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A Charged Capacitor Lifts the Liquid

Irodov 3.144DifficultyDifficulty 3 of 5UniquenessUniqueness 4 of 5

Problem Irodov 3.144

A parallel-plate capacitor is held with its plates horizontal: the lower plate is under the surface of a liquid and the upper plate is above it. The liquid has permittivity ε\varepsilon and density ρ\rho. The plates are then given charges of surface density σ\sigma (and −σ-\sigma). By how much does the liquid level between the plates rise?

The horizontal capacitor before charging: the lower plate under the liquid, the upper plate above its free surface, a lead from the middle of each plate.

The horizontal capacitor before charging: the lower plate under the liquid, the upper plate above its free surface, a lead from the middle of each plate.

Given
  • liquid: permittivity ε\varepsilon, density ρ\rho
  • surface charge density σ\sigma on the plates
Find
the rise hh of the liquid level between the plates

Solution

Step 1The fields in the air and in the liquid

Neglecting edge effects, the field between the plates is vertical. The free charge σ\sigma is fixed on the plates, and the normal component of D\vect D is continuous across the liquid surface, so D=σD = \sigma in both layers whatever the liquid level:

Eair=σε0,Eliq=σε0ε(1) E_{\mathrm{air}} = \frac{\sigma}{\varepsilon_0}, \qquad E_{\mathrm{liq}} = \frac{\sigma}{\varepsilon_0\varepsilon} \tag{1}

The energy density ε0εE2/2\varepsilon_0\varepsilon E^2/2 is therefore σ2/2ε0\sigma^2/2\varepsilon_0 in the air and σ2/2ε0ε\sigma^2/2\varepsilon_0\varepsilon in the liquid.

Step 2The field energy released as the liquid rises
In equilibrium the liquid has risen by h between the plates. The field in the liquid is ε times weaker than in the air, and the lines that stop at the raised surface end on its negative bound charge.

In equilibrium the liquid has risen by hh between the plates. The field in the liquid is ε\varepsilon times weaker than in the air, and the lines that stop at the raised surface end on its negative bound charge.

Let the level between the plates, of area SS, stand a height xx above the outside level, and let it rise by dxdx. A layer of air of volume S dxS\,dx is replaced by liquid, and with the charges fixed the field energy changes by

dWel=(σ22ε0ε−σ22ε0)S dx=−(ε−1) σ22ε0ε S dx(2) dW_{\mathrm{el}} = \left(\frac{\sigma^2}{2\varepsilon_0\varepsilon} - \frac{\sigma^2}{2\varepsilon_0}\right)S\,dx = -\frac{(\varepsilon - 1)\,\sigma^2}{2\varepsilon_0\varepsilon}\,S\,dx \tag{2}

The field energy falls, so the field pulls the liquid up.

Step 3The gravitational energy it costs

The added layer, of mass ρS dx\rho S\,dx, comes from the wide outer surface, whose level does not change, and is lifted through the height xx:

dUg=ρgx S dx(3) dU_{\mathrm{g}} = \rho g x\,S\,dx \tag{3}
Step 4Equilibrium

The liquid stops where a further rise no longer lowers the total energy, dWel+dUg=0dW_{\mathrm{el}} + dU_{\mathrm{g}} = 0 at x=hx = h. With (2) and (3):

ρgh S dx=(ε−1) σ22ε0ε S dx\rho g h\,S\,dx = \frac{(\varepsilon - 1)\,\sigma^2}{2\varepsilon_0\varepsilon}\,S\,dx
h=(ε−1) σ22ε0ε ρgh = \dfrac{(\varepsilon - 1)\,\sigma^2}{2\varepsilon_0\varepsilon\,\rho g}
(4)
Check

With ε=1\varepsilon = 1 the liquid is electrically the same as air and h=0h = 0. In the limit ε→∞\varepsilon \to \infty (a conducting liquid) the rise tends to σ2/2ε0ρg\sigma^2/2\varepsilon_0\rho g: the liquid surface then carries −σ-\sigma itself and is pulled up by the pressure σ2/2ε0\sigma^2/2\varepsilon_0 of a charged conducting surface, which the column’s hydrostatic pressure ρgh\rho g h balances. Dimensions: σ2/ε0\sigma^2/\varepsilon_0 is a pressure and ρg\rho g a pressure per length, so hh is a length.

Remark

Read as a pressure balance, the field pulls up on the liquid surface with (σ2/2ε0)(1−1/ε)(\sigma^2/2\varepsilon_0)(1 - 1/\varepsilon), the difference between the energy densities above and below it: a field normal to a dielectric boundary pulls the boundary toward the side of lower permittivity. Because σ\sigma is fixed, the pull does not depend on how high the liquid has climbed, which is why the rise is the simple ratio of that pressure to ρg\rho g.