
1437O. Yagci, S. Kapdasli / Ocean Engineering 30 (2003) 1433–1451
to be difficult to control or uncertainty in the wave climate is high, or foundation
instability is expected, then interlocking blocks, like dolosse or core-loc, may be
unreliable because of potential breakage. Burcharth et al. (2000) proposed an empiri-
cal formula for breakage of dolosse and tetrapods.
The H/
⌬
D
n50
parameter can be used to define the relationship between different
structures. Structures such as caissons or structures with large armor units are charac-
terized by small values of H/
⌬
D
n50
. Large values imply gravel beaches and sand
beaches (Van der Meer, 1988).
N
s
⫽H
⌬D
n50
(6)
where N
s
=Hudson’s stability number; H=characteristic wave height;
⌬
=
(ρ
s⫺
r
w
)/r
w
=relative submerged mass density; r
s
and r
w
=mass densities of armor
unit and water, respectively; and D
n50
=nominal diameter of the stone determined
from median mass from mass distribution curve or median weight from weight distri-
bution curve and it is computed as:
D
n50
⫽
冉
W
50
g
s
冊
⫽
冉
M
50
r
s
冊
(7)
where W
50
=median weight from weight distribution curve; g
s
=the specific weight
of armor unit; M
50
=median mass from mass distribution curve.
Losada et al. (1986) defined three different damage levels based on the visual
evaluation. These are “Initiation of Damage”,“Iribarren’s Damage”and “Destruc-
tion”. Vidal et al. (1991) mentioned an additional damage level naming it as
‘Initiation of Destruction’. These four damage levels are briefly explained below.
Initiation of This state is defined as situation attained when a certain number of
Damage: armor units were displaced from their original places to a new position
at a distance longer than a side of the unit.
Iribarren’s This state occurs when there is failure covering area so extensive in
Damage: the upper layer of the armor as to allow the extraction of units from
the lower one (two-layer armor).
Initiation of A small number of units, two or three, in the lower armor layer are
Destruction: forced out and the waves work directly on pieces of the second layer.
Destruction: In this case, the failure is large enough to uncover the underlayer. The
armor units leave the mound continuously, and if the test is not
stopped, the whole cross-section will be destroyed after a sufficiently
long period.
4. Theoretical approach
Three different types of block movement were considered and it was assumed that
each type has different contribution to damage (Yagci, 2000). The movement types
are as follows: