Mode-I Fracture Behavior and Fracture Process Zone Evolution of Synthetic Ice-Bearing Loose Sediments Simulating Flammable Ice
摘要
Hydraulic fracturing is a promising approach for the efficient exploitation of flammable ice reservoirs, for which Mode-I fracture toughness (KIC) is a key indicator of fracturability. Given the similar physical–mechanical properties of flammable ice and ordinary ice, this study employs synthetic ice-bearing loose sediments as flammable ice analogs to investigate Mode-I fracture behaviors. Artificial specimens with six controlled ice saturation levels (S = 0–90%) were prepared, and notched semi-circular bend (NSCB) tests combined with digital image correlation (DIC) were conducted to examine the effects of S on fracture behaviors and fracture process zone (FPZ) evolution. A DIC-based criterion was developed to identify the FPZ initiation. Low saturation specimens exhibited brittle failure with minimal pre-peak deformation, whereas higher saturations enhanced ductility, delayed crack initiation and mitigated abrupt propagation. Both peak load and KIC followed a non-monotonic, upward-opening quadratic relation with S, showing slow initial growth, a slight drop at 30% saturation, and a rapid increase thereafter. At 90% saturation, the mean KIC reached 0.347 MPa·m1/2, 3.88 times higher than the dry value. FPZ initiation shifted from 65–70% of peak load for S ≤ 30% to 85–90% for S ≥ 50%. FPZ width stabilized near 4.8 mm beyond 30% saturation, while final length decreased at S = 30% and then increased sharply to about 9 mm (over twice the dry value) at S = 70%. These FPZ characteristics explain the transition from brittle to ductile fracture morphologies, offering quantitative insight into ice-induced toughening in flammable ice analogs.