Page 316 - Physical Principles of Sedimentary Basin Analysis
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298                        Flexure of the lithosphere

                 Exercise 9.6 Let the surface load q(x) be given as a piecewise linear curve, where the load
                 at position x in interval i from x i to x i+1 is

                                                                q i+1 − q i
                                  q(x) = c i (x − x i ) + q i where c i =           (9.67)
                                                                x i+1 − x i
                 and where q i is the load at position x i . The piecewise linear surface load can be represented
                                          ∞

                                             a
                 as a Fourier series q(x) =  n=1 n sin(k n x) where k n = πn/L. Show that the Fourier
                 coefficients are
                         2         x           1        
   (q i − c i x i )    x i+1
                            N
                    a n =      c i   cos(k n x) +  sin(k n x) −       cos(k n x)    (9.68)
                         L         k n         k 2              k n
                           i=1                  n                             x i
                                                      b
                 when N is the number of intervals and [ f (x)] is used as notation for f (b) − f (a).
                                                      a
                 Solution: Each interval i has the contribution
                                              2     x i+1
                                        I n,i =      q(x) sin(k n x)dx              (9.69)
                                              L
                                                 x i

                 to each Fourier coefficient a n . Useful integral:  x sin(ax)dx =−(x/a) cos(ax) +
                     2
                 (1/a ) sin(ax).
                 Comments: The basis function sin(k n x) imposes the boundary condition w = 0atthe
                 boundaries x = 0 and x = L. The Fourier solution is in this respect different from the
                 superposition of point load solutions (see Note 9.3), because the point load solutions have
                 w = 0at x =±∞. The Fourier series solution is more computationally demanding than
                 the corresponding point load solution, because of the sum over n in addition to the sum
                 over intervals i. The infinite sum over n can be truncated at a sufficiently large number,
                 depending on the wanted accuracy, and could typically be 100.
                 Exercise 9.7 Show that coefficients in the Fourier series (9.65) are zero for every even n,
                 (n = 2, 4,...) when the load q(x) is symmetric around L/2.



                                 9.5 The deflection of a plate under compression
                 An already bent lithospheric plate will buckle further under the action of an external com-
                 pressive horizontal force (see Figure 9.11). We therefore start by extending the equation for
                 the deflection of a plate by adding the bending moment (torque) from the horizontal force.
                 The bending moment from a horizontal force F becomes Fw when the vertical deflec-
                 tion is w. The torque balance, where the internal bending moment is equal to the external
                 bending moment, is
                                  2
                                 d w      ∞




                               D     =     (x − x) q(x ) −   gw(x ) dx − Fw         (9.70)
                                 dx 2   x
                 where the internal bending moment is the left-hand side, and the external bending moment
                 is the right-hand side. The pressure on the plate in the vertical direction is the surface load
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