Jaime Gómez Morales

Rhombohedral-scalenohedral calcite transition produced by adjusting the solution electrical conductivity in the system Ca(OH)2-CO2-H2O.

This work is aimed to investigate the effects of the adjustment of the electrical conductivity (kappa25) during the semicontinuous carbonation of Ca(OH)2 suspension (slaked lime) on the morphology of the precipitated calcite (CaCO3) particles. The experiments were carried out at 30, 45, and 60 degrees C. A gradual morphological change from rhombohedral to scalenohedral shapes was produced with an increase of kappa25 from 1 to 7 mS/cm at each temperature. The explanation of this morphological change is given in terms of the increase of both the supersaturation and the ratio between concentrations of charged species containing calcium and carbonate ([Ca]ch/[CO3]ch) in the aqueous phase as the kappa25 set-point increases, prior to the precipitation process. In addition to the rise of the supersaturation this change most probably takes place because the increase of the [Ca]ch/[CO3]ch ratio affects the growth rate of the rhombohedral {104} and scalenohedral {21-1} faces in a different manner: (i) favoring the equality between the surface coverage of Ca2+ and CO3(2-) on the stoichiometric {104} face, thus enhancing the formation of CaCO3(0) growth units and then its growth rate and (ii) inhibiting the growth of the {21-1} face by adsorption of the excess calcium species.

Local pH oscillations witness autocatalytic self-organization of biomorphic nanostructures

Bottom-up self-assembly of simple molecular compounds is a prime pathway to complex materials with interesting structures and functions. Coupled reaction systems are known to spontaneously produce highly ordered patterns, so far observed in soft matter. Here we show that similar phenomena can occur during silica-carbonate crystallization, the emerging order being preserved. The resulting materials, called silica biomorphs, exhibit non-crystallographic curved morphologies and hierarchical textures, much reminiscent of structural principles found in natural biominerals. We have used a fluorescent chemosensor to probe local conditions during the growth of such self-organized nanostructures. We demonstrate that the pH oscillates in the local microenvironment near the growth front due to chemical coupling, which becomes manifest in the final mineralized architectures as intrinsic banding patterns with the same periodicity. A better understanding of dynamic autocatalytic crystallization processes in such simple model systems is key to the rational development of advanced materials and to unravel the mechanisms of biomineralization.

Self-assembled crystalline materials of calcium carbonate and silica

C283 resulting precipitates were characterized by Infrared Spectroscopy, X-ray diffraction and the morphology of crystals was observed by an optical microscope and a scanning electron microscope. The results showed that SOM influences not only on the agglomeration, morphology, size and polymorphism of the CaCO3 crystals but also narrows the range of calcium and carbonate critical concentrations necessary to induce nucleation, the “Crystals-Growing Space”. Thus, it appears evident that in gelling environment the SOM is able to select a specific calcium and carbonate concentration. That, respecting the supersaturation laws, confines the nucleation and growth processes.