The Daniell cell, drawn four ways

One battery, four pictures

Zinc in zinc sulfate, copper in copper sulfate, a salt bridge between them. John Frederic Daniell's cell of 1836 is the first battery most chemistry students meet, and it makes about 1.10 V. Ask where those 1.10 volts actually are, and you get at least four different answers.

Each answer is a picture of the same cell. Each is correct, each makes something easy to see, and each hides something else. The bar just below this paragraph stays pinned to the top of the screen, and it drives every picture on this page at once: change what's in the beakers, connect a load, or swap the salt bridge for Daniell's original porous pot, and see what each picture does with it. It starts with a 100 Ω load connected, which pulls the cell down to about 0.59 V; slide the load all the way left, to open circuit, and it reads the full 1.10.

The celldrives every picture
V 1.10I 0.0 mA

The crowd

Picture 1 · particles

Up close there is no voltage to see, only particles. At the zinc plate, atoms keep leaving the metal as Zn²⁺ ions, each leaving two electrons behind, and Zn²⁺ ions keep landing and turning back into metal. At the copper plate the same two-way traffic runs with Cu²⁺.

Set the load to open circuit (slider all the way left). Each plate's traffic now balances: as many ions leave as land. Equilibrium here doesn't mean nothing is happening. It means two opposite processes are tied.

Zn²⁺Cu²⁺SO₄²⁻K⁺Cl⁻e⁻
Filled dots are positive ions, rings negative; flashes mark single reaction events at the plates. Counts and speeds are schematic; event rates follow the same model as the other pictures. With Hold steady on, the particles obey the diagrams' rules: beakers and bridge are topped up like large reservoirs, and each ion stays in its own region plus the mixing zones (dashed) where the diagrams show it fading out. Turn it off and they run free, as a time-lapse with hours squeezed into seconds: the cell really discharges, the current fades as the copper runs out, the bridge leaks and runs down, and the pictures below, which are snapshots, stop matching. Reset refills everything.

Connect a load and the tie breaks. Zinc dissolves faster than it redeposits; the electrons it leaves behind run through the wire to the copper, where Cu²⁺ ions pick them up and plate out as metal. Inside the cell, ions close the circuit: positive ions drift toward the copper, negative ions toward the zinc, and in the bridge K⁺ and Cl⁻ carry the current across the gap.

Shows

That everything is motion, and that equilibrium is a balance of rates.

Hides

Why the answer is 1.10 volts and not 0.5 or 3. Almost all of it is energetics: how tightly each metal holds its atoms and how strongly water binds each ion, summed up in the standard free energy of the reaction Zn + Cu²⁺ → Zn²⁺ + Cu. The statistics of the crowd (how many ions there are) add only the Nernst concentration term, tens of millivolts at most. Moving dots show neither.

The ledger

Picture 2 · the textbook

A chemistry course turns the cell into bookkeeping. Each half-reaction gets a standard potential, measured against the standard hydrogen electrode (SHE: platinum in hydrogen gas and acid of unit activity, agreed to be zero): −0.76 V for Zn²⁺/Zn, +0.34 V for Cu²⁺/Cu. The Nernst equation corrects each for its actual concentration, and the cell voltage is the difference.

Draw current and the ledger adds line items: the resistance of the electrolyte, an overpotential at each plate to drive its reaction, and a concentration term once the ions next to the plates start to run short (or pile up). It's quick, and given good parameters, what it leaves out is the liquid junction, usually a few millivolts. That's why it's the textbook's picture.

Shows

The numbers, fast, and a clean list of where the voltage goes.

Hides

Position: the ledger never says where in the cell a loss happens. It also carries a quiet assumption, that both electrodes are measured against one and the same hydrogen reference. The "liquid junction" row is the price of that assumption, and textbooks usually set it to zero.

The levels

Picture 3 · electron levels, with the reference drawn in

Put position back, and plot what a voltmeter actually responds to: the energy of the electrons, expressed as a voltage. Up is more positive voltage, which for an electron, being negative, means lower energy. In each metal the electrons' level is the Fermi level, the energy it takes to add one more electron. For each redox couple in solution it's the redox level: the electron voltage at which the couple is balanced, with no net reaction either way.

Then do what the ledger doesn't, and draw the reference itself. The dash-dot line is where a hydrogen electrode's level would sit if unit-activity H⁺ could be placed at that spot without disturbing anything. It's a model quantity: exact for ideal solutions, but inside a junction no instrument can measure it, because it rests on the activity of a single kind of ion. The standard potentials E° are distances measured up or down from that line (the dashed levels).

Voltage axis with the zinc terminal at 0. Position is schematic: the thin layers beside each plate are stretched to be visible. Hover or drag across the plot to read values.

At open circuit each metal's Fermi level lies exactly on its couple's redox level, and the voltmeter reads the gap between the two metals. Connect a load and gaps open at both plates. Those are the overpotentials, and in this picture you read them straight off as voltage drops. The reference line isn't flat either. It tilts through the electrolyte as current flows, and it steps slightly at each liquid junction. The textbook's E(Cu) − E(Zn) equals the terminal voltage only at open circuit, and then only if that line is level from one plate to the other.

Shows

Where each loss happens, as a voltage you can read, and where the reference would be.

Hides

Every ion that isn't in a redox couple. The sulfate, and the K⁺ and Cl⁻ that carry the current through the bridge, get no line at all.

Every species

Picture 4 · species voltages

The last picture gives every charged species its own line. Take each species' electrochemical potential (its free energy per particle, electrical part included) and divide by its charge. What comes out is a voltage, Vi = μ̃i / ziF, on the same axis as the electrons. Zinc ions, copper ions, sulfate, potassium, chloride and electrons all share one plot.

Read it like a landscape for current. Each species carries current down its own slope, and a flat line means that species carries none. Each ion also has a dashed companion, its standard level; the gap between the two encodes the ion's concentration on a log scale. Don't compare the heights of different species: those depend on a convention. What means something is each line's slope, and the gap between an ion and the electrons where they react.

Solid: species voltage Vi. Dashed: standard level V°i. The zinc terminal is at 0 V; position is schematic. Hover or drag across the plot to read values.

Connect a load, and several things that picture 3 couldn't show become plain:

Now compare with picture 3. In the convention used here, neutral elements like zinc metal have zero chemical potential, so the Zn²⁺ line is the zinc redox level. And each ion's standard level sits a tabulated distance from the H⁺ rung of the floating ladder, which is exactly the hydrogen reference line of picture 3, so the dashed V°(Zn²⁺) is its E° line. For zinc and copper, pictures 3 and 4 carry the same information. Picture 4 adds the ions that picture 3 leaves out, and doesn't draw the hydrogen reference, though the dashed V° rungs are placed relative to it.

Shows

Every ion's push, which ions carry the current where, and (next) the slow leak at the junctions.

Hides

Overpotentials read as one clean gap here only because each metal is its own reactant, so its electrons and its ion are both on the plot. For other electrodes, such as hydrogen on platinum or two dissolved ions trading an electron, the overpotential isn't a single gap on this plot. The vertical offsets between different ions depend on conventions, so reading them takes practice.

All four at once

Same cell, same moment, four pictures. Move the load slider and watch one event land four ways: the particles start streaming, the ledger grows loss lines, gaps open in the levels, and every species tilts together.

The crowd particles

The ledger textbook

The levels electron levels

Every species species voltages

Show the numbers

What the Daniell cell is hiding

Textbooks describe an unloaded Daniell cell as being at equilibrium. It isn't, quite. Set the load to open circuit and look at the junctions in picture 4: wherever two solutions meet, lines that are flat on one side plunge or climb on the other. Zn²⁺ dives into the bridge; K⁺ dives into the zinc sulfate. A sloping line is a push, and a push means flow. Even with nothing connected, ions are diffusing out of their own compartment and into the next one; the bridge's K⁺ and Cl⁻ creep into both beakers, and a little zinc and copper sulfate creeps into the bridge.

That leak does two things. The first is a small liquid junction potential: the step in the hydrogen reference line in picture 3, and the "liquid junction" row in the ledger. A concentrated KCl bridge keeps it to a few millivolts, because K⁺ and Cl⁻ move at nearly the same speed and, when the two beakers are alike, the junctions at the two ends of the bridge nearly cancel. Switch to the porous pot, Daniell's original design, and the two sulfate solutions meet directly. Make their concentrations very different and the junction potential grows past ten millivolts.

The second is slower and worse. Copper ions that wander all the way to the zinc plate are reduced right there, no wire needed, and the cell quietly discharges itself. Choose the porous pot, untick Hold steady in picture 1, and watch the zinc plate for copper-coloured flashes. Real Daniell cells were designed to slow this down, never to stop it.

Load makes all of it worse, because under current a junction can't hold still. At the zinc end of the bridge, Zn²⁺ keeps arriving from one side while K⁺ leaves from the other, and Cl⁻ is pushed out into the zinc sulfate. Real junctions drift and smear out. The diagrams here, like the textbook Henderson treatment behind them (which assumes the two solutions blend linearly across the junction), hold each junction in place as a fixed mixing zone. That is a good approximation for the voltage, and a poor description of what the ions are actually doing. Hold steady is that approximation, made visible; untick it to watch the particles do what the diagrams won't.

So "equilibrium" is an approximation with a clock on it, good for minutes to hours but not forever. The particles show the leak happening; picture 4 shows it as slopes. The ledger books it as a correction assumed to be zero, and picture 3 shows only its side effect, the step in the reference.

Which picture, when?

PictureMakes easyHides
The crowdEquilibrium as a balance of rates; what physically moves where.Where the voltage comes from.
The ledgerQuick numbers; designing a cell; a list of losses.Position, and the single-reference assumption.
The levelsReading overpotentials as voltage drops; seeing where the reference would sit.Ions outside redox couples, including the ones carrying the current.
Every speciesWho carries current where; the junction leak; how the other pictures fit together.Overpotentials in general; it depends on conventions and takes practice to read.

None of them is the truth about the cell. They're one set of physics in four notations, and it's worth being able to move between them.