Visual walkthrough — Calculate electrical power (P = VI, P = I²R)
Step 1 — What is charge, and what is a "drop"?
WHAT. Picture a bucket of tiny beads. Each bead is a chunk of electric charge. We measure a pile of charge in coulombs (symbol , unit C). One coulomb is just "this many beads."
WHY start here. Every energy idea in a circuit is really "beads falling down a hill." Before we talk about speed or power, we need the two actors: the beads (charge) and the hill (the voltage drop). No hill, no fall, no energy.
PICTURE. The hill on the left is the voltage drop; the pile of beads at the top is the charge waiting to slide down.
Step 2 — Voltage = energy handed to each bead
WHAT. Voltage is the height of the hill: how much energy one coulomb gains by falling down it. Its unit, the volt, is defined as joules-per-coulomb:
Here is total energy in joules (J), is the charge in coulombs.
WHY this definition. We could describe the hill by "how steep" or "how long," but what a circuit cares about is: how much energy does each unit of charge pick up? That is exactly . A taller hill (bigger ) means each bead arrives at the bottom carrying more energy.
PICTURE. Two hills side by side — a short one (small ) and a tall one (big ). The same bead drops further on the tall hill, so it delivers more energy. See Voltage and Potential Difference.
Step 3 — Current = how many beads fall per second
WHAT. Current is the flow rate of charge: how much charge passes a point each second. Its unit, the amp, is coulombs-per-second:
is time in seconds (s).
WHY this definition. Energy alone isn't power. A slow trickle of beads and a roaring flood might drop the same beads down the same hill — but one does it slowly and one does it fast. To capture "fast," we need a rate, and is that rate. See Electric Current.
PICTURE. A pipe with beads streaming past a checkpoint. Count how many cross the dashed line in one second — that count is .
Step 4 — What is power? A rate of energy
WHAT. Power is energy delivered per second:
Its unit is the watt (W), and .
WHY. Component ratings, heat, battery drain — they all ask "how fast is energy moving right now?" not "how much total." That's a rate, so we divide energy by time. See Energy and the Joule.
PICTURE. Two devices delivering the same 100 J: one over 10 s (low power), one over 1 s (high power). Same energy, very different power.
Step 5 — Snap the pieces together:
WHAT. We now have three facts, each a little Lego brick:
- From Step 2:
- From Step 3:
- From Step 4:
Substitute in order. First put into : Now put in place of :
WHY the cancels. The in "beads per second" and the in "energy per second" are the same clock. When both appear top and bottom, they divide out — leaving a formula with no time in it at all. Power depends only on the hill height and the flow rate .
PICTURE. The three bricks flowing into one box: the 's meet and cancel (struck out in red), leaving the clean result.
Step 6 — Feed in Ohm's law to get the other two forms
WHAT. Ohm's Law (V = IR) says the drop across a resistor is , where is resistance in ohms (). Slot it into two different ways:
Replace with : Replace with (since ):
WHY. Sometimes you don't know both and . Ohm's law lets you rewrite the same power using whichever pair you actually measured. All three describe the identical wattage.
PICTURE. One triangle (, , ) with three doors out — each door drops you into one of the three power formulas.
Step 7 — The degenerate cases (never let the reader get stuck)
WHAT. Check the extremes so nothing surprises you:
PICTURE. Four dials, each pinned to an edge case, with the resulting power labelled.
- No current (): an open switch, a broken wire. . There is a hill (voltage present), but no beads fall — so zero power. Voltage alone burns nothing.
- No voltage (): two points at the same height, a dead short with no drop. . Beads may drift, but they fall nowhere — zero energy delivered.
- Zero resistance (): using , dividing by a shrinking makes . A real short circuit tries to dump huge power — this is why fuses exist. See Resistors and Power Ratings.
- Huge resistance (): an insulator. , so . Almost no current flows, almost no power. (Careful: too — same answer, no contradiction.)
The one-picture summary
Everything on one canvas: charge and hill (Steps 1–2) → flow rate (Step 3) → rate of energy (Step 4) → the 's cancel into (Step 5) → Ohm's law fans it into the trio (Step 6).
Recall Feynman retelling of the whole walkthrough
Imagine beads at the top of a hill. How tall the hill is = voltage (energy each bead gets). How many beads slide down per second = current . Multiply "energy per bead" by "beads per second" and the per-bead and per-second stitch together into energy per second = power. That's — and notice the clock cancelled, so power doesn't care how long you wait, only how tall the hill and how fast the flood. If the hill is rough (resistance ), Ohm's law () lets you rewrite the same power as or depending on what you measured. The square in warns you: crank the current and the heat rockets up fourfold. Turn off the flow and power vanishes; short the hill flat and it vanishes too. Same one idea, drawn every way.
Recall Quick self-check
Why does the cancel in the derivation? ::: Because carries a on top, and has a on the bottom — they are the same clock, so they divide out, leaving no time in the formula. With but , what is the power? ::: — voltage alone delivers nothing. Doubling the current in a fixed resistor multiplies power by how much? ::: By 4, because and .
Connections
- Parent topic — full note
- Voltage and Potential Difference — the "hill height," source of .
- Electric Current — the "flow rate," source of .
- Energy and the Joule — what and the watt (J/s) actually measure.
- Ohm's Law (V = IR) — the bridge to and .
- Resistors and Power Ratings — why the short-circuit case matters.
- Heat Dissipation and Cooling — the real-world cost of the square.