Peridynamic modeling of the crack velocity dependence via an incubation time fracture criterion

This study utilizes a peridynamic approach with an incubation time fracture criterion to model Ravi-Chandar and Knauss's experiments on Homalite-100, revealing that variations in the Mode-I stress intensity factor at constant crack velocities and the onset of micro-branching at higher velocities provide new insights into the nature of crack-velocity dependence in dynamic fracture.

Original authors: M. Ignatev, P. Weißgraeber, E. Oterkus, L. Radtke

Published 2026-05-29
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Original authors: M. Ignatev, P. Weißgraeber, E. Oterkus, L. Radtke

Original paper licensed under CC BY 4.0 (http://creativecommons.org/licenses/by/4.0/). This is an AI-generated explanation of the paper below. It is not written or endorsed by the authors. For technical accuracy, refer to the original paper. Read full disclaimer

Imagine you are watching a crack race across a piece of brittle plastic, like a sheet of Homalite-100. In the old days of physics, scientists thought that if you knew how fast the crack was moving, you could calculate exactly how much "stress" (or pressure) was pushing it forward. It was like thinking that if a car is going 60 mph, the engine must be producing exactly 100 horsepower. Simple, right?

But experiments in the 1980s showed this wasn't true. Sometimes, the crack was moving at the exact same speed, but the pressure pushing it was wildly different. It was as if two cars were both doing 60 mph, but one had a tiny engine and the other had a rocket booster. Scientists were puzzled: Why does the same speed have different "pushes"?

This paper is a detective story where the authors use a new kind of computer simulation to solve this mystery.

The Detective Tool: Peridynamics

Most computer models of cracks are like a chain of dominoes. If one domino falls, it pushes the next one. But if a domino is missing (a crack), the chain breaks, and the math gets stuck.

The authors used a method called Peridynamics. Think of this not as a chain, but as a swarm of bees. Every bee can talk to every other bee within a certain distance, even if there is a gap in the middle. If a bee flies away (a crack forms), the other bees just stop talking to it, but the rest of the swarm keeps moving perfectly fine. This allows the computer to handle breaking and cracking without getting confused.

The Secret Ingredient: The "Incubation Time"

The real breakthrough in this paper is how they decided when a crack should actually break.

In the old way, if the pressure got high enough, the material broke instantly. But the authors used a rule called the Incubation Time Criterion.

Imagine you are trying to snap a dry twig. You don't just pull and it snaps instantly. You pull, hold it there for a split second while the fibers stretch and weaken, and then it snaps. That split second is the "incubation time."

The authors programmed their computer swarm to remember the last few microseconds of pressure. The material only breaks if the average pressure over that short "incubation" period is high enough. This accounts for the fact that materials need a tiny bit of time to "decide" to break.

What They Found

They ran simulations of the plastic plates being pulled apart, just like the real experiments. Here is what they discovered:

  1. The Speed vs. Pressure Puzzle: Just like the real experiments, their computer showed that for the same crack speed, the pressure (Stress Intensity Factor) wasn't a single number. It was a range. Sometimes it was low, sometimes high.
  2. The "Micro-Branching" Effect: When the crack moved slowly, it went straight. But when it sped up (over 400 meters per second), it started to get jittery. It began to sprout tiny, microscopic side-cracks, like a tree branch splitting into twigs.
    • The Analogy: Imagine a runner sprinting. At a steady jog, they run in a straight line. But when they sprint at top speed, they start to wobble and zigzag slightly to maintain balance.
    • The Result: These tiny "wobbles" (micro-branches) caused the pressure reading to jump up and down wildly. This explained why the pressure wasn't unique for a given speed; the crack was physically changing its shape slightly as it raced.

The Conclusion

The paper concludes that the reason we see different pressure values for the same crack speed is because the crack isn't a smooth, perfect line. It's a chaotic, living thing that fluctuates.

  • At lower speeds: The crack is steady, and the pressure is relatively stable.
  • At higher speeds: The crack starts to "micro-branch" (sprout tiny side-cracks). This chaos causes the pressure to bounce around, creating the scatter seen in the experiments.

By using this "swarm of bees" (Peridynamics) combined with the "waiting period" (Incubation Time), the authors successfully recreated the messy, non-unique relationship between crack speed and pressure that real-world experiments had shown for decades. They proved that the "noise" in the data isn't a mistake; it's a real physical feature of how fast-moving cracks behave.

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