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Comparative analysis on plastic zone in deep soft rock roadway surrounding rock considering rheology or not

This study demonstrates that incorporating rock mass rheology and long-term strength into theoretical and numerical analyses is essential for accurately predicting the deformation and plastic zone of deep soft rock roadways, as neglecting these factors leads to significant overestimation of rock strength and deviation from actual engineering conditions.

Original authors: Hailong Dong, Jingyu Ran, Junhui Zou, Wei Jing, Pengwei Hao, Zhengxin Zhang

Published 2026-07-15
📖 4 min read☕ Coffee break read

Original authors: Hailong Dong, Jingyu Ran, Junhui Zou, Wei Jing, Pengwei Hao, Zhengxin Zhang

Original paper licensed under CC BY 4.0 (https://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 digging a tunnel deep underground, like a secret base for a mine. The walls of this tunnel are made of "soft rock," which is a bit like a very dense, wet sponge that doesn't just sit still; it slowly squishes and shifts over time. Scientists call this shifting behavior rheology.

For a long time, engineers building these deep tunnels had a big problem: they kept guessing wrong about how much the rock would break and how big the "cracked zone" (or plastic zone) would be around their tunnels. They were using a map that was way too optimistic.

The Big Mistake: The "Super-Rock" Fantasy

The paper explains that most engineers used to calculate tunnel safety by looking at how strong a rock sample is when you crush it right now in a lab. They treated the rock like a super-hard, unyielding brick.

The paper argues strongly against this. It says that if you ignore the fact that rock slowly creeps and weakens over time, you are basically pretending the rock is made of steel when it's actually made of clay. This leads to a dangerous overestimation of strength. If you think the rock is stronger than it really is, you might build a tunnel that looks safe on paper but actually collapses or deforms badly in real life.

The Real Deal: The "Slow-Motion" Rock

To find the truth, the researchers went to a real mine at a depth of -848 meters. They didn't just look at the rock; they watched it. They set up monitors to see how the tunnel walls moved over time.

Here is what they found:

  1. The Rock is Patient but Weak: They tested the rock in the lab. They found that while the rock could handle a huge squeeze for a short time (the peak strength was around 46.90 MPa to 81.28 MPa depending on pressure), it couldn't hold that stress forever.
  2. The "Long-Term" Limit: After the rock sat under pressure for a while, it settled into a weaker state. This is called the long-term strength. For the same rock that could handle 46.90 MPa briefly, it could only handle 28.13 MPa in the long run.
  3. The Rule: The paper states that for a tunnel to be stable, the stress on the rock must not exceed this lower, long-term limit. If it does, the rock will keep deforming forever, like a slow-motion avalanche.

The Great Comparison: Two Different Maps

The researchers used three methods to see what happens when you use the "Super-Rock" map versus the "Slow-Motion" map:

1. The Math (Theory):

  • Ignoring Rheology (The Wrong Way): When they calculated the broken zone using the strong, short-term strength, the math said the broken area was tiny—only about 0.68 meters deep from the wall. It looked like the tunnel was almost perfectly safe.
  • Considering Rheology (The Right Way): When they used the weaker, long-term strength, the math said the broken zone was huge—about 2.70 meters deep.
  • The Reality Check: When they looked at the actual tunnel with special detectors, the broken zone was between 2.7 and 3.2 meters deep. The "Slow-Motion" math was almost spot on. The "Super-Rock" math was wildly wrong.

2. The Computer Game (Simulation):
They built a digital model of the tunnel in a computer program called ABAQUS.

  • Without Rheology: The computer showed a tiny, horseshoe-shaped broken area of only 0.58 meters.
  • With Rheology: The computer showed a much larger, oval-shaped broken area of 2.12 meters.
  • The Verdict: The simulation that included the slow, creeping weakness of the rock matched the real world much better.

The Takeaway

The main finding is simple but critical: You cannot ignore time when dealing with deep soft rock.

If you design a tunnel based on how strong the rock is today, you are building on a lie. The rock will slowly give way, and your tunnel will become unstable. The paper proves that to keep a deep tunnel safe for the long haul, you must design it based on the rock's long-term strength, not its peak strength.

The authors are very sure of this because they didn't just guess; they combined lab tests, computer simulations, and real-world measurements from a mine that had already suffered severe deformation (with walls moving about 1 meter a year before they fixed it). Their new approach, which accounts for the rock's "creep," matches what actually happens underground, while the old way leads to dangerous miscalculations.

So, next time you think about a tunnel deep underground, remember: the rock isn't a statue; it's a slow-motion dancer, and if you don't dance with it, it will eventually knock you over.

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