Clarify loading histories and relative metrics
Browse filesAdd undergraduate-friendly loading-history rationale, recommended scale-free metrics, fixed reference denominators, and the MAPE caveat. Data and splits are unchanged.
README.md
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@@ -43,6 +43,58 @@ Current trajectory accounting:
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| Prospective sealed test | 128 | Published after model freeze; never used for training or selection |
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| **Total** | **3,788** | Complete histories, not exchangeable independent experiments |
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## Releases
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- **T2 v1:** 1,008 proportional cyclic J2 trajectories for loading-memory
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| Prospective sealed test | 128 | Published after model freeze; never used for training or selection |
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| **Total** | **3,788** | Complete histories, not exchangeable independent experiments |
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## What is a loading history, and why does it matter?
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A loading history is the ordered sequence of deformation applied to a material.
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For an elastic spring, only the present deformation matters. For an
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elastoplastic metal, the route matters as well: loading, unloading, reversing,
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rotating the loading direction or adding a mean strain changes the material's
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internal state. Two specimens can therefore arrive at the same current strain
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with different stresses because they arrived there by different routes.
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This dataset varies the history deliberately rather than merely sampling more
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points on one curve:
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| History variation | Question being tested |
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| Proportional and reversed cycles | Can the model reproduce yielding, unloading and the Bauschinger effect? |
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| Non-proportional and rotating multiaxial paths | Can it track changing stress directions and coupled material memory? |
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| Nested minor loops and non-periodic sequences | Can it remember partial unload/reload events instead of resetting its state? |
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| Amplitude and mean shifts | Can it extrapolate when the load becomes larger or biased to one side? |
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| 100--200-cycle histories | Does a small state error accumulate into long-term drift? |
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| Matched coarse/fine discretizations | Is the prediction tied to the physical path or to a particular step size? |
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| Material-parameter variation | Can one conditioned model represent a family of materials rather than one fixed curve? |
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The scientific object is therefore not an isolated stress value. It is the
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mapping from **material parameters + ordered loading history + current internal
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state** to the next stress and state. Randomly shuffling time steps or mixing
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related resolution groups across data roles would destroy this meaning.
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## Recommended evaluation metrics
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Report absolute stress RMSE in MPa together with a scale-free metric. MPa is
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needed for engineering interpretation; a relative metric makes results easier
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to compare across cohorts and stress levels.
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- **Relative L2 error (%)** = `||stress_pred - stress_ref||2 / ||stress_ref||2 × 100`.
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This is the preferred scale-free trajectory/state metric for signed cyclic
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stresses.
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- **Yield-normalized RMSE (%)** = `RMSE / reference_yield_stress × 100`.
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This answers how large the average error is relative to the 280 MPa reference
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yield stress used by the sealed protocol.
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- **R2** is useful as a supplementary global fit indicator, but should not
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replace an engineering error in MPa.
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- **MAPE is not recommended** because cyclic stress repeatedly crosses zero;
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division by values near zero can make an accurate prediction look arbitrarily
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poor.
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For the sealed reference data, the stress RMS scales are 359.540 MPa for global
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path OOD, 91.411 MPa for 150/200-cycle histories, 371.687 MPa for amplitude and
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mean shifts, and 206.814 MPa over all 128 trajectories. These denominators are
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published so every model can be compared under the same convention. Model
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scores remain in the model repository to keep this page focused on the data and
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evaluation contract.
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## Releases
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- **T2 v1:** 1,008 proportional cyclic J2 trajectories for loading-memory
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