MRI Study of Liesegang Patterns: Mass Transport and Banded Inorganic Phase Formation in Gel


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A new non-optic method for the study of Liesegang patterns was tested. Liesegang patterns are periodically banded precipitates produced by the reaction–diffusion process, mostly occurring in geology. The Liesegang experiment (5.5 M NH4OH, gelatin matrix with 0.4 M MgSO4) was monitored using a 9.4 T magnetic resonance imaging (MRI) system, allowing the acquisition of sample images in any location and orientation without interfering with the process studied. The development of patterns in a gel matrix was observed for 7 days after starting the reaction. Qualitative data (T2- and T2*-weighted images) and quantitative T2 maps were acquired. Preliminary experiments show that MRI is able to distinguish the regions between the precipitated bands and the structural changes in the gel matrix during the reaction. A damaged gel matrix was measured to reveal the effect of the initial reagent-gel contact area. MRI study of Liesegang patterns provides empirical data which can be used in theoretical model testing.

作者简介

Nikola Klanicová

Department of Geological Sciences, Faculty of Sciences, Masaryk University

编辑信件的主要联系方式.
Email: klanicova@mail.muni.cz
ORCID iD: 0000-0002-6196-1505
捷克共和国, Kotlářská 2, Brno, 611 37

Aneta Malá

Department of Condensed Matter Physics, Faculty of Sciences, Masaryk University; Institute of Scientific Instruments, CAS

Email: klanicova@mail.muni.cz
捷克共和国, Kotlářská 2, Brno, 611 37; Královopolská 147, Brno, 612 64

Ondřej Macíček

Institute of Scientific Instruments, CAS

Email: klanicova@mail.muni.cz
捷克共和国, Královopolská 147, Brno, 612 64

Josef Zeman

Department of Geological Sciences, Faculty of Sciences, Masaryk University

Email: klanicova@mail.muni.cz
捷克共和国, Kotlářská 2, Brno, 611 37

Zenon Starčuk

Institute of Scientific Instruments, CAS

Email: klanicova@mail.muni.cz
捷克共和国, Královopolská 147, Brno, 612 64

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