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Capillary-gravity dispersion and conserved linear surface energy

Statement

Let h,g,ρ,k,Ly>0, σ≥0, and a∈R. Set λ=2π/k and TL=R/(LZ); use horizontal coordinates (x,y)∈Tλ×TLy and vertical coordinate z∈[−h,0], positive upward, with the mean surface at z=0. Let S,C:R→R be real sine and cosine. For x∈Tλ, choose any representative x~∈R. Define

ωσ=(gk+σρk3)tanh⁡(kh),G(z)=cosh⁡(k(z+h))cosh⁡(kh),θσ=kx~−ωσt.

Only S(θσ) and C(θσ) are used: changing x~ by nλ, n∈Z, changes the real phase by 2πn and leaves these values unchanged. Thus the formulas below define fields on the torus rather than a globally real-valued phase there. The fields

ησ(t,x,y)=aC(θσ),ϕσ(t,x,y,z)=aωσktanh⁡(kh)G(z)S(θσ)

are smooth, independent of y, periodic with horizontal periods λ,Ly, and solve exactly the linear capillary-gravity potential equations

Δϕ=0(−h<z<0),ϕz(t,x,y,−h)=0,

ηt(t,x,y)=ϕz(t,x,y,0),ϕt(t,x,y,0)+gη(t,x,y)−σρΔHη(t,x,y)=0,

where Δ=∂x2+∂y2+∂z2 and ΔH=∂x2+∂y2. Here h is depth, g gravitational acceleration, ρ constant density, σ surface tension, and ΔH is the horizontal Laplacian. In particular, the positive frequency obeys

ωσ2=(gk+σρk3)tanh⁡(kh).

At σ=0 this mode is exactly the finite-depth gravity-wave mode. For any T>0, let η∈C1([0,T];C2(Tλ×TLy)) and ϕ∈C1([0,T];C2(Tλ×TLy×[−h,0])) extend with these regularities to a neighborhood of the closed slab and satisfy the same equations. Define the energy in one horizontal cell by

E(t)=ρ2∫0Ly∫0λ∫−h0(∣ϕx∣2+∣ϕy∣2+∣ϕz∣2) dz dx dy+ρg2∫0Ly∫0λη2 dx dy+σ2∫0Ly∫0λ(∣ηx∣2+∣ηy∣2) dx dy.

Then E(t) is nonnegative and constant on [0,T]. These are exact deductions within the stated linear model; they do not assert a nonlinear free-surface solution, a sharp-interface convergence theorem, or an experimental observation. In SI units, [h]=[Ly]=m, [g]=m s−2, [ρ]=kg m−3, [σ]=N m−1, [k]=m−1, [a]=[η]=m, [ωσ]=s−1, [ϕ]=m2 s−1, and [E]=J for the chosen finite transverse span.

Statement references

Finite-depth gravity-capillary boundary conditions, hyperbolic vertical profile, and dispersion derivation: MIT 18.357, Chapter 19, printed pp. 78–79 (PDF pp. 78–79).

Independent surface-tension pressure derivation and deep-water gravity-capillary relation: ETH Zürich, Mechanics of Continuous Media, lecture 23, printed pp. 185–187 (PDF pp. 5–7).

Independent gravity-capillary dispersion context and finite-depth gravity relation: Firing, OCN 620, §19.4.

Finite-depth gravity-wave mode used at zero surface tension: Finite-depth gravity-wave dispersion with quantitative limits.

Model equations and conventions: Common-wall residual and capillary boundary model.

Facts & Assumptions

Given: The positive parameters, horizontal periods, smooth fields, and linear boundary equations in the Statement.

[A1]

The capillary-gravity potential model is the mathematical model defined in Common-wall residual and capillary boundary model: harmonic potential in −h<z<0, impermeable bottom, kinematic condition ηt=ϕz at z=0, and dynamic condition ϕt+gη−(σ/ρ)ΔHη=0.

[F1]

Finite-depth gravity-wave dispersion with quantitative limits: for h,g,k>0, ω0=gktanh⁡(kh)>0 and the fields η0=aC(kx−ω0t′), ϕ0=(ag/ω0)G(z)S(kx−ω0t′) solve the finite-depth linear gravity-wave system; G(z)=cosh⁡(k(z+h))/cosh⁡(kh).

[F2]

By The reals are complete, R is a complete totally ordered field. Apply Square roots exist: a unique a≥0 with (a)2=a; the positives are {x2:x≠0} with F=R: every nonnegative real radicand has a unique nonnegative real square root, positive for positive radicands.

[F3]

The chain rule, in one line from Carathéodory: if g is differentiable at c and f is differentiable at g(c), then f∘g is differentiable at c with (f∘g)′(c)=f′(g(c)) g′(c): if differentiable real functions are composed at points satisfying its limit-point hypotheses, then (f∘g)′=(f′∘g)g′.

[F4]

Green's first identity on a glued elementary solid region: for a finite gluing E of elementary solid regions, u∈C1 and v∈C2 on an open neighborhood, ∭E(⟨∇u,∇v⟩+uΔv)=∬∂Eu⟨∇v,n⟩.

[F6]

Leibniz's rule on a compact rectangle: an interior parameter derivative with a continuous extension may be passed through a Riemann integral: if g,h are continuous on a compact rectangle and ∂xg=h in the interior, the parameter integral of g is differentiable and its derivative is the corresponding integral of h.

[F7]

The real restrictions S,C in Real sine and cosine as real restrictions of complex trigonometric functions agree with real sine and cosine. Their derivatives satisfy S′=C and C′=−S by Derivative identities for the real restrictions of complex sine and cosine, and both are 2π-periodic by The zero sets of sine and cosine and the least positive common period 2 pi. The hyperbolic identities Addition formulas, identities, parity, and derivatives of the hyperbolic functions give cosh⁡′=sinh⁡, sinh⁡′=cosh⁡, cosh⁡>0, and tanh⁡(s)>0 for s>0. Differentiability implies continuity by A function differentiable at c is continuous at c.

[F8]

A function continuous on an interval I whose derivative vanishes at every interior point of I is constant on I; consequently two such functions with the same derivative differ by a constant: a real function continuous on an order-convex interval and differentiable with derivative zero at every interior point is constant on the whole interval.

Proof

Given: The assumptions above, with σ≥0 and positive h,g,ρ,k.

1.1givenF1F2algebra

Let ω0=gktanh⁡(kh)>0 and let cσ=1+σk2/(ρg)>0, whose existence and positivity follow from [F1] and [F2]. Set ω=cσω0. Then ω2=(1+σk2/(ρg))gktanh⁡(kh)=(gk+σk3/ρ)tanh⁡(kh), and the radicand in the Statement is positive, so its positive square root is this ω.

1.2givenF1F3F5F7algebra

First, [F7] and repeated differentiation show that every derivative of S,C is one of S,C,−S,−C, and every derivative of sinh⁡,cosh⁡ alternates between those two continuous functions. All four functions are therefore C∞. By [F3] and [F5], compositions with the affine phases and products with G(z) are smooth on real coordinates, extending across both vertical endpoints; the denominator cosh⁡(kh) is a fixed positive number. The 2π-periodicity in [F7] makes the formulas unchanged under x~↦x~+nλ for every integer n, and independence of y gives period Ly. Hence the smooth formulas and all their derivatives descend to the horizontal torus. Write θ0(t′,x~)=kx~−ω0t′, and take the gravity mode η0,ϕ0 from [F1]. Define t′=cσt, η(t,x,y)=η0(t′,x,y), and ϕ(t,x,y,z)=cσϕ0(t′,x,y,z). The chain rule [F3] gives ηt=cσ(η0)t′=cσ(ϕ0)z=ϕz; harmonicity and the bottom condition persist because this transformation only rescales time and amplitude.

1.3givenA1F4F5F6algebra

Let Q=[0,λ]×[0,Ly]×[−h,0]. Apply [F6] successively to the rectangular cell integrals and use [F5] to differentiate the squared gradients; the fields and time derivatives are continuous on the compact cell, so the hypotheses hold. Apply [F4] with u=ϕt and v=ϕ. The interior term ϕtΔϕ vanishes; opposite periodic faces cancel; the bottom term vanishes by ϕz(−h)=0. Hence K′(t)=ρ∫0Ly∫0λϕt(t,x,y,0)ϕz(t,x,y,0) dx dy.

1.4givenA1F4F5F6algebra

Differentiate the two surface terms in E using [F5] and [F6]. For the gradient term apply [F4] on Q to u=ηt(x,y) and v=η(x,y), extended constantly in z; the top and bottom normal derivatives vanish and the paired periodic-face terms cancel. Dividing the identity by h gives ∫0Ly∫0λ∇Hη⋅∇Hηt dx dy=−∫0Ly∫0ληtΔHη dx dy, so V′(t)=∫0Ly∫0λ(ρgη−σΔHη)ηt dx dy.

2.1givenF1step 1.1step 1.2algebra

The gravity mode is independent of y, so ΔHη0=−k2η0. Its gravity dynamic condition is (ϕ0)t′+gη0=0. Therefore ϕt+gη−(σ/ρ)ΔHη=cσ2(ϕ0)t′+gη0+(σk2/ρ)η0=(−gcσ2+g+σk2/ρ)η0=0, since cσ2=1+σk2/(ρg). Thus the transformed fields satisfy the capillary dynamic condition.

2.2givenF1step 1.1step 1.2algebra

Since ω=cσω0 and ω02=gktanh⁡(kh), the coefficient of G(z)S(θσ) in ϕ=cσϕ0(cσt) is agcσ/ω0=aω/(ktanh⁡(kh)). Also θ0(cσt,x~)=θσ. This proves the displayed mode formula, including a=0. At σ=0, cσ=1 and the same formulas are exactly the gravity mode [F1].

3.1givenA1F8step 1.3step 1.4algebra∎

The kinematic condition makes ϕz(t,x,y,0)=ηt. The dynamic condition makes ρϕt+ρgη−σΔHη=0. Adding the derivatives in steps 1.3 and 1.4 therefore gives E′(t)=K′(t)+V′(t)=0. The integrands are continuous in time and space on the compact cells, so their uniform continuity makes E continuous on [0,T]; steps 1.3 and 1.4 give differentiability on (0,T). The interval [0,T] is order-convex, and [F8] applied to the vanishing derivative proves that E is constant on the whole interval, including its endpoints. Each term in E is nonnegative because ρ,g>0 and σ≥0, so E is nonnegative.

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