Tzu-Ching
Chuang
a,
Selvaraj
Nagarajan
a,
Chean-Cheng
Su
b,
Li-Ting
Lee
*c and
Eamor M.
Woo
*a
aDepartment of Chemical Engineering, National Cheng Kung University, No.1, Tainan, 701-01, Taiwan. E-mail: emwoo@mail.ncku.edu.tw; Fax: +886 6 234 4496; Tel: +886 6 275 7575 x 62670
bDepartment of Chemical and Materials Engineering, National University of Kaohsiung, No. 700, Kaohsiung University Rd., Nan-Tzu Dist, Kaohsiung, 811, Taiwan
cDepartment of Materials Science and Engineering, Feng Chia University, Taichung, 407-24, Taiwan. E-mail: ltlee@fcu.edu.tw
First published on 31st January 2024
The grating structure and periodic assembly in D-(−)-poly(3-hydroxybutyrate) (PHB), or simply poly(3-hydroxybutyrate), with diluent-modulated optical regularity are analyzed using microscopy techniques coupled with a unique 3D interior dissection technique. The top-surface valley band is a result of impingement of branching crystals evolving from normal-oriented main lamellar stalks, and the top-surface band is a result of the protruding lamellar stalks. The 3D dissection shows direct experimental proof of discontinuous interfaces between the successive bands, which are created by periodic impingement of neighboring lamellar bundles growing in the normal direction from the substrate. The iridescence phenomenon from the PHB periodic bands can be attributed to the grating-assembly structures with cross-bar pitches tuned to a suitable range by combination of diluents and temperature of growth, whose function resembles those seen in nature's iridescent crystals.
It is worth noting that many polymers or their blends may exhibit quite diverse morphologies upon crystallization, such as typical well-rounded Maltese-cross spherulites, straight-lamellae dendrites, hexagonal-shape,16 feather-like spherulites,17 and seaweed-like spherulites,18 in addition to the widely-known periodic ring-bands. In some special cases, several different patterns co-evolve from a common center to form unique composite-face or Janus-face aggregates.19,20 Thus, the complexity in assembly may defy simple or monotonous descriptive assumptions. Among these diversified patterns of crystal aggregates, periodic ring-banded spherulites seen in many polymers have drawn the most attention; however, the formation mechanisms have remained quite controversial and highly debated among prevailing propositions. Yet, many of these propositions in the past decades have been difficult to solidly and experimentally prove without doubt, due to the small dimensions of constituent lamellae and extreme crowdedness of the aggregates. A recent study has shed new light that a periodic architecture can be composed of lamellae that branch or spawn new crystals periodically and some lamellae change their orientation alternately at periodic intervals, instead of propositions of continuous helix-twist lamellae.21
Newer approaches by interior 3D dissection22–31 and synchrotron microbeam X-ray analysis31,32 have been demonstrated to be useful for better insights of probing the crystal-assembly mechanisms. Earlier studies in the literature indicate that phase-separated domains in lamellae may confine and alter the arrangement of lamellae during aggregation of crystals. Therefore, phase separation with domain-confinement may strongly affect the birefringence types of spherulites, as demonstrated in poly(L-lactic acid) (PLLA).16 Similarly, the PHB crystallization behaviour may change after addition of other amorphous polymers as diluents; that is to say, the morphology of PHB can be manipulated to display the desired crystal assembly patterns. The periodically banded morphology is very typical in PHB or its blends, as well as in many other semicrystalline polymers such as biodegradable poly(p-dioxanone) (PPDO),32 and aliphatic polyesters, polyethylene (PE),16,22,25–31,33–35etc. Further observation of the inter-lamellar crevices in the periodically banded PHB by SEM microscopy techniques30,31 has proved that PHB exhibits periodic bands composed of vertically-oriented lamellae and horizontally-oriented plates underneath the alternating ridge–valley bands. These breakthrough findings of the interior assembly16,22,25–31,33–35 reported very different mechanisms from the conventional propositions4–8 of periodic bands composed of continuous screw-like helix-twist lamellae simultaneously radiating out from a common center and all these lamellae, not only helix-twist, but also undergo synchronizing paces with an identical screw pitch. Such propositions of millions of continuous helix-twist lamellae possessing the same synchronized pitch require impractically stringent conditions (such as million pairs of gene-guided strong H-bonding in DNA-macromolecule screws) that may not be existent in common crystal plates. Crystallization and growth is controlled not just by thermodynamic but more by kinetic driving forces. Thermodynamic stability alone cannot possibly dictate all lamellae to display the same and precisely synchronized helix-twist conformation from nucleation all the way to completion. A typical spherulite can measure up to 30–300 μm in diameter or larger, but a discrete single-crystal lamella usually has a length not exceeding 5 μm or so, which hardly justifies the uninterrupted continuity from the nucleus to the periphery of a spherulite.
Neat poly(3-hydroxybutyrate) (PHB) (without blending with diluents) exhibits rough ring-bands at Tc = 40–100 °C;30,31 the patterns are usually too rough to allow clear analyses on the top-surface or interior lamellar morphology via SEM characterization. A few recent studies30,31 showed that the banding patterns are discretely assembled by two perpendicularly oriented crystal species in cross-hatch intersection, resembling a rib-strut structure with interior lamellae mutually intersecting at an angle ranging from 60 to 90°. Interestingly, such a grating structure in the banded PHB resembles nature's iridescent crystals. This work further probed the detailed morphology and assembly mechanisms by subjecting PHB to modulation with multiple diluent combinations of several suitable amorphous polymers that are known to be thermodynamically miscible with PHB. The objective was to search for the best modulation or regulation of crystal assembly in PHB for convenience of 3D dissection and trustworthy analyses leading to fundamental knowledge to establish an accountable interpretation of the existence of periodicity in crystal assembly.
The polymer solution was cast on glass substrates and dried at 45 °C into thin-film samples with an average thickness = 20–30 μm. The dried film samples were then heated on a hot stage to the maximum melting temperature (Tmax = 220 °C) for two minutes in order to erase prior crystals, and then rapidly removed to another hot stage pre-set at designed isothermal Tc till full crystallization. These crystallized samples were treated by solvent-etching using acetone and p-dioxane as the etching agent for 10 minutes in a sealed container at room temperature in order to wash out the amorphous polymer and imperfect crystals, and hence the etched specimens were considered to be more likely to reveal finer details in crystal assemblies.
X-ray diffraction was performed using a 5 × 7 μm2 microbeam at TPS-25A National Synchrotron Radiation Research Center (NSRRC, Hsin-Chu, Taiwan) with 15.03 keV photon energy. 2D-XRD patterns were recorded with a Dectris Eiger 1 M detector at 0.136 m (13.6 cm) distance and a q range of 0.179–113.41 Å, calibrated with cerium oxide in transition mode.
Fig. 1 POM graphs of PHB/PVAc/PMA blends crystallized at Tc = 100 °C of different ternary compositions: (a) 60/20/20, (b) 70/15/15, (c) 80/10/10, and (d) 90/5/5 [scale bar = 50 μm]. |
To confirm the miscibility in mixtures of PHB with PMA, DSC characterization was performed on several compositions of the ternary blend of PHB/PTA/PVAc. For brevity, DSC traces showing single composition-dependent Tg are demonstrated in Fig. S2 (ESI†). The numerical values of thermal properties of the PHB/PMA/PVAc blend are listed in Table S1 (ESI†). The DSC result shows that all ternary compositions of the polymer mixtures are miscible. Alternatively, a fixed ternary composition of PHB/PVAc/PMA = 80/10/10 was crystallized at various Tc values from 60–120 °C. For brevity, the POM characterization results are placed in Fig. S3 (ESI†), where Fig. S3a–c† show that at lower Tc = 60–80 °C, the ring bands are not quite regular; however, Fig. S3d–h† show that Tc = 90–110 °C leads to periodically banded spherulites with very regular patterns with the inter-band spacing being ca. 15–20 μm. Only at Tc exceeding 110 °C (Tc = 120 °C), the rings start to become corrupted. As a result, this work chose PHB/PVAc/PMA (80/10/10) fully crystallized at Tc = 105 °C as a model for in-depth morphology analysis and micro-beam X-ray analysis.
The topology of surface-relief patterns is usually masked by expelled impurities (molten species, amorphous polymers, etc.). Thus, appropriate etching treatments on specimens might be needed. Fig. 2a shows the SEM graphs for the top surface of the PHB/PVAc/PMA (80/10/10) blend crystallized at Tc = 105 °C. Fig. 2a shows the SEM image of a whole PHB spherulite without solvent etching, where fine textures of the top surface are hidden. Solvent-etching was conducted on crystallized specimens in order to expose the lamellar textures; however, solvent etching might induce cracks (Fig. 2b). Proper control of etching time was manipulated to obtain the best compromise. Fig. 2c shows the solvent-etched morphology of the top-surface banding patterns, where lamellae appear to evolve as a double spiral (spin in the clockwise direction) from a nucleus center. Cracks in the nucleus center are obvious, which are due to the fact that most of the nucleus sheaf-bundles are parallel and normal-oriented with respect to the substrate plane. Therefore, cracks, upon solvent etching, tend to align along the interfaces of sheaf-crystal bundles. A more careful examination can identify that cracks are not only in the nucleus center, but also on the ring bands. Interior dissection in later sections will expound this phenomenon.
Fig. 3 further shows zoomed-in micrographs to identify the detail of the surface-relief patterns of the periodic PHB spherulites crystallized from the ternary blend. Fig. 3a shows the whole PHB spherulite, where the top surface clearly displays periodic packing in repetitive cycles. The valley region is packed with tail-bending with spin pointing in the clockwise direction, which is in line with the double-spiral spin direction (clockwise direction). Apparently, the direction of tail-bending in the valley zone is well correlated with and perhaps determined by the lamellae spin direction. Fig. 3b and c show zoomed-in graphs of the ridge zone and valley zone, respectively. Radial-oriented cracks are present only in the ridge zone; by contrast, cracks are never seen in the valley zone. The valley zone is characterized only with lamellae tail-bending. The reason why cracks are present only in the ridge zone but not in the valley zone will become clear after interior-lamellae dissection analysis to be discussed in later sections.
Fig. 3 SEM graphs for (a) the top surface of the PHB/PVAc/PMA (80/10/10) ternary blend crystallized at Tc = 105 °C; zoomed-in graphs of the (b) ridge zone and (c) valley zone. |
Fig. 5a shows the zoomed-in SEM graph for interior dissection of PHB/PVAc/PMA (80/10/10) crystallized at the same Tc = 105 °C. The tangential-oriented interfaces/cracks (white dashed lines) mark the periodic impingement of the interior lamellae, creating discontinuous interfaces aligned in the normal direction (tangential). Note that there are bundles of normal-oriented lamellae that evolve upward from the substrate; these normal-oriented lamellae initially slant at an oblique angle, and then bend further in the radial direction. These tail-bent lamellae are parallel and point in the radial direction. These radial-oriented lamellar bundles, upon detachment along the stress-prone interfaces between different species of crystal plates, create radial crevices/cracks (marked with yellow lines), which signify the pre-existing interfaces between the radial-oriented lamellae. These radial-oriented lamellae do not grow continuously or un-interruptedly; instead, they evolve from normal-oriented lamellae that are originally located periodically at a distance apart. Thus, when the radial-oriented lamellae grow to a matured length, they impinge with the neighbouring radial-oriented lamellae. As the growth of these lamellae is synchronized, they reach the impingement almost simultaneously at the same length and then impinge at the same time, creating a long tangential-oriented interface. Note again, the impingement pitch of the interior lamellae matches with the top-surface inter-band spacing (ca. 15–20 μm). Black dashed-lines mark the periodic location of impingement between two sets of lamellar bundles that are oriented from the bottom substrate and grow initially in the normal direction with accompanying fractal branches. The pitch of the interior lamellae perfectly matches with the periodic banding rhythm on the top surface. Apparently, the interior morphology of the banded PHB is not assembled as the classical propositions of continuous screw-like helix-twist lamellae pointing out from a common nucleus center.
In continuation, Fig. 5b shows the schematic for fractal-growth lamellae with side branches at oblique angles, till final impingement with interfaces. The mutual impingement of fractal-bundles of lamellae creates boundaries of discontinuities. The discussion focus is placed on revealing that the interior normal-oriented lamellae actually evolve from the substrate–specimen interface, where numerous branches grow sideward at 60–90° angles in two oblique directions. The mutual impingement of these two groups of sideward branches then creates distinct interfaces of discontinuities. Upward white arrows are used to mark the normal-oriented lamellae; downward white arrows mark a ridge zone on the top surface. The impingement of the two neighbouring groups of sideward branches, being nearly horizontal-oriented upon reaching the top surface, naturally appear to be flattened as a valley band.
For 3D dissection, interiors in all space aspects must be covered. After analysis of specimens fractured in the radial direction, circumferential-dissection was attempted. Again, several specimens were tested in trials till finding the best one. Here, the term “circumferential’ means along the circular rim of a certain circular band that happened to be fractured. Interior dissection analysis provides a unique opportunity to examine how lamellae go through a transition from top-surface ridges to valleys. Obviously in previous top-surface SEM micrographs, it was not possible to discern how lamellae self-assemble in zones from ridges to valleys, as all top-surface lamellae are highly jammed and crowded. The dissected interiors, however, provide a much clearer view for such a purpose. Fig. 6 shows the SEM graphs of the fractured surface of PHB/PVAc/PMA (80/10/10) crystallized at Tc = 105 °C, which was fractured in the circumferential direction of circular bands. A specific spot was zoomed-in at a greater magnification on a ridge zone (Fig. 6a1), where the interior lamellae underneath the ridge are all normal-oriented and parallel-bundled, with each bundle showing an individual thickness of ca. 0.5 μm. By comparison, the interior lamellae underneath the valley are all horizontal (radial)-oriented and parallel-bundled (Fig. 6a1), with each bundle showing an individual thickness slightly thinner at ca. 0.2–0.4 μm. Fig. 6b shows a schematic for picturing the circumferential-fractured surface of a PHB ring-banded spherulite at Tc = 105 °C. A zoomed-in image of a valley zone of the banded PHB is to be discussed subsequently in the next figure.
Furthermore, several spots of the interiors were examined for universality. Fig. 7a shows the ow-mag. SEM micrograph of circumferential-fractured interiors of PHB/PVAc/PMA (80/10/10) crystallized at Tc = 105 °C. Fig. 7a1 shows the zoomed-in image for the interior lamellae that are located directly underneath a transition zone from ridges crossing into valleys (images stacked to cover the wider zone). The schematic (inset at upper right) exemplifies the valley zone showing bent lamellae in the circumferential-direction. The lamellae just underneath the valley zone are all radially oriented with an inverted “U”-bend (i.e., convex). Directly adjacent to the radially (horizontally) oriented lamellae are the normal-oriented lamellar bundles (marked with blue arrows). The left-hand-side of the zoomed-in SEM graph in Fig. 7a1 shows that as the initially normal-oriented lamellae (underneath a ridge) approach the valley zone, they bend and twist into an inverted “U”-shape (underneath a valley). The assembly repeats similarly and repetitively on the other right-hand side of the valley to start a new cycle.
For the top surface of banded PHB, further evidence is displayed to prove the existence of discontinuity from band to band created by lamellae's sudden change of direction from the radial direction to a tangential one, rather than the conventional thought of a gradual linear screw-like helix twist in the radial direction. Fig. 8a and b show the SEM micrograph and scheme for periodic bands as viewed on the top surface of banded PHB. The SEM images on the top-surface bands support the interior 3D dissection that the band-to-band transition is discontinuous, with the lamellae being assembled alternately in the radial direction and then a sudden change to the tangential direction. An AFM phase image, adapted and taken from an earlier study,31 is re-used here for further supporting the evidence given in the SEM characterization on the top surface of the ridge–valley transition.
To view the universal mechanisms of crystal assembly leading to periodic bands, we combine the results of the assembled lamellae underneath the ridge and valley zones, respectively. Fig. 9a and b show generalized schemes (fractured along the circumferential direction) revealing the correlation of periodicity on the top surface vs. interiors of PHB crystallized at Tc = 105 °C. The circumferential-fractured interior displays periodic lamellae being self-assembled in alternate normal-to-horizontal orientation changes, just like that observed in the radial-fractured interiors. Consistency in 3D dissection suggests a universal feature of lamellar assembly leading to similar periodic architectures. By contrast, when fractured along the radial direction (instead of the circumferential one), a different view on discontinuity can be exposed. Schematic illustrations for two different common modes of creating an inter-band discontinuity: impingement of inter-bundles vs. sudden twist of same lamellae. Fig. 9c and d show generalized schemes for illustrating two different modes of creating an inter-band discontinuity: (a) inter-bundle impingement (blue dashed lines marking the impingement) and (b) lamellae sudden twist from flat-on to edge-on orientation near the end of a pitch. Emphatically for the assembly shown in graph-b, the lamellae do twist but the twist is not a 360°-angle rotating continuously as a screw-like helix, but rather a 90° twist from edge-on to flat-on, and the growth cycle ends. A new cycle repeats the same way. These two schemes (a and b) both represent two common ways of correlation of the top-surface pattern with interior lamellae assembly, and such a grating cross-hatch is responsible for the periodic optical rings as viewed in POM. The difference of these two modes lies on mainly how the interior lamellae self-assemble periodically to create periodic ridge to valley zones.
Fig. 10 depicts a trend illustrating the modulation of X-ray diffraction intensity across various crystal planes (indicated in the y-axis). This modulation corresponds to the sequential movement from the central point of one ridge to the other ridge. The intensity of crystals is intricately linked to the arrangement patterns of lamellae and unit cells. Oscillations in the crystal-plane intensity signify both parallel and perpendicular orientations concerning the micro-beam axis within the ridge-to-valley distance. The manifestation and cessation of diffraction signals hinge upon the precise alignment of the crystal planes and lamellae in relation to X-ray incidence, whether parallel or perpendicular. In the ridge zone, robust signals are emanated from crystal planes such as (111) and (101), and SAXS for lamellar orientations. Conversely, the valley region exhibits distinctive signals corresponding to the (020), (130), and (040) planes. Furthermore, the signals of the (110) planes manifest in both ridge and valley areas (ESI† Fig. S4). Significantly, the presence of the signal of the (020) crystal plane in the valley region suggests prevalence of flat-on crystals, while the appearance of the signal of the (101) crystal planes on the ridges corresponds to the ac-axis crystal plane, confirming an abundance of edge-on crystals. The two-dimensional plot of SAXS in Fig. 10 underscores the maximal intensity difference of X-ray signals in a radial direction within the ridge-to-ridge distance. Derived from the one-dimensional correlation function in Fig. S5,† the estimated long-period is Lo = 84 Å, with a crystal thickness (Lc) measuring 35 Å and an amorphous thickness (La) of 47 Å for the PHB/PVAc/PMA banded spherulite. Significantly, the 2D SAXS signals reinforce the observed lamellar alignment in the WAXD crystal signals, which collectively are experimentally supported by the SEM interior-dissection morphology discussed earlier.
Fig. 10 Positioning of the PHB spherulite in the POM micrograph with respect to the incident microbeam and 2D X-ray diffraction patterns (SAXS and WAXD) recorded in rings at spot locations #1 to #4. |
For nature's organic living species (plants and animals), their functional iridescence is tuned in million years of evolution to the most suitable nano- or micro-structures. In this work, we demonstrate novel techniques for polymers to display fine-tuned assemblies by using diluents in crystallization as morphology modulation. Orderly-assembled crystals may display interference of white light if the scales of periodic order are near or within the visible-light wavelengths. Neat PHB displays ring bands but does not possess clear order, which however, can be tailor-made by introducing suitable modulating agents.
By comparison with the miscible diluent-modulated PHB (diluted by amorphous PVAc and PMA), iridescence of neat PHB specimens at various Tc values was also tested, and is shown in Fig. 11. Test set-ups for interference with white light are similar to those in previous work.31 Obviously, the neat PHB specimens (with no diluents), upon crystallization at Tc = 65–100 °C, all display corrupted ring bands (highly irregular rings) and lead to non-iridescence, although some weak iridescence is barely visible but not comparable to those in the PHB/PVAc/PMA systems. This proves that PHB, only when properly modulated with diluents and tailor-made, can take orderly microstructures to perform iridescence functions. If crystallized at an even lower Tc such as 30 °C, neat PHB is totally ringless with small sizes of spherulites, which are not expected to display effective light interference.
Fig. 11 Non-iridescence or weak iridescence of neat PHB with irregular bands crystallized at Tc = 65 °C, 80 °C, and 100 °C, respectively (left to right). |
Neat PHB displays irregularly rough ring bands at Tc = 65–100 °C with no clear order, which however, can be tailor-made into orderly patterns by introducing suitable modulating agents. As discussed above, neat PHB crystallized at low Tc displayed barely discernible ring bands and weak iridescence. Yet, introduction of modulating miscible diluents such as PVAc and PMA (both non-crystalline) into PHB crystallized at the same range of Tc = 65–100 °C led to periodic orderly bands. Fig. 12 shows the dramatic effect of morphology modulation on capacity for iridescence properties. At Tc = 65 °C, although the banding pattern of PHB/PVAc/PMA (80/10/10) is slightly better in regularity than that of neat PHB at the same Tc, it is still not perfect (inset POM on the upper left corner), and iridescence is visible but not intense (top row of Fig. 12). By comparison, the periodic morphology becomes totally different to display orderly ring bands leading to effective white-light interference and intense iridescence (bottom row of Fig. 12). At Tc = 100 °C or higher, the banding pattern of PHB/PVAc/PMA (80/10/10) starts to become corrupted and irregular, and the iridescence is still visible but becomes less intense than that of the specimen crystallized at Tc = 75 °C.
Fig. 13 shows the side-by-side comparison of non-iridescence from ringless PHB spherulites of neat PHB versus intense iridescence from orderly bands crystallized from the PHB/PTA (80/20) blend (both crystallized at Tc = 30 °C). Obviously, no orderly grating microstructures are present in ringless PHB spherulites, which expectedly display non-iridescence (Fig. 13a1). By contrast, intense iridescence is seen in orderly ring bands of the PHB/PTA (80/20) blend, which is in agreement with the previous result for the regularly banded PHB crystallized from PHB/PVAc/PMA (80/10/10) at 75 °C and 100 °C.
Thermodynamically, it is an unlikely stringent condition to maintain a synchronized identical helix pitch for millions of lamellae radiating simultaneously outward from a common nucleus, considering that these lamellar crystals, unlike DNA molecules, do not possess gene-guided molecular structures with millions of pairs of base units for H-bonding that are fundamental for holding continuously stable helices along the same molecular axis. It should be emphasized on a crystal key feature. Even though the thousands of lamellae were assumed to be capable of individually helix-twisting; however, they still would not display clear optical bands if these helix-twist plates were not synchronized in a perfect pace with the same pitch. Any miss-matching or offsets of the helix pitches simply would result in extinction of birefringence, as one should always bear in mind that the light does not interact with only a single lamella, but with hundreds of pitch-offset lamellae in stacked bundles across the entire film thickness. Kinetically, on the other hand, it would be more plausible that growth of crystals and their re-orientation or deformation (such as twisting or scrolling) can be modulated to be in a synchronized pace intermittently. Such assembly with periodic modulation of growth leads to a grating structure. Obviously, the PHB ring bands (as viewed in the POM and SEM evidence) are constructed by periodic grating assembly of discrete crystals self-packed as fractal branches along with their parental main stalk lamellae.
Unique 3D morphology interior dissection was conducted to expose the lamellar architectures on surfaces and in the interior. A grating assembly with cross-hatch fractal growth of periodic branches is confirmed, where a “pitch” of a periodic band (as seen in the fractured interiors via SEM evidence) is in perfect match with the optical inter-band spacing. Conventional propositions of continuous helix-twist lamellae for periodic optical bands are re-examined and testified with solid experimental observations.
The unique 3D dissection technique allows direct experimental proof of discontinuous interfaces between the successive bands, which are created by periodic impingement of neighbouring lamellar bundles growing in the normal direction from the substrate. The valley band on topology exhibits a discontinuous interface that is a result of impingement of the crystals of slant-angle-oriented branches originally evolving from the interior normal-oriented main lamellar stalks; by contrast, the ridge band is a result of the protruding normal-oriented lamellar stalks. In the ring-banded PHB spherulites, all “lamellae” (branches or main stalks) are not in helix-twist conformation; instead, they are assembled by discrete single-crystals. For continuous helix-twist propositions to work in accounting for the periodic optical rings, thousands of interior lamellae must helix-twist in a perfectly synchronized pace, and each of the screw-like helical plates' conformation must be firmly held by strong forces of H-bonding. Obviously, both molecular requirements are absent in the crystal plates.
The periodic assembly of discrete crystals self-packed as fractal branches along with their parental main-stalk lamellae, leading to a grating structure, which possesses nano- to micro-architectures effective for interference with white light. By using a chiral biodegradable polyester, PHB modulated with suitable diluents, critical light is shed on understanding the crystal self-assembly leading to hierarchical periodicity that has long intrigued the science community. Such periodic assemblies with nano-gratings can display iridescence.
Footnote |
† Electronic supplementary information (ESI) available. See DOI: https://doi.org/10.1039/d3ce01241g |
This journal is © The Royal Society of Chemistry 2024 |