1948
DOI: 10.1109/t-aiee.1948.5059797
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A Transmission Line Fault Locator Using Fault-Generated Surges

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Cited by 20 publications
(4 citation statements)
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“…Its use was implemented initially in the middle of the 20th century by Stevens and Lewis [5,6] but they were gradually abandoned 1970s later due to their high cost, poor reliability and maintenance problems. In general, the methods are founded on the work of Carson [7,8] and are based on measure the time that takes the wavehead to propagate from the point where a discontinuity occurs in the line to the measuring terminals.…”
Section: Travelling Wave Based Fault Locationmentioning
confidence: 99%
“…Its use was implemented initially in the middle of the 20th century by Stevens and Lewis [5,6] but they were gradually abandoned 1970s later due to their high cost, poor reliability and maintenance problems. In general, the methods are founded on the work of Carson [7,8] and are based on measure the time that takes the wavehead to propagate from the point where a discontinuity occurs in the line to the measuring terminals.…”
Section: Travelling Wave Based Fault Locationmentioning
confidence: 99%
“…The analysis of the reflected signals, together with additional information about the cable, yields the estimation of the position and characteristics of the discontinuity points in the cable. The first and more natural application of reflectometry is cable fault detection and localization [ 1 ], but this technique has also been used for many other measurement problems over the years. Some examples are liquid levels and properties monitoring [ 2 ], measurement of salinity and humidity in materials [ 3 , 4 ], measurement of complex soil dielectric permittivity [ 5 ], and skin hydration monitoring [ 6 ].…”
Section: Introductionmentioning
confidence: 99%
“…1. They basically operate as time-domain reflectometry methods, exploiting the fault surge signal v f (t) itself to estimate the fault distance [4], e.g., by measuring the propagation delay between the first observation of the fault surge and subsequent reflections over the fault. To do so, TWM need to separate impinging and reflected portions of the fault transient signal, which may require relatively large bandwidths, potentially a drawback, but also the reason behind their good spatial resolution.…”
Section: Introductionmentioning
confidence: 99%