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380                             Handbook of Properties of Textile and Technical Fibres

            The oriented amorphous domains are primarily in the intrafibrillar region and the
         unoriented components are mainly in the interfibrillar region (see Fig. 12.13). These
         amorphous phases are different in packing density and interchain structure. The chain
         segments inside the oriented amorphous region are more densely packed and their
         interchain interactions are more like crystals. Interactions for the unoriented amorphous
         region are similar to those in the polymer melt. This structural disparity leads to the
         two amorphous domains responding differently in processing (i.e., drawing and heat
         setting) and environmental conditions (i.e., humidity and temperature). The unoriented
         components probably have a greater influence on the dye/moisture diffusion rate than
         oriented amorphous components.
            The basic characteristic of the noncrystalline phase is the glass transition
         temperature T g since it has a considerable effect on both the processing and properties
         of the polyamide fibers. It defines the temperature at which mobility of chain segments
         or structural units begins. Processes affecting this phase have a corresponding effect on
         the glass transition temperature. This is particularly evident in its response to the
         concentration of water absorbed in polyamides. An increase in water content results

         in a steady decrease of T g towards a limiting value (83% in C from dry T g for PA
         6 and 77% from dry T g for PA 66) (Yang, 2006).
            This phenomenon may be explained by a sorption mechanism according to which
         3 mol of water interacts with two neighboring amide groups (see Fig. 12.14).
            Polymers crystallizing from the melt are free from external stresses exhibited by
         spherulitic structures (see Fig. 12.15). Spherulites originate from their crystal nuclei
         and grow radially in all directions.
            Typical, is the radial arrangement of individual crystallite-fibrils in formation with
         the spherical symmetry. The radial fibrils normally diverge. When they are branching
         (creating more fibrils at greater radial distances) the spherulite space will be uniformly
         filled (Puffr and Kubanek, 1991a).
            During deformation up to high strains (usually due to elongational flow in melt spin-
         ning and plastic deformation in drawing), almost all isotropic spherulites are transformed


         Figure 12.14 Interaction of water
         with polyamides.
                                                                        C   O
                                                                 H
                                                                    HN
                                          C  O  H O  HN          O
                                                               H
                                      HN          H      C  O
                                                               H
                                                                  O
                                                               H
                                                         C  O
                                                               H
                                          C  O  H O  HN          O
                                                                     HN
                                      HN          H              H
                                                                        C   O
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