Figure 2 shows POM and OM graphs for effects of T
max on the relative fractions of Type-1 over Type-2 banded PNT spherulites upon crystallization at T
c = 85 °C by quenching from different T
max. It is noted that the Type-1 and Type-2 morphology remains the same at T
c = 85 °C regardless of changing T
max; only the relative fractions of two types vary with T
max. By comparing the T
c and T
max effects, T
c causes only morphological changes (e.g., double ring-banded spherulites existing in higher T
c regions); however, T
max changes the relative percentages of Type-1 vs. Type-2 spherulites. With the T
max effects on PNT banded types and their formations, the responsible mechanisms inducing the various fractions of dual types of ring-banded spherulites under a specific T
c are the objective of the subsequent investigation. That is, in general, higher T
c and lower T
max (110 °C or lower) are kinetically more favorable for formation of Type-1 bands; oppositely, lower T
c and higher T
max (110 °C or lower) are favorable for the formation of Type-2 bands.
In a prior study [
33] preceding this current work, influence of crystallization temperature (T
c) on morphology and banding patterns in PNT was investigated in detail; however, the T
max effects on the relative fractions of Type-1 vs. Type 2 are yet to be investigated in greater details. A series of different T
max were chosen because T
max might be one of main factors influencing the formation and growth of banded spherulites. The varying trend of Type-1 vs. Type-2 with the temperature at which the specimens were treated at T
max can be clearer if the fractions are plotted as a function of T
max. Consequently, T
max was varied from 110 to 130 °C, with T
c fixed at a constant 85 °C. Results as a line plot and numerical values are as shown in
Figure 3, which reveal that both volume and number percentages of Type-1 increase with increasing T
max. In regard to the fractions of Type-2 spherulites, the trend is just opposite to that of Type-1. The line plots show the variation of the volume and number percentages, respectively, for Type-1 PNT banded spherulites, where (Type-2)% = (100–Type-1)%. The “number%” is counted by the number of spherulites of Type-1 divided by the total number of Type-1 + Type-2, by disregarding the various sizes of individual spherulites. Volume% was estimated by taking into account the actual variations of individual sizes of these two bands. The number percentage of the Type-1 band is always greater than the volume percentage of the same band, as the average size of Type-2 is significantly greater than that of Type-1 (as clearly shown earlier in
Figure 2). On the basis of the quantitative results, aided with literature research by Weber, et al. [
34], we speculate that the molecular level
π-stacking interaction might influence the nucleation process of this Type-2 spherulite. At low T
max, higher amount of ‘
π-π’ interaction may be involved in the nucleation process of Type-2 spherulites. At the same time, a higher T
max may eliminate ‘
π-
π’ interaction in the melt stage, so that the Type-2 spherulite’s volume and number percentages might decrease.
In-Situ Growth Monitoring
Co-existence of two nuclei geometry shapes at initiation of crystallization held at T
c = 85 °C is thus quite apparent, showing two types of nuclei (t = 2 h at T
c = 85 °C): (1) highly elongated sheaves, and (2) well-rounded nuclei.
Figure 6 shows in-situ POM with CCD monitoring on the initiation stages of morphology evolution of Type-1 and Type-2 spherulites, both being crystallized at T
c = 85 °C, from t
i (2 h) to t
i + 120 min (ca. t
i + 2 h). The nuclei for Type-2 and Type-1 banded PNT spherulites are tiny and discrete, but of distinctly different geometric shapes. They are marginally distinguishable in their unique optical birefringence characteristics. The nuclei for Type-2 are initially well-rounded, appearing as a tiny dot-like aggregate. By contrast, the nuclei for Type-1 are highly asymmetrically elongated-rod-like, appearing as a stick-like sheaf with a single birefringence color (orange color), which means that the crystal sheaf-bundle is initially in only one orientation. When fully grown, the highly asymmetric nucleus center for the Type-1 band eventually leads to an asymmetrically packed banded spherulite, as proved in an earlier study.
It should be noted, though, that the “incubation time” (time for nuclei to first appear), defined as the time for the first appearance of traceable nuclei after equilibrilating at T
c, for different types of banded PNT spherulties varies dramatically, which means that the initial nuclei for different banded spherulites may appear at different times after being quenched from the molten state at T
max to T
c for crystallization. The lamellar assemblies of PNT being packed into different birefrigent patterns of Type-1 and Type-2a,b banded spherulites will be discussed in details later.
Figure 7 shows that by quenching the PNT melt from T
max = 120 °C to crystallization at T
c = 85 °C, the nuclei (well-rounded shape) for Type-2 (double-ring banded including Type 2a and Type 2b) spherulites appear almost immediately upon equilibrating at T
c = 85 °C; by contrast, it takes about 45 min after equilibrating at T
c before first traces of nuclei (elongated sheaf-like lamellae) for Type 1 banded spherulites appear. One can easily see from the in-situ POM results in
Figure 7a–k that although the sheaf-like nuclei (For Type-1 banded spherulites) appear later than those well-rounded ones for Type-2, the nuclei density of the elongated sheaf-like nuclei, once formed, are more densely populated than the well-rounded nuclei whose number density stays almost unchanged with time. This fact leads to eventually higher volume/number fractions of Type-1 over Type-2 banded spherulites when crystallization is completed at any given T
c. Apparently, higher T
c is favorable for greater fractions of Type-2 (over Type-1), but higher T
max tends to decrease it as higher T
max supposedly suppresses more Type-2 nuclei. Moreover, all these factors (T
max and T
c) possibly govern the relative fractions of different types of banded PNT spherulites at the nucleation stage, but not during the spherulites’ growth period as the growth rates are almost the same for different types of banded spherulites.
Figure 7l shows that that fully grown Type-1 crystals are smaller than the Type-2 ones, and both types mutually impinge on each other. The POM images clearly indicate that two different types of ring bands evolve and grow independently from two geometrically different nuclei, where Type-1 ring-banded PNT spherulites (marked with red arrow) grow from elongated rods nuclei and Type-2 mirror-paired ring-banded spherulites (marked with green arrow) grow from initially well-rounded dot-like nuclei.
Note that at Tc = 85 °C, it took quite long times for the first traces of nuclei to appear: for the rod-like nuclei, ti = 2 h; for the well-rounded nuclei, ti = 4 h. That is, not only thegeometry shapes differ significantly, but also the times of “incubating” the first traces of nuclei are also different dramatically (t = 2 h vs. 4 h for Type-1 and Type-2 respectively). Apparently, the types (either Type-1 or -2) of ring bands in PNT spherulites are mostly determined by the initial geometry of the nuclei at the nucleation stage, and patterns of ring bands were fixed and did not change further upon crystallization and growth, leading to the final Type-1 vs. Type-2 ring bands. These two different geometries of nuclei both grow eventually to ring-banded PNT spherulites, which differ significantly in their optical birefringence pattern and lamellar assembly.
Depending on the sites of nucleation (near top surface or bottom substrate), crystallized PNT may take a different geometry of banded structures.
Figure 8 shows that the nuclei of Type-1 PNT banded spherulites (T
c = 85 °C), at the very center of the periodic bands, take an asymmetric sheaf-like geometry. The lamellae grow along the sheaf direction and spray out like a fan; and upon growing outward, they periodically wave up and down. By contrast, along the perpendicular direction normal to the bundled sheaf, the lamellae are packed as layered plates pointing vertically to the paper, which upon fracture, display some ductile textures. Thus, the lamellae are self-assembled in an asymmetric pattern with respect to the nucleus center. Along the sheaf-crystal direction, the lamellae are mostly flat-on on the paper, other than waving up and down. The lamellae in the perpendicular direction to the nucleus sheaf point to a normal direction to the paper. Owing to the highly elongated nucleus geometry and subsequent directional growth, the interior lamellae in fully grown Type-1 banded spherulites are not circularly symmetric, but highly asymmetric to display two-face dissymmetry in its interior lamellae assembly as revealed in an earlier study [
33]. Obviously, the structured and oriented growth from sheaf-like nuclei lead to a highly asymmetric morphology in poly(nonamethylene terephthalate) (PNT) upon packing into periodic bands [
24].
As described in detail in the scheme (
Figure 8b), the two tail-ends of rod-like nucleus-sheaves first evolve needle-like fine lamellae that bend into curvature as they grow outward from the ends. Eventually, the bent lamellae grow in a spiral-spin pattern into ridges (aligned circumferentially), then from which daughter branches further grow in the perpendicular direction (i.e., aligned radially) to fill the inter-ridge space. Cycles repeat in the same manner until drainage or impingement.
Figure 9 shows in-situ POM-CCD monitoring on the intermediate stages of the morphology evolution of Type-1 and Type-2 spherulites crystallized at T
c = 85 °C, from t
i + 135 min (ca. 2 h) to t
i + 255 min (ca. 4 h). Type-2 and Type-1 banded PNT spherulites are discrete and distinguishable in their unique optical birefringence characteristics. They are ca. 60–80 μm in diameter, and both become oval-shape (Type-1) or well-rounded (Type-2). At the intermediate stage, the initially asymmetric stick-like nuclei of Type-1 now grow into oval-shape spherulites with visible optical bands. The initially well-rounded dot-like nuclei for Type-2 still retain a ball-like shape but grow into bigger round-shape spherulites with similar visible optical bands as those in Type-1.
Figure 10 shows in-situ POM monitoring on the later or final stages of morphology evolution of Type-1 and Type-2 spherulites crystallized at T
c = 85 °C from t
i + 675 min (ca. 11 h) to t
i + 795 min (ca. 13 h). Type-2 banded PNT spherulites are now fully grown but severely impinged with the neighboring Type-1 banded spherulites. Population of Type-1 banded aggregates dramatically out-numbers that of Type-2 ones.
Figure 11 shows AFM height images and height profiles for Type-1 (left column of images) in comparison with Type-2 (right column of images) PNT spherulites fully crystallized at T
c = (a) 75, (b) 80 and (c) 85 °C by quenching from T
max = 120 °C. The nuclei centers of both types of PNT ring bands are located at the lowest regions of the entire banded spherulites of either Type-1 or Type-2. As the spherulites grow away from the nucleus, periodic bands develop, with corresponding heights up and down at ridge and valley, respectively. The height drops from the ridge to valley are greater for Type-2 bands than for the Type-1 bands. In addition, the inter-band spacing for a Type-2 band is 2–3 times larger than that for a Type-1 band. That is, the surface characteristics of the Type-1 PNT band differ dramatically from those of Type-2.
For universal comparison, additional PNT specimens crystallized at T
c = 80 °C were similarly analyzed using AFM using procedures reported in a previous work [
16].
Figure 12 shows (a) POM graph and (b) AFM height images for Type-1 and Type-2 PNT spherulites fully crystallized at T
c = 80 °C until completion, after quenching from T
max = 120 °C.
Figure 12c,d shows the AFM height profiles for Type-1 and Type-2, respectively. The main characteristics for PNT specimens crystallized at T
c = 80 °C are similar to those crystallized at either lower T
c = 75 °C or higher T
c = 85 °C. The nuclei center is consistently the lowest region of the entire banded spherulites, either of Type-1 or Type-2. Away from the nucleus center, the AFM height profiles (
Figure 12c) for Type-1 and Type-2 both show periodic heights waving up and down. The height drops from the ridge to valley are greater for the Type-2 bands than for the Type-1 bands. In addition, both POM and AFM results indicate that the inter-band spacing for a Type-2 band is visibly much larger than that for a Type-1 band. All these features clearly indicate that these are two different types of PNT bands.
The correlation of the top surface with the fractured surface of Type-1 spherulite with the nuclei center near the interface (polymer/air) was analyzed in detail in an earlier work [
33]. Crystallized Type-1 PNT spherulites were dissected by fracturing the specimens with different nucleus positions relative to the bottom substrate or top surface to see whether or not there may be any discrepancy in its interior lamellar arrangement.
Figure 13a–c shows SEM graphs of the top surface and interiors of Type-1 banded spherulites with nuclei near the top surface (i.e., interface of polymer/air), which reveal that the crossbar pitch of the interior grating structure tends to be same or similar to the inter-band spacing on the top surface. In addition, the ridge on the top surface can be correlated directly to the protruded ductile fracturing zones while the valley on the top surface is correlated to the convex brittle detaching zones. The periodic ductile fracturing zones suggest that the lamellae in those zones are oriented “along” the fracturing direction, while brittle detaching, next to the ductile pull-out, indicates that the lamellae in the brittle zones are oriented perpendicularly to the fracturing direction. The alternate ductile-brittle failures in the interior lamellae give a hint that the interior lamellae are aligned in an alternate tangential/radial direction, forming a grating architecture in the interiors that are correlated with the periodic up-and-down topology of the ridge and valley bands on the top surface. The crossbar pitch of the interior periodic gratings is ca. 7 μm (as revealed in SEM), which is the same as the inter-band spacing of 7 μm on the top surface as revealed in POM results, whose main characteristics of periodicity are shown in the schematic of
Figure 13d.
Two kinds of discontinuities in lamellar arrangement are present in the interior lamellae assembly of Type-1. The lamellae of Type-1 spherulites demonstrate the different arrangements upon being observed from different dissection angles; in addition, the nuclei positions either near the top surface or more inside the spherulite influence the final arrangement and complexity of the interior lamellae. With regard to Type-2 spherulites of PNT, strong correlation between the topography and interior lamellar assembly is observed; that is to say, both the lamellar arrangement on the top surface and inside the bulk display similarly lamellar-tilted characteristics. More interestingly, the interior lamellae of Type-2 spherulites clearly demonstrate the periodically tail-bending and twisting nature when the sample thickness is increased to a certain level; however, with film thickness decreases to sub-microns and nano-meters, such bending and twisting nature is no longer present, eventually leading to non-periodic or ring-less assemblies.
Earlier investigation [
35] has revealed the detail morphologies of Type-2 PNT aggregates, which have two morphologies, and are sub-divided into two categories. Once again, their respective nucleus morphologies are assessed.
Figure 14a,b shows schematics of evolution from the nucleation stage to fully grown spherulties of Type-2a vs. Type-2b PNT ring bands. As discussed earlier, Type-2 ring bands further differ in geometric shapes and can be sub-divided into two categories (Type-2a and -2b). Further analyses will expound in more detail on lamellar architectures of the “mirror-pair ring (Type-2a)” and “Fermat’s spiral ring-banded (Type-2b)” PNT spherulites. The corresponding schematics for Type-2a and 2b are drawn in the right diagram of the figure to differentiate the specific differences in the morphologies of these two types of banded PNT spherulites. Type-2a and Type-2b banded PNT spherulites both originate from nuclei of a well-rounded shape, but they are different in the birefrigent patterns, which lead to variation of subsequent lamellar growth orientations. For the mirror-paired ring-banded PNT spherulites (Type-2a), as shown in
Figure 14a, the polymer crystals start to grow concentrically from the nucleus regions with symmetrical arrangements (mirro-image). The Fermat-spiral ring-banded PNT spherulites (Type-2b) are shown in the right-hand-side scheme of
Figure 14b, where the spiral-shape nuclei are initially formed first, to be followed by two crystal arms growing out from the tips of the spiral nuclei, then further grow to fully fill the entire space of the spherulite. It is noteworthy to mention that Type-2a is more abundant but Type-2b spherulites occur only sporadically; sometimes there is no or only a trace amount of Type-2b spiral-banded spherulites in a fully-crystallized PNT sample at T
c = 85 °C. Such morphologically sporadic occurrence of the spiral-spin band patterns was discovered as documented in the literature in PE [
36], PCL [
20], PDT [
37] and PTT [
38]. However, interpretation of supercooling effects on the formation of Type-2b PNT spherulites is not certain and still needs to be confirmed in future work. From the clear microscopic evidence on interior anatomy as shown, the growth in either types of banded PNT spherulties definitely cannot be described as a lamellar plate undergoing synchronized helix-twist from the nuclei center to periphery of spherulites, as claimed by overly simplified classical models of continuous helix-twisting lamellae [
35]. Note here that interior 3D-dissected morphology for PNT Type-2 banded spheruites (which are further classified into two sub-classes: Type-2a and Type-2b) were analyzed in detail in a previously published paper [
35]; thus, we do not elaborate on the issue here.
Spiral-spin growth from a nucleus center appears to be quite universal in polymer spherulites with periodic ring bands. It is worthy to mention that poly(ʟ-lactic acid) (PLLA) also displays similar spiral-spins from its nucleation center, forming multiple types of assemblies with periodic aggregates [
39]. Based on the dissected microscopic evidence on the Type-1 ring-banded PLLA spherulites, the growth starts with sheaf-like nuclei, which from two ends would twist and bend, then continue into a full-length double-spiral (or mathematically a “Fermat’s spiral”). The result is formation of a concave U-shape valley between two successive lamellae spirals, where the branching lamellae constitute the parallel lamellae underneath the “valley band”, leading to a periodic grating architecture. Such grating structure in the ringed PLLA spherulite is quite similar to that in ring-banded poly(ethylene adipate) (PEA) spherulites crystallized at T
c = 28 °C, as earlier reported in the literature [
1], and these periodically-grating PEA ring bands can display the nature of common bio-photonic crystals [
40].
Obviously, from the in-situ monitoring from nucleation to final impingement for Type-1 and Type-2 banded PNT spherulties, the growth processes are composed of two stages. At the early age, sheaf-like nuclei, accompanied with a slanted 45°-angle, initiate at nearly two hours after quenching from Tmax to Tc; then, polymer branches start to grow asymetrically from the two ends of nuclei-sheaves. Growth from the nuclei takes place by lengthening radially and branches evolve into fan-like sprays, which first widen and extend in the radial direction (i.e., ridge region on the top surface), then the tail-ends of the branches suddenly taper to bend down and precipitate to form a valley region. Subsequently, a new cycle starts and repeats in a similar manner until there is complete drainage of all molten species. In each cycle, the valley crystals are followed by a second-cycle growth, which continues periodically to form repetitive ring-banded PNT spherulites, whose crystal-aggregated patterns tend to be guided by the initial nucleus geometries, which in turn are influenced by kinetics parameters such as Tc and Tmax.