HEADING PAGE - port of ploce authority * welcome
HEADING PAGE - port of ploce authority * welcome
HEADING PAGE - port of ploce authority * welcome
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ENVIRONMENTAL IMPACT STUDY<br />
Rn: 03-033 CONTAINER TERMINAL PLOCE <strong>PAGE</strong>: 50<br />
A.3.4.3.3. SEISMIC CHARACTERISTICS<br />
The river delta territory is seismically active. It is shown ba the density <strong>of</strong><br />
earthquake epicenters, their frequency as well as the magnitude size <strong>of</strong><br />
seismic impacts. The cause <strong>of</strong> elevated seismic activity is the the Adriatic slab<br />
slipping under the Dinarides, i.e. under the High Karst zone. The contact<br />
between those zones is characterized by seicmically very active Biokovodubrovacka<br />
fracture zone, stretching through the river Neretva delta as well.<br />
In the last 50 years, in 1942. and 1961. this area was struck by earthquakes <strong>of</strong><br />
7 to 8 0 magnitute on the MCS scale, causing greater material damage on<br />
buildings.<br />
According to the valid data, the basic seismic intensity on the river Neretva<br />
delta is <strong>of</strong> 8 0 <strong>of</strong> the MCS scale. The expected intensities with 63% probability<br />
<strong>of</strong> occurrence are: 6 0 MSK-64 for the 50 year return period, 7 0 MSK-64 for<br />
100 and 200 year return period and 8 0 MSK-64 for 500 year return period.<br />
According to the ground seismic stability analyses in the river Neretva delta<br />
zone since 1986, the maximum magnitude can be M = 6.1, while the basic<br />
seismicity degree Imax = 9.15 <strong>of</strong> MCS scale. The same analyses have shown<br />
the psosibility <strong>of</strong> liquefaction in the mud and sand sediments <strong>of</strong> the delta.<br />
A.3.4.3.4. GEOMECHANICAL INFORMATION<br />
According to the information from the geotechnical study by the IGH, the<br />
Institute <strong>of</strong> Geotechnics, the area where the Ploce Port is located lies on the<br />
wide delta <strong>of</strong> the river Neretva. Therefore, this territory is formed mainly <strong>of</strong><br />
sediment formations from the Quarternary age which in form <strong>of</strong> thick<br />
formations are accumulated over the karst paleorelief. On the area foreseen<br />
for container terminal and Quay 7 construction, the thickness <strong>of</strong> Quarternary<br />
formations exceeds 100 m. sediment formations are <strong>of</strong> very different grain<br />
size content and are <strong>of</strong>ten intermixed. According to the research studies<br />
performed in 1989, for the phase I <strong>of</strong> the container terminal construction in the<br />
Quay 7 background, the following types <strong>of</strong> ground were established:<br />
From elevation 0 to elevation –20 mud and sand material<br />
From elevation –20 to elevation –35 clayley materials<br />
From elevation –35 to elevation –42 sand<br />
From elevation –42 to elevation –52 gravel<br />
These research studies were elaborated in the text: Study on Engineering<br />
Geological and Geotechnical Ground Characteristics and Requirements for<br />
the Object Funding for the First Phase <strong>of</strong> Container Terminal in the «Ploce<br />
Port» in Kardeljevo, Institute for Geotechnics and Funding <strong>of</strong> the Faculty <strong>of</strong><br />
Civil Engineering in Sarajevo, Reference number D-1815, Sarajevo, I/1990<br />
(cited from the quote in the Geotechnical Study <strong>of</strong> the IGH, project number<br />
Rn-03-033-04-IR-03).<br />
According to these information, the ground where the container terminal shall<br />
be built is <strong>of</strong> extremely low carrying capacity and is subject to subsidence. In<br />
the geotechnical study for the preliminary design, the terms <strong>of</strong> construction<br />
and ground consolidation with gravel piles were determined, in order that<br />
foreseen loads from the container terminal could be taken over.<br />
RIJEKAPROJEKT d.o.o.