Crack propagation in saline ice (a model sea ice) is investigated in t
his study in an attempt to understand the processes of crack growth at
one loading rate and two temperatures. As has been previously observe
d in cold sea ice and warm or cold fresh-water ice, crack growth occur
s in initiation/arrest increments. The energetic stability criteria of
crack growth are examined in saline ice and crack growth is character
ized in terms of the fracture-resistance parameter K-R. This paper off
ers the development of a new fracture geometry capable of sustained st
able crack growth and the presentation of fracture-resistance curves f
or saline ice at -25 degrees and -15 degrees C. The important findings
of this paper are that: (i) in warm saline ice, extensive local crack
-tip damage is accompanied by a limited amount of slow, stable crack e
xtension; (ii) fracture in cold saline ice is characterized by locally
negative K-R behavior; and (iii) fracture in cold or warm saline ice
is characterized by globally positive K-R curve behavior.