1. The two fascines that are positioned closeted to the wave overtopping simulator. We saw
that the waves overshoots these fascines for the most part. These fascines could be more
effective when they are placed a bit further downslope, in the area where the first fascines
were lost.
2. The ribbons of lashing straps. These ribbons are too narrow in width to cover the damaged
area and provide protection against the force of the waves. Hence, all the sandbags
underneath the wig of lashing straps were lost/washed away.
3. The steel anchor pins that were used for the fascines. The anchor pins that were facing
slope upwards turned in such a way that they were facing slope downwards after a period
of wave action (see figure 12). The fascines than could start to flutter and come loose. The
anchor pins placed in pairs, facing slope upwards and slope downwards and tied together
with an iron wire is recommended.
4. The structural integrity of the jute ribbons. The ribbons were made by cutting ribbons of a
cloth of jute with a knife. Therefore, the ribbons could fray and the ribbons couldn’t cover
as much as whole ones, but still they could protect the area. Perhaps jute ribbons (about
30cm wide) could be prepared in advance with sides hemmed.
5. The jute layering of the slope and the damaged area performed well. The jute didn’t
rupture despite heave wave action and pounding waves on it. However the jute was
delivered in strips of about 1m wide, the strip layering of the jute on the slope and
damaged area did hold with enough anchor pins placed. Preferably jute layering as much
from a whole is recommended.
6. The jute ribbons protected the damaged area well. The sandbags underneath stayed in
place despite heave wave action and pounding waves on it, especially the sandbags close
to the scarp of the damage. Jute has the property of soaking up water, hence getting more
weight. The heavy jute ribbons stay in place and cover the damaged area. Also a next
wave will be more guided/speeded up by the wet, heavy jute ribbons.
7. After 360 minutes of waves (end of the challenge), there was a slight erosion pit
(elongated hole, cigar like, of about 40 – 50cm in depth). Figures 13 to 15 shows the
damaged area. The other areas of the damaged section were not affected by erosion.
Above the erosion pit, some slope instability occurred. Figures 13 to 15 shows the
damaged area.
In the corner of the scarp and right hand side of the damaged area, the jute layers were
not overlapping enough so the water flow could get underneath of some of the layers. And
therefore erosion took place, resulting in slope instability and the erosion pit.