5.1 Yield Criteria and Flow Rules for HTSC Powders Compaction 225
test (Fig. 5.3a), in which three pairs of anvils compress the powder in three
mutually perpendicular directions. However, note that tests of granular ma-
terials (e.g., soils) or cemented materials (e.g., concrete or rock), presented
in Fig. 5.3b and c, have shown that associated flow rule cannot depict test
data satisfactorily [1114]. At the same time, satisfactoriness of associated (or
non-associated) plasticity has not been stated for compacted HTSC powders.
Therefore, it is very important to additionally consider non-associated flow
rules for which the plastic strain rate is not orthogonal to the yield surface.
5.1.2 Non-Associated Plasticity of HTSC Powders
Base hypothesis of normality [224], which forms a basis of associated plas-
ticity and is very successful in the description of metallic compositions, can
be broken for non-metallic granular materials in free filling, in particular for
HTSC powders. The key circumstance is that the associated plasticity can-
not validly describe shear dilatancy of granular material (i.e., the change in
volume that is associated with shear distortion of an element in the material,
consisting of multiple particles as microelements). As has been shown [1114],
the material, retaining constant volume under plasticity, reacts otherwise on
loading, demonstrating plastic expansion. The differences are related to both
the “load–deformation” curve and the value of critical loading. In order to
characterize a dilatant material, dilatancy angle Ψ is introduced, presenting
the ratio of plastic volume change over plastic shear strain.
An ideal triaxial test should permit independent control of all three princi-
pal stresses so that general states of stress could be examined. Typical results
in a standard triaxial test of granular material in free filling are shown in
Fig. 5.4. In elastic region (I), as usual, the strains are reversible at loading.
In hardening regime (II), the strain of granular material becomes more and
more inelastic due to particle sliding. Here, non-linear elasticity predicts con-
tinuing contraction of the specimen under continued loading in compression.
However, such a prediction is disproved by experimental evidence (Fig. 5.5),
which shows a dilatant volume increase at subsequent loading [1114]. This
phenomenon takes place due to frictional sliding along particles. The elastic
strain rate in the hardening regime is almost zero. Moreover, there exists a
linear relation between the volume change and the change of the axial strain
near the end of the hardening regime (II) and in the softening regime (III)
(see Fig. 5.4c). Then, following [1114], the constant dilatancy angle, Ψ, may
be introduced as
sin Ψ =
˙e
p
−2˙e
p
1
+˙e
p
. (5.10)
Equation (5.10) defines constant rate of dilatation, and it is valid under
conditions of triaxial compression. For broad row of granular materials, the
dilatancy angle, Ψ , approximately equals 0–20
◦
; at the same time, the inter-
nal friction angle, Φ = 15–45
◦
[1114]. Because the dilatancy angle can be
considerably smaller than internal friction angle, it is necessary to apply for