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Before any relay can be set, the engineer must know three boundary values at each relaying point:
Any unbalanced set of three-phase quantities can be resolved into three balanced sets:
Each sequence has its own Thevenin equivalent network. Only the positive-sequence network contains driving voltages (the pre-fault source EMFs).
The sequence networks are interconnected differently for each fault type. The boundary conditions at the fault determine the connection.
Residual quantities are the vector sum of the three phase quantities. They are zero in a balanced system and non-zero only when an earth-return current path exists.
Sequence voltages distribute differently across the network during a fault. This is critical for directional and distance relay polarisation.
Technical line graph showing sequence voltage distribution along a transmission line during an A-E fault. X-axis: distance from source to fault point. Y-axis: per-unit voltage magnitude. Three curves: V1 (blue) starts at 1.0 pu at source, dips to near zero at the fault; V2 (orange) starts near zero at source, rises to maximum at fault; V0 (red) mirrors V2. Dark background, clean grid lines, labeled axes.
The ratio is the single most important parameter governing earth fault behaviour. It is set entirely by the neutral earthing method.
In a meshed network, fault current splits between parallel branches. The fraction reaching a relay through a specific branch is given by the sequence distribution factors.
Given: A-E fault at Bus A. Pre-fault voltage V = 63.5 V (phase-neutral, secondary). System sequence impedances at the fault: . Branch OB distribution factors: , .