| """Streamlit app (Hugging Face Spaces): shear-wave velocity prediction from a |
| phase-velocity dispersion curve with the phase-only DispFormer trained on |
| OpenSWI-shallow. |
| |
| Self-contained: model code, checkpoint, and assets live in this folder. |
| Run locally with: |
| streamlit run app.py |
| """ |
| import io |
| import os |
| import sys |
|
|
| import streamlit as st |
| from streamlit import runtime |
|
|
| if not runtime.exists(): |
| |
| |
| port = os.environ.get("PORT", "7860") |
| os.execvp(sys.executable, [ |
| sys.executable, "-m", "streamlit", "run", |
| os.path.abspath(__file__), |
| "--server.port", port, |
| "--server.address", "0.0.0.0", |
| "--server.headless", "true", |
| "--server.enableCORS", "false", |
| "--server.enableXsrfProtection", "false"]) |
|
|
| import numpy as np |
| import pandas as pd |
| import matplotlib.pyplot as plt |
| import torch |
|
|
| from model import DispersionTransformerAblate |
|
|
| APP_DIR = os.path.dirname(os.path.abspath(__file__)) |
|
|
| |
| CKPT = os.path.join(APP_DIR, "checkpoints", "best_model.pth") |
| PERIOD = np.load(os.path.join(APP_DIR, "assets/period_grid.npy")) |
| DEPTH = np.load(os.path.join(APP_DIR, "assets/depth_grid.npy")) |
| C1, C3 = 1 / 3, 1 / 2 |
|
|
| st.set_page_config(page_title="Vs from dispersion curve", page_icon="🌍", |
| layout="wide") |
|
|
|
|
| @st.cache_resource |
| def load_model(): |
| device = "cuda:0" if torch.cuda.is_available() else "cpu" |
| model = DispersionTransformerAblate( |
| model_dim=128, num_heads=8, num_layers=3, output_dim=72, |
| scale_factor=4.5, local=False, decoder="depthq", |
| depth_values=DEPTH, decoder_layers=1).to(device) |
| model.load_state_dict(torch.load(CKPT, map_location=device)) |
| model.train() |
| return model, device |
|
|
|
|
| @st.cache_data |
| def load_examples(): |
| d = np.load(os.path.join(APP_DIR, "assets/examples.npz")) |
| return d["curves"], d["profiles"], list(d["names"]) |
|
|
|
|
| def snap_to_grid(periods, velocities): |
| """Place picks on the fixed 100-period grid (nearest period; picks that |
| share a grid node are averaged). Returns (curve on grid, n_used, n_out).""" |
| grid = np.full(len(PERIOD), -1.0, dtype=np.float32) |
| counts = np.zeros(len(PERIOD)) |
| sums = np.zeros(len(PERIOD)) |
| n_out = 0 |
| for T, c in zip(periods, velocities): |
| if not (PERIOD.min() <= T <= PERIOD.max()) or c <= 0: |
| n_out += 1 |
| continue |
| j = int(np.abs(PERIOD - T).argmin()) |
| sums[j] += c |
| counts[j] += 1 |
| used = counts > 0 |
| grid[used] = (sums[used] / counts[used]).astype(np.float32) |
| return grid, int(used.sum()), n_out |
|
|
|
|
| def usable_depth_range(curve): |
| """Constrained depth interval from the wavelength heuristic.""" |
| valid = curve > 0 |
| if not valid.any(): |
| return 0, len(DEPTH) |
| p, v = PERIOD[valid], curve[valid] |
| dmin = C1 * p.min() * v[p.argmin()] |
| dmax = C3 * p.max() * v[p.argmax()] |
| lo = max(0, int(np.abs(DEPTH - dmin).argmin()) - 1) |
| hi = min(len(DEPTH), int(np.abs(DEPTH - dmax).argmin()) + 1) |
| return lo, hi |
|
|
|
|
| def predict(curve): |
| model, device = load_model() |
| x = np.full((1, 3, len(PERIOD)), -1.0, dtype=np.float32) |
| x[0, 0] = PERIOD |
| x[0, 1] = curve |
| x = torch.from_numpy(x).to(device) |
| mask = (x[:, 1] == -1) & (x[:, 2] == -1) |
| with torch.no_grad(): |
| out = model(x, mask) |
| return out[0, :len(DEPTH)].cpu().numpy() |
|
|
|
|
| def parse_table(df, period_col, vel_col, freq_input, vel_unit): |
| p = pd.to_numeric(df[period_col], errors="coerce").to_numpy(dtype=float) |
| v = pd.to_numeric(df[vel_col], errors="coerce").to_numpy(dtype=float) |
| ok = np.isfinite(p) & np.isfinite(v) |
| p, v = p[ok], v[ok] |
| if freq_input: |
| p = np.where(p > 0, 1.0 / p, np.nan) |
| v = v[np.isfinite(p)] |
| p = p[np.isfinite(p)] |
| if vel_unit == "m/s": |
| v = v / 1000.0 |
| return p, v |
|
|
|
|
| |
| st.title("Shear-wave velocity from a phase-velocity dispersion curve") |
| st.markdown( |
| "Inverts a fundamental-mode Rayleigh **phase-velocity** curve (the SASW/MASW " |
| "observable) for a 70-layer 1-D Vs profile in one forward pass — no initial " |
| "model. Proposed physically-coded transformer encoder–decoder (2.44 M params: " |
| "period tokens in, depth-query tokens out) trained on **OpenSWI-shallow** " |
| "(22 M curve/profile pairs).") |
|
|
| with st.sidebar: |
| st.header("Input") |
| source = st.radio("Curve source", |
| ["Example from test data", "Upload CSV", "Paste values"]) |
| st.divider() |
| st.header("Site scale") |
| st.caption("The physics is scale-invariant: measured periods are multiplied " |
| "by k to enter the model's 0.2–10 s band, and output depths are " |
| "divided by k. Velocities are never rescaled.") |
| preset = st.selectbox( |
| "Scale factor k", |
| ["Native (k = 1): 0.2–10 s, 0–2.76 km", |
| "Engineering ≈ 30 m (k = 100): 2 ms–0.1 s, 0–27.6 m", |
| "Custom k"]) |
| if preset.startswith("Custom"): |
| k = float(st.number_input("k (period multiplier)", min_value=1.0, |
| max_value=10000.0, value=100.0, step=1.0)) |
| elif preset.startswith("Engineering"): |
| k = 100.0 |
| else: |
| k = 1.0 |
| if source == "Example from test data" and k != 1.0: |
| st.info("Examples are native-scale; k is applied to uploaded/pasted " |
| "curves only.") |
| k = 1.0 |
| st.caption( |
| f"Accepted measured band at k = {k:g}: " |
| f"{PERIOD.min()/k:.4g}–{PERIOD.max()/k:.4g} s " |
| f"({k/PERIOD.max():.3g}–{k/PERIOD.min():.3g} Hz). " |
| f"Output depth range: {DEPTH.max()/k*1000:.3g} m." |
| if k > 1 else |
| f"Model grid: {len(PERIOD)} periods, {PERIOD.min():.1f}–{PERIOD.max():.0f} s. " |
| f"Output: {len(DEPTH)} layers, 0–{DEPTH.max():.2f} km (40 m spacing).") |
| st.divider() |
| st.caption("Picks are snapped to the nearest grid period; the model accepts " |
| "gaps and band-limited curves natively. Velocity support " |
| "≈ 0.3–4.5 km/s at any scale (velocities are not rescaled).") |
|
|
| |
| DEPTH_DISP = DEPTH / k |
| PERIOD_DISP = PERIOD / k |
| DEPTH_IN_M = DEPTH_DISP.max() < 0.2 |
| DUNIT = "m" if DEPTH_IN_M else "km" |
| DSC = 1000.0 if DEPTH_IN_M else 1.0 |
|
|
| curve = None |
| true_vs = None |
|
|
| if source == "Example from test data": |
| curves, profiles, names = load_examples() |
| labels = [f"{n} #{i}" for i, n in enumerate(names)] |
| pick = st.sidebar.selectbox("Example", labels) |
| idx = labels.index(pick) |
| curve = curves[idx].copy() |
| true_vs = profiles[idx] |
| lo_p, hi_p = st.sidebar.slider( |
| "Restrict period band (s) — simulates a band-limited survey", |
| float(PERIOD.min()), float(PERIOD.max()), |
| (float(PERIOD.min()), float(PERIOD.max()))) |
| curve[(PERIOD < lo_p) | (PERIOD > hi_p)] = -1.0 |
|
|
| elif source == "Upload CSV": |
| st.sidebar.markdown("CSV with one column of period (s) **or** frequency (Hz), " |
| "and one of phase velocity.") |
| up = st.sidebar.file_uploader("CSV file", type=["csv", "txt"]) |
| freq_input = st.sidebar.checkbox("First column is frequency (Hz)", False) |
| vel_unit = st.sidebar.radio("Velocity unit", ["km/s", "m/s"], horizontal=True) |
| if up is not None: |
| df = pd.read_csv(up) |
| cols = list(df.columns) |
| c1_, c2_ = st.sidebar.selectbox("Period/frequency column", cols, index=0), \ |
| st.sidebar.selectbox("Velocity column", cols, |
| index=min(1, len(cols) - 1)) |
| p, v = parse_table(df, c1_, c2_, freq_input, vel_unit) |
| curve, n_used, n_out = snap_to_grid(p * k, v) |
| st.sidebar.success( |
| f"{n_used} grid periods filled" |
| + (f" · {n_out} picks outside the accepted band dropped" if n_out else "")) |
|
|
| else: |
| st.sidebar.markdown("One `period_s, velocity_km_s` pair per line:") |
| default = "\n".join(f"{t:.3f}, {c:.3f}" for t, c in |
| zip(PERIOD[::12], load_examples()[0][0][::12]) |
| if c > 0) |
| txt = st.sidebar.text_area("Values", default, height=200) |
| try: |
| rows = [list(map(float, ln.replace(",", " ").split())) |
| for ln in txt.strip().splitlines() if ln.strip()] |
| arr = np.array([r[:2] for r in rows if len(r) >= 2]) |
| curve, n_used, n_out = snap_to_grid(arr[:, 0] * k, arr[:, 1]) |
| st.sidebar.success(f"{n_used} grid periods filled") |
| except Exception as e: |
| st.sidebar.error(f"Could not parse input: {e}") |
|
|
| |
| if curve is None or (curve > 0).sum() == 0: |
| st.info("Provide a dispersion curve in the sidebar to run the inversion.") |
| st.stop() |
|
|
| if (curve > 0).sum() < 5: |
| st.warning("Very few valid picks — the prediction will be poorly constrained.") |
|
|
| vmin_meas = float(curve[curve > 0].min()) |
| if vmin_meas < 0.3: |
| st.warning( |
| f"Lowest measured phase velocity is {vmin_meas*1000:.0f} m/s — below the " |
| "training support (≈ 0.3–4.5 km/s, unchanged by the scale factor). " |
| "Typical of soft-soil sites; predictions there are extrapolation and the " |
| "recommended path is fine-tuning on engineering-scale synthetics " |
| "(paper3 §6.2).") |
|
|
| vs = predict(curve) |
| lo, hi = usable_depth_range(curve) |
|
|
| col1, col2 = st.columns(2) |
| valid = curve > 0 |
|
|
| with col1: |
| fig, ax = plt.subplots(figsize=(5.5, 4)) |
| ax.plot(PERIOD_DISP[valid], curve[valid], "o-", ms=3.5, lw=1.2, color="#1f77b4") |
| ax.set_xscale("log") |
| ax.set_xlabel("period (s)" + (f" [measured; k = {k:g}]" if k != 1 else "")) |
| ax.set_ylabel("phase velocity (km/s)") |
| ax.set_title(f"Input curve ({int(valid.sum())} of {len(PERIOD)} grid periods)") |
| ax.grid(alpha=0.3) |
| st.pyplot(fig, use_container_width=True) |
| plt.close(fig) |
|
|
| with col2: |
| fig, ax = plt.subplots(figsize=(5.5, 4)) |
| D = DEPTH_DISP * DSC |
| if true_vs is not None: |
| ax.step(true_vs, D, where="mid", color="k", lw=1.6, label="true Vs") |
| ax.step(vs, D, where="mid", color="#d62728", lw=1.6, label="predicted Vs") |
| if lo > 0: |
| ax.axhspan(0, D[lo], color="gray", alpha=0.15) |
| if hi < len(DEPTH): |
| ax.axhspan(D[hi - 1], D[-1], color="gray", alpha=0.15) |
| ax.invert_yaxis() |
| ax.set_xlabel("Vs (km/s)") |
| ax.set_ylabel(f"depth ({DUNIT})") |
| ax.set_title("Predicted 1-D Vs profile") |
| ax.legend(fontsize=8) |
| ax.grid(alpha=0.3) |
| st.pyplot(fig, use_container_width=True) |
| plt.close(fig) |
|
|
| st.caption( |
| f"Gray bands mark depths outside the range the input band physically " |
| f"constrains (wavelength heuristic: ≈ ⅓·λ_min to ½·λ_max → " |
| f"{DEPTH_DISP[lo]*DSC:.2f}–{DEPTH_DISP[min(hi, len(DEPTH)) - 1]*DSC:.2f} " |
| f"{DUNIT} here); treat the profile there as extrapolation." |
| + (f" Scale factor k = {k:g}: periods ×{k:g} into the model, depths ÷{k:g} " |
| "on output; velocities unchanged." if k != 1 else "")) |
|
|
| if true_vs is not None: |
| err = vs - true_vs |
| m1, m2, m3 = st.columns(3) |
| m1.metric("RMSE vs truth", f"{np.sqrt((err ** 2).mean()):.3f} km/s") |
| m2.metric("MAE vs truth", f"{np.abs(err).mean():.3f} km/s") |
| m3.metric("MAPE vs truth", f"{(np.abs(err) / true_vs).mean() * 100:.1f} %") |
|
|
| out_df = pd.DataFrame({f"depth_{DUNIT}": DEPTH_DISP * DSC, "vs_km_s": vs, |
| "constrained": [(lo <= i < hi) for i in range(len(DEPTH))]}) |
| buf = io.StringIO() |
| out_df.to_csv(buf, index=False) |
| st.download_button("Download predicted profile (CSV)", buf.getvalue(), |
| file_name="predicted_vs_profile.csv", mime="text/csv") |
|
|
| with st.expander("Model & protocol details"): |
| st.markdown( |
| "- **Model:** physically-coded encoder–decoder (paper3): each dispersion " |
| "pick is a token carrying its physical period; each output depth is a query " |
| "token carrying its physical depth, reading the period tokens by masked " |
| "cross-attention — band-limited and gappy curves are handled natively " |
| "(no interpolation), and its learned attention reproduces the classical " |
| "λ/3 sensitivity rule (paper3, Fig. 7).\n" |
| "- **Checkpoint:** v4 finalist (valid masked MSE 0.0216 (km/s)²); test " |
| "accuracy 0.151 km/s full-profile RMSE / 6.0 % MAPE / R² 0.949 on 50 k " |
| "held-out samples; Long Beach field data 38 m/s MAE vs the tomographic " |
| "reference (5,297 real curves).\n" |
| "- **Scope:** trained on 0.2–10 s periods, 0–2.76 km depth, Vs ≈ 0.3–4.5 km/s " |
| "(OpenSWI-shallow). Curves outside this envelope — e.g. soft-soil sites with " |
| "Vs < 0.3 km/s — are out of distribution.\n" |
| "- **Site scale factor k:** the elastodynamic problem is scale-invariant, so " |
| "a high-frequency engineering curve is inverted by stretching its periods " |
| "×k into the training band and shrinking the output depths ÷k (e.g. k = 100 " |
| "→ 70 layers over 0.4–27.6 m at 0.4 m spacing). Velocities are never " |
| "rescaled — the ≈ 0.3–4.5 km/s support applies at every scale; see paper3 §6.2.") |
|
|