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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.

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