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The crystallization of calcium carbonate in a continuous organic medium using the classic ammonium carbonate gas diffusion system was recorded with an optical microscope. Surprisingly, dendritic structures were obtained consistently when the product gas mixture combined with calcium chloride already dissolved in the organic medium. Characterization studies revealed these crystals to be composite mixtures of calcium carbonate and ammonium chloride.
To the best of our knowledge, till date, crystallization studies of calcium carbonate have always been carried out either in pure water or in homogeneous mixtures of water with hydrophobic organic solvents. The main role of water is to dissolve the individual precursor salts in order to form the solvated calcium cations and carbonate anions respectively. There are currently no reports on using pure organic solvents for calcium carbonate formation. For this purpose, considering Coulomb's equation, organic solvents withvery high dielectric constants are preferred. Among the potential compounds, propylene carbonate (PC) is one of the suitable candidate with a dielectric constant of about 65. The ammonium carbonate gas diffusion method provides an advantage when calcium chloride is dissolved in the organic solvent, because the evaporation products (CO2, NH3, and H2O) have a rather high solubility in organic solvents. For every mole of ammonium carbonate salt that decomposes, 2 moles of ammonia, 1 mole of carbon dioxide and in fact 1 mole of water are produced. The water formation is unimportant in aqueous systems but essential during calcium carbonate crystallization in pure organic continuous phases for the formation of the corresponding precursor ions (NH4+, CO32-).
We have used a setup as shown in figure S1 (in Suppl. Info.) allowing on-line monitoring of the crystallization process with optical microscopy. For this, an optical glass cuvette filled with a calcium chloride in PC solution is connected via a tubing to a glass vial containing 0.5 g of ammonium carbonate. We were able to dissolve only sparingly soluble calcium chloride up to 0.2 wt.% in PC. Solid ammonium carbonate gradually decomposes into gaseous carbon dioxide, ammonia, and water. The decomposition products diffuse into the cuvette, driven by chemical potential differences. In order to facilitate the diffusion, the vial with the ammonium carbonate is put above the cuvette considering that carbon dioxide is denser than ambient air. Using a special holder, the cuvette is placed upright in front of the objective of the optical microscope that is subsequently connected to a computer allowing real time imaging of the cuvette. All experiments have been carried out at room temperature.
To study calcium carbonate crystallization in a continuous organic medium containing dissolved calcium chloride while using ammonium carbonate gas diffusion method to feed the reaction precursors.
Typical crystals of calcium carbonate exhibit rhombohedral, orthorhombic or hexagonal crystal structures depending on the polymorph generated under the particular experimental conditions with respect to temperature, composition, and concentration. Surprisingly, under the experimental conditions in this study, only dendritic crystals have been detected by optical microscopy, cf. images put together in figure A1–4 (taken after 30 h of reaction time). The multiple dendritic crystals had grown exclusively from interfaces, either from the vapor-PC interface (Fig. A1) or from all sites of the glass-PC interface (Fig. A2–4), and stretched into the PC phase. In all repeats, dendrites were the only crystals detected with optical microscopy. In general, these crystals resemble to the shape of pine trees. However, it also may happen that some lower primary branches are shorter than others grown nearer the tip, probably due to space constraints imposed by neighboring main trunks. In addition, secondary branches were also growing from the primary branches and their maximum size appeared to be also limited by the interspacing between primary branches.
In order to check on the influences of higher supersaturation levels, experiments were also performed in glass cuvettes but with smaller internal diameters. In general, the overall number of crystals obtained in cuvettes with 1 and 5 mm thickness was much higher but their sizes were smaller, only in the range of 50 to 100 µm compared to the 10 mm cuvette. We also found that the general dendritic structure was preserved, but the pine tree shape has changed. In most cases the crystals exhibited patterns with trigonal, tetrahedral and occasionally octahedral symmetries corresponding to the number of main trunks that had grown from a single nucleation site (cf. Fig. S2).
To investigate the structure of the dendritic crystals, X-ray powder diffraction analysis was performed. Figure S3 (Suppl. Info.) shows a typical XRD pattern of the crystals. The XRD pattern clearly reveals a composite structure of the crystals, a distinct difference to corresponding experiments carried out in aqueous continuous phases. However, this is not a big surprise, since in aqueous systems the solubility product of ammonium chloride is several orders of magnitude higher than that of calcium carbonate, but is obviously not the case for PC as the continuous phase. The solubility of ammonium chloride in water is 39.5 g/100 g H2O while that of calcium carbonate is 0.001 g/100 g H2O. In contrast, it might be considered as surprise that the calcium carbonate polymorph is vaterite and not the thermodynamically more stable calcite. The presence of vaterite and ammonium chloride was reaffirmed with Fourier transform infrared spectroscopy, Raman spectroscopy and elemental analysis (cf. Fig. S4–6). These results confirm the above conclusion that the dendrites are essentially composite structures made of ammonium chloride and vaterite.
Considering that ammonium chloride is a kind of standard textbook example for dendrite formation, the generation of composite dendrites in the experiments described here is not surprising. Dendrites are structures formed in the presence of diffusion limitations that are present during crystal growth. These diffusion irregularities often lead to higher supersaturations at specific areas such as corners and edges, and the resulting faster growth rates generate the final dendritic morphology. Like ice crystals, ammonium chloride also possesses a crystalline anisotropy that favors the formation of dendrites during its crystallization.
To obtain more material and information about the growth mode, experiments were repeated in larger containers made of PTFE. Figures A5–12 show scanning electron micrographs of several isolated dendrites and reveal their composite structure. Figure A5 shows the main trunk of one dendrite reaching to about 100 µm in height. The definitions of the primary branches and the interspacing between each branch have significantly diminished indicating a high level of overgrowth. In addition, many clusters of spherical structures with diameters up to 1 µm can be seen clearly deposited on the exterior surface of the dendrites (cf. Fig. A6–8). These clusters resemble very closely to the vaterite particles synthesized in several works.
Judging from the significant difference between crystal sizes, 100 µm dendrites and only 1 µm spherical clusters, the growth mechanism may then be formulated as a two stage process. During the decomposition of ammonium carbonate, both ammonia and carbon dioxide gases combine with water to form the respective ammonium (NH4+) and carbonate (CO32-) ions. Assuming similar diffusion speed and solubility, the propylene carbonate phase becomes saturated first with respect to ammonium chloride which thus nucleates and grows as the first stage. This suggestion that ammonium chloride precipitate first is supported by the stoichiometry of the ammonium carbonate decomposition which leads to 2 moles of ammonia for every mole of carbon dioxide produced. In addition, the affinity of ammonia to water molecules is much higher due to hydrogen bonding compared to its counterpart. As the dendritic ammonium chloride crystals are growing, the propylene carbonate phase is also reaching the supersaturation with respect to calcium carbonate, in this case the less stable polymorph vaterite. The precipitated ammonium chloride dendrites act as seed crystals and provide interfaces that favor the subsequent nucleation and thereby growth of vaterite crystals.
The SEM micrographs of figure A9–12 illustrate the composite nature of the dendrites quite clearly with a shell made of many triangular calcium carbonate crystallites of sizes up to 600 nm overlaying in a scaly fashion an inner homogenous almost monolithical ammonium chloride core (cf. Fig. A11). This microscopic structure is in accordance with the macroscopic observation that the dendrites collapse after water addition (cf. Fig. S7).
In conclusion, this is the first time calcium carbonate is crystallized in a continuous organic medium. Unexpectedly, well defined dendritic crystals were obtained consistently. Characterization studies revealed the crystals to be composite-like made of vaterite and ammonium chloride.
Characterization of single dendrites grown is not trivial due to their poor mechanical and water stability.
A starting solution was prepared by dissolving CaCl2 (Acros) in propylene carbonate (Sigma-Aldrich) to a concentration of 0.2 wt.% overnight using magnetic stirrer and with nitrogen gas bubbling at room temperature. The solution was subsequently filled into a optical glass cuvette and sealed. Thereafter, a 1 mL glass vial filled with 0.5 g of ammonium carbonate (Sigma-Aldrich) was connected to the top of the cuvette. Using a customized sample holder, the cuvette is placed perpendicularly with regards to a VHX optical microscope.
Shape and morphology of the samples were investigated with either optical or electron microscopy. Optical microscope images were taken with a digital VHX microscope (Keyence, Japan) directly with lens objective VH-Z100 allowing up to 1000X magnification. Scanning electron microscopy (SEM) was performed according to standard procedures with a high-resolution scanning electron microscope operating at an acceleration voltage of 3 kV (LEO1550 Gemini, Carl Zeiss AG, Germany). X-ray diffraction (XRD) was measured on a Bruker D8-Advance X-ray powder diffractometer using Cu Kα radiation (λ = 1.5406 Å) and a scintillation counter (KeveX Detector). Default measurements were then made with scattering angles (2θ) from 5–80° with step size and scan time of 0.005 and 0.5 s respectively. Raw data was treated by performing background subtraction, removing Cu Kα radiation and smoothening using the program Match! (Version 3.3.0 Build 88). Fourier-Transform Infrared (FT-IR) spectroscopy was measured with a Varian 1000 spectrometer using attenuated total reflection (ATR) mode.
We would like to acknowledge financial support from the Max Planck Institute of Colloids and Interfaces. In addition, E.P. acknowledges a scholarship from the IMPRS on Multiscale Bio-systems.