Abstract
Giant single crystals of isotactic polypropylene (iPP) were obtained using a specific kinetic pathway through the mesophase of iPP; the pre-quenched iPP mesophase was heated to 166 °C at a rate of 75 °C min−1 and maintained at this temperature for 24 h. The obtained crystallites exhibited a very high melting temperature, Tm, of 183.7 °C, which is ∼19 °C higher than the iPP’s nominal Tm (∼165 °C); namely, the observed Tm is immediately close to the literature value of iPP’s equilibrium melting temperature, Tm0 (186.2 °C). The crystallites have bamboo leaf-like or needle-like morphology and are ∼35 μm in length and ∼3.5 μm in width. The thickness of the crystallites was estimated to be 88 nm according to the melting temperature. The number density of the crystallites in a unit volume was controlled by adjusting the heating rate. As the result, well-isolated single crystals of iPP with the above-mentioned morphologies were obtained.
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Introduction
Single crystals of isotactic polypropylene (iPP), especially large sized crystals, have attracted the interest of researchers for many years.1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12 However, the crystal aggregate—the so-called spherulite rather than the single crystal—is usually obtained during the conventional crystallization of iPP from the molten state. Spherulite consists of both crystalline lamella and non-crystalline amorphous regions, which are alternatively arranged with a certain periodicity, that is, long-range order. To obtain thick lamella, considerably long annealing times at high temperatures are usually required; for example, Hikosaka et al.13 obtained iPP spherulite with 66-nm-thick lamellae by annealing at 166 °C for 6 months. This record value for the lamella thickness resulted in a melting temperature of ∼183 °C,14, 15 which is close to the equilibrium melting temperature, Tm0. Several values have been reported for the Tm0 of iPP that range from 183.8 °C to 208 °C.14, 15, 16, 17
In addition to the lamella thickness, isolation between the lamellae or the crystallites is another important factor for qualifying the single crystal.2, 4, 10 Although such an isolated single crystal is readily obtained using the solution crystallization method,3, 4, 5, 6, 7 it is difficult to obtain an isolated single crystal when iPP is crystallized from the bulk melt. Stacks and crosshatches of the lamellae easily occur during the crystallization from the bulk melt.18, 19, 20, 21, 22 The branching of lamellae also inhibits the formation of a single crystal18 and results in the formation of the spherulite. Because of these obstacles, well-isolated iPP single crystals usually only exist during the early stage of the crystallization process.4, 12 As a natural consequence, the size of the iPP single crystal is small when iPP is crystallized from the bulk melt.
In contrast to the above-mentioned conventional crystallization of iPP from the melt, we have reported that a rapid heating of iPP from the mesophase yielded large crystallites that have needle-like or ‘bamboo leaf-like’ (BL) morphology.9, 10 Because the BL crystal was found by chance, neither the formation mechanism nor the optimization of the formation conditions have been clarified in detail. From a structural point of view, it was initially speculated that the BL crystal is a single crystal and not crystal aggregates, such as spherulite, because it presented very sharp X-ray diffraction peaks compared with the normal melt-crystallized spherulite and showed a monochrome image within each domain of the BL crystal in a polarized microscopy observation.9 However, the thermal properties, which directly correlate to the thickness of a single crystal, have not been clarified.
In a previous study, we have observed that a certain temperature region immediately below the melting point with a specific heating rate of ∼60–80 °C min−1 resulted in the maximum growth rate of the crystalline grains when iPP was crystallized from the pre-quenched mesophase.23 Although this result is very useful information for forming BL crystals with good reproducibility, the optimal conditions for the growth rate do not necessarily correspond to the optimal conditions for isolating the single crystal. Therefore, in the present study, by controlling the number density of crystallites in a unit volume, we will clarify the relationship between the melting point of the BL crystal and the formation conditions, such as the heating rate from the mesophase and the annealing temperature.
Experimental procedure
Materials and sample preparations
The iPP material was supplied from the Idemitsu Unitech Co., Ltd; the weight-average molecular weight was Mw=35 3000, with a polydispersity of Mw/Mn=4.4, and a degree of isotacticity (a meso pentad value) of mmmm=0.98. This isotacticity is greater than the critical value (0.68) of isotacticity required to form the mesophase.24 Sample films with a thickness of 200 μm were prepared by quenching molten iPP to 0 °C by dipping the films into ice water. The prepared films were macroscopically transparent and presented two broad peaks in a wide-angle X-ray diffraction (WAXD) pattern, which are characteristic of mesophase iPP.25, 26, 27
Time–temperature protocol
As mentioned in the introduction, the formation conditions for the BL crystal were narrowed in the previous study; specifically, a certain temperature region immediately below the melting point and a specific heating rate of ∼60–80 °C min−1 resulted in the maximum growth rate of the crystalline grain.23 In this study, we prepared two groups of time–temperature protocols based on the above-mentioned condition: first, the heating rate was fixed at 75 °C min−1 and the final annealing temperature was scanned (Figure 1a); and second, the final annealing temperature was fixed at 164 °C and the heating rate was scanned (Figure 1b). In both protocols, the final annealing period was fixed to 24 h.
Optical microscopy observation
Observations with an optical microscope were performed using an Optiphot2-Pol, a product of Nikon, Tokyo, Japan. The bright-field mode was used to avoid counting loss in the number of crystallites because only the crystallites arranged in a specific orientation are detected in the polarized mode. The pre-quenched sample films were heated and annealed according to the prescribed protocol (Figure 1) using a laboratory-made hot stage. The hot stage consisted of a heater block and a control unit. The heater block, to which the sample was in contact, was controlled by a programmable CPU unit, KV-3000 and a PID unit, KV-TF40; both the CPU and the PID units were products of KEYENCE, Osaka, Japan. The temperatures presented in the results were the calibrated temperatures using the actual measured temperatures at the sample position.
Differential scanning calorimetry
Differential scanning calorimetry (DSC) measurements were performed using a Diamond DSC, a product of Perkin-Elmer, Waltham, MA, USA. The pre-quenched sample films were heated and annealed within the DSC instrument according to the prescribed protocol (Figure 1), similar to the optical microscope observations. Immediately after the annealing, the DSC data were recorded during the heating process at a rate of 10 °C min−1. In the latter heating process, the melting behavior of the crystallites was observed. The temperature was calibrated from the melting temperatures of pure In and Sn. All of the measurements were performed under a nitrogen atmosphere.
Wide-angle X-ray diffraction
WAXD measurements were performed using a NANO-Viewer, a product of Rigaku, Tokyo, Japan, with an imaging plate detector at a sample-to-detector distance of 44.5 mm.
Results and discussion
Effect of annealing temperature on crystallization
Figure 2 presents selected optical microscope images after the samples were annealed for 24 h at various temperatures (152–172 °C) following heating at a rate of 75 °C min−1, according to the prescribed protocol (Figure 1a).
As observed in Figure 2, the crystalline entities were only detected when the samples were annealed within a specific temperature window of 157–164 °C. Within the specific temperature window, the size and number density of the crystallites were considerably dependent on the annealing temperature; well-isolated large BL crystals were observed when the sample was annealed at 164 °C (Figure 2b), whereas densely populated small crystallites, although not clear because of overlapping, were observed when the sample was annealed at 157 °C (Figure 2c). On the outer boundaries of the specific temperature window, the images were transparent. The reasons for the transparency below and above the specific window are considered to be different, as follows. Above the specific window (172 °C, Figure 2a), the transparency is unquestionably due to the complete melting, that is, non-existence of crystallites, whereas below the specific window (152 °C, Figure 2d), the absence of the detectable entities does not mean the non-existence of crystallites. At 152 °C, the majority of the mesophase actually transforms into the α-crystal;10, 28, 29 however, the α-crystal exists in the nodular form with a diameter of several tens of nm at most,29 that is, the dimension of the structure is far less than the optical wavelength. Consequently, the iPP film consisting of such nano-crystallites is macroscopically transparent.30 On the basis of Figure 2, well-isolated large BL crystals are obtained when the pre-quenched iPP mesophase is annealed at ∼164 °C following heating at a rate of 75 °C min−1.
Effect of heating rate on crystallization
Figure 3 presents selected optical microscope images after the samples were annealed for 24 h at 164 °C following heating at various rates (5–108 °C min−1), according to the prescribed protocol (Figure 1b). As observed in Figure 3, the crystalline entities were detected when the heating rate was greater than 20 °C min−1. At a heating rate of 5 °C min−1, the images were transparent (Figure 3a). The reason for the transparency is not the non-existence of crystallites but the formation of the nano-crystallites, similar to the case in Figure 2d. Densely populated small crystallites, although not clear because of overlapping, were observed when the sample was heated at a rate of 20 °C min−1 (Figure 3b). At a heating rate of 39 °C min−1, fairly well-isolated large BL crystals were observed (Figure 3c). With increasing heating rate, the isolation between neighboring crystallites was improved (75 °C min−1, Figure 2b). Finally, a unique isolated BL crystal within a scope was attained when the heating rate reached 108 °C min−1 (Figure 3d). At present, we have not yet succeeded in extracting the crystallite from the matrix; the matrix in this case is the mesophase when the crystallization process is stopped by quenching. In this sense, we should say, ‘a single crystal embedded in the mesophase.’
When the annealing temperature was fixed at 164 °C, the heating rate was demonstrated to be an effective parameter for controlling the isolation and the morphology of the crystallites for the crystallization of iPP from the mesophase. Furthermore, note that the annealing temperature of 164 °C is considered to be considerably high in the conventional sense because at such a high temperature it takes a very long time for iPP to crystallize from the normal molten state.31 One of the characteristics of crystallization from the mesophase is that the crystallization proceeds properly at such a high temperature. Another mechanism for crystallization from the mesophase is discussed below.
In what follows, the size and number density of the obtained crystallites are discussed quantitatively on the basis of the image analysis of the micrographs. First, we determined the average longitudinal and lateral sizes, which were apparently determined from the micrographs. Because the crystallites were far thinner than the resolution of the optical microscope, we discuss it below on the basis of the DSC analysis. Figure 4 shows a representation of the size-distribution histogram when iPP was crystallized at 164 °C following heating from the mesophase at a rate of 75 °C min−1. The condition corresponds to Figure 2b, but the sampling was performed covering a wider scope than the displayed microscope image to obtain reasonable statistics. By fitting the Gaussian function to the histogram, the average and standard deviation of the longitudinal and lateral sizes were obtained.
The longitudinal and lateral sizes of the BL crystals as a function of the heating rate are shown in Figures 5a and b, respectively. With increasing heating rate, the longitudinal size increased from ∼7 to ∼35 μm. In parallel, the lateral size slightly increased with increasing heating rate, although the quantitative value for the thinnest case (heating rate of 20 °C min−1) could not be determined because of the resolution of the microscope.
The aspect ratio of the BL crystals as a function of the heating rate was estimated by dividing the longitudinal size by the lateral size, and this ratio is shown in Figure 6. Although the aspect ratio increased with the increasing heating rate, it showed inherently high values of ∼5–10, in common with the case of the single crystals that were produced during the early stage of the melt-crystallization.12
The number density in a unit area was estimated by simply counting the number of crystallites within a unit area in the micrographs. Assuming that only the crystalline entities distributed within the focal depth were detected, the number density in a unit volume was calculated by dividing the number density in a unit area by the focal depth; the focal depth of the present optics was estimated to be 6.2 μm based on the numerical aperture of the lens. Figure 7 shows the estimated number density of the crystallites in a unit volume. The number density varied more than two orders of magnitude with increasing heating rate until ∼60 °C min−1. Therefore, the heating rate was shown to be an effective parameter for controlling the number density of the crystallites; specifically, the isolation between the single crystals can be controlled by the heating rate in the present specific crystallization of iPP from the mesophase. A further increase in the heating rate slightly decreased the number density.
Effect of annealing temperature on the melting behavior of the obtained BL crystals
Figure 8 presents selected thermograms from the DSC measurements during heating scans at a rate of 10 °C min−1 for the samples annealed within the DSC instrument according to the prescribed protocol (Figure 1a) at various temperatures (130–167 °C) for 24 h. The heating scans were started from the prescribed annealing temperatures to 200 °C immediately after the annealing processes. As observed in Figure 8, the endothermic melting peak shifted toward higher temperatures with increasing annealing temperature.
In Figure 9, the melting temperature Tm is plotted as a function of the annealing temperature or the crystallization temperature Tc, the so-called Hoffman–Weeks plots. The diagonal thick solid line indicates the relation of Tm=Tc. In normal Hoffman–Weeks plots, Tm is often linearly proportional to Tc or near-linearly in the region above the Tm=Tc line, and the intersection with the Tm=Tc line is considered to give the Tm0.32
It is clear in Figure 9 that the present behavior is quite different from the normal behavior of the above-mentioned Hoffman–Weeks plots. Paradoxically speaking, the fact that one cannot draw single linear line in the Hoffman–Weeks plots indicates the existence of different crystal forms, and accordingly, the existence of different crystallization mechanisms. In this sense, we should say that Figure 9 is the ‘apparent’ Hoffman–Weeks plot. Below Tc=ca. 155 °C, Tm was almost independent of Tc. As previously discussed, the transparency of the micrograph obtained at 152 °C (Figure 2d) indicates that the crystallites in this temperature region exist in the form of a nodule. Therefore, the Tm is restricted by the nodular size. Above Tc=ca. 155 °C, Tm increased rapidly and seems to plateau at ∼185 °C. The gradient of the Tm vs Tc plots is an index of the perfection and morphology of the crystal;32, 33, 34, 35 with the crystal approaching the infinitely thick or the limiting thickness due to the chain structure, the gradient decreases and becomes horizontal in the ultimate case. Therefore, the observed plateau behavior is the indication that the present BL crystal is near the certain limitation, hopefully an infinitely thick crystal.
The relationships between the Tm and the thickness of the crystallites have been discussed quantitatively in literature.14, 15, 16 Here, we estimated the thickness of the BL crystals assuming the following relationship proposed by Yamada et al.14, 15
The values of Tm are dependent on the methods, such as optical microscopy and DSC. In this study, we determined the Tm using DSC; therefore, the thickness of the crystallites 〈l〉 is an averaged thickness weighted by the DSC. Figure 10 shows an estimated value of 〈l〉 as a function of the annealing temperature, Tc. The 〈l〉 was almost independent of Tc below Tc=ca. 155 °C and the behavior of Tm, whereas the 〈l〉 showed a tendency to diverge above Tc=ca. 155 °C in contrast to the behavior of Tm. Apart from the diverging tendency, we have attained a crystal thickness of 88 nm. Although the obtained value is similar to or slightly larger than the reported value of the lamella thickness of 66 nm when crystallized from the melt,15 the present annealing process greatly reduced the annealing time; the annealing time required 24 h when crystallized from the mesophase, whereas it required 6 months when crystallized from the melt.
Crystal form of giant single crystal
Figure 11 shows the WAXD pattern from the sample obtained by annealing at 164 and 135 °C. The peak at ∼2θ=31.6° arises from the diffraction from the α-2 form.17 It is obvious from this figure that the crystal form for the lower temperature (nodular crystals) is α-1 and that of the higher temperature (BL crystals) is the α-2. The unusual behavior in the Hoffman–Weeks plots in Figure 9 should be associated with the transition from the α-1 to the α-2 form.
Possible mechanism for the formation of a giant single crystal
The formation conditions and characteristics of the BL crystals have been substantially elucidated as thus far described. Finally, the possible mechanism for forming the BL crystals is discussed.
In the α-crystal of iPP, the branching, which results in the formation of spherulite, is induced by a rupture of the sequence of alternating left- and right-handed helices.36 In general, annealing at higher temperatures is more favorable for producing defect-free crystals.37 Accordingly, (i) the selection process of the helix-sense and (ii) annealing at a temperature as high as possible must be essential for obtaining a giant single crystal of iPP.
The requisite (i) will be satisfied by the multiple steps of the crystallization from the mesophase. Because left- and right-handed helices are randomly distributed in the mesophase of iPP,38 translational rearrangements of both-handed helices are necessary to form the defect-free α-crystal. In the course to obtain the BL crystals from the mesophase, iPP experiences many steps that are as follows: first, the mesophase transforms into the crystalline phase within the nodule. Consecutively, the size of the nodule increases by repeating the partial melting and recrystallization. There is a distribution in nodule size,39 and there is also likely a distribution in the rate of defects. Such distributions facilitate the partial melting and recrystallization because the larger and the less defective nodular crystals survive and grow by consuming the smaller and the more defective nodular crystals in the heating and the annealing processes. Such multiple steps, including the partial melting and recrystallization, will provide enough opportunities to select the helix-sense. There should be an optimal heating rate that is favorable for such recrystallization.23
The crystallization from the mesophase also facilitates requisite (ii). It is a matter of course that the nucleation at very high temperatures is a difficult process without the appropriate nucleus. Fortunately, the crystallization from the mesophase provides the nucleus, which has the advantage of having fewer defects, as discussed in the previous paragraph. Such a nucleus with few defects strongly assists the crystallization process in the high temperature region.
These advantages of the crystallization from mesophase will enable the formation of a large single crystal with fewer defects.
Conclusion
Giant single crystals of iPP have been obtained using a specific kinetic pathway through the mesophase. The obtained crystals possess a large size without branching, a high aspect ratio, isolation and a high melting temperature. These characteristics demonstrate the quality of the single crystal. In addition to the quality, the present crystals are obtained using a relatively short annealing period.
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Asakawa, H., Nishida, K., Kanaya, T. et al. Giant single crystal of isotactic polypropylene showing near-equilibrium melting temperature. Polym J 45, 287–292 (2013). https://doi.org/10.1038/pj.2012.136
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DOI: https://doi.org/10.1038/pj.2012.136
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