# Green's identities

In mathematics, Green's identities are a set of three identities in vector calculus relating the bulk with the boundary of a region on which differential operators act. They are named after the mathematician George Green, who discovered Green's theorem.

## Green's first identity

This identity is derived from the divergence theorem applied to the vector field F = ψφ: Let φ and ψ be scalar functions defined on some region URd, and suppose that φ is twice continuously differentiable, and ψ is once continuously differentiable. Then[1]

where is the Laplace operator, U is the boundary of region U, n is the outward pointing unit normal of surface element dS and dS is the oriented surface element.

This theorem is a special case of the divergence theorem, and is essentially the higher dimensional equivalent of integration by parts with ψ and the gradient of φ replacing u and v.

Note that Green's first identity above is a special case of the more general identity derived from the divergence theorem by substituting F = ψΓ,

## Green's second identity

If φ and ψ are both twice continuously differentiable on UR3, and ε is once continuously differentiable, one may choose F = ψεφφεψ to obtain

For the special case of ε = 1 all across UR3, then,

In the equation above, φ/∂n is the directional derivative of φ in the direction of the outward pointing normal n to the surface element dS,

In particular, this demonstrates that the Laplacian is self-adjoint in the L2 inner product for functions vanishing on the boundary.

## Green's third identity

Green's third identity derives from the second identity by choosing φ = G, where the Green's function G is taken to be a fundamental solution of the Laplace operator, ∆. This means that:

For example, in R3, a solution has the form

Green's third identity states that if ψ is a function that is twice continuously differentiable on U, then

A simplification arises if ψ is itself a harmonic function, i.e. a solution to the Laplace equation. Then 2ψ = 0 and the identity simplifies to

The second term in the integral above can be eliminated if G is chosen to be the Green's function for the boundary of the region U where the problem is posed (Dirichlet boundary condition),

This form is used to construct solutions to Dirichlet boundary condition problems. To find solutions for Neumann boundary condition problems, the Green's function with vanishing normal gradient on the boundary is used instead.

It can be further verified that the above identity also applies when ψ is a solution to the Helmholtz equation or wave equation and G is the appropriate Green's function. In such a context, this identity is the mathematical expression of the Huygens Principle.

## On manifolds

Green's identities hold on a Riemannian manifold, In this setting, the first two are

where u and v are smooth real-valued functions on M, dV is the volume form compatible with the metric, is the induced volume form on the boundary of M, N is oriented unit vector field normal to the boundary, and Δu = div(grad u) is the Laplacian.

## Green's vector identity

Green’s second identity establishes a relationship between second and (the divergence of) first order derivatives of two scalar functions. In differential form

where pm and qm are two arbitrary twice continuously differentiable scalar fields. This identity is of great importance in physics because continuity equations can thus be established for scalar fields such as mass or energy.[2]

In vector diffraction theory, two versions of Green’s second identity are introduced.

One variant invokes the divergence of a cross product [3][4][5] and states a relationship in terms of the curl-curl of the field

This equation can be written in terms of the Laplacians,

However, the terms

could not be readily written in terms of a divergence.

The other approach introduces bi-vectors, this formulation requires a dyadic Green function.[6][7] The derivation presented here avoids these problems.[8]

Consider that the scalar fields in Green's second identity are the Cartesian components of vector fields, i.e.

Summing up the equation for each component, we obtain

The LHS according to the definition of the dot product may be written in vector form as

The RHS is a bit more awkward to express in terms of vector operators. Due to the distributivity of the divergence operator over addition, the sum of the divergence is equal to the divergence of the sum, i.e.

Recall the vector identity for the gradient of a dot product,

which, written out in vector components is given by

This result is similar to what we wish to evince in vector terms 'except' for the minus sign. Since the differential operators in each term act either over one vector (say ’s) or the other (’s), the contribution to each term must be

These results can be rigorously proven to be correct through evaluation of the vector components. Therefore, the RHS can be written in vector form as

Putting together these two results, a result analogous to Green’s theorem for scalar fields is obtained,

Theorem for vector fields.

The curl of a cross product can be written as

Green’s vector identity can then be rewritten as

Since the divergence of a curl is zero, the third term vanishes to yield

Green's vector identity.

With a similar procedure, the Laplacian of the dot product can be expressed in terms of the Laplacians of the factors

As a corollary, the awkward terms can now be written in terms of a divergence by comparison with the vector Green equation,

This result can be verified by expanding the divergence of a scalar times a vector on the RHS.

## References

1. Strauss, Walter. Partial Differential Equations: An Introduction. Wiley.
2. M. Fernández-Guasti. Complementary fields conservation equation derived from the scalar wave equation. J. Phys. A: Math. Gen., 37:4107–4121, 2004.
3. A. E. H. Love. The Integration of the Equations of Propagation of Electric Waves. Philosophical Transactions of the Royal Society of London. Series A, Containing Papers of a Mathematical or Physical Character, 197:pp. 1–45, 1901.
4. J. A. Stratton and L. J. Chu. Diffraction Theory of Electromagnetic Waves. Phys. Rev., 56(1):99–107, Jul 1939.
5. N. C. Bruce. Double scatter vector-wave Kirchhoff scattering from perfectly conducting surfaces with infinite slopes. Journal of Optics, 12(8):085701, 2010.
6. W. Franz, On the Theory of Diffraction. Proceedings of the Physical Society. Section A, 63(9):925, 1950.
7. Chen-To Tai. Kirchhoff theory: Scalar, vector, or dyadic? Antennas and Propagation, IEEE Transactions on, 20(1):114–115, jan 1972.
8. M. Fernández-Guasti. Green's second identity for vector fields. ISRN Mathematical Physics, 2012:7, 2012. Article ID: 973968.