Energy & the power grid

Load flow (power flow analysis)

Load flow is the question every grid operator asks before dawn: given the power each generator will inject and each city will draw, exactly how much current will run through every line, and how high or low will the voltage sag at every substation? It is the weather forecast of electricity — not predicting faults, but the ordinary steady state, so planners can see in advance which transmission line is about to overheat or which town will brown out at the evening peak.

The hard part is that power, unlike water, refuses to follow a simple pipe equation: the flow through each line depends on the voltage magnitudes and phase angles at both ends, and these are tangled together nonlinearly across the whole network at once. So load flow is solved by iteration — guess the voltages everywhere, compute the resulting power mismatches, nudge the guesses, and repeat (the Newton-Raphson method converges in a handful of steps). The output sets everything from how much power a country can safely import to where the next billion-dollar line must be built.

P_i = Σ_k |V_i||V_k|(G_ik cosθ_ik + B_ik sinθ_ik) — solved by Newton-Raphson

Load flow needs one 'slack bus' — a reference generator that mops up whatever power is left over to make the books balance, since losses in the lines aren't known until the flow is solved. Choosing the slack bus poorly can mask instability.

Also called
power flowload-flow study潮流計算功率潮流