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?
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?
Which method is used to pinpoint a jacket or sheath fault on a direct-buried cable?