Abstract
Silica–barium carbonate biomorphs are complex precipitate microstructures that form by purely inorganic processes. They display life-like morphologies with smoothly curved surfaces that are not restricted to crystallographic symmetries. We investigate the morphogenetic influence of inorganic dopants that compete with the barium carbonate precipitation. Trace deposition of alkaline earth or transition metal additives causes significant changes to the crystal morphologies. In the case of Pb2+ and Ag+ ions, biomorph growth is disrupted by the formation of competing precipitates. Similarly, the addition of Ca2+, Mg2+, and Zn2+ induces the rapid crystallization of witherite or amorphous silica–carbonate aggregates at enhanced growth rates. By comparison, the addition of strontium ions results in the assembly of classic biomorphs such as cardioid sheets and helices. The procedures reported here exemplify the use of co-depositing agents to influence the compositional and crystallographic properties in a manner similar to magnesium-doped biogenic calcites.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.