Abstract
Freeze‐casting is a technique used to produce structures with
anisotropic porosity in the form of well‐defined microchannels
throughout a sample. Here, this technique is used on the magnetocaloric
ceramic La0.66Ca0.26Sr0.07 Mn1.05O3.
We show that a dynamic freezing profile, where the temperature is
decreased continuously at −10 K/min, results in homogeneous, lamellar
channels with widths of ∼15 µm, while static freezing, where the
temperature is kept constant at 177 K, results in channels of increasing
size away from the initial ice crystal nucleation site. The effect of
gelation before freeze‐casting is also investigated. Gelation inhibits
ice crystal growth, which significantly changes the morphology by making
channel cross sections less elongated, while additionally introducing
more dendrites and ceramic bridges in the structure. The latter
significantly dominates the flow path through the gelated structures,
affecting the calculated tortuosity, which increases to τ ≈ 4 when compared to non‐gelated samples where calculated tortuosities are in the range of ∼1.3 to ∼3.
Finally, we present a systematic and automatic approach for evaluating
channel and wall sizes and calculating tortuosities. This is based on
analysis of images obtained by scanning electron microscopy using a
continuous particle size distribution method and the TauFactor
application in MATLAB®.
Original language | English |
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Journal | Journal of the American Ceramic Society |
Volume | 102 |
Issue number | 10 |
Pages (from-to) | 5796-5806 |
Number of pages | 11 |
ISSN | 0002-7820 |
DOIs | |
Publication status | Published - 2019 |
Keywords
- Directional porosity
- Dynamic freezing
- Freeze‐casting
- Gelation
- Gelation‐freeze‐casting
- Ice‐templating
- Magnetocaloric
- Static freezing