Environmental Engineering Reference
In-Depth Information
element, the Young modulus and the cable straight section [ 13 ]. This section is a
normal section of the floating barrier which is composed of three kinds of materials:
the curtain fabric, the upper aerial leach and the subsea chain.
The approximation of the continuous equilibrium equation permits to define a
discrete problem. The curvilinear derivative operator on the internal force
d
)
is transformed into a vectorial difference at each node between neighbouring element
tensions. A weighted summation of the external force F ext (
ds F int (
s
is made at each node
over its two adjacent elements. The nodal displacement vector is denoted U .We
use the same notations F int and F ext after the transformations from the continuous
to the discrete formulations. They depend on the discrete problem unknown U , i.e.,
the equivalent internal force vector F int (
s
)
U
)
and external force vector F ext (
U
)
.The
non-linear discrete equation is written in term of the residual vector R
(
U
)
R
(
U
) =
F int (
U
)
F ext (
U
) =
0
.
(7.8)
The equation is solved using the Newton-Raphson method. The method uses the
derivative
d
. The derivative of the internal force vector is defined on each
element by a stiffness matrix. The external force vector derivative is not taken into
account here.
dU R
(
U
)
Remark 7.3 The current pressure p
(
s
)
is defined by a classical hydrodynamic rule
1
2 ˁ w Cv
2
p
(
s
) =
(
s
)
,
(7.9)
where
ˁ w is the water density, C the drag coefficient and v
(
s
)
the current velocity.
The atmospheric wind action on the aerial part of the barrier can be defined by
using a similar rule than those for the current pressure by considering the air density
ˁ air and the wind velocity taken at the altitude of the float.
The waves generated by the wind act on the subsea part of the barrier. A wave
pressure can be added to the current pressure by using an incident velocity v w sup-
plementary to the current velocity v
. The velocity v w can be defined by using the
square root of the significant wave height.
(
s
)
7.2.4 Operational Point of View of the Numerical Results
From the operational point of view the 2D model gives the boom tensions t
(
A
)
and
(
)
t
at both end-points A and B of a boom section. The direction of the mooring
tensions T
B
(
)
(
)
are also given by the numerical model. The hydrodynamic
current can vary in time depending on the tide stages. As a consequence boom tension
and boom tangent direction can be time-dependent.
A
and T
B
 
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