ft, but actual damage estimates would have to be
Some structures were observed to sustain dam-
augmented by an analysis of structural integrity
age during icebreaking operations when the ice
on a site-by-site basis. The 1-ft criterion was only
cover was so violently disrupted that chunks of
meant to define river areas where reasonably well
ice were thrown against them. While most dam-
built structures could be exposed to damaging
age was minor, three of the docking structures
ship effects and to compare the damage poten-
monitored had portions substantially destroyed,
tial of various fleet mixes.
and a boat house was so severely damaged dur-
In forming their estimate of the potential for
ing the opening of navigation in March that it
vessel-related structural damage, Hodek et al.
later collapsed.
(1986) considered both vertical and horizontal
In that study (USACE 1974) arrays of survey
dynamic loadings. For the areas of St. Marys River
stakes were laid out at six sites to monitor ice
considered in the report, they felt that dynamic
movement in the offshore direction. At one site
horizontal loadings would be small for cases with
the ice was found to have moved as much as 30 ft
a continuous ice sheet (such as those that com-
offshore over a period of 40 days, but typical ice
monly occur during the extended season). If ves-
movements were on the order of 10 ft or less. Some
sel passage were sufficient to break the ice cover
lateral movement was also observed at three sites.
into individual pans (as documented in USACE
In connection with some of their recordings of
1974), the potential for damage by horizontal forces
water level fluctuations, they also measured the
would increase. For vertical ice forces, they felt
relative motion of the ice sheets on either side of
that gravity structures, such as rock-filled tim-
an active crack. These data indicated that the off-
ber cribs, would not be damaged by vertical forces.
shore ice sheet could move at least several tenths
The rest of their analysis was limited to uplift forces
of a foot offshore during vessel passage (appar-
on vertical piles. They concluded that all piles,
ently in response to the drawdown-induced move-
unless properly engineered and installed, will be
ment of water) and that the ice cover did not fully
subjected to tensile loads in excess of their ca-
return to its original horizontal position when the
pacity and will eventually move upward.
water returned to its prior elevation.
It is postulated here that this mechanism re-
sults in a gradual horizontal jacking of the ice
Field studies of
cover towards the navigation channel, since the
structure damage
The first field study of shore structure dam-
water in the open shore crack can partially or
age during winter navigation was conducted by
totally refreeze before the next ship passage. Start-
the Detroit District on the St. Marys River begin-
ing from this new position the next event will
ning in 1972 (USACE 1974). They selected sev-
leave the offshore ice sheet slightly farther from
eral docks in two reaches of the river for moni-
its original location. Repeated cyclings of this
toring: near Six Mile Point on Lake Nicolet and
backing process could lead to the large horizon-
Johnson's Point on Neebish Island. Some of the
tal motions recorded over the winter season and
docks monitored were pile supported, while others
lead to increased ice volumes in the vessel track.
were constructed with rock-filled timber cribs or
If the crack were to pass through a structure, this
steel piling. Monitoring was limited to visual
horizontal jacking could incrementally pull the
observations and photographs. Their conclusions
structures apart.
were that water level fluctuations and ice floes
A follow-up study by the consulting firm of
can cause structural damage and that navigation
Dalton, Dalton, Little and Newport, Inc. (1975)
in ice can be a contributing factor.
concluded that although ship passage during ice-
The pile-supported portions of structures were
covered conditions can contribute to structure
found to be the most susceptible to damage, but
damage, a major factor is the inadequate design
even timber crib structures were not immune. Jack-
and construction of many structures on the river.
ing of finger piers due to vertical ice forces in-
They concluded that control of vessel speed was
duced by natural water level fluctuations and
not important since they considered ship-gener-
drawdown was common, and several structures
ated waves to be of minimal importance. Instead,
were damaged as the result of differential ice move-
they recommended improved structural design
ments along active cracks that passed through
to withstand natural forces and consideration of
them. Water levels were high enough that some
removable, floating structures.
structures were damaged by ice in contact with
Carey (1980) reviewed the potential for win-
the horizontal members of the superstructure.
ter-navigation-related shore structure damage on
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