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Flow-driven pattern formation in the calcium-oxalate system

Journal Article · · Journal of Chemical Physics
DOI:https://doi.org/10.1063/1.4947141· OSTI ID:22657940
; ;  [1];  [2]
  1. Department of Physical Chemistry and Materials Science, University of Szeged, Aradi vértanúk tere 1., Szeged H-6720 (Hungary)
  2. Department of Applied and Environmental Chemistry, Rerrich Béla tér 1., Szeged H-6720 (Hungary)

The precipitation reaction of calcium oxalate is studied experimentally in the presence of spatial gradients by controlled flow of calcium into oxalate solution. The density difference between the reactants leads to strong convection in the form of a gravity current that drives the spatiotemporal pattern formation. The phase diagram of the system is constructed, the evolving precipitate patterns are analyzed and quantitatively characterized by their diameters and the average height of the gravity flow. The compact structures of calcium oxalate monohydrate produced at low flow rates are replaced by the thermodynamically unstable calcium oxalate dihydrate favored in the presence of a strong gravity current.

OSTI ID:
22657940
Journal Information:
Journal of Chemical Physics, Journal Name: Journal of Chemical Physics Journal Issue: 16 Vol. 144; ISSN JCPSA6; ISSN 0021-9606
Country of Publication:
United States
Language:
English

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