Page 366 - Fiber Fracture
P. 366

348                                                          J.W.S. Hearle

               in Fig.  12d,e are found by fitting stress-strain  curves for one type of fibre and are then
               used  to  predict  the  response  for  the  other type.  Although  this  model  provides  some
               insights into the structural mechanics, it neglects many features, notably the influence of
               orientation.

               Fracture

                 Fracture in these solution-spun fibres is probably triggered by the amorphous material
               reaching  its limiting  extension and polymer molecules breaking.  Fig.  13a shows how
               two  crystalline  regions  in  viscose  rayon  will  be  linked  together  by  tie-molecules,
               which  break  when  they  reach  a  critical  load.  In  the  wet  state,  the  free  chain  ends
               will not  contribute  to the tension.  Consequently, as shown in Fig.  13b, the degree of
               polymerisation (DP) has a major effect on the fibre strength. At low DP, there will be a
               large number of  free chain ends, but as chain length increases there will be fewer and
               the strength approaches an asymptotic maximum. Fig.  13b also shows the considerable
               influence on strength of degree of orientation, as given by the birefringence.
                 Although one can identify the cause of fracture with chain breakage, its manifestation
               is determined by larger-scale structural discontinuities in solution-spun fibres. The fibres
               coagulate  in  a  sponge-like  form  with  solid  material  separated  by  voids  of  residual
               solvent. On  drying,  the  solvent is removed  and  stretching  elongates  the  voids. What
               remains is a coarse structure with regions of integral material separated by  weaknesses
               in the structure corresponding to the original void surfaces. The rupture of  one integral
               zone does not lead to continuous crack propagation, because of the region of weakness,
               but  does  transfer  sufficient stress  to  neighbouring  zones  to  cause  them  to  break  in
               contiguous  positions.  This  leads  to  granular  breaks  as  shown  in  fig.  5  of  the  3rd
               paper (this volume). These SEM pictures are similar to low-magnification views of the


                            f
                   L




















              Fig.  12. A  model  for the stress-strain  properties of  viscose rayon, Hearle (1967). (a-c)  Composite models
              of crystalline C and disordered D material in (a) lamellar L, (b) micellar M, and (c) fibrillar F forms.
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