Power system fault
A fault is what happens when the grid's careful insulation fails and current finds a path it was never meant to take — a tree branch bridging two phases, a cracked insulator letting a wire arc to a tower, a digger slicing through a buried cable. With the only thing limiting the current now being the tiny impedance of the wires themselves, the flow explodes: a point that normally carries a few hundred amps can suddenly conduct tens of thousands, an arc hot enough to vaporise copper and explode equipment in a fraction of a second.
Engineers classify faults by how the wires touch: a single line-to-ground fault (by far the most common, ~80%) where one phase finds earth, line-to-line, double-line-to-ground, and the rare but most violent three-phase fault that determines the maximum interrupting rating every breaker must withstand. Calculating the fault current at every point — the 'short-circuit study' — is the bedrock of grid design: it sizes the breakers, sets the protection relays, and decides how thick the busbars must be to survive the magnetic blow of a fault without bending.
Counterintuitively, the symmetrical three-phase fault is the easiest to calculate (the system stays balanced, so per-unit and single-phase maths work) yet is the worst-case for breaker rating. Unbalanced faults need 'symmetrical components' — splitting into positive, negative, and zero sequences.