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Issue 33, 2014
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Self-organization of calcium oxalate by flow-driven precipitation

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Abstract

We have analyzed the emerging precipitate pattern of calcium-oxalate in a flow system. The circular symmetry is broken because of the hydrodynamic instability at the tip of the underlying gravity current. The presence of a concentration gradient maintained by the flow leads to the enrichment of the thermodynamically unstable calcium oxalate dihydrate form.

Graphical abstract: Self-organization of calcium oxalate by flow-driven precipitation

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Article information


Submitted
09 Jan 2014
Accepted
29 Jan 2014
First published
29 Jan 2014

Chem. Commun., 2014,50, 4289-4291
Article type
Communication
Author version available

Self-organization of calcium oxalate by flow-driven precipitation

B. Bohner, G. Schuszter, O. Berkesi, D. Horváth and Á. Tóth, Chem. Commun., 2014, 50, 4289
DOI: 10.1039/C4CC00205A

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