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Thermal Stability
Thermal Properties

Ampacity calculations form the heart of underground transmission and distribution cable system design. Accepted ampacity calculation procedures have existed for many decades - the classic Neher-McGrath procedure was published in 1957. However there have been significant recent improvements in portions of the calculations, in cable materials such as laminated paper-polypropylene insulation and cross linked polyethylene cables and, most importantly, in backfill thermal quality and in the accuracy of characterizing the effects of the cable's external environment (i.e. soil). Published papers report a 34% improvement in ampacity by modifying the cable thermal environment, and a 10 - 15% improvement is considered common.

Although many engineers routinely perform cable ampacity calculations with PC-based programs, there is still a need for a good understanding of the basic principles and calculation procedures. This is especially true as higher ampacities are required, and as it becomes more difficult to install new circuits, so that existing circuits must be operated more efficiently. Trench optimization is becoming more common as utilities attempt to obtain the maximum amperes from a cable. More attention is being paid to proper modeling of daily, weekly, and even monthly loss factors to take into account cooldown periods during load cycling, which permits higher loading during peak periods.

In an underground cable thermal circuit, the earth portion provides the largest single thermal resistance and thermal capacitance, and it also has by far the greatest variability - both with distance along the route and with time. Earth thermal resistance (a function of soil thermal resistivity and cable burial depth) can easily vary threefold on a specific circuit, and the cable must be rated for the worst-case condition.

This most important thermal resistance is, unfortunately, also the least well understood by cable engineers. The recent improvements in thermal measurement instruments and techniques, coupled with a better understanding of soil mechanics, and innovations in corrective thermal backfills - such as Fluidized Thermal Backfill™ (FTB™) - permit much better representation and control of the earth thermal circuit, resulting in significant ampacity increases.

Topics of particular importance to underground cable users include:

  • How can I install the lowest cost system today, and meet the required loadings in twenty years?
  • Ampacity effects of different XLPE cable shield constructions and dielectric losses in distribution cables.
  • Effects of higher cable temperature operation.
  • Ampacity implications of open-cut vs. directional drilling: burial depth effect, grout material in the casing, soil thermal resistivities, temperature and load monitoring.
  • Installing extruded-dielectric cables in steel pipe.
  • Do measures to reduce magnetic field always reduce ampacity as well?
  • Uprating existing cables in order to defer new installations.
  • Soil thermal stability: interface temperature vs. heat flux density.
  • Effects of hourly load profiles - daily vs. weekly.
  • Monitoring cables and using results effectively.
Particular topics pertaining to the earth thermal circuit include:
  • Soils: classification and geotechnical testing.
  • Factors affecting soil thermal resistivity.
  • Thermal resistivity measurement and test equipment.
  • Soil thermal diffusivity.
  • Thermal stability ("thermal runaway").
  • Elements of a cable route thermal survey.
  • Effect of soil moisture and soil compaction on thermal resistivity.
  • Corrective thermal backfills - design, installation, and quality control.
  • Special situations: submarine cables, directional drilling.
These topics can be explained and discussed in seminars presented by Geotherm

 

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