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@ARTICLE{Rheinheimer:887840,
author = {Rheinheimer, Wolfgang and Hoffmann, Michael J.},
title = {{G}rain growth transitions of perovskite ceramics and their
relationship to abnormal grain growth and bimodal
microstructures},
journal = {Journal of materials science},
volume = {51},
number = {4},
issn = {1573-4803},
address = {Dordrecht [u.a.]},
publisher = {Springer Science + Business Media B.V},
reportid = {FZJ-2020-04466},
pages = {1756 - 1765},
year = {2016},
abstract = {Barium titanate, strontium titanate, and lithium lanthanum
titanate (LLTO) were used to study grain growth in
perovskite ceramics. In these materials, a grain growth
transition was found. In the case of barium titanate, grain
growth shows a gradual transition to faster growth with
increasing temperature, whereas strontium titanate indicates
exponentially decreasing grain growth with increasing
temperature. In reducing atmosphere, strontium titanate
shows two transitions; the additional second transition is
attributed to a reversible wetting transition. In LLTO, a
single grain growth transition was found and seems to be
caused by a wetting transition as well. In all cases, the
grain growth transitions are strongly correlated to abnormal
grain growth. This non-Arrhenius behavior of grain growth in
perovskites is discussed in relation to abnormal grain
growth and bimodal microstructures: the existence and
coexistence of two grain boundary types with different grain
boundary mobility is proposed. In this framework, a gradual
transition of the boundary population from type 1 to type 2
with temperature seems to cause the growth phenomena in
perovskites on a macroscopic scale. Most likely, this
gradual transition is driven by the anisotropy of the grain
boundary energy. Possible microscopic origins of the grain
growth transitions are discussed. The consequences of
bimodal growth and boundary anisotropy for classical mean
field modeling of grain growth are assessed: the grain
growth constant k is not capable to appropriately reflect
grain growth in perovskites, and boundary anisotropy cannot
be included in standard mean field approaches.},
cin = {IEK-1},
ddc = {670},
cid = {I:(DE-Juel1)IEK-1-20101013},
pnm = {899 - ohne Topic (POF3-899)},
pid = {G:(DE-HGF)POF3-899},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000367647100009},
doi = {10.1007/s10853-015-9535-6},
url = {https://juser.fz-juelich.de/record/887840},
}