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3. Results and discussion
3.1. FTIR analysis
FTIR spectra are commonly employed to identify the change of
characteristic groups. Fig. 1 presented the FTIR spectra of PAL samples.
It could be seen that the absorption bands at 1030 and
983 cm−1 were ascribed to the Si\O stretching vibrations [22], and
the absorption bands at 519 and 478 cm−1 were attributed to the
Si\O bending vibrations. The bands at 3411 and 1646 cm−1 were
assigned to the characteristic O\H stretching and H\O\H bending
vibration of the coordinated and adsorbed water in PAL samples,
respectively. The broad bands at 3621¨C3543 cm−1 were ascribed to
the stretching vibrations of (Al)O\H and (Mg)O\H bonds. As could
be seen from Fig. 1, compared with the spectrum of PAL-0, for PAL-6,
the absorption bands (1030 and 983 cm−1) became blunt and the
strength reduced. And there were no other obvious differences among
the characteristic absorption bands of PAL samples.3.2. FESEM analysis
The FESEM micrographs of PAL-0, PAL-4, PAL-6 and PAL-8 were
observed and shown in Fig. 2. It can be seen from Fig. 2a, the rodlike
crystals of PAL were well developed with a length up to 1 ¦Ìm
and a diameter of about 50¨C80 nm. The rod-like crystals of PAL
were tightly packed due to the actions of van der Waals force and
hydrogen bonds. After grinding treatment (PAL-4 and PAL-6), some
rod-like crystals of PAL became shorter (Fig. 2b and c), the crystal
bundles were partially dissociated and the dispersion degree of PAL
crystals was improved. However, the rod-like crystals obviously got
shorter when the grinding times were further increased (PAL-8),
and most of them were in the form of granules (Fig. 2d). The crystal
aggregates were significantly dissociated and the structure of
PAL-8 was modified. The results could be explained as follows. The
interaction among the rod¨Clike single crystals of PAL is weak because
of a line¨Cline like contact [23]. When raw PAL was grinded, the two
disks of stone miller generated strong compression, shearing stress
and looping stress, which split the crystal bundles into individual rodlike
crystals and the crystal aggregates were dissociated. With increasing
the grinding times, the continual shearing stress and looping stress
acting on the rod-like crystals of PAL increased, and induced the breakage
of rod-like crystals, and therefore the crystal rods will be shorter.
That is to say, large shearing forces resulting from the stone miller operating
on the PAL can make the crystal aggregates and bundles into several
crystal bundles or single crystals. However, if the strong shearing
stress continues for a long time, it can cause serious damage to the
long single crystals of PAL before obtaining high dispersion. In this
case, to search out appropriate grinding times is essential and it can
be said that the method of grinding treatment on PAL with appropriate
grinding times can disperse part of the crystal aggregates into small
crystal bundles and rod-like single  crystals, which is helpful to extend
the practical application of PAL.
3.3. XRD analysis
X-ray diffraction patterns of PAL samples were presented in Fig. 3.
A characteristic reflection peak of PAL at 2¦È=8.38º (d=10.6 Å [24]
can be observed for all the PAL samples with greater intensity, indicating
the order¨Cdisorder structural degree of PAL was very high.
The appearance of the diffraction peak at 2¦È=26.5º (d=3.36 Å
and 2¦È=31.0º (d=2.88 Å revealed that PAL contains minor contents
(contaminants) of quartz and dolomite [24,25]. As the grinding
times increased to 4, no significant change in diffraction peaks can be
observed between the X-ray patterns of PAL-0, PAL-2 and PAL-4, suggesting
the crystal structure of PAL was not affected in the processesystals, which is helpful to extend the practical application of PAL.

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