the far end to a healthy conductor of the same size, and a resistance bridge measures the ratio of the two legs. Fault distance is proportional to that ratio times the total loop length. Requirements and limits worth knowing:
- Needs a healthy return conductor of the same size and length — which is why it suits multi-conductor cable and fails on a single-conductor run.
- Works on low-resistance faults; a high-resistance fault must first be burned down.
- Extremely accurate when its conditions are met, and it needs no expensive instrument.
Pinpointing Methods
Prelocation gets you to a stretch of route. Pinpointing puts you on the spot.
- Acoustic (thumping). The surge generator repeatedly discharges into the fault, producing an audible thump. An acoustic-magnetic receiver listens for the sound and simultaneously senses the magnetic pulse; because the magnetic field arrives essentially instantly and the sound travels at roughly 1,100 ft/s, the time difference between the magnetic and acoustic signals shrinks to zero as you stand over the fault. This is the standard pinpointing method on direct-buried and duct cable.
- Earth gradient / A-frame. For sheath and jacket faults, a DC voltage is applied between the sheath and earth, and an A-frame with two ground probes measures the voltage gradient in the soil. The needle deflects toward the fault and reverses when you pass over it. A TDR cannot find a jacket fault — the conductor insulation is intact.
- Route tracing. Before pinpointing, trace and mark the cable route with a transmitter and receiver so your measured distance follows the actual path. Distance along a cable is not distance across a parking lot; slack in vaults and route bends routinely add 5-10%.
Safety Rules for Thumping
Surge generators store lethal energy and put high voltage on a cable that people may assume is dead.
- Ground and short both ends before and after every test, and discharge through a resistive stick before touching a conductor. A long cable stores enough capacitive charge to kill after the source is removed.
- Guard the far end. The remote termination must be secured and attended or physically isolated; the surge appears there too.
- Limit energy and duration. Every thump degrades cable insulation and can extend a fault or damage sound insulation elsewhere. Use the lowest energy setting that produces a usable signal, prelocate before you thump so you thump for minutes rather than hours, and stop when you have the location.
- Never thump a cable with an unknown or attached load. Disconnect terminations, potheads, and any connected apparatus — transformers, arresters, and PTs will not survive surge energy and will also mask the fault.
Method Selection Summary
| Fault | Prelocate with | Pinpoint with |
|---|---|---|
| Open conductor | TDR | Route trace and TDR distance |
| Low-resistance fault | TDR or bridge | Acoustic thump |
| High-resistance fault | Arc reflection | Acoustic thump |
| Flashover only at high voltage | Decay method | Acoustic thump |
| Sheath / jacket fault | Sheath integrity test | A-frame earth gradient |
A 15 kV feeder megs at 60 megohms phase-to-ground but flashes over during a hipot. A low-voltage TDR shot shows only the far-end open reflection. Why?
The TDR is defective and should be recalibrated
The fault is high resistance and does not conduct at the TDR's low pulse voltage, so no reflection is produced until a surge creates an arc
The cable has no fault; the hipot result was a false positive
TDRs cannot be used on cables rated above 5 kV
A TDR is set for a velocity of propagation appropriate to XLPE cable, but the circuit under test is paper-insulated lead-covered cable with a lower VOP. What is the effect on the result?
No effect — VOP only affects the amplitude of the reflection
Every reported distance is scaled by the same error, so the fault will be dug for in the wrong place
The TDR will fail to display any reflection at all
Only faults beyond 1,000 feet are affected
Which method is used to pinpoint a jacket or sheath fault on a direct-buried cable?
Time domain reflectometry from both ends
Transformer turns ratio testing
A DC voltage applied to the sheath with an A-frame earth-gradient receiver
Acoustic thumping at maximum surge energy
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