Control of Polymorphs on the Crystallization of Glycine Using a WWDJ Batch Crystallizer

The control of crystal polymorphs was investigated using a WWDJ batch crystallizer and glycine as a model compound. The WWDJ batch crystallizer is a newly developed crystallizer, which is equipped with a slurry sprinkler named Wall Wetter fixed on the shaft of an impeller and a double‐deck jacket. When a conventional crystallizer was used, the unstable α‐form crystals were always obtained. However, when the WWDJ batch crystallizer was used, the stable γ‐form crystals were obtained. The appearance of different polymorphs depends on the cooling rate during the crystallization. The γ‐form crystals were obtained by slow cooling, while the α‐form was obtained by rapid cooling. It means that the solvent‐mediated transformation of glycine crystal polymorphs can be controlled by changing the cooling rate in the WWDJ crystallizer. These results were obtained due to the fact that the WWDJ batch crystallizer accelerates the dissolution of metastable crystals and the growth of stable crystals.     

Freezing of tissue-limits for the autoradiographic localization of diffusible substances

Frozen thin sections and sections from freeze-dried and embedded tissue are used for the autoradiographic localization of diffusible substances at the electron microscope level. The presence of ice crystals in such sections may limit the autoradiographic resolution. Ice crystals are formed during freezing and may grow during subsequent processing of tissue. The contribution of ice crystal growth to the final image was estimated by measuring the distribution of the ice crystal sizes in freeze-etch replicas and in sections from freeze-dried and embedded tissues. A surface layer (10-15 mu) without visible ice crystals was present in both preparations. Beneath this surface layer the diameter of ice crystals increased towards the interior with the same relationship between crystal size and distance from the surface in the freeze-etch preparation as in the freeze-dry preparation. Ice crystal growth occurring during a much longer time during freeze-drying compared to freeze-etching does not significantly contribute to the final image in the electron microscope. The formation of ice crystals during freezing determines to a large extent the image (and therefore the autoradiographic resolution) of freeze-dry preparations and this probably holds also for thin cryosections of which examples are given.     

Ice crystals formed in tissue during cryosurgery. II. Electron microscopy

Tissues frozen by means of a cryosurgical probe have been examined by electron microscopy following techniques designed to preserve the ice crystal spaces.Ice crystals appeared similar whether tissues were quenched or not following cryosurgery and the various techniques of dehydration resulted in similar ice crystal architecture.Ice crystal spaces in the area deep to the freezing probe were intracellular both in epithelium and muscle although in the muscle zone some fibers contained large and others small crystal spaces. It is suggested that this might be due to variations in the local blood supply.At the periphery of the frozen area ice crystals were usually extracellular producing gross distortion of the cells which, however, retained intracellular structural integrity. These results are consistent with the belief of many workers that intracellular ice is lethal while extracellular ice is not, but no evidence of penetration of cell membrane by ice crystals was seen.     

Enhancement of insect antifreeze protein activity by antibodies

Antifreeze proteins, produced by many cold water marine teleost fish and terrestrial arthropods (insects, spiders, etc.), inhibit ice crystal growth by a non-colligative mechanism, probably by adsorbing onto the surface of potential seed ice crystals and thereby blocking growth at preferred growth sites. In this study it is demonstrated that the activity of two insect antifreeze proteins is greatly increased by the addition of specific rabbit polyclonal antibodies to the antifreezes. A model is presented which suggests that the enhancement occurs because the antifreeze-antibody complex, being much larger than the antifreeze protein alone (a minimal 7-8-fold increase in size), blocks a larger area of the ice crystal surface and extends further above the surface, thus requiring the temperature to be further lowered before crystal growth proceeds. This idea is further supported by the finding that addition of goat anti-rabbit IgG to the antifreeze protein + anti-antifreeze protein antibody complexes further enhanced activity.     

A model for binding of an antifreeze polypeptide to ice.

A model is proposed, based on recent peptide analog and ice crystal etching studies, whereby an alanine-rich, alpha-helical antifreeze polypeptide (AFP) from the winter flounder inhibits the growth of ice crystals by hydrogen bonding of Thr, Asn, and Asp side chains in a specific pattern to the [2021] hexagonal bipyramidal planes of ice. It is further suggested that this mode of binding is unidirectional, maximizing opportunities for packing of AFPs on the ice surface, and that ice crystal growth inhibition occurs by a two-step mechanism involving hydrogen bonding and hydrophobic interpeptide interactions.     

Cholesterol crystal formation and growth in model bile solutions

Cholesterol monohydrate crystal formation was studied in supersaturated model bile solutions, containing unlabeled cholesterol, sodium cholate and soybean phosphatidylcholine, and tracer amounts of [3H]cholesterol. Solutions were either seeded with cholesterol crystals to initiate growth, or not seeded to allow self-nucleation and subsequent crystal growth to occur. Crystal growth at 37 degrees C was measured by two methods. First, radioactive cholesterol crystals were isolated by filtration, and the mass of cholesterol that had precipitated was calculated. In unseeded solutions, there was a long lag period before crystal growth was detected. This lag time was decreased by increases in the cholesterol concentration, temperature, and lipid concentration. In seeded solutions, crystal growth also was dependent on the cholesterol concentration, temperature, and lipid concentration. The second method used to measure crystal growth involved the Coulter Counter. At 37 degrees C, reproducible results were not obtained using unseeded solutions due to blocking of the counter aperture with large crystals. In seeded solutions, crystal growth could be measured as an increase in total particle volume. However, comparison of growth rate estimates from the Coulter Counter with those obtained radiochemically revealed poor agreement between the two methods. It is probable that the Coulter Counter is inaccurate in measuring the volume of cholesterol monohydrate crystals due to their anisometric shape.     

Effect of type III antifreeze protein dilution and mutation on the growth inhibition of ice.

Mutation of residues at the ice-binding site of type III antifreeze protein (AFP) not only reduced antifreeze activity as indicated by the failure to halt ice crystal growth, but also altered ice crystal morphology to produce elongated hexagonal bipyramids. In general, the c axis to a axis ratio of the ice crystal increased from approximately 2 to over 10 with the severity of the mutation. It also increased during ice crystal growth upon serial dilution of the wild-type AFP. This is in marked contrast to the behavior of the alpha-helical type I AFPs, where neither dilution nor mutation of ice-binding residues increases the c:a axial ratio of the ice crystal above the standard 3.3. We suggest that the ice crystal morphology produced by type III AFP and its mutants can be accounted for by the protein binding to the prism faces of ice and operating by step growth inhibition. In this model a decrease in the affinity of the AFP for ice leads to filling in of individual steps at the prism surfaces, causing the ice crystals to grow with a longer c:a axial ratio.     

Direct visualization of spruce budworm antifreeze protein interacting with ice crystals: basal plane affinity confers hyperactivity

Antifreeze proteins (AFPs) protect certain organisms from freezing by adhering to ice crystals, thereby preventing their growth. All AFPs depress the nonequilibrium freezing temperature below the melting point; however AFPs from overwintering insects, such as the spruce budworm (sbw) are 10-100 times more effective than most fish AFPs. It has been proposed that the exceptional activity of these AFPs depends on their ability to prevent ice growth at the basal plane. To test the hypothesis that the hyperactivity of sbwAFP results from direct affinity to the basal plane, we fluorescently tagged sbwAFP and visualized it on the surface of ice crystals using fluorescence microscopy. SbwAFP accumulated at the six prism plane corners and the two basal planes of hexagonal ice crystals. In contrast, fluorescently tagged fish type III AFP did not adhere to the basal planes of a single-crystal ice hemisphere. When ice crystals were grown in the presence of a mixture of type III AFP and sbwAFP, a hybrid crystal shape was produced with sbwAFP bound to the basal planes of truncated bipyramidal crystals. These observations are consistent with the blockage of c-axial growth of ice as a result of direct interaction of sbwAFP with the basal planes.     

第一类鱼抗冻蛋白对冰晶生长界面层结构的影响

根据冰晶在水溶液中生长的基本热力学性质,应用多层界面模型,分别得到了冰晶在纯水及抗冻蛋白溶液中生长界面层的吉布斯自由能.由冰晶生长界面层的吉布斯自由能,分析了冰晶在三种不同第一类鱼抗冻蛋白分子溶液中,热平衡状态下生长界面层的微观平衡结构,发现冰晶在抗冻蛋白溶液中生长与其在纯水中生长相比,界面层结构有明显变化,结合抗冻蛋...     

抗冻糖蛋白溶液中冰晶生长速率的研究

在分析了溶液中抗冻糖蛋白与冰晶表面的相互作用的基础上,提出了在抗冻糖蛋白溶液中冰晶沿c轴方向生长的理论。给出了冰晶在抗冻糖蛋白溶液中生长速率的定量计算,而且理论值与实验结果有较好的符合,解释了冰晶在抗冻糖蛋白溶液中生长速度和生长习性的各向异性。     

Recrystallization of Ice Crystals in Trehalose Solution at Isothermal Condition

An isothermal ice recrystallization behavior in trehalose solution was investigated. The isothermal recrystallization rate constants of ice crystals in trehalose solution were obtained at ?5 °C, ?7 °C, and ?10 °C. Then the results were compared to those of a sucrose solution used as a control sample. Simultaneous estimation of water mobility in the freeze-concentrated matrix was conducted by ¹H spin–spin relaxation time T₂ to investigate mechanisms causing the different ice crystal recrystallization behaviors of sucrose and trehalose. At lower temperatures, lower recrystallization rates were obtained for both trehalose and sucrose solutions. The ice crystallization rate constants in trahalose solution tended to be smaller than those in sucrose solution at the same temperature. Although different ice contents (less than 3.6%) were observed between trehalose and sucrose solutions at the same temperature, the recrystallization behaviors of ice crystals were not markedly different. The ¹H spin–spin relaxation time T₂ of water components in a freeze-concentrated matrix for trehalose solution was shorter than in a sucrose solution at the same temperature. Results show that the water mobility of trehalose solutions in freeze-concentrated matrix was less than that of sucrose solutions, which was suggested as the reason for retarded ice crystal growth in a trehalose solution. Results of this study suggest that the replacement of sucrose with trehalose will not negatively affect deterioration caused by ice crystal recrystallization in frozen foods and cryobiological materials.     

The formation and distribution of ice within dormant and deacclimated peach flower buds

Abstract A freeze-fixation technique was used to examine the distribution of ice crystals and the pattern of freezing in peach flower buds. In dormant buds, ice crystals formed at localized sites within the bud axis and scales. Ice crystal formation disrupted tissues and mechanical injury from repetitive freezethaw cycles was apparent. There was evidence of ice formation in the floral organs of dormant buds exposed to ?25°C but none observed in buds exposed to either ?5 or ?10°C. The distribution of ice crystals was different in deacclimated buds. In addition to large ice crystals within the subtending bud axis and scales, evidence of large crystals within the developing floral organs was noted. These crystals were most prominent in the lower portions of the developing flower and peduncle, and caused a separation of the epidermal layer from adjacent cells. The distribution of ice crystals within both dormant and deacclimated peach flower buds corroborated the results of previous thermal analysis experiments.     

Ice Morphology: Fundamentals and Technological Applications in Foods

Freezing is the process of ice crystallization from supercooled water. Ice crystal morphology plays an important role in the textural and physical properties of frozen and frozen-thawed foods and in processes such as freeze drying, freeze concentration, and freeze texturization. Size and location of ice crystals are key in the quality of thawed tissue products. In ice cream, smaller ice crystals are preferred because large crystals results in an icy texture. In freeze drying, ice morphology influences the rate of sublimation and several morphological characteristics of the freeze-dried matrix as well as the biological activity of components (e.g., in pharmaceuticals). In freeze concentration, ice morphology influences the efficiency of separation of ice crystals from the concentrated solution. The cooling rate has been the most common variable controlling ice morphology in frozen and partly frozen systems. However, several new approaches show promise in controlling nucleation (consequently, ice morphology), among them are the use of ice nucleation agents, antifreeze proteins, ultrasound, and high pressure. This paper summarizes the fundamentals of freezing, methods of observation and measurement of ice morphology, and the role of ice morphology in technological applications.     

Effect of annealing time of an ice crystal on the activity of type III antifreeze protein

Antifreeze proteins (AFPs) possess a unique ability to bind to a seed ice crystal to inhibit its growth. The strength of this binding has been evaluated by thermal hysteresis (TH). In this study, we examined the dependence of TH on experimental parameters, including cooling rate, annealing time, annealing temperature and the size of the seed ice crystal for an isoform of type III AFP from notched-fin eelpout (nfeAFP8). TH of nfeAFP8 dramatically decreased when using a fast cooling rate (0.20 degrees C x min(-1)). It also decreased with increasing seed crystal size under a slow cooling rate (0.01 degrees C x min(-1)), but such dependence was not detected under the fast cooling rate. TH was enhanced 1.4- and 2.5-fold when ice crystals were annealed for 3 h at 0.05 and 0.25 degrees C below T(m), respectively. After annealing for 2 h at 0.25 degrees C below T(m), TH activity showed marked dependence on the size of ice crystals. These results suggest that annealing of an ice crystal for 2-3 h significantly increased the TH value of type III AFP. Based on a proposed adsorption-inhibition model, we assume that type III AFP undergoes additional ice binding to the convex ice front over a 2-3 h time scale, which results in the TH dependence on the annealing time.     

Understanding the mechanism of ice binding by type III antifreeze proteins

Type III antifreeze proteins (AFPs) are present in the body fluids of some polar fishes where they inhibit ice growth at subzero temperatures. Previous studies of the structure of type III AFP by NMR and X-ray identified a remarkably flat surface on the protein containing amino acids that were demonstrated to be important for interaction with ice by mutational studies. It was proposed that this protein surface binds onto the (1 0 [\bar 1] 0) plane of ice with the key amino acids interacting directly with the water molecules in the ice crystal. Here, we show that the mechanism of type III AFP interaction with ice crystals is more complex than that proposed previously. We report a high-resolution X-ray structure of type III AFP refined at 1.15 A resolution with individual anisotropic temperature factors. We report the results of ice-etching experiments that show a broad surface coverage, suggesting that type III AFP binds to a set of planes that are parallel with or inclined at a small angle to the crystallographic c-axis of the ice crystal. Our modelling studies, performed with the refined structure, confirm that type III AFP can make energetically favourable interactions with several ice surfaces.     

Experimental study of intracellular ice growth in human umbilical vein endothelial cells

Study of the intracellular ice formation (IIF) and growth is essential to the mechanistic understanding of cellular damage through freezing. In the aid of high speed and high resolution cryo-imaging technology, the transient intracellular ice formation and growth processes of the attached human umbilical vein endothelial cells (HUVEC) were successfully captured during freezing. It was found that the intracellular ice nucleation site was on the cell membrane closer to the nucleus. The ice growth was directional and toward the nucleus, which covered the whole nucleus before growing into the cytoplasm. The crystal growth rate in the nucleus was much larger than that in the cytoplasm, and its morphology was influenced by the cooling rate. During the thawing process, small crystals fused into larger ones inside the nucleus. Moreover, the cumulative fraction of the HUVEC with IIF was mainly dependent on the cooling rate not the confluence of the cells attached.     

Relationships between ice crystal size, water content and proton NMR relaxation times in cells

Biological specimens were frozen under controlled conditions. We questioned how the size of ice crystals, as measured in cryosectioned and cryoadsorbed sections of these biological specimens, relates to the water content and to the proton NMR relaxation times (T1 and T2) of the unfrozen specimens. The results permit the following conclusions: After rapid freezing in liquid propane cooled in a liquid nitrogen bath, the average size of ice crystals at distances of 150 microns or more from the surface of a particular tissue was always the same. Thus, the average size of the ice crystals was found to be characteristic of the type of biological tissue studied. Linear regression analysis showed average ice crystal size to have a significant correlation coefficient to T1 relaxation time and to water content. Specifically ice crystal size increased with T1 relaxation time and with water content. Multiple regression and path analysis demonstrated a positive correlation between the T1 relaxation time and the ice crystal size variation. Path analysis showed that both water content and T2 relaxation time were less directly correlated with ice crystal size. The findings from the path analysis and other observations show that the average size of ice crystals in subcellular compartments is best predicted by the proton T1 relaxation time. A working model is put forth to explain differences in ice crystal size observed between specimens enriched in globular or in parallel filamentous proteins.     

Inhibition of Ice Growth and Recrystallization by Zirconium Acetate and Zirconium Acetate Hydroxide

The control over ice crystal growth, melting, and shaping is important in a variety of fields, including cell and food preservation and ice templating for the production of composite materials. Control over ice growth remains a challenge in industry, and the demand for new cryoprotectants is high. Naturally occurring cryoprotectants, such as antifreeze proteins (AFPs), present one solution for modulating ice crystal growth; however, the production of AFPs is expensive and inefficient. These obstacles can be overcome by identifying synthetic substitutes with similar AFP properties. Zirconium acetate (ZRA) was recently found to induce the formation of hexagonal cavities in materials prepared by ice templating. Here, we continue this line of study and examine the effects of ZRA and a related compound, zirconium acetate hydroxide (ZRAH), on ice growth, shaping, and recrystallization. We found that the growth rate of ice crystals was significantly reduced in the presence of ZRA and ZRAH, and that solutions containing these compounds display a small degree of thermal hysteresis, depending on the solution pH. The compounds were found to inhibit recrystallization in a manner similar to that observed in the presence of AFPs. The favorable properties of ZRA and ZRAH suggest tremendous potential utility in industrial applications.     

Repair of impurity-poisoned protein crystal surfaces

The surface morphology of Bence-Jones protein (BJP) crystals was investigated during growth and dissolution by using in situ atomic force microscopy (AFM). It was shown that over a wide supersaturation range, impurities adsorb on the crystalline surface and ultimately form an impurity adsorption layer that prevents further growth of the crystal. At low undersaturations, this impurity adsorption layer prevents dissolution. At greater undersaturation, dissolution takes place around large particles incorporated into the crystal, leading to etch pits with impurity-free bottoms. On restoration of supersaturation conditions, two-dimensional nucleation takes place on the impurity-free bottoms of these etch pits. After new growth layers fill in the etch pits, they cover the impurity-poisoned top layer of the crystal face. This leads to the resumption of its growth. Formation of an impurity-adsorption layer can explain the termination of growth of macromolecular crystals that has been widely noted. Growth-dissolution-growth cycles could be used to produce larger crystals that otherwise would have stopped growing because of impurity poisoning.     

Adsorption of alpha-helical antifreeze peptides on specific ice crystal surface planes.

The noncolligative peptide and glycopeptide antifreezes found in some cold-water fish act by binding to the ice surface and preventing crystal growth, not by altering the equilibrium freezing point of the water. A simple crystal growth and etching technique allows determination of the crystallographic planes where the binding occurs. In the case of elongated molecules, such as the alpha-helical peptides in this report, it also allows a deduction of the molecular alignment on the ice surface. The structurally similar antifreeze peptides from winter flounder (Pseudopleuronectes americanus) and Alaskan plaice (Pleuronectes quadritaberulatus) adsorb onto the (2021) pyramidal planes of ice, whereas the sculpin (Myoxocephalus scorpius) peptide adsorbs on (2110), the secondary prism planes. All three are probably aligned along (0112). These antifreeze peptides have 11-amino acid sequence repeats ending with a polar residue, and each repeat constitutes a distance of 16.5 A along the helix, which nearly matches the 16.7 A repeat spacing along (0112) in ice. This structural match is undoubtedly important, but the mechanism of binding is not yet clear. The suggested mechanism of growth inhibition operates through the influence of local surface curvature upon melting point and results in complete inhibition of the crystal growth even though individual antifreeze molecules bind at only one interface orientation.