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BALTIC SEAENVIRONMENT PROCEEDINGS No. 59 - Helcom

BALTIC SEAENVIRONMENT PROCEEDINGS No. 59 - Helcom

BALTIC SEAENVIRONMENT PROCEEDINGS No. 59 - Helcom

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1.3<br />

2.<br />

d) Spreading<br />

Spreading ist one of the most significant processes during the early<br />

stages of a spill. The main driving force behind the initial spreading<br />

of the oil is its weight. A large instantaneous spill will therefore<br />

spread more rapidly than a slow discharge. This gravity assisted spreading<br />

is quickly replaced by surface tension effects. During these early<br />

stages, the oil spreads as a coherent slick and the rate is influenced<br />

by the viscosity of the oil. High viscosity oils spread slowly and<br />

those spilled at temperatures below their pour point hardly spread at<br />

all. After a few hours the slick begins to break up and form narrow<br />

bands or "windrows" parallel to the wind direction.<br />

Observation of Oil at Sea<br />

Aerial reconnaissance is essential for an effective response to oil spills,<br />

both to facilitate the location of oil at sea and to improve the control of<br />

clean-up operations. It is necessary to locate the oil in order that timely<br />

measures may be taken to protect coastlines threatened by pollution.<br />

The aircraft chosen for aerial observation must feature good all round visibility<br />

and carry suitable navigational aids. Over nearshore waters the flexibility<br />

of helicopters may provide an advantage, for instance, in surveying<br />

an intricate coastline with cliffs, coves and islands. However over the open<br />

sea the requirements for rapid changes in flying speed, direction and altitude<br />

are less acute and instead the speed and range of fixed-wing aircraft<br />

are generally desirable. Details see chapter 5.<br />

It can be assumed, that nearly 90 % of the total outflow quantity of oil in<br />

case of a tanker accident cover only 10 % of the entirely contaminated seasurface.<br />

These slick concentrations must be selected with proper remote sensing<br />

equipment, at least consisting of a side-looking-airborne radar for<br />

wide range detection and an infra-red-line-scanner for the slick analysis.<br />

In case of a spontaneous outflow e.g. with 10.000 m3 of a <strong>No</strong>rth Sea Crudeoil<br />

a coverage of 25 - 50 skm can be assumed after 24 hours spreading time.<br />

Pollutions of this dimension need the aerial assistance in order to fulfil<br />

the a.m. assumption with a clean-up coverage capacity of at least 10 % of<br />

the polluted surface. For predictions of the oil spill movement it has been<br />

found empirically that floating oil will move downwind at about 3 % of the<br />

wind speed. Additional movements of oil can be superimposed in proportion<br />

to the presence of surface currents.<br />

Annex 1 shows a table containing a Guide to the Relation between the<br />

Appearance, Thickness and Volume of Floating Oil.<br />

Strategy<br />

Highest priority must always be given to prevention of any kind of pollution<br />

or threat of pollution. Lightering operations can eliminate or minimise the<br />

risk of an outflow. If - in case of a collision or grounding - ruptured<br />

338

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