MPEMathematical Problems in Engineering1563-51471024-123XHindawi Publishing Corporation37189010.1155/2012/371890371890Research ArticleGaussian Curvature in Propagation Problems in Physics and EngineeringBakhoumEzzat G.TomaCristianDepartment of Electrical and Computer EngineeringUniversity of West Florida11000 University ParkwayPensacola, FL 32514USAuwf.edu20121812012201201092011091020112012Copyright © 2012 Ezzat G. Bakhoum.This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

The computation of the Gaussian curvature of a surface is a requirement in many propagation problems in physics and engineering. A formula is developed for the calculation of the Gaussian curvature by knowledge of two close geodesics on the surface, or alternatively from the projection (i.e., image) of such geodesics. The formula will be very useful for problems in general relativity, civil engineering, and robotic navigation.

1. Introduction

In many propagation problems in physics and engineering, it becomes necessary to compute the Gaussian curvature of a two-dimensional surface. In physics, this becomes necessary in the applications of general relativity, where it is sometimes desired to calculate the Gaussian curvature at a point in space from the observed geodesic paths of planets or light rays [1, 2]. In engineering, engineers who are involved in the design of structures such as geodesic domes frequently require a practical formula for computing the Gaussian curvature, where relations exist between the Gaussian curvature at any point on the surface of the structure and the stability of such a structure . In certain other engineering applications, such as computer vision and robotic navigation, engineers sometimes find themselves facing the complicated problem of having to compute the Gaussian curvature of a surface in order to calculate 3-dimensional depth data (or range) .

From the basic principles of differential geometry, the Gaussian curvature G at any point of a two-dimensional surface S is given byG=k1k2, where k1 and k2 are the maximum and the minimum normal curvatures . Unfortunately, in many practical situations, k1 and k2 are simply unknown. In the following section, we will derive a formula for computing the Gaussian curvature at any point on a surface by knowledge of two close geodesics on the surface, or alternatively from the projection (i.e., image) of such geodesics (this is very important in applications such as general relativity and robotic navigation, where no direct knowledge of the geodesics exists, but only an image of the geodesics is available). A simple test of the formula is given in Section 3 (the test shows that G, as computed from the formula, must vanish in an Euclidean 2-space). In Section 4, it is proven that the Gaussian curvature is a projective invariant and hence can be calculated from any projected image of two geodesics.

2. Calculation of the Gaussian Curvature from Geodesic Deviation

It is well known that any general 2-dimensional surface is topologically equivalent at any given point to a surface of revolution . Hence, two close geodesics on the surface, when considered only within a small surface patch, can be treated as embedded in a surface of revolution. Such curves, however, will not necessarily be geodesics in the surface of revolution. Consider now a surface of revolution, where the smooth curve S is a general curve that is embedded in the surface (Figure 1). S is a copy of S that is obtained by rotating S through a small angle θ.

A general curve S that is embedded in a surface of revolution and a copy S that is separated from S by a small rotation.

pr is a position vector, defined over a circular ring passing by S-S. Let us select two parameters u and v, such that u varies as we travel along the curve S, but v is constant, and v varies as we pass from one curve to another, but u is constant. Obviously,u=s,v=θ, where θ is the rotation angle of the axis from S to S. Given such parameters on any surface in space, it can be shown that (sθ2δρ)dθ-(θs2δρ)dθ=ζ,μ,νRζμνρδζδνpμ, where δr is the unit tangent vector to the curve, Rbcda is the mixed curvature tensor , and the symbol is the covariant derivative operator [6, 7]. If the curve S was a geodesic in the surface, we must have had [6, 7]sδr=0, since the covariant derivative of the unit tangent vector to a geodesic vanishes along the curve [6, 7]. Since S is a general curve, however, then sδr will be the components of a vector of finite length, normal to the vector δr . On the other hand, due to circular symmetry in a surface of revolution, the vector sδr, clearly, is parallel transported [6, 7] along a circular ring in the surface. Hence, we must conclude thatθ(sδr)=θs2δr=0, at any point on S. Further, given the parameters s and θ, it can be shown that  (sθ2δr)dθ=s2pr, for any 2-dimensional surface. From (2.4) and (2.5), (2.2) is rewritten ass2pρ=ζ,μ,νRζμνρδζδμpν, where ζ, μ, ν=1,2. Moreover, it has be shown that Rbcda=G(δcagbd-δdagbc), for a smooth 2-dimensional manifold, where G is the Gaussian curvature, δba is the Kronecker delta, and gab are the components of the metric tensor at any point on the surface. Substituting from (2.7) into (2.6) and carrying out the summation, we obtains2pρ+Gpρ=Gδρμ,νgμνδμpν, where we have used the identityμ,νgμνδμδν=1. Equation (2.8) is analogous to the equation of geodesic deviation [6, 7]. Once again, if S was a geodesic in the surface, we must have had an orthogonality conditionμ,νgμνδμpν=0, and (2.8) would have reduced to the well-known equation of deviation of two geodesics in a Riemannian 2-manifold. Equation (2.8), in its given form, will not allow the computation of the Gaussian curvature G, since the metric tensor components, as well as all the covariant derivatives on the surface, are unknown. However, (2.8) can be further reduced as follows: for an infinitesimal rotation dθ,pr=xrθdθ. Thus,prs=δrθdθ. Now,δSr=δSr+δSrθdθ=δSr+prs, where δSr, δSr are unit tangent vectors at S and S, respectively, separated by a rotation dθ (Figure 2).

Unit tangent vectors to S and S, respectively.

Given that, for any vector pr on the surface ,spρ=pρs+μ,νΓμνρpμxνs, where Γbca is a Christoffel symbol of the second kind, we can always select coordinates such that Christoffel symbols vanish at the origin [6, 7] (e.g., we can select coordinates on the surface, at the location of the vector pr). Then, the vector μ,νΓμνρpμδν is generally very small in the vicinity of the origin, and can be neglected (i.e., a linear approximation of spρ is assumed here. This approximation will be further justified in the following discussion and in Section 3). Therefore, letηr=(δSr-δSr)=prsspr. Further, let us define the deviation angle, ψ, as the angle between the two unit tangent vectors δSr, δSr, at any point along the curve S. Generally, the angle between two curves is given by cosψ=μ,νgμνdxμdsdxνds, but since s=s is the length of the curve, and having δr=dxr/ds, we can writecosψ=μ,νgμν(δμ)S(δν)S. Hence, from (2.15) and (2.17),μ,νgμνημην=μ,νgμν[δSμδSν+δSμδSν-2δSμδSν]=2(1-cosψ)μ,νgμν(spμ)(spν). We also see thatcosψμ,νgμνδμ[δν+spν]1+μ,νgμνδμ(spν). Now, consider (2.8) and the summationμ,νgμνpμ(s2pν)+G  μ,νgμνpμpν=G  α,βgαβpαδβ  [μ,νgμνδμpν]=G  [μ,νgμνδμpν]2, and letP=μ,νgμνpμpν denote the Euclidean norm of the vector pr; thus,dds  P2=2μ,νgμνpμ(spν),d2ds2  P2=2μ,νgμν[pμ(s2pν)+(spμ)(spν)]. Substitution from (2.18), (2.21), and (2.23) into (2.20) gives12  d2P2ds2-2(1-cosψ)+GP2=G  [μ,νgμνδμpν]2. To evaluate the last term in (2.24), we rewrite (2.8) aspρ=δρμ,νgμνδμpν-1Gs2pρ. Now, from (2.22) and (2.25), we havedP2ds=2  μ,νgμν[δμα,βgαβpαδβ-1Gs2pμ](spν)=2  (μ,νgμνpμδν)(μ,νgμνδμ(spν))-2G  μ,νgμν(s2pμ)(δsν-δsν). Each of the components in the last term of (2.26) vanishes identically. To prove this, we evaluate each of the components for each of the curves, S and S, by substitution from (2.6). We have μ,νgμνδμ(s2pν)=αδα[ρ,ζ,μ,νgαρRζμνρδζδμpν]=α,ζ,μ,νRαζμνδαδζδμpν=α,ζ,μ,νG(gαμgζν-gανgζμ)δαδζδμpν. A straightforward summation shows that the right-hand side of (2.27) vanishes. We therefore conclude that s2pr is in the direction normal to the curve. In plus spr is in the direction of the tangent to the curve.

Finally, substitution from (2.19) into the first term of (2.26) givesdP2ds=2  (μ,νgμνpμδν)(cosψ-1), orμ,νgμνpμδν=-dP2/ds2(1-cosψ), and hence (2.24) is further reduced toG=(1/2)d2P2/ds2    -    2(1-cosψ)[(dP2/ds)/2(1-cosψ)]2-P2, where G is the Gaussian curvature of the surface at the location of the vector P. In the following section, we prove that the Gaussian curvature given by (2.30) must vanish in an Euclidean 2-space. In Section 4, it is further proven that G is a projective invariant and hence can be calculated from any projected image of the curves S and S.

3. Investigation of the Behavior of <inline-formula><mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" id="M107"><mml:mrow><mml:mi>G</mml:mi></mml:mrow></mml:math></inline-formula> in an Euclidean Space

Here, we illustrate by a simple example that the Gaussian curvature G, given by (2.30), must vanish in an Euclidean 2-space.

Consider a right circular cone, shown in Figure 3.

A right circular cone and the corresponding geometry.

P is the Euclidean norm of the position vector, and θ is the rotation angle (as discussed in the above text).

From the Figure 3, we see thatP2=2r2(1-cosθ),r=ssinα, where s is the length of the generator. Hence,P2=2(1-cosθ)(s2sin2α),dP2ds=4ssin2α(1-cosθ). Thusd2P2ds2=4sin2α(1-cosθ). For an infinitesimal rotation, cosθ is expressed by the first two terms of its power series, that is,cosθ1-θ22!, and thus, (3.3) is written asd2P2ds2=2sin2αθ2. Furthermore, we can see thatr2θ2=2s2(1-cosψ), where ψ is the deviation angle, or(1-cosψ)=12sin2αθ2. From (3.5) and (3.7), we have d2P2ds2=4(1-cosψ). By comparison of (2.30) and (3.8), we immediately see that G must vanish in an Euclidean 2-space. This proves the correctness of (2.30).

4. Proof That the Gaussian Curvature <inline-formula><mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" id="M123"><mml:mrow><mml:mi>G</mml:mi></mml:mrow></mml:math></inline-formula> Is a Projective Invariant

Now, we will reach our final goal by demonstrating that G, formulated by (2.30), can be measured directly in the image plane.

We rewrite (2.8) asG=-s2pρpρ-δρμ,νgμνδμpν. From (2.27), we saw that s2pr is a vector in the direction normal to the curve. Now, by using (2.9) and taking the summationμ,νgμνδμpν-μ,νgμνδμδν[μ,νgμνδμpν]=0, it is easy to see that the denominator in (4.1) is also a vector in the direction normal to the curve.

If we now lets2pρ=αvρ,pρ-δρμ,νgμνδμpν=βvρ, where α, β are scalars, and vρ is a vector in the direction normal to the curve, thenG=-αβ. Now, consider the orthographic projection of the two vectors in (4.3), written ass2pρ¯=σJσρ(s2pσ)=ασJσρvσ,pρ-δρμ,νgμνδμpν¯=σJσρ(pσ-δσμ,νgμνδμpν)=βσJσρvσ, where Jba is a transformation Jacobian between a coordinate system on the surface and a coordinate system in the image plane.

If measured in the image plane, the Gaussian curvature G is now given byG¯=-s2pρ¯pρ-δρμ,νgμνδμpν¯=-αβ, as we can easily see from (4.5).

Hence,G=G¯. The Gaussian curvature is therefore a projective invariant. It should be noted that, while orthographic projection is assumed, the image plane may be placed in any arbitrary position with respect to the curve S, and for all such positions, the Gaussian curvature K holds the same numerical value. Equation (2.30) should be used in the image plane to obtain a correct measurement of K.

BlauS. K.Gravity probe B concludes its 50-year questPhysics Today20116471416BakhoumE. G.TomaC.Relativistic short range phenomena and space-time aspects of pulse measurementsMathematical Problems in Engineering200820082010.1155/2008/4101564101562471419ZBL1163.83319RothmanT.Geodesics, domes, and spacetimeScience a la Mode1989Princeton University PressDudaR. O.HartP. E.Pattern Classification and Scene Analysis1973New York, NY, USAWileyHornB. K.Robot Vision1987The MIT Pressdo CarmoM. P.Differential Geometry of Curves and Surfaces1976Englewood Cliffs, NJ, USAPrentice-Hallviii+5030394451SyngeJ. L.SchildA.Tensor Calculus1978New York, NY, USADoverix+324521984