Geoscience Reference
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and partly by traction. Therefore, procedures A-C
in Figure 3.5 are followed in counterclockwise or-
der: Equations (3.13) and (3.17) are inverted so that
f i
3.4.4 Microstructure-sensitive behavior of
elasticity and viscosity
That the elasticity and viscosity tensors,
Equations (3.18) and (3.19), are derived as
functions of the contact function means that
the contact function X C , or more practically,
contiguity
at X C
σ ij S
p L
=
1 is constrained by
+
δ ij (proce-
f
ij is calculated from u i at X C
dure C'), and
1
(procedure A'). Then, procedure B becomes the
elastic deformation of a sphere under a given trac-
tion, and this can be solved analytically using
generalized spherical harmonics. In the viscous
case, unlike the elastic case, procedures A-C are
followed in clockwise order: by assuming each
contact face to be a circular plane surrounded by
the wetted region, the Poisson equation in (3.16)
can be solved analytically.
The elastic compliance tensor is given in an
analytical form as follows:
ε
=
, is the essential geometrical factor
in determining the elastic and viscous properties
of the solid framework. Figure 3.6b shows these
properties as functions of contiguity
ϕ
,where
X C is assumed to have 14 circular contact faces
(Figure 3.6a). In Figure 3.6b, the results are shown
for k sk and
ϕ
µ sk , corresponding to a Poisson's ratio
of
0.25 in the solid. More general results
are presented in Takei (1998b); the variations
of k sk and
ν S =
µ sk , with
ϕ
(0.03
ϕ
1) and
ν S
(0.05
0.45) are given as fitting formulae.
The results for
ν S
l
1
1
1) m
2 l +
3(
ξ sk and
η sk are closely fitted by
S ijpq =
1
α =−
1
β =−
1
l
=
0
m
=−
l
2
ξ sk cc =
0.37
ϕ
l ( i j ) D αβ χ β m
.
(3.20)
T 1
iji j χ α m
l ( p q ) T 1
·
(3.18)
p q pq
2
η sk cc =
0.2
ϕ
where subscripts i , j , p ,and q ,aswellasthosewith
a prime, are used in a Cartesian coordinate system
( x , y , z ), and a summation convention for repeated
subscripts is employed for those subscripts. The
RHS of Equation (3.18) consists of the geometrical
factors ( T ijpq - 1 and
Figure 3.6b demonstrates that elasticity and vis-
cosity differ significantly in their dependence on
ϕ
, even though both decrease with a decrease in
the contiguity (
2 )ismuchmore
ϕ
). Viscosity (
ϕ
2 ),
and the reason for this is clear from the deriva-
tions. Because a macroscopic stress applied to the
solid framework is supported by the contact faces,
a decrease in the contact area increases the con-
tact stress (the stress concentration effect). The
mild decrease in the elastic moduli k sk and
1
/
structure sensitive to
ϕ
than is elasticity (
ϕ
χ α m
l ( pq ) ), determined by the con-
tact function X C , and the intrinsic factor ( D αβ ),
determined by the intrinsic elasticities, k S and
µ S . Explicit forms of these factors are given in
Takei (1998a). The viscosity tensor is given in an
analytical form as follows:
µ sk ,
with decreasing
is caused by this stress concen-
tration effect. In addition, for viscosity, a decrease
in the contact area decreases the length of the
diffusion path through the grain boundaries (the
short-circuit effect). The significant decrease in
viscosities
ϕ
a f
R
4
nf
45
16 η cc
n i n j n f k n l
C ijkl =
( S ijkl ) 1
=
f
=
1
(3.19)
where nf represents the number of the circular
contact faces, a f represents the radius of the f th
( f
is caused
by the combination of the stress concentration
effect and the short-circuit effect.
Another remarkable difference between elas-
ticity and viscosity is the singularity. Without
the presence of a melt (
ξ sk and
η sk with decreasing
ϕ
, nf ) contact face, and n f represents
the exterior unit normal vector on the grain sur-
face at the center of the f th contact face. Similar
to the elastic case, the RHS of Equation (3.19)
consists of the geometrical factors ( a f /
=
1, 2,
...
µ sk ap-
proach the intrinsic elastic moduli of a solid, k S
and
ϕ =
1), k sk
and
R and n f )
and the intrinsic factor (
η cc ).
µ S
(Figure 3.6b). However, neither
ξ sk nor
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