Question 7 of 8: CaO Coordination Number; Porosity, Grain Size, and Weibull Statistics in Ceramics
Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)
Notes on this paper
National Exam 04-BS-11, Properties of Materials — May 2014. 3 hours,
closed-book examination (approved Casio or Sharp calculator only). Any five questions constitute
a complete paper; only the first five questions as they appear in the answer book are marked. All
eight questions are solved below for completeness.
Find. (a) Coordination number of CaO. (b) Porosity and grain-size effects on
ceramic tensile strength. (c) Why statistical (Weibull) methods are used for ceramic failure
prediction.
Approach
Part (a) applies the radius-ratio rule directly. Parts (b) and (c) are conceptual: porosity and
grain size are treated as flaw-population parameters that control the size of the critical crack a
ceramic can tolerate before brittle fracture, and the Weibull distribution is introduced as the
standard statistical framework for a strength that is controlled by the largest flaw in a random
population rather than by a single deterministic material property.
(a) Radius ratio.
$$\frac{r_{cation}}{r_{anion}}=\frac{r_{Ca^{2+}}}{r_{O^{2-}}}=\frac{0.100}{0.140}=\boxed{0.714}.$$
This falls in the range $0.414\text{–}0.732$, which predicts octahedral coordination,
CN $=\boxed{6}$ — consistent with CaO's actual rock-salt (NaCl-type) crystal
structure.
(b) Porosity effect. Pores act as pre-existing stress-concentrating flaws and
also directly reduce the load-bearing cross-sectional area, so tensile strength decreases
with increasing volume fraction porosity $P$, commonly modeled as an exponential decay
$\sigma=\sigma_0\exp(-nP)$; even a few percent porosity can substantially cut strength because
strength is controlled by the largest/sharpest pore, not the average pore size.
Grain size effect. Finer grain size increases tensile
strength (a Hall-Petch-type relationship, $\sigma\propto d^{-1/2}$), because grain boundaries
impede crack propagation and a fine-grained structure statistically limits the maximum flaw size
that can exist within any one grain or grain facet.
(c) Why statistical (Weibull) methods. Ceramics fail in a brittle
manner, with essentially no plastic deformation to blunt a crack tip or redistribute stress away
from a flaw; fracture strength is therefore controlled by the single most severe flaw in the
stressed volume, and flaw size/severity varies randomly from specimen to
specimen (and even from region to region within one specimen). This makes ceramic strength an
inherently statistical, not deterministic, property — unlike a ductile metal's yield strength,
which is comparatively insensitive to any one flaw.
Weibull distribution. The Weibull distribution models the probability of
survival at stress $\sigma$ for a component of volume $V$ as
$$P_{surv}=\exp\!\left[-\frac{V}{V_0}\left(\frac{\sigma}{\sigma_0}\right)^m\right],$$
where $m$, the Weibull modulus, is a shape parameter describing scatter (a large
$m$ means tightly-clustered strengths / a narrow flaw-size distribution; a small $m$ means widely
scattered strengths). Because $P_{surv}$ depends on volume $V$, the distribution also predicts (and
correctly captures) the observed size effect in ceramics: larger specimens are
statistically more likely to contain a critical flaw and therefore test weaker, on average, than
smaller specimens of the identical material.
Quantity
Result
(a) Radius ratio / coordination number
0.714 → CN = 6 (octahedral, rock-salt)
(b) Porosity effect
strength decreases (exponentially) with % porosity
(b) Grain-size effect
strength increases as grain size decreases (Hall-Petch-type)
(c) Weibull modulus $m$
shape parameter: large $m$ = low scatter, small $m$ = high scatter