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Capillary-gravity dispersion and conserved linear surface energy
Statement
Let , , and . Set and ; use horizontal coordinates and vertical coordinate , positive upward, with the mean surface at . Let be real sine and cosine. For , choose any representative . Define
Only and are used: changing by , , changes the real phase by and leaves these values unchanged. Thus the formulas below define fields on the torus rather than a globally real-valued phase there. The fields
are smooth, independent of , periodic with horizontal periods , and solve exactly the linear capillary-gravity potential equations
where and . Here is depth, gravitational acceleration, constant density, surface tension, and is the horizontal Laplacian. In particular, the positive frequency obeys
At this mode is exactly the finite-depth gravity-wave mode. For any , let and extend with these regularities to a neighborhood of the closed slab and satisfy the same equations. Define the energy in one horizontal cell by
Then is nonnegative and constant on . 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, , , , , , , , , and 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.
The capillary-gravity potential model is the mathematical model defined in Common-wall residual and capillary boundary model: harmonic potential in , impermeable bottom, kinematic condition at , and dynamic condition .
Finite-depth gravity-wave dispersion with quantitative limits: for , and the fields , solve the finite-depth linear gravity-wave system; .
By The reals are complete, is a complete totally ordered field. Apply Square roots exist: a unique with ; the positives are with : every nonnegative real radicand has a unique nonnegative real square root, positive for positive radicands.
The chain rule, in one line from Carathéodory: if is differentiable at and is differentiable at , then is differentiable at with : if differentiable real functions are composed at points satisfying its limit-point hypotheses, then .
Green's first identity on a glued elementary solid region: for a finite gluing of elementary solid regions, and on an open neighborhood, .
Sums, scalar multiples, products and quotients: , , , and when : differentiable products satisfy .
Leibniz's rule on a compact rectangle: an interior parameter derivative with a continuous extension may be passed through a Riemann integral: if are continuous on a compact rectangle and in the interior, the parameter integral of is differentiable and its derivative is the corresponding integral of .
The real restrictions in Real sine and cosine as real restrictions of complex trigonometric functions agree with real sine and cosine. Their derivatives satisfy and by Derivative identities for the real restrictions of complex sine and cosine, and both are -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 , , , and for . Differentiability implies continuity by A function differentiable at is continuous at .
A function continuous on an interval whose derivative vanishes at every interior point of is constant on ; 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 and positive .
Let and let , whose existence and positivity follow from [F1] and [F2]. Set . Then , and the radicand in the Statement is positive, so its positive square root is this .
First, [F7] and repeated differentiation show that every derivative of is one of , and every derivative of alternates between those two continuous functions. All four functions are therefore . By [F3] and [F5], compositions with the affine phases and products with are smooth on real coordinates, extending across both vertical endpoints; the denominator is a fixed positive number. The -periodicity in [F7] makes the formulas unchanged under for every integer , and independence of gives period . Hence the smooth formulas and all their derivatives descend to the horizontal torus. Write , and take the gravity mode from [F1]. Define , , and . The chain rule [F3] gives ; harmonicity and the bottom condition persist because this transformation only rescales time and amplitude.
Let . 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 and . The interior term vanishes; opposite periodic faces cancel; the bottom term vanishes by . Hence .
Differentiate the two surface terms in using [F5] and [F6]. For the gradient term apply [F4] on to and , extended constantly in ; the top and bottom normal derivatives vanish and the paired periodic-face terms cancel. Dividing the identity by gives , so .
The gravity mode is independent of , so . Its gravity dynamic condition is . Therefore , since . Thus the transformed fields satisfy the capillary dynamic condition.
Since and , the coefficient of in is . Also . This proves the displayed mode formula, including . At , and the same formulas are exactly the gravity mode [F1].
The kinematic condition makes . The dynamic condition makes . Adding the derivatives in steps 1.3 and 1.4 therefore gives . The integrands are continuous in time and space on the compact cells, so their uniform continuity makes continuous on ; steps 1.3 and 1.4 give differentiability on . The interval is order-convex, and [F8] applied to the vanishing derivative proves that is constant on the whole interval, including its endpoints. Each term in is nonnegative because and , so is nonnegative.
Depends on
Common-wall residual and capillary boundary model
Finite-depth gravity-wave dispersion with quantitative limits
The chain rule, in one line from Carathéodory: if is differentiable at and is differentiable at , then is differentiable at with
Square roots exist: a unique with ; the positives are
Green's first identity on a glued elementary solid region
Sums, scalar multiples, products and quotients: , , , and when
Leibniz's rule on a compact rectangle: an interior parameter derivative with a continuous extension may be passed through a Riemann integral
The reals are complete
Real sine and cosine as real restrictions of complex trigonometric functions
Derivative identities for the real restrictions of complex sine and cosine
The zero sets of sine and cosine and the least positive common period 2 pi
Addition formulas, identities, parity, and derivatives of the hyperbolic functions
A function differentiable at is continuous at
A function continuous on an interval whose derivative vanishes at every interior point of is constant on ; consequently two such functions with the same derivative differ by a constant