Leakage location methods
Abstract
A method of determining the location and/or amplitude of a leakage signal from a network includes measuring at various times and locations leakage believed to be associated with the leakage signal and constructing a data base of leakages and associated locations. Leakage signal values are selected from the data base. Each of the selected leakage signal values is multiplied by a locus of points on which a leakage signal associated with that respective signal strength may be assumed to reside in order to develop a number of relationships among leakage signal strength, leakage and location. A first pair of these relationships among leakage signal strength, leakage and location is solved for a first locus of points common to the first pair. A second pair of these relationships among leakage signal strength, leakage and location is solved for a second locus of points common to the second pair. The first and second loci are projected onto a common surface, and an intersection of the thus-projected first and second loci on the common surface is determined.

Term
Projected expiry 7 August 2027.
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12 claims: 2 independent, 10 dependent
- 1CA 02596213 2007-08-07 What is claimed is:1. A method of determining the location of a leakage signal from a network, the method including measuring at various times and locations leakage believed to be associated with the leakage signal, constructing a data base of leakages and associated locations, selecting 5 from the data base a number of leakage values, multiplying each of the selected leakage signal value times a locus of points on which a leakage signal associated with that respective signal strength may be assumed to reside to develop a number of relationships among leakage signal strength, leakage and location, solving a first pair of these relationships among leakage signal strength, leakage and location for a first locus of common points to the first pair, solving a 10 second pair of these relationships among leakage signal strength, leakage and location for a second locus of common points to the second pair, projecting the first and second loci onto a common surface, and determining the intersection of the first and second loci on the common surface.
- 7A method of determining the amplitude of a leakage signal from a network, the method including measuring at various times and locations leakage believed to be 5 associated with the leakage signal, constructing a data base of leakages and associated locations, selecting from the data base a number of leakage values, multiplying each of the selected leakage signal value times a locus of points on which a leakage signal associated with that respective signal strength may be assumed to reside to develop a number of relationships among leakage signal strength, leakage and location, solving a first pair of these relationships among 10 leakage signal strength, leakage and location for a first locus of common points to the first pair, solving a second pair of these relationships among leakage signal strength, leakage and location for a second locus of common points to the second pair, projecting the first and second loci onto a common surface, and determining the intersection of the first and second loci on the common surface. 15
Independent claims2
89 paragraphs in 5 sections, as filed
CA 02596213 2007-08-07
LEAKAGE LOCATION METHODS
Background of the Invention
This invention relates to methods for determining the location of leakage from, for example, CATV cables, taps, fittings, drops and other CATV plant facilities.
Disclosure of the Invention
A method of determining the location of a leakage signal from a network includes measuring at various times and locations leakage believed to be associated with the leakage signal and constructing a data base of leakages and associated locations. Leakage signal values are selected from the data base. Each of the selected leakage signal values is multiplied by a locus of points on which a leakage signal associated with that respective signal strength may be assumed to reside in order to develop a number of relationships among leakage signal strength, leakage and location. A first pair of these relationships among leakage signal strength, leakage and location is solved for a first locus of points common to the first pair. A second pair of these relationships among leakage signal strength, leakage and location is solved for a second locus of points common to the second pair. The first and second loci are projected onto a common surface, and an intersection of the thus-projected first and second loci on the common surface is determined.
Further illustratively, the method includes determining the strength of the leakage signal by substituting the intersection of the first and second loci on the common surface back into a selected relationship among leakage signal strength, leakage and location and solving for the strength of the leakage signal.
Illustratively, solving a first pair of the relationships among leakage signal strength, leakage and location for a first locus of common points to the first pair and solving a second pair of the relationships among leakage signal strength, leakage and location for a second locus of common points to the second pair together comprise selecting a location about which the solutions are to be normalized and solving the first and second pairs of the relationships about the location about which the solutions are to be normalized.
CA 02596213 2007-08-07
Illustratively, solving a first pair of the relationships among leakage signal strength, leakage and location for a first locus of common points to the first pair and solving a second pair of the relationships among leakage signal strength, leakage and location for a second locus of common points to the second pair, and projecting the first and second loci onto a common surface together comprise converting an angular distance into a linear distance.
Illustratively, converting an angular distance into a linear distance comprises using a table to convert an angular distance into a linear distance.
Alternatively or additionally illustratively, converting an angular distance into a linear distance comprises calculating a linear distance from an angular distance.
Brief Description of the Drawings
The invention may best be understood by referring to the following detailed description and accompanying drawings which illustrate the invention. In the drawings:
Fig. 1 illustrates a perspective view useful in understanding the present invention;
Fig. 2 illustrates a graph useful in understanding the present invention;
Fig. 3 illustrates a plan view useful in understanding the present invention; and,
Fig. 4 illustrates a graph useful in understanding the present invention.
Detailed Descriptions of Illustrative Embodiments
Leakage measurements of signal from a CATV plant including, for example, CATV cables, taps, fittings, drops and other CATV plant facilities, may readily be made by, for example, CATV system employees during their conduct of their daily activities. Such leakage measurements, stored in leakage measurement equipment of the type described in, for example, Trilithic Seeker GPS leakage management system available from Trilithic, Inc., 9710 Park Davis Drive, Indianapolis, IN 46235, are uploaded from such CATV system employee equipment into a server at a CATV headend, for example, at the ends of the employees’ shifts. Such CATV system employees’ daily activities may include, for example, visiting subscriber sites to conduct maintenance and repairs, driving the CATV system to log leakage levels, and so on.
This activity can provide a database of cable system leakage strengths measured at multiple locations, which can be determined with considerable accuracy by associating with each such measurement a location, such as a latitude and longitude provided by a Global
CA 02596213 2007-08-07
Positioning System (GPS) device. Such data sets might look like the following table when sorted in order of descending detected leakage level and eliminating leakage levels below a certain threshold (10 μΥ in this example):
<td> 5</td><td> Latitude</td><td> Longitude</td><td> Leakage (pV or other suitable dimension)</td>
<td></td><td> 39.502145°</td><td> -85.594748°</td><td> 26</td>
<td></td><td> 39.502003°</td><td> -85.594720°</td><td> 23</td>
<td></td><td> 39.502089°</td><td> -85.594722°</td><td> 21</td>
<td></td><td> 39.502066°</td><td> -85.594746°</td><td> 20</td>
<td> 10</td><td> 39.502131°</td><td> -85.595057°</td><td> 19</td>
<td></td><td> 39.502223°</td><td> -85.594751°</td><td> 16</td>
<td></td><td> 39.502210°</td><td> -85.595003°</td><td> 16</td>
<td></td><td> 39.502188°</td><td> -85.595096°</td><td> 16</td>
<td></td><td> 39.502183°</td><td> -85.595142°</td><td> 16</td>
<td> 15</td><td> 39.502208°</td><td> -85.594939°</td><td> 15</td>
<td></td><td> 39.502011°</td><td> -85.594726°</td><td> 14</td>
<td></td><td> 39.502145°</td><td> -85.594750°</td><td> 14</td>
<td></td><td> 39.502303°</td><td> -85.594753°</td><td> 13</td>
<td></td><td> 39.502054°</td><td> -85.594725°</td><td> 13</td>
<td> 20</td><td> 39.502196°</td><td> -85.595049°</td><td> 13</td>
<td></td><td> 39.502172°</td><td> -85.595028°</td><td> 13</td>
<td></td><td> 39.502095°</td><td> -85.594724°</td><td> 12</td>
<td></td><td> 39.502094°</td><td> -85.595056°</td><td> 12</td>
<td></td><td> 39.502182°</td><td> -85.595002°</td><td> 12</td>
<td> 25</td><td> 39.502194°</td><td> -85.594972°</td><td> 12</td>
<td></td><td> 39.502098°</td><td> -85.594727°</td><td> 11</td>
<td></td><td> 39.502175°</td><td> -85.594723°</td><td> 11</td>
<td></td><td> 39.502226°</td><td> -85.594959°</td><td> 11</td>
<td></td><td> 39.502226°</td><td> -85.594959°</td><td> 11</td>
<td> 30</td><td> 39.502181°</td><td> -85.595188°</td><td> 11</td>
<td></td><td> 39.502067°</td><td> -85.595321°</td><td> 11</td>
CA 02596213 2007-08-07
<td> 39.502062°</td><td> -85.595106°</td><td> 11</td>
<td> 39.502063°</td><td> -85.594713°</td><td> 11</td>
<td> 39.502175°</td><td> -85.594727°</td><td> 10</td>
<td> 39.502114°</td><td> -85.595058°</td><td> 10</td>
<td> 39.502146°</td><td> -85.595055°</td><td> 10</td>
<td> 39.502160°</td><td> -85.595045°</td><td> 10</td>
Using this data, which, again, is typically extracted from a larger data set accumulated over days, weeks, months, etc., of data collection and then sorted and limited by differences of latitude and longitude from the largest system leak in the list, the location and magnitude of a leakage source giving rise to this data may be isolated. The method employs leakage signal strength versus distance considerations.
Leakage detectors and their associated antenna systems are calibrated to be accurate at a fixed distance from a radiation source, such as the source of a leak. It is not uncommon in the CATV industry to use three meters as a measurement standard. So, in the case of a 10 pV/m leak, for example, which is calibrated to be accurate at a distance of three meters from the leakage source, a leak indicated as having a strength of 10 pV/m could reside anywhere on a radius three meters from the leakage antenna. If the leakage strength were doubled to 20 pV/m and the antenna were six meters from the source, the leakage detecting instrument would still indicate a leakage signal strength of 10 pV/m. So, for a given measured 10 pV/m leak, one can envision an inverted cone of potential leakage sources and leakage signal strengths which would all give rise to the same 10 pV/m reading at the location of the leakage detecting antenna, with the x and y dimensions of the cone being the longitude and latitude of the cone’s surface at various points and z being the indicated strength of the leakage signal. In this example, there is a three meter circle of potential 10 pV/m leaks around the leakage antenna, a six meter circle of 20 pV/m leaks, a nine meter circle of 30 pV/m leaks, and so on in circles of increasing radius at increasing heights (z values) corresponding to increasing leakage signal strength. If one imagines the location for this 10 pV/m reading on the leakage detector to be defined by latitude and longitude coordinates with x mapping to longitude, y mapping to latitude and z mapping to leakage level, then the increasing circles around the current location of the leakage detector can be visualized as a cone standing on its apex. Every leak stored in the database can be
CA 02596213 2007-08-07 represented in this way with its apex at the GPS-determined position of the antenna at the time the particular leakage signal strength is measured. The equation for each leakage cone may then be written as:
z = Lisqrt((x - xj<sup>2</sup> + (y - yi)<sup>2</sup>) where sqrt is the square root operator;
Li = the measured leakage value at a calibrated distance (three meters in the following examples);
xi = the longitude of the measured leak; and, yi = the latitude of the measured leak.
For purposes of this discussion, z<sub>n</sub> will indicate the nth detected leak. Using (arbitrarily) the first four rows of the above data set, the following four equations are obtained:
zi = Lisqrt((x - xi)<sup>2</sup> + (y - yi)<sup>2</sup>);
z<sub>2</sub> = L<sub>2</sub>sqrt((x - x<sub>2</sub>)<sup>2</sup> + (y - y<sub>2</sub>)<sup>2</sup>);
z<sub>3</sub> = L<sub>3</sub>sqrt((x - x<sub>3</sub>)<sup>2</sup> + (y - y<sub>3</sub>)<sup>2</sup>); and,
Z4 = L<sub>4</sub>sqrt((x - Χ4)<sup>2</sup> + (y - y<sub>4</sub>)<sup>2</sup>), where x„, y<sub>n</sub> and z„ are the longitude, latitude and leakage signal strength displayed in the nth row of the above table, and
Li = 26/3 pV/m;
L<sub>2</sub> = 23/3 pV/m;
L<sub>3</sub> = 21/3 pV/m; and
L<sub>4</sub> = 20/3 pV/m, using the above convention, leakage signal strength detected at three meters from the leakage antenna. From the above table:
xj = -85.594748°;
CA 02596213 2007-08-07 x<sub>2</sub> = -85.594720°;
x<sub>3</sub> = -85.594722°;
X4 = -85.594746°;
yi = 39.502145°;
y<sub>2</sub> = 39.502003°;
y<sub>3</sub> = 39.502089°; and, y<sub>4</sub> = 39.502066°.
If the intersection of two adjacent inverted cones, for example, zi and z<sub>2</sub>, is plotted, the intersection is an arc 20, as illustrated in Fig. 1. An enlarged, two dimensional illustration of this intersection is illustrated in Fig. 2. If the intersection of another two adjacent inverted cones, for example, z<sub>3</sub> and Ζ4, is then plotted, another similar intersection is formed. Look down from above on the two arcs formed by the intersections of pairs of the four data points, a point of intersection is illustrated in Fig. 3.
Again, looking into any of these cones zi, z<sub>2</sub>, z<sub>3</sub>, Z4 from above, at any given leakage signal strength (that is, any vertical elevation), it may be visualized as a circle. In Fig. 3, circle 30 illustrates the downward view along the z axis of zj. Circle 32 illustrates the downward view along the z axis of z<sub>2</sub>. Continuing to look down from above, then, the intersection of these two inverted cones is the arc 20. Circle 36 illustrates the downward view along the z axis of z<sub>3</sub>. Circle 40 illustrates the downward view along the z axis of Z4. The intersection of the cones z<sub>3</sub> and Z4 is the arc 42. Arcs 20,42 projected downward intersect at a point 44 in latitude and longitude, which is the calculated location of the leak which is the source of this data.
Now that a specific x and y, that is, longitude and latitude, of interest have been identified, those values can be substituted back into any one of the equations above for zi, z<sub>2</sub>, z<sub>3 </sub>or Z4 to calculate the strength of the leak at that x and y. For purposes of illustration, the equation for Zi will be used to demonstrate this. First, the differences (y - y 1 ) and (x - Xi) in latitude and longitude need to be converted into meters. Tables stored in instruments such as the above-mentioned server at a CATV headend, a separate computer associated therewith, or calculators provided in such instruments, or some combination of these, are used for these conversions, since such conversions depend upon the latitudes and longitudes which are the
CA 02596213 2007-08-07 subjects of the calculations, that is, upon the curvature of the earth’s surface at the latitudes and longitudes of interest. See, for example, http://www.csgnetwork.com/degreelenllavcalc.html, for such a calculator.
zi = (26/3)sqrt((x + 85.594748°)<sup>2</sup> + (y - 39.502145°)<sup>2</sup>);
z<sub>2</sub> = (23/3)sqrt((x + 85.594720°)<sup>2</sup> + (y - 39.502003<sup>0</sup>)<sup>2</sup>);
z<sub>3</sub> = (21/3)sqrt((x + 85.594722<sup>0</sup>)<sup>2</sup> + (y - 39.5Ο2Ο89<sup>0</sup>)<sup>2</sup>); and,
Z4 = (20/3)sqrt((x + 85.594746°)<sup>2</sup> + (y - 39.502066°)<sup>2</sup>).
The longitudes and latitudes are normalized to coordinates which lie fairly centrally among them, in this case, -85.594735°, 39.502070°. See Fig. 4. This particular point is at about the intersection of a line drawn between (xi, yi) and (x<sub>2</sub>, y<sub>2</sub>) and a line drawn between (x<sub>3</sub>, y<sub>3</sub>) and (x4, y4). This point can also be determined by solving the simultaneous equations (y - yi)/(x - xi) <sup>=</sup> (y2 - yι)/( X2 - xi) and (y - y<sub>3</sub>)/(x - x<sub>3</sub>) = (y4 - yi)l( X4 - X3) for x and y. Normalization is performed to implement the above-discussed conversion to meters, which then yields the leakage field strength in pV/m. The calculations thus become:
zi = (26/3)sqrt((.000013°)<sup>2</sup> + (-.000075<sup>0</sup>)<sup>2</sup>);
z<sub>2</sub> = (23/3)sqrt((-.000015°)<sup>2</sup> + (.000067<sup>0</sup>)<sup>2</sup>);
z<sub>3</sub> = (21/3)sqrt((-.000013°)<sup>2</sup> + (-.000019°)<sup>2</sup>); and,
Ζ4 = (20/3)sqrt((.000011°)<sup>2</sup> + (.000004<sup>0</sup>)<sup>2</sup>), where, at this latitude and longitude, 14 X 10'<sup>6</sup>° ~ 1.55435 m and 67 X 10<sup>6</sup>° ~ 5.76273 m at x = -85.594735° and y ~ 39.502070°. Picking zi and converting the latitude and longitude differences to meters as discussed above yields a leakage strength of about 51.7285 pV/m at the location of the leak.
Fig. 4 illustrates the projected leakage position graphically from the latitudes yi,.
.. y4 and longitudes Xi,... Χ4 of the four measured leakage signal strengths Zi,... Z4.
Contents5
5 sheets
Sheet 1 Sheet 2 Sheet 3 Sheet 4 Sheet 5
8 priority claims, no other members on record
Priority claims8
| Document | Office | Kind | Date |
|---|---|---|---|
| 60836036 | United States of America | – | |
| 83603606 | United States of America | P | |
| 11742184 | United States of America | – | |
| 74218407 | United States of America | A | |
| 11742184 | – | – | – |
| 60836036 | – | – | – |
| US20060836036P | – | – | – |
| US20070742184 | – | – | – |
2 legal events, as the office reported them to INPADOC
Over the term
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| Event | Code | |
|---|---|---|
| LapsedLapsedMKLA | MKLA | |
| Examination requestEEER | EEER |
Numbers
- Publication
- 2596213
- Publication, DOCDB
- 2596213
- Publication, EPODOC
- CA2596213
- Application
- 2596213
- Application, DOCDB
- 2596213
- Application, EPODOC
- CA20072596213
Titles2
- English
- LEAKAGE LOCATION METHODS
- French
- METHODES DE LOCALISATION DE FUITES
Classification
- CPC, 4
- G01R31/025
- G01R31/52
- G01R31/50
- G01R31/001
- IPC, 3
- G01R31 08
- H04B3 46
- H04N17 00