Environmental Engineering Reference
In-Depth Information
Fig. 2.1 View of domain D
from above
Fig. 2.2 Cross-sectional
area of domain D
S +
S
vector to the boundary
D
=
S T
S B of domain D ,
∂/∂
n is the derivative
t is the unit vector directed upward in the
Cartesian coordinate system (Fig. 2.2 ). We observe that
in the normal direction, and k
= (
0
,
0
,
1
)
0on S +
S
k
·
n
=
and U
·
n
=
0on S T
S B .
(2.12)
Also note that the boundary conditions ( 2.6 )-( 2.9 ) are general (i.e., not only for
horizontal free and bottom surfaces S T and S B ), and hence, the dispersion model can
take into account free surface wave motion and marine topography.
First of all we show that the solution of dispersion model ( 2.4 )-( 2.11 ) satisfies
the mass balance equation. Indeed, integrating Eq. ( 2.4 ) over domain D we get
D ˆ
+
· ˆ
∇· μ ˆ
+
˃ˆ
+
∇· ˆ s dr
dr
U
dr
dr
dr
t
D
D
D
D
N
=
Q i (
t
)ʴ(
r
r i )
dr
.
i
=
1
D
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