In this type of system, a phase-to-earth
fault only produces a weak current through the
phase-to-earth capacity of the fault-free
phases.
It can be shown that Id = 3 CwV
V being the simple voltage,
C the phase-to-earth capacity of a phase,
wthe frequency of the system (w = 2* pi
*f).
The Id current can remain for a long time,
in principle, without causing any damage since
it does not exceed a few amperes
(approximately 2 A per km for a 6 kV singlepole
cable, with a 150 mm2 cross-section, PRC
insulated, with a capacity of 0.63 mF/km).
Action does not need to be taken to clear
this 1st fault, making this solution advantageous in
terms of maintaining service continuity.
However, this brings about the following
consquences:
c if not cleared, the insulation fault must
be signalled by a permanent insulation monitor, c subsequent fault tracking
requires device made all the more complex by the fact that it is automatic, for
quick identification of the faulty feeder, and also maintenance personnel
qualified to operate it, c if the 1st fault is not cleared, a second fault
occurring on another phase will cause a real two-phase short circuit through
the earth, which will be cleared by the phase protections.
Advantage
The basic advantage is service continuity
since the very weak fault current prevents automatic tripping.
Drawbacks
The failure to eliminate overvoltage
through the earth can be a major handicap if overvoltage is high. Also, when
one phase is earthed, the others are at delta voltage (U = V* sqrt 3) in
relation to the earth increasing the probability of a 2nd fault.
Insulation costs are therefore higher since
the delta voltage may remain between the phase and earth for
a long period as there is no automatic
tripping. A maintenance department with the equipment
to quickly track the 1st insulation fault
is also required.
Applications
This solution is often used for industrial
systems (< or = 15 kV) requiring service continuity.
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