Abstract

The self-assembly of alkaline earth carbonates in the presence of silica at high pH leads to a unique class of composite materials displaying a broad variety of self-assembled superstructures with complex morphologies. A detailed understanding of the formation process of these purely inorganic architectures is crucial for their implications in the context of primitive life detection as well as for their use in the synthesis of advanced biomimetic materials. Recently, great efforts have been made to gain insight into the molecular mechanisms driving self-assembly in these systems, resulting in a consistent model for morphogenesis at ambient conditions. In the present work, we build on this knowledge and investigate the influence of temperature, supersaturation, and an added multivalent cation as parameters by which the shape of the forming superstructures can be controlled. In particular, we focus on trumpet- and coral-like structures which quantitatively replace the well-characterised sheets and worm-like braids at elevated temperature and in the presence of additional ions, respectively. The observed morphological changes are discussed in light of the recently proposed formation mechanism with the aim to ultimately understand and control the major physicochemical factors governing the self-assembly process.

Highlights

  • Silica biomorphs are an interesting type of self-assembling inorganic–inorganic composite material with remarkably complex architectures

  • We show that temperature variation is a straightforward means to obtain further interesting ultrastructures, if the conditions are carefully chosen

  • Studies, biomorphs were grown on indium tin oxide (ITO) substrates (Osslia), which were placed in

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Summary

Introduction

Silica biomorphs are an interesting type of self-assembling inorganic–inorganic composite material with remarkably complex architectures. They form in silica-rich solutions at high pH in the presence of alkaline earth metal cations like barium, strontium, and calcium under ambient conditions [1,2,3,4,5,6]. Minerals 2017, 7, 75 similar structures can be obtained with other carbonates, including orthorhombic analogues like evidence that similar structures can be obtained with other carbonates, including orthorhombic strontianite (SrCO3 ) [8,9] or aragonite (CaCO3 ) [10,11,12].

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