Page 103 - Caldera Volcanism Analysis, Modelling and Response
P. 103

78                                         Roberto Sulpizio and Pierfrancesco Dellino





























          Figure 10  (a) Sketch of the changes in driving and resisting forces for a PDC that moves over
          an inclined obstacle; (b) simple diagram showing the splitting of the initial velocity (v 0 ) into
          the normal (v n ) and the tangential (v t ) components due to the steepening of slope.


          (r ¼ 0) v t ¼ 0. Hence, the kinetic energy of the moving flow can be written as:
                                              1   2
                                         E c ¼ rhn t                            (7)
                                              2
             To reach a complete stop of the moving current, the work exerted by frictional
          forces (W f ) and transformation in potential energy (E p ) must equal the available
          kinetic energy:
                                      E c þ E p þ W f ¼ 0                       (8)
          under the assumption that frictional forces are dissipated only as work (W f ) at the
          flow base:
                                      W f ¼ krhgL cos y                         (9)
          where k is the coefficient of dynamic friction, L the travelled length on slope and
          y the slope angle (Figure 10), and:
                                       E p ¼ rhgL sin y                        (10)

          then, we can obtain the length travelled along slope, L:
                                       2
                                   L ¼ n ½2gðk cos y þ sin yފ  1              (11)
                                       t
             Inspection of Equation (11) reveals that it represents a power-law function (i.e.
          a parabola in L vs. v space) and that L critically depends on slope but increases
          dramatically for very fast currents.
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