Table 3. Summary of modeling tasks and appro-
of refrigerated sheets and uniform consistency
priate model ice materials.
and thickness of nonrefrigerated ice materials.
Placement of particulate model ice materials, like
Modeling task or
Suitable model ice
beads, may result in nonuniform thickness or
property
material choices
porosity. Nonuniform material properties may
Water velocity profiles
RS, BR, PB, (RIN, RIFG,
result in cover failure at weak points, overestima-
NRS)1
tion of thickness, improper piece size, and so
Ice movement
BR, PB, (RIN, RIFG,
NRS)2
forth. Careful sampling prior to testing should be
PB, (RIN, RIFG, NRS)3
Iceshore interaction
carried out to ensure uniformity.
Ice thickness
RS, BR, PB, RIN, RIFG,
NRS4
PB, (RIN, RIFG, NRS)5
Ice jam thickness
SUMMARY
PB, (RIN, RIFG, NRS)5
Ice jam evolution and movement
Table 3 was prepared to aid in selection of
Ice sheet deflection
RIN, RIFG, NRS
Ice cover breakup
RIN, RIFG, NRS
model ice. It suggests choices of model ice materi-
Ice breaking
RIN, RIFG, NRS
al to suit the primary process to be modeled. For
Icestructure interaction
RIN, RIFG, NRS
example, if only the shear stress or drag of the un-
RS
Rigid sheet (plywood, Styrofoam, etc.)
derside of an ice cover is of interest, then almost
BR
Blocks and random shapes (wood, plastic, wax, etc.)
any model ice material could be used. For most
PB
Plastic beads and other particulates
applications, unbreakable sheets of buoyant ma-
RIN
Refrigerated ice (freshwater, urea-doped, saline-
doped)
terial (e.g., plywood or Styrofoam) with addi-
RIFG
Fine-grained refrigerated ice (FGX, EG/AD/S, etc.)
tional roughness are the easiest to use in terms of
NRS
Nonrefrigerated sheet mixtures
cost and handling during experimentation. If the
1
Flowing water beneath the sheet may change rough-
process involves shoving and thickening of an
ness characteristics with time
2
Assumes that sheet has been broken into pieces
evolving ice jam, material choices become more
3
Assumes movement along shore and sufficiently
constrained. Other factors, such as availability of
broken pieces
refrigerated space, material handling require-
4
Generally controlled by scaling factor
ments, and cost must also be considered in the
5
Assumes sheet has been broken into sufficiently
sized pieces
final determination of which material to use.
Table 4. Ice strength properties of model ice materials.
Static
Flexural
Elastic
Compressive
Shear
coeff. of
Model ice
strength
modulus
strength
strength
Specific
material
(kPa)
flex. strn.
(kPa)
(kPa)
gravity
(iceice)
Sea ice (cold)
700800
25004500
8K12K (v)
15002100
0.91
0.450.5
Freshwater ice
5001500
15006000
10K (v)
700 (v)
0.92
0.50.7
1.53K (h)
1200 (h)
Saline-doped
2080
10001700
100275 (v)
4085 (v)
0.89
0.45
75180 (h)
45110 (h)
Urea-doped
20120
10002500
120250 (v)
3070 (v)
0.930.94
0.35
75160 (h)
3565 (h)
WARC-FG
2075
10002000
50400 (v)
1045
0.89
0.45
FGX
1590
7008000
15180
1045
0.880.91
NR
Urea, fine-grained
1545
200310
1045
NR
0.92
NR
EG/AD/S
20100
15002500
150370 (v)
NR
0.93
NR
80280 (h)
CD ice
NR
22003400
NR
NR
0.830.93
NR
GE ice
1590
10002000
1555
NR
NR
NR
MOD-ICE
1080
7003000
1282 (h)
7120
0.700.89
NR
Plaster of Paris
100200
5001000
5001000 (h)
250500 (v)
0.94
NR
SYG-ICE
2328
3900
62 (h)
7 (v)
0.90
0.50
(v) and (h) signify vertical and horizontal directions, respectively.
17