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Xi'an Xu&Hui Electromechanical Technology Co., Ltd.

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China Cable Fault Locator |Low Voltage Hidden Acoustic Magnetic Synchronization
China Cable Fault Locator |Low Voltage Hidden Acoustic Magnetic Synchronization

  1. China Cable Fault Locator |Low Voltage Hidden Acoustic Magnetic Synchronization
  2. China Cable Fault Locator |Low Voltage Hidden Acoustic Magnetic Synchronization
  3. China Cable Fault Locator |Low Voltage Hidden Acoustic Magnetic Synchronization

Cable Fault Locator |Low Voltage Hidden Acoustic Magnetic Synchronization

  1. MOQ: 1unit
  2. Price: Negotiable
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Payment Terms T/T
Supply Ability 3000unit/year
Delivery Time 5-8 work days
Packaging Details wooden packaging
Brand Name XZH TEST
Model Number XHHD530M
Certification ISO/CE
Place of Origin Xi'an, Shaanxi, China

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Product Specification

Payment Terms T/T Supply Ability 3000unit/year
Delivery Time 5-8 work days Packaging Details wooden packaging
Brand Name XZH TEST Model Number XHHD530M
Certification ISO/CE Place of Origin Xi'an, Shaanxi, China
High Light Concealed Cables Cable Fault Locator ,Precise Location Cable Fault Detector ,Acoustic-Magnetic Synchronization Cable Tester
Product Overview

The XHHD530M Low Voltage Hidden Cable Fault Locator is a dedicated instrument for finding faults on underground and concealed low-voltage lines. It is used by the power, broadcast and postal sectors as well as by industrial and mining enterprises and rural users to locate underground cables — including direct-buried shielded cable lines and buried lines — and to identify their faults.

It can detect the route of a buried line, its approximate underground position and basic burial depth, and can locate various earth-leakage faults and broken-core faults. It also works on lines under paddy fields, under concrete, brick, stone or asphalt pavement, on lines inside building walls, and on waterproof cable and cable laid on the ground, all of which can be detected with the appropriate method.

The fault locator consists of a signal transmitter, a signal receiver, a probe and probe rod, and insertion rods. Both the transmitter and the receiver are small, well-built and neatly styled. The instrument offers high sensitivity, strong acoustic-meter synchronization and anti-interference capability, and is easy to carry and quick and accurate in locating fault points. The receiver uses acoustic-meter synchronization with high and low sensitivity gears; the transmitter provides output indication and a KΩ measurement function that can replace a multimeter or a megger to check line continuity, open and mixed faults, and measure earth leakage resistance to determine the nature of the fault. The transmitter adds an "Output 2" terminal that widens the detection methods and functions.

Key Features
High-sensitivity reception with acoustic-meter synchronization
Strong anti-interference capability for on-site work
Receiver with high and low sensitivity gears
Transmitter with output indication and a KΩ measurement function that can replace a multimeter or megger
Extra "Output 2" terminal for finding direct line-to-line short-circuit faults
Compact, well-built transmitter and receiver, easy to carry
Working Principle

The instrument is composed of a transmitter, a receiver, a probe rod and a probe, a set of insertion rods and plugs, and connecting lines.

The transmitter mainly outputs an intermittent pulse signal as the signal source for fault location, and its KΩ function checks line continuity, open and mixed faults, and measures leakage resistance to determine the nature of the fault. Its "Output 2" terminal outputs a large current.

The receiver uses the probe and the insertion rods to pick up, by the induction method and the insertion method, the space magnetic-field signal and the ground electric-field signal produced by the transmitter signal along the line. After amplification and processing by the receiver, these are turned into sound and meter-pointer deflection.

Detection Principles Induction method

When a pulse signal is fed into the line, a magnetic field exists in the space around the line. The induction method uses the probe to sense and receive the space magnetic-field signal, which is amplified by the receiver into sound and meter-pointer deflection. By listening to the loudness of the speaker and observing the amplitude of the pointer swing, the operator determines the route of the buried line, the general area of the fault point, the accurate position of the buried line and its basic burial depth.

Insertion method

After the pulse signal is fed into the buried line, a regular distributed electric field related to the nature of the fault forms on the ground surface above the line and the fault point. The insertion method uses two insertion rods to pick up the potential difference between two points in the distributed electric field; after amplification by the receiver this becomes pointer swing and sound. By observing the size and direction of the pointer swing and the loudness of the sound, the operator accurately determines the underground position of the buried line and the exact position of the fault point.

Technical Specifications
Item Specification
Transmitter output signal form Pulse period 1.34 ± 0.15 ms; width 0.2 ± 0.1 ms; intermittent period 1.8 ± 1 s
Transmitter output voltage (pulse Upp) High gear > 1000 V; medium gear > 60 V; low gear > 30 V
KΩ measurement Checks line continuity, open and mixed faults and leakage resistance to determine the nature of the fault
"Output 2" terminal Peak pulse short-circuit current 1–5 A
Output power Pulse power > 2.5 W (high gear, load resistance 80 KΩ)
Transmitter power supply 8.4 V
Receiver signal form Pulse period ≈ 1.36 ms; width ≈ 0.2 ms; intermittent period 1.8 s
Receiver power supply 6 V (4 × AA batteries)
Detection range and accuracy For a 3 km line, 2 m depth, earth short-circuit or leakage fault with leakage resistance below 500 kΩ: insertion positioning error < 0.2 m. For a 1 km line, 2 m depth, good-insulation broken-core fault: positioning error < 0.4 m. Actual detectable length can exceed 1–5 km with depth of 2–3 m
Anti-interference The received signal is clear enough to detect buried-line faults under 220 kV lines
Working conditions Continuous operation at ambient temperature −15 °C and atmospheric pressure 86–108 kPa
Operating Guide Checking before use
Transmitter: set the power switch to "On"; the power indicator should light and a faint intermittent oscillation sound should be heard. Set the output selection switch to high, medium or low. With the function switch set to "Output indication", the meter pointer swings with the output; with it set to "KΩ measurement", short-circuit the two output terminals and the pointer should read KΩ zero — this shows the transmitter is working normally and can feed a signal to the line or be used for KΩ measurement.
Receiver: open the battery cover on the back and fit AA batteries, taking care not to reverse the polarity. Set the power switch to "On"; the power indicator should light. Set the function switch to the high gear and a faint noise should be heard, showing the receiver is normal. Insert the probe plug into the receiver and bring the probe close to the speaker area — a self-excited whistle should be heard, showing the probe is intact and the receiver is working normally; otherwise check the probe and plug for broken or mixed lines.
Determining the nature and type of the fault

First separate the faulty line at both the leading-in and leading-out ends, including branch loads and meters connected to the faulty line, and then cut off the power before making KΩ measurements. When measuring, both exposed ends of the buried line must be left dangling separately, and must not touch each other or the ground. Measure KΩ for each line from one leading-out end and record the earth resistance of each line to find the fault-line earth resistance and judge the nature and type of the fault. If necessary, do the same test at the other end. Feed the test signal into the line with the smaller earth resistance. This process also verifies whether the transmitter is working normally.

Leakage-to-earth faults: most buried-line faults are caused by damage to the insulation layer causing leakage, or corrosion burning the line so it cannot carry power. These include non-broken-core high-resistance and broken-core high-resistance faults, low-resistance earth faults, line-to-line short-circuit high- and low-resistance earth faults, and near-metallic earth faults with large-area insulation damage. For detection purposes, earth faults are divided by earth resistance: about 20 kΩ and below is low-resistance earthing; between 20 and 500 kΩ is high-resistance earthing.
Good-insulation broken-core fault: the core is broken so power cannot be supplied, and the earth resistance is above MΩ.
Induction detection of route, position, depth and faults

Make the transmitter and receiver work normally. Connect the black output terminal to earth (with a good earth connection, not shared with other earth lines) and the red terminal to the buried line or faulty line. Select the output gear according to the fault type — for measuring the route only, medium or high gear can be used. Set the receiver function switch to the high gear and bring the probe near the transmitter or the buried line; the receiver speaker gives an intermittent "du-du-du" sound. Changing the position of the probe relative to the buried line changes the loudness, and the position with the loudest sound is directly above the buried line's route. Walking along the direction of loudest sound gives the line's laying direction; the accurate underground position and basic burial depth are found by experience.

Low-resistance earth fault (including broken-core low-resistance earthing): set the transmitter to low gear and detect from the signal-feeding end. At first the sound is roughly constant; when the sound clearly decreases at some point and, after walking another 3–5 m, the decreased signal is still heard, the low-resistance earth fault point is about 0.3–0.5 m back from where the sound clearly decreased. This method also applies to broken-core earthing faults.
Good-insulation broken-core fault: the method is basically the same, but the signal is weaker, so set the output selection to medium or high gear. For greater accuracy, use the "two-time positioning method": feed the signal from one end and mark where the decreased signal is no longer heard after 3–5 m; then feed from the other end and mark similarly; the point below the middle of the line joining the two marks is the broken-core fault point. This method also applies to low-resistance earthing and broken-core low-resistance earthing faults, but must not be used when a line has two faults — solve one fault first.
Broken-core detection of waterproof lines and in-wall lines: the method is the same, except the probe can come within about 0.3 m of the line, so the sound increases and the pointer also swings. When the pointer swing clearly decreases, the fault point is 0.1–0.2 m back. Waterproof line can be laid flat on the ground, with the black terminal earthed and the red terminal connected to the faulty line.
Short-circuit fault of waterproof lines and in-wall lines: the method is the same, except the black output terminal is not earthed — the red and black terminals are connected to the two short-circuited lines. When the sound and pointer swing suddenly increase at some point, that is the fault point. Note that the transmitter operates in short-circuit mode and consumes a lot of battery, so it should not run for long; use low gear or the "Output 2" terminal.
Insertion detection of route, position and exact fault point

Make the transmitter and receiver work normally. Connect the black output terminal to earth with a good earth connection placed in the direction opposite to the buried line and in line with it; if the fault point is close to the signal-feeding end, the earthing point should be 5–10 m away from the feeding point. Connect the red terminal to the buried or faulty line and set the output selection to low gear. Set the receiver function switch to high gear and insert the two insertion-rod plugs into the receiver input socket (the probe and the rods share one socket). Hold the receiver in one hand and the red and black rod handles in the other, bring the two tips near the transmitter, then draw the tips about 0.5 m apart and insert them into the ground near the buried line; an intermittent "du-du" sound is heard and the pointer swings with the pulses — otherwise check the rod connections and plugs for broken or mixed lines.

Then separate the two rod tips by a distance chosen between 0.1 and 0.5 m, so that after insertion the pointer swing is about 1–5 divisions. Insert vertically to the line's direction, keeping the red rod in front and the black rod behind, and observe the pointer direction: if it swings to "+", move the two rods toward the red rod; if it swings to "−", move them toward the black rod, until the sound is minimal and the pointer is basically still — then the midpoint between the two rod insertion points is directly above the accurate underground position of the buried line. This is the "lateral symmetric method". It can be verified by the "lateral verification method": keep one rod fixed at the midpoint and insert the other rod at two points on either side; the pointer direction and magnitude, and the sound, should be the same, confirming the accurate midpoint. Inserting every 3–10 m along the general direction finds several midpoints whose line is the accurate route, position and direction of the buried line.

The "longitudinal symmetric method" can also be used: insert the two rods directly above the buried line along its direction, red rod first and black rod behind, with the same rod spacing. When the sound increases but the pointer swing decreases, reduce the rod spacing or switch to the low-sensitivity gear. If the pointer changes from "+" to "−", the fault point has been passed; move the rods back carefully in small steps (or fix one rod and move the other) until the sound is minimal and the pointer is basically still — the midpoint below the two rod insertion points is the fault point. This can be verified by the "longitudinal symmetric verification method", the "cross intersection method" (combining lateral and longitudinal midpoints), the "equipotential circle verification method", the "X-type verification method", and the "long-distance insertion method" with its lateral-side and equal-distance comparison, side-angle, short-distance and two-time comparison variants. Under difficult ground (concrete, brick, or frozen in winter) the rods may be wrapped with water-soaked cloth ("moistening method") to improve contact. Because the electromagnetic field above a buried line is complex, false points may appear near leading-out sections, joints, coils, T-branches, corners, crossings with other buried lines and metal pipes, and changes in burial depth; the nature of the fault must be confirmed and the appropriate verification method used to eliminate false points. All earth-leakage faults are verified by the "equipotential circle verification method".

Precautions
During use, the transmitter must never be connected to a live power line — the line under test must not be live, from the start of testing until power is restored, to protect people and prevent burning out the transmitter.
Before detection, a "KΩ measurement" must be carried out first to confirm the faulty line, the nature and type of the fault and the size of the leakage resistance; this also checks whether the transmitter works normally and whether the wiring is correct. Multiple KΩ measurements can be made during detection to observe any change in the KΩ value.
When using the insertion method, if the sound increases but the pointer swing decreases, reduce the rod spacing again or switch to the low-sensitivity gear.
If the feeding point is close to the fault point, move the transmitter's working earth 5–20 m in the direction opposite to the buried line and set the output selection to medium or low gear, or feed the signal from the other end.
In paddy fields or water, simply place the copper tips in the water; the insertion method is unchanged.
Remove the batteries when the instrument is not in use; there are no adjustment parts inside, so the case need not be opened.
Replace the receiver batteries when the voltage drops from 6 V to 5 V or below; recharge the transmitter battery when it drops from 9 V to 7.5 V.
Store the instrument in a dry, ventilated place and protect it from moisture and corrosive gases.
Under conditions of proper use and maintenance, the instrument carries a one-year warranty.
Who It Is ForField crews facing lines under concrete, brick, stone or asphalt pavement, who need to find both the route and the exact fault point.FAQ

Q1. What can the XHHD530M detect?
The XHHD530M is a dedicated instrument for finding faults on underground and concealed low-voltage lines. It can detect the route, approximate underground position and basic burial depth of a buried line, and can locate earth-leakage faults and broken-core faults — including lines under paddy fields, under concrete, brick, stone or asphalt pavement, inside building walls, and waterproof cable laid on the ground.

Q2. How are the induction method and the insertion method different?
The induction method uses the probe to sense the space magnetic-field signal around the line, giving the route, the general fault area and the burial depth. The insertion method uses two insertion rods to pick up the potential difference of the distributed electric field on the ground, and gives the accurate underground position and the exact fault point.

Q3. What is the KΩ measurement function for?
The transmitter's KΩ function can replace a multimeter or a megger to check line continuity, open and mixed faults, and to measure earth leakage resistance, so the nature and type of the fault can be determined. It should be carried out before detection and can be repeated during detection to see whether the KΩ value changes.

Q4. What are the accuracy and working conditions?
For a 3 km line at 2 m depth with an earth short-circuit or leakage fault below 500 kΩ, the insertion positioning error is less than 0.2 m; for a 1 km line at 2 m depth with a good-insulation broken-core fault, the error is less than 0.4 m. The instrument works continuously at −15 °C and 86–108 kPa, and can detect faults under 220 kV lines.

Q5. What must be noted during use, and what is included?
The transmitter must never be connected to a live line — the line under test must not be live throughout testing. After detection, the earth-leakage fault should be verified with the equipotential circle verification method to remove false points, and in short-circuit detection the transmitter runs in short-circuit mode so it must not work for long. The instrument carries a one-year warranty under proper use and maintenance. The package includes one transmitter, one receiver, one probe, one probe rod, two insertion rods (red and black), two connecting lines and one charger


Company Details

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 from Quality China Factory
  • Business Type:

    Manufacturer

  • Year Established:

    2013

  • Total Annual:

    1000000-5000000

  • Employee Number:

    50~100

  • Ecer Certification:

    Verified Supplier

                        Xi'an Xu&Hui Electromechanical Technology Co., Ltd. /Xian XZH Electric Power Technology Co., Ltd. Has found in 2013, located in Xi'an, China. which is a highly experienced team dedicated to developing electrical...                         Xi'an Xu&Hui Electromechanical Technology Co., Ltd. /Xian XZH Electric Power Technology Co., Ltd. Has found in 2013, located in Xi'an, China. which is a highly experienced team dedicated to developing electrical...

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  • Xi'an Xu&Hui Electromechanical Technology Co., Ltd.
  • Building B8-01, Phase I, Ronghao Industrial City, No. 2098, Weiyang 9th Road, Gaoling District, Xi'an, China
  • https://www.xzhtest.com/

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