Abstract

Negatively ionisable poly-L-glutamic acid (pGlu) and poly-L-aspartic acid (pAsp), considered as analogues of the naturally occurring acidic macromolecules involved in biomineralization processes, were used as additives in the calcium carbonate precipitation systems in order to investigate their interactions with the vaterite crystallites. Poly-L-lysine (pLys), a positively ionisable poly(amino acid), was also used in order to elucidate the impact of the side chain charge. The growth kinetics of vaterite was found parabolic, indicating that the integration of growth units into the spiral step at the vaterite crystal surfaces is the rate-determining mechanism. The presence of small amounts of pGlu and pAsp inhibited the crystal growth. At the highest concentrations of both acidic macromolecules the exponential rate law was observed, which indicates the surface nucleation as the rate controlling mechanism. The addition of pLys in the range of applied concentrations did not significantly influence the crystal growth of the vaterite. Thus, the kinetic results, corroborated by morphological observations, pointed out to the significance of the negative charge of the side chains of selected polypeptides in the interfacial interactions with mineral planes.

Highlights

  • C ALCITE and aragonite are the thermodynamically most stable calcium carbonate polymorphs, which can be frequently found in biomineralized tissues of many invertebrate organisms

  • Negatively ionisable poly-L-glutamic acid and poly-L-aspartic acid, considered as analogues of the naturally occurring acidic macromolecules involved in biomineralization processes, were used as additives in the calcium carbonate precipitation systems in order to investigate their interactions with the vaterite crystallites

  • The results showed that the ζ-potential of vaterite crystals suspended in the saturated CaCO3 solution was negative (–4 mV ≤ ζ ≤ –26mV) within the whole pH range (9.0 ≤ pH ≤ 10.6), while the addition of 2 ppm poly-L-aspartic acid (pAsp) or 2 ppm poly-L-glutamic acid (pGlu) caused the ζpotential to become even more negative

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Summary

Introduction

C ALCITE and aragonite are the thermodynamically most stable calcium carbonate polymorphs, which can be frequently found in biomineralized tissues of many invertebrate organisms. The vaterite seed crystals and the appropriate concentration of the poly(amino acids) (pAsp, pGlu or pLys) were suspended into the 200 cm3 of Na2CO3 solution.

Results
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