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Integration with variables Notes_Part_4

Course: MATH 5587, Fall 2010
School: UCF
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proof The of the converse -- that any function whose real and imaginary components satisfy the CauchyRiemann equations is differentiable -- will be omitted, but can be found in any basic text on complex analysis, e.g., [3, 65, 118]. Remark : It is worth pointing out that equation (7.19) tells us that f satisfies f /x = - i f /y, which, reassuringly, agrees with the first equation in (7.5). Example 7.4. Consider...

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proof The of the converse -- that any function whose real and imaginary components satisfy the CauchyRiemann equations is differentiable -- will be omitted, but can be found in any basic text on complex analysis, e.g., [3, 65, 118]. Remark : It is worth pointing out that equation (7.19) tells us that f satisfies f /x = - i f /y, which, reassuringly, agrees with the first equation in (7.5). Example 7.4. Consider the elementary function z 3 = (x3 - 3 x y 2 ) + i (3 x2 y - y 3 ). Its real part u = x3 - 3 x y 2 and imaginary part v = 3 x2 y - y 3 satisfy the CauchyRiemann equations (7.18), since v u = 3 x2 - 3 y 2 = , x y u v = -6xy = - . y x Theorem 7.3 implies that f (z) = z 3 is complex differentiable. Not surprisingly, its derivative turns out to be f (z) = u v v u +i = -i = (3 x2 - 3 y 2 ) + i (6 x y) = 3 z 2 . x x y y Fortunately, the complex derivative obeys all of the usual rules that you learned in real-variable calculus. For example, d n z = n z n-1 , dz d cz e = c ec z , dz 1 d log z = , dz z (7.20) and so on. The power n can be non-integral -- or even, in view of the identity z n = en log z , complex, while c is any complex constant. The exponential formulae (7.14) for the complex trigonometric functions implies that they also satisfy the standard rules d cos z = - sin z, dz d sin z = cos z. dz (7.21) The formulae for differentiating sums, products, ratios, inverses, and compositions of complex functions are all identical to their real counterparts, with similar proofs. Thus, thankfully, you don't need to learn any new rules for performing complex differentiation! Remark : There are many examples of seemingly reasonable functions which do not have a complex derivative. The simplest is the complex conjugate function f (z) = z = x - i y. Its real and imaginary parts do not satisfy the CauchyRiemann equations, and hence z does not have a complex derivative. More generally, any function f (z, z) that explicitly depends on the complex conjugate variable z is not complex-differentiable. 1/19/12 225 c 2012 Peter J. Olver Power Series and Analyticity A remarkable feature of complex differentiation is that the existence of one complex derivative automatically implies the existence of infinitely many! All complex functions f (z) are infinitely differentiable and, in fact, analytic where defined. The reason for this surprising and profound fact will, however, not become evident until we learn the basics of complex integration in Section 7.6. In this section, we shall take analyticity as a given, and investigate some of its principal consequences. Definition 7.5. A complex function f (z) is called analytic at a point z0 C if it has a power series expansion f (z) = a0 + a1 (z - z0 ) + a2 (z - z0 ) + a3 (z - z0 ) + = which converges for all z sufficiently close to z0 . 2 3 n=0 an (z - z0 )n , (7.22) Typically, the standard ratio or root tests for convergence of (real) series that you learned in ordinary calculus, [7, 129], can be applied to determine where a given (complex) power series converges. We note that if f (z) and g(z) are analytic at a point z0 , so is their sum f (z) + g(z), product f (z) g(z) and, provided g(z0 ) = 0, ratio f (z)/g(z). Example 7.6. All of the real power series found in elementary calculus carry over to the complex versions of the functions. For example, e = 1+z + z + z + = z 1 2 2 1 6 3 n=0 zn n! (7.23) is the power series for the exponential function based at z0 = 0. A straightforward application of the ratio test proves that the series converges for all z. On the other hand, the power series 1 = 1 - z2 + z4 - z6 + = (-1)k z 2 k , (7.24) 2+1 z k=0 converges inside the unit disk, where | z | < 1, and diverges where outside, | z | > 1. Again, convergence is established through the ratio test. The ratio test is inconclusive when | z | = 1, and we shall leave the more delicate question of precisely where on the unit disk this complex series converges to a more advanced treatment, e.g., [3]. In general, there are three possible options for the domain of convergence of a complex power series (7.22): (a) The series converges for all z. (b) The series converges inside a disk | z - z0 | < of radius > 0 centered at z0 and diverges for all | z - z0 | > outside the disk. The series may converge at some (but not all) of the points on the boundary of the disk where | z - z0 | = . (c) The series only converges, trivially, at z = z0 . The number is known as the radius of convergence of the series. In case (a), we say = , while in case (c), = 0, and the series does not represent an analytic function. 1/19/12 226 c 2012 Peter J. Olver An example determining converges is delegated to that has = 0 is the power series n! z n . In the intermediate case (b), precisely where on the boundary of the convergence disk the power series quite delicate, and will not be pursued here. The proof of this result is Exercise ; see also [3, 65, 118] for further details. Remarkably, the radius of convergence for the power series of a known analytic function f (z) can be determined by inspection, without recourse to any fancy convergence tests! Namely, is equal to the distance from z0 to the nearest singularity of f (z), meaning a point where the function fails to be analytic. In particular, the radius of convergence = if and only if f (z) is analytic for all z, with no singularities; examples include ez , cos z, and sin z. On the other hand, the rational function f (z) = z2 1 1 = +1 (z + i )(z - i ) has singularities at z = i , and so its power series (7.24) has radius of convergence = 1, which is the distance from z0 = 0 to the singularities. Thus, the extension of the theory of power series to the complex plane serves to explain the apparent mystery of why, as a real function, (1 + x2 )-1 is well-defined and analytic for all real x, but its power series only converges on the interval ( -1, 1 ). It is the complex singularities that prevent its convergence when | x | > 1. If we expand (z 2 + 1)-1 in a power series at some other point, say z0 = 1 + 2 i , then we need to determine which singularity is closest. We compute | i - z0 | = | -1 - i | = 2, while | - i - z0 | = | -1 - 3 i | = 10, and so the radius of convergence = 2 is the smaller. Thus we can determine the radius of convergence without any explicit formula for its (rather complicated) Taylor expansion at z0 = 1 + 2 i . There are, in fact, only three possible types of singularities of a complex function f (z): Pole. A singular point z = z0 is called a pole of order n > 0 if and only if f (z) = h(z) , (z - z0 )n (7.25) Essential singularity. By definition, a singularity is essential if it is not a pole or a branch point. Essential singularities are considerably more complicated than poles and branch points. The quintessential example is the essential singularity of the function e1/z at z0 = 0. Example 7.7. The complex function f (z) = 1/19/12 ez ez = z3 - z2 - 5 z - 3 (z - 3)(z + 1)2 227 c 2012 Peter J. Olver Branch point. We have already encountered the two basic types: algebraic branch points, such as the function n z at z0 = 0, and logarithmic branch points such as log z at z0 = 0. The degree of the branch point is n in the first case and in the second. where h(z) is analytic at z = z0 and h(z0 ) = 0. The simplest example of such a function is f (z) = a (z - z0 )-n for a = 0 a complex constant.
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UCF - MATH - 5587
is analytic everywhere except for singularities at the points z = 3 and z = -1, where its denominator vanishes. Since f (z) = h1 (z) , z-3 where h1 (z) = ez (z + 1)21 is analytic at z = 3 and h1 (3) = 16 e3 = 0, we conclude that z = 3 is a simple (order
UCF - MATH - 5587
if and only if it has vanishing divergence: v = u v + = 0. x y (7.36)Incompressibility means that the fluid volume does not change as it flows. Most liquids, including water, are, for all practical purposes, incompressible. On the other hand, the flow is
UCF - MATH - 5587
Using formula (7.19) for the complex derivative, d = -i = u - i v, dz x y so = u, x = v. yThus, = v, and hence the real part (x, y) of the complex function (z) defines a velocity potential for the fluid flow. For this reason, the anti-derivative (z) is k
UCF - MATH - 5587
gDFigure 7.14.Mapping to the Unit Disk.Remark : In this section, we have focused on the fluid mechanical roles of a harmonic function and its conjugate. An analogous interpretation applies when (x, y) represents an electromagnetic potential function;
UCF - MATH - 5587
Figure 7.16.The Effect of = z 2 on Various Domains.obtained by cutting the complex plane along the negative real axis. On the other hand, vertical lines Re z = a are mapped to circles | | = ea . Thus, a vertical strip a &lt; Re z &lt; b is mapped to an annulu
UCF - MATH - 5587
zph zFigure 7.18.Complex Curve and Tangent.notation x(t) = ( x(t), y(t) ) to complex notation z(t) = x(t)+ i y(t). All the usual vectorial curve terminology - closed, simple (non-self intersecting), piecewise smooth, etc. - is employed without modific
UCF - MATH - 5587
Center: .1 Radius: .5Center: .2 + i Radius: 1Center: 1 + i Radius: 1Center: -2 + 3 i Radius: 3 2 4.2426Center: .2 + i Radius: 1.2806 Figure 7.21.Center: .1 + .3 i Radius: .9487Center: .1 + .1 i Radius: 1.1045Center: -.2 + .1 i Radius: 1.2042Airfoi
UCF - MATH - 5587
Example 7.35. The goal of this example is to construct an conformal map that takes a half disk D+ = | z | &lt; 1, Im z &gt; 0 (7.73) to the full unit disk D = cfw_ | | &lt; 1 . The answer is not = z 2 because the image of D+ omits the positive real axis, resulting
UCF - MATH - 5587
7.5. Applications of Conformal Mapping.Let us now apply what we have learned about analytic/conformal maps. We begin with boundary value problems for the Laplace equation, and then present some applications in fluid mechanics. We conclude by discussing h
UCF - MATH - 5587
Figure 7.25.A NonCoaxial Cable.Example 7.39. A non-coaxial cable. The goal of this example is to determine the electrostatic potential inside a non-coaxial cylindrical cable, as illustrated in Figure 7.25, with prescribed constant potential values on th
UCF - MATH - 5587
0 Figure 7.29.15 Fluid Flow Past a Tilted Plate.30Note that = ( 1, 0 ), and hence this flow satisfies the Neumann boundary conditions (7.95) on the horizontal segment D = . The corresponding complex potential is (z) = z, with complex velocity f (z) = (
UCF - MATH - 5587
on the unit disk D for an impulse concentrated at the origin; see Section 6.3 for details. How do we obtain the corresponding solution when the unit impulse is concentrated at another point = + i D instead of the origin? According to Example 7.25, the lin
UCF - MATH - 5587
as long as n = -1. Therefore, we can use the Fundamental Theorem of Calculus (which works equally well for real integrals of complex-valued functions), to evaluate n+1 1 -1 = n = 2 k + 1 odd, 0, 2 t + i (t - 1) 2 z n dz = = , n = 2 k even. n+1 P t = -1 n+
UCF - MATH - 5587
Figure 7.32.Orientation of Domain Boundary.Theorem 7.48. If f (z) is analytic on a bounded domain C, then f (z) dz = 0.(7.118)Proof : If we apply Green's Theorem to the two real line integrals in (7.109), we find u dx - v dy = - u v - x y = 0,v dx +
UCF - MATH - 5587
Proof : Note that the integrand f (z) = 1/(z - a) is analytic everywhere except at z = a, where it has a simple pole. If a is outside C, then Cauchy's Theorem 7.48 applies, and the integral is zero. On the other hand, if a is inside C, then Proposition 7.
UCF - MATH - 5587
0 Figure 7.36.15 Kutta Flow Past a Tilted Airfoil.30which remains asymptotically 1 at large distances. By Cauchy's Theorem 7.48 coupled with formula (7.123), if C is a curve going once around the disk in a counter-clockwise direction, then i 1 dz = - 2
UCF - MATH - 5587
is analytic in the disk | z | 2 since its only singularity, at z = 3, lies outside the contour C. Therefore, by Cauchy's formula (7.135), we immediately obtain the integral ez dz = z2 - 2 z - 3 f (z) i dz = 2 i f (-1) = - . z+1 2eCCNote: Path independe
UCF - MATH - 5587
Chapter 12 Dynamics of Planar MediaIn previous chapters we studied the equilibrium configurations of planar media - plates and membranes - governed by the two-dimensional Laplace and Poisson equations. In this chapter, we analyze their dynamics, modeled
UCF - MATH - 5587
In this manner, we arrive at the basic conservation law relating the heat energy density and the heat flux vector w. As in our one-dimensional model, cf. (4.3), the heat energy density (t, x, y) is proportional to the temperature, so (t, x, y) = (x, y) u(
UCF - MATH - 5587
for the diffusion equation. See [35; p. 369] for a precise statement and proof of the general theorem. Qualitative Properties Before tackling examples in which we are able to construct explicit formulae for the eigenfunctions and eigenvalues, let us see w
UCF - MATH - 5587
Theorem 12.1. Suppose u(t, x, y) is a solution to the forced heat equation ut = u + F (t, x, y), for (x, y) , 0 &lt; t &lt; c,where is a bounded domain, and &gt; 0. Suppose F (t, x, y) 0 for all (x, y) and 0 t c. Then the global maximum of u on the set cfw_ (t, x
UCF - MATH - 5587
so there are no non-separable eigenfunctions . As a consequence, the general solution to the initial-boundary value problem can be expressed as a linear combination u(t, x, y) =m,n = 1cm,n um,n (t, x, y) =m,n = 1cm,n e- m,n t vm,n (x, y)(12.41)of
UCF - MATH - 5587
Let us start with the equation for q(). The second boundary condition in (12.50) requires that q() be 2 periodic. Therefore, the required solutions are the elementary trigonometric functions q() = cos m or sin m , where = m2 , (12.53)with m = 0, 1, 2, .
UCF - MATH - 5587
15 10 5 -4 -2 -5 -10 -15 2 4Figure 12.3.The Gamma Function.Thus, at integer values of x, the gamma function agrees with the elementary factorial. A few other values can be computed exactly. One important case is when x = 1 . Using 2 the substitution t
UCF - MATH - 5587
Remark : The definition of a singular point assumes that the other coefficients do not both vanish there, i.e., either q(x0 ) = 0 or r(x0 ) = 0. If all three functions happen to vanish at x0 , we can cancel any common factor (x - x0 )k , and hence, withou
UCF - MATH - 5587
we find that the only non-zero coefficients un are when n = 3 k +1. The recurrence relation u3 k+1 = u3 k-2 (3 k + 1)(3 k) yields u3 k+1 = 1 . (3 k + 1)(3 k)(3 k - 2)(3 k - 3) 7 6 4 3The resulting solution isx3 k+1 . (3 k + 1)(3 k)(3 k - 2)(3 k - 3) 7 6
UCF - MATH - 5587
two different Frobenius expansions. Usually, this expectation is valid, but there is an important exception, which occurs when the indices differ by an integer. The general result is summarized in the following list: (i ) If r2 - r1 is not an integer, the
UCF - MATH - 5587
We have thus found the series solution (-1)k xm+2k . 22k k(k - 1) 3 2 (r + k)(r + k - 1) (r + 2)(r + 1) k=0 k=0 (12.93) So far, we not paid attention to the precise values of the indices r = m. In order to continue the recurrence, we need to ensure that t
UCF - MATH - 5587
where h0 = 0, while = limkhk = 1 +1 1 1 + + + , 2 3 k (12.102)hk - log k .5772156649 . . .is known as Euler's constant. All Bessel functions of the second kind have a singularity at the origin x = 0; indeed, by inspection of (12.101), we find that th
UCF - MATH - 5587
of the Bessel boundary value problem (12.5455) are the squares of the roots of the Bessel function of order m. The corresponding eigenfunctions are wm,n (r) = Jm (m,n r) , n = 1, 2, 3, . . . , m = 0, 1, 2, . . . , (12.112)defined for 0 r 1. Combining (12
UCF - MATH - 5587
t=0t = .04t = .08t = .12 Figure 12.6.t = .16 Heat Diffusion in a Disk.t = .212.5. The Fundamental Solution of the Heat Equation.As we learned in Section 4.1, the fundamental solution to the heat equation measures the temperature distribution result
UCF - MATH - 5587
for the planar heat equation is given by the linear superposition formula u(t, x, y) = 1 4 t f (, ) e- [ (x-)2+(y-)2 ]/(4 t)d d.(12.125)We can interpret the solution formula (12.125) as a two-dimensional convolution u(t, x, y) = F (t, x, y) f (x, y)
UCF - MATH - 5587
Vibration of a Rectangular Drum Let us first consider the vibrations of a membrane in the shape of a rectangle R= 0 &lt; x &lt; a, 0 &lt; y &lt; b ,with side lengths a and b, whose edges are fixed to the (x, y)plane. Thus, we seek to solve the wave equation utt = c2
UCF - MATH - 5587
A table of their values (for the case c = 1) can be found in the preceding section. The Bessel roots do not follow any easily discernible pattern, and are not rational multiples of each other. This result, known as Bourget's hypothesis, [142; p. 484], was
UCF - MATH - 5587
following table, we display a list of all relative vibrational frequencies (12.158) that are &lt; 6. Once the lowest frequency 0,1 has been determined - either theoretically, numerically or experimentally - all the higher overtones m,n = m,n 0,1 are simply o
UCF - MATH - 5587
For example, on a unit square R = 0 &lt; x, y &lt; 1 , an accidental degeneracy occurs whenever m2 + n2 = k 2 + l2 (12.163) for distinct pairs of positive integers (m, n) = (k, l). The simplest possibility arises whenever m = n, in which case we can merely reve
UCF - MATH - 5587
Chapter 9 Linear and Nonlinear Evolution EquationsIn this chapter, we analyze several of the most important evolution equations, both linear and nonlinear, involving a single spatial variable. Our first stop is to revisit the heat equation. We introduce
UCF - MATH - 5587
Chapter 3 Fourier SeriesJust before 1800, the French mathematician/physicist/engineer Jean Baptiste Joseph Fourier made an astonishing discovery. Through his deep analytical investigations into the partial differential equations modeling heat propagation
UCF - MATH - 5587
Chapter 8 Fourier TransformsFourier series and their ilk are designed to solve boundary value problems on bounded intervals. The extension of Fourier methods to the entire real line leads naturally to the Fourier transform, an extremely powerful mathemat
UCF - MATH - 5587
Chapter 6 Generalized Functions and Green's FunctionsBoundary value problems, involving both ordinary and partial differential equations, can be profitably viewed as the infinite-dimensional function space versions of finite dimensional systems of linear
UCF - MATH - 5587
Math 5587 September 8, 2011Homework #1Problems: Chapter 1: 1.1ae, 1.2b,d, 1.5a,e, 1.6, 1.12a, 1.16ad, 1.18, 1.19, 1.20, 1.24. Chapter 2: 2.1 2, 3c,e, 4, 6.Due: Thursday, September 15
UCF - MATH - 5587
Math 5587 September 20, 2011Homework #2Problems: Chapter 2: 2.2 2.3 2a, 3b, 9, 17, 26, 27. 2, 5, 14, 15.Due: Thursday, September 29 First Midterm: Tuesday, October 11 Will cover chapters 1 &amp; 2. You will be allowed to use one 8&quot; 11&quot; sheet of notes. Note
UCF - MATH - 5587
Math 5587 September 29, 2011Homework #3Problems: Chapter 2: 2.4 2, 3, 4c,d, 8, 11, 12.Also, in 2.4.8, determine the domain of influence of the point (0,2) and the domain of dependence of the point (3,-1). Discuss what these tell you about the solution.
UCF - MATH - 5587
Math 5587 October 13, 2011Homework #4Problems: Chapter 3: 3.1 3.2 2b, 5. 1, 2g, 3a, 5, 6a,g, 15a,d, 16a,d, 24, 25, 34, 35, 41b, 52, 53.Due: Thursday, October 20
UCF - MATH - 5587
Math 5587 October 25, 2011Homework #5Problems: Chapter 3: 3.3 1, 2, 8. 3.4 2b, 3c, 7, 9 (just use one of the two methods). 3.5 2b,c,d, 4, 8, 11a,b,c. Due: Tuesday, November 1 Second Midterm: Thursday, November 17 Will cover chapters 3 &amp; 4. You will be a
UCF - MATH - 5587
Math 5587 November 3, 2011Homework #6Problems: Chapter 3: 3.5 13, 21c,e, 22b,c, 27b,d, 30, 31, 35a, 42. Chapter 4: 4.1 2, 4c, 10, 17a,b. Due: Thursday, November 10 Second Midterm: Thursday, November 17 Will cover chapters 3 &amp; 4. You will be allowed to u
UCF - MATH - 5587
Math 5587 November 10, 2011Homework #7Problems: Chapter 4: 4.2 3a, 4b,e, 8, 14a,d,e, 26. 4.3 4, 7, 10c, 11, 12a, 16, 24a, 29, 31. Due: Tuesday, November 22 Second Midterm: Thursday, November 17 Will cover chapters 3 &amp; 4. You will be allowed to use one 8
UCF - MATH - 5587
Math 5587 December 6, 2011Homework #8Problems: Chapter 4: 4.4 2a,e,f, 12a,e,f, 13, 17a,b. Chapter 6: 6.1 1b,d, 2d, 3, 5b, 8, 13, 19, 35. 6.2 2, 6. 6.3 1, 2, 6. Due: Tuesday, December 13 Final Exam: Take Home, to be handed out on Tuesday, December 13 and
UCF - MATH - 5587
Chapter 2 Linear and Nonlinear WavesOur exploration of the vast mathematical continent that is partial differential equations will begin with simple first order equations. In applications, first order partial differential equations are most commonly used
UCF - MATH - 5587
Chapter 5 Numerical Methods: Finite DifferencesAs you know, the differential equations that can be solved by an explicit analytic formula are few and far between. Consequently, the development of accurate numerical approximation schemes is essential for
UCF - MATH - 5587
Chapter 11 Numerical Methods: Finite ElementsIn Chapter 5, we introduced the first, the oldest, and in many ways the simplest class of numerical algorithms for approximating the solutions to partial differential equations: finite differences. In the pres
UCF - MATH - 5587
Chapter 10 A General Framework for Linear Partial Differential EquationsBefore pressing on to the higher dimensional forms of the heat, wave, and Laplace/ Poisson equations, it is worth taking some time to develop a general, abstract, linear algebraic fr
UCF - MATH - 5587
Chapter 12 Partial Differential Equations in SpaceAt last we have reached the ultimate rung of the dimensional ladder (at least for those of us living in a three-dimensional universe): partial differential equations in physical space. As in the one- and
UCF - MATH - 5587
Chapter 4 Separation of VariablesThere are three paradigmatic linear second order partial differential equations that have collectively driven the development of the entire subject. The first two we have already encountered: The wave equation describes v
UCF - MATH - 5587
Chapter 1 What are Partial Differential Equations?Let us begin by specifying our object of study. A differential equation is an equation that relates the derivatives of a (scalar) function depending on one or more variables. For example, d4 u du + u2 = c
University of Florida - CEG - 4012
Lecture 1 Review of Geostatic Stresses Unit WeightsYw = unit weight of water Ym = moist unit weight of unsaturated soil Ysat = unit weight of saturated soil y' = &quot;effective&quot; unit weight of soil = (Ysat - Yw) if soil saturated= Ym if soil not saturated=
University of Florida - CEG - 4012
Geostatic Stresses These self-weight stresses (ay, a'y, ah' a'h) are called geostatic stresses For a level surface there are no shear forces induced by the geostatic stresses, and therefore they are also principal stresses: a, =ay and a3 = ah Karl Terzag
University of Florida - CEG - 4012
using the effective weight concept:= 0&quot; h6'(100 pet + 4'(118-62.4 pet + 6'(126-62.4 pet+4'(120-62.4 pet 230 pst: 1434 pst= 600 pst + 222 pst + 382 pst +=-K (J'y : 0.5 (1434 pst) : 717 pst 14' (62.4 pet): 874 pst U(a' h + u): 717 pst + 874 pst: 15
University of Florida - CEG - 4012
S1 Stresses Changes Due to Surface Loads (Aerv) o Stresses within a soil mass will change as a result of surface loads. The change in total stress spreads and diminishes with distance from the load. Equations and charts are available to calculate both th
University of Florida - CEG - 4012
S2 Pyramid Approximation For Surface Loads: The &quot;2:1 melhod &quot;used for &quot;back of Ihe envelope&quot; solutions (seen on the PE exam). o A=LoadedArea =BxLQ = Tolal Load = q x B x LQr+-&quot;q=unit pressurewhere B = width (short sjde, alwill's) L _ length !loM-si
University of Florida - CEG - 4012
S3 Point Load on the Surface: Boussinesq (1883) - French Physicist(with the parameters as shown at right)Qo Assumotionc:. I. nALF-SPACE - semi-infinite 2. ELASTIC 3. HOMOGENEOUS - same properties throughout 4. ISOTROPIC - same properties in all directi