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In a viscous fluid, objects are dragged by the surrounding fluid.
(Imagine when you are in water pool or the sea.)
 |
(3.10) |
Boundary value problem (Dirichlet problem).
Expanding the integrand in the right-hand side
of Eq. (3.10),
we have
![$\displaystyle \bm{u} (\bm{x}) = - \frac{1}{n!} \sum_{n=0}^{\infty} \frac{1}{8\p...
...t^n \int_S {\rm d}S(\bm{y})\ \Bigl[ \bm{y} - \bm{y}_0 \Bigr]^n \bm{f}(\bm{y}) ,$](img126.png) |
(3.11) |
where we assume that the surface
consists of a single sphere
and
is its center.
Note that the surface integral in the right-hand side
is a tensor of order
and
is called the force moment
![$\displaystyle \mathcal{F}^{(n)} (\bm{y}_0) := - \int_S {\rm d}S(\bm{y})\ \Bigl[ \bm{y} - \bm{y}_0 \Bigr]^n \bm{f}(\bm{y}) ,$](img131.png) |
(3.12) |
and
Taking the terms up to
and substituting the above,
we have an expression[6]
 |
(3.15) |
where
and
are given by
Up to this order of expansion,
if we introduce the corresponding velocity moments, that is,
the translational and angular velocity
and
and the rate of strain tensor
,
we have the closed linear set of equations
written in the matrix form as
![$\displaystyle \left[ \begin{array}{c} \bm{U}\\ \bm{\Omega}\\ \bm{E} \end{array}...
...t] \cdot \left[ \begin{array}{c} \bm{F}\\ \bm{T}\\ \bm{S} \end{array} \right] .$](img146.png) |
(3.18) |
From the mathematical property of Eq. (3.10),
the whole matrix relating two vectors
and
should be symmetric.
That is,
However, we should note that
once we reduce the elements of vectors,
the symmetry does not hold.
From the definition, the second order tensors
and
are symmetric and traceless, so that only 5 components
out of
are independent.
Without the reduction to the independent components,
the linear set of equation becomes ill-defined
and the inverse matrix (with the full components) are not unique.
Subsections
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Kengo Ichiki 2008-10-12