Summary of Working Paper No. 110-1998
I.1.8
Part II of the INSROP Project I.1.8 was initiated to find better ways than the
subjective ball scale to describe the ice compression and it
The model tests were performed in the ice laboratory of the Helsinki
University of Technology. Two models were used for the testing. One was a model of an
icebreaker similar to the full scale reference vessel icebreaker Lenin and the
other was a model of an arctic cargo vessel. The model test results with the ice
breaker model showed that a useful measure to describe the ice compression is
Compaction Factor. This is the ratio between the areas of an uncompressed ice
field and the area of a compressed ice field. It is assumed that the forces
within the ice field are transferred through compaction. This is a fact at least in
larger scale and in ice fields that are broken due to compression. Based on the
comparison between full and model scale results, it seems that Compaction
Factors in the range of 1.20 - 1.53 are comparable to ice compression of 2 balls on
the 0 - 3 balls scale.
The results with the model of the arctic cargo vessel proved to be somewhat
doubtful. Based on these results the Compaction Factor has lower influence on the
resistance increase with the cargo vessel than with the icebreaker. The tests
were performed with a segmented model and that offers an opportunity for
further analysis of the forces acting on the vessel. It is recommended that this
analysis and possible further testing will be performed at a later stage.