Submitted:
25 May 2023
Posted:
26 May 2023
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Abstract
Keywords:
1. Introduction
- from seconds to minutes if applying test signals in off-service conditions: time intervals of seconds are necessary for polarization of electrolytes in the test circuit to take place, after which test quantities can be measured with care to reject external noise with a sufficiently long observation times;
- from hours to weeks if using track electric quantities during train service:
- from days to years considering the normal evolution of track insulation degradation, with aging of insulating materials, pollution of surfaces, stagnation of water, etc.
- method A.2, track insulation with civil structure: the important point that makes this less invasive compared to method A.3 is that the running rails are continuous and do not need to be sectioned; however, the test setup is more complex, with more measured quantities involved and an overall worse accuracy; the evaluation of uncertainty and optimal test conditions is discussed in Section 2;
- method A.3, track insulation without civil structure: the presence or absence of the civil structure is not the relevant point here, as the running rails must be sectioned to the desired length, either by cutting them or exploiting the presence of insulating rail joints; this is a more accurate method and should be preferred whenever possible, especially for high track insulation values;
- method A.4, lateral voltage gradient method in open area sites: this method measures the voltage gradient in the soil caused by running trains, with the field laterally extending from the tracks at two points at different distances; it is suitable for large open areas, but necessitates access to soil as homogeneous as possible and may thus be disturbed by buried structures and installations, such as in an urban context.
2. Method A.2: continuous track, line closed to traffic
2.1. Method description and setup
2.2. Practical factors
- The longitudinal impedance of a running rail is made of an internal inductance term and an AC resistance term, both accounting for AC effects such as skin effect and hysteresis, and related losses [33,34]; values for low current () amount to about H/m and 100 /m, with the former contributing less than 25 /m of inductive reactance at 50 Hz.
- The stray capacitance of a running rail amounts to less than 10 nF/m (obtained by multiplying by 2 the values shown in [35]), providing more than 300 of capacitive reactance, easily shunted by the transversal track insulation term considered here.
2.3. Variability and uncertainty analysis
- a long track section is tested: a 10 times longer track ( 1 km) will provide a 10 times larger and the resulting errors will be this time about 20 % (large, but acceptable);
- a track with poor insulation is tested: similarly an insulation level of only 10 km will provide a similar distribution of the errors, so a 10 times larger , again reaching an uncertainty in the order of 20 %.
3. Method A.3: sectioned track, line closed to traffic
3.1. Method description and setup
3.2. Practical factors
- an earth electrode may be used driven into the soil at a convenient distance from the tested track (the EN 50122-2 requires 30 m minimum); the reason for such distance is avoiding distortion of the electric field in the soil if too close; the earthing resistance is quite limited anyway, for which even in good soil values lower than about 50 are difficult to achieve, so that this earthing system is suitable for the voltmetric terminals, but not for the test supply;
- using the remaining part of the system before the injection point and the rail cut earthing the test supply with a resistance usually of some ; with systems of limited length, instead, reaches too high values; the influence of this parameter was evaluated in [39] and is considered later in Section 3.3;
- earthed parts, such as cable trays, sharing the earthing resistance of the power distribution system, usually in the order of 1 or less, can be used for both purposes;
- the concrete structure supporting the track, if provided of reinforcement which is usually accessible through bonding terminals welded to it.
3.3. Variability and uncertainty analysis
4. Method A.4: lateral potential gradient in normal service
4.1. Method description and setup
4.2. Practical factors
- accessibility of the area to place the test electrodes in a line, as prescribed by the Wenner method (4 electrodes in a line, with external ones for test current and the inner ones for the voltage reading , spaced by s); the resulting apparent soil resistivity value can be calculated from the resistance reading as ; the resistivity value refers to the depth s, so that to double the probed depth the electrodes span is doubled as well;
- often, the Schlumberger method is used instead, because it requires the movement of 2 electrodes only, keeping the inner ones for voltage more compact; keeping their separation s and calling p the separation between each external one and the nearest voltage electrode (with ), the resistivity may be estimated again from the calculated resistance value as and the depth is , so deeper than the previous one; in other words, for a given target depth, the Schlumberger method is more compact and faster;
- specifically focusing on the track geometry and roads nearby, keeping s in the order of 1m–2m, the separation p may increase to what allowed by the areas nearby (e.g. 5m–20m); depth values to focus on are in this range and they should be supported by a careful analysis of resistivity values behavior to determine abnormal distributions and lack of homogeneity;
- it is in fact observed that interference by other metallic/conductive buried structures is almost certain in a urban/suburban context and larger volumes of soil (going deeper) help averaging the contributions.
4.3. Variability and uncertainty analysis
- first, a practical example of an extensive test campaign carried out along a tramway line is considered, in order to focus on data dispersion, determination of the linear regression slope , etc.; results are reported in the next Section 4.4 for homogeneity with previous sections;
- then, formulations are analyzed for sensitivity to the parameters and to robustness to extreme situations caused by practical issues, such as issues in placing electrodes;
- last, propagation of uncertainty is calculated along the given formulations, having already evaluated the behavior for uncommon values of parameters.
- For it’s a matter of propagating the uncertainty of and through the least-mean-square (LMS) regression, as it was done in [43] for the determination of stray capacitance (as the intercept and not the slope, as in the present case).
- For it is not a matter of uncertainty alone: the measurement itself is carried out by automatic volt-amperometric measurements at undisturbed frequencies, and the calibration with reference resistors indicates an instrumental uncertainty on the order of 1%–2% depending on resistance values. Variability of soil resistivity instead should be accounted for, as depending on location, depth and environmental/seasonal conditions. The latter may be ruled out if soil resistivity is measured immediately before (or after) the track measurements. The former can be accounted for by repeated measurements and taking then a weighted average as the value, and their dispersion as a Type A estimate of their uncertainty.
4.4. Application to a tramway system
5. Discussion and Conclusions
Funding
Institutional Review Board Statement
Informed Consent Statement
Conflicts of Interest
References
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| Brand / Model | Uncert. expression | @ 1 mV | @ 3 mV |
| Weilekes Elektronik MiniLog2 |
0.5 % + 10 V | 1.5 % | 0.83 % |
| National Instruments USB 6210 |
0.05 % FS + 12 V | 8.9 % | 3.0 % |
| Gossen Metrawatt H29S |
0.02 % + 0.01 % FS + 5 cts. |
0.02 % + 0.01 %
300
mV + (2* 300 mV/30000)/ 1 mV = 0.02 % + 3 % + 2 % = 5.02 % |
0.02 % + 0.01 %
300
mV + (2* 300 mV/30000)/ 3 mV = 0.02 % + 3 % + 0.66 % = 3.68 % |
| Fluke 117 | 0.5 % + 2 cts. | 0.5 % + (2*
600
mV/6000)/
1
mV = 20.5 % |
0.5 % + (2*
600
mV/6000)/
3
mV = 7.17 % |
| Location |
() |
a () |
b () |
() |
() |
() |
|
| 1 | 17.1 | 11.1 | 37.8 | 1.5 | 6.7 | 0.000605 | 0.0436 |
| 2 | 19.8 | 14.2 | 46.2 | 1.5 | 3.7 | 0.0026 | 0.1525 |
| 3 | 38.6 | 8.6 | 45.7 | 1.5 | 3.9 | 0.0038 | 0.0949 |
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