geodepoly 0.1.2

Series-reversion polynomial solver with bootstrap and deflation

geodepoly — Series-Reversion Polynomial Solver (MVP)

geodepoly is a small Python package that finds all roots of a complex polynomial using a shift–recenter + truncated series reversion with optional bootstrap iterations, and only falls back to classical iterations when strictly necessary.

This implements the impact-first MVP discussed:

• Compositional inverse (via Lagrange inversion in coefficient form) around a local recentering point to obtain an analytic series for a nearby root.
• Bootstrap: update the center by the series estimate and re-expand (typically a few steps).
• Deflation: synthetic division to peel off roots one-by-one.
• Safe fallbacks: Halley or Durand–Kerner if series degenerates (multiple root / tiny derivative).

Note: This is a minimal working scaffold you can publish and iterate on. It is self-contained (numpy optional), tested, and provides a SymPy hook.

Install (editable)

pip install -e .

Quickstart

from geodepoly import series_solve_all

# Coefficients lowest-degree first: a0 + a1 x + ... + aN x^N
coeffs = [1, 0, -7, 6]  # 1 + 0 x - 7 x^2 + 6 x^3 = 0  (roots near 1, 2, 3 after rescale)
roots = series_solve_all(coeffs, verbose=True)
print(roots)

CLI

python -m geodepoly.scripts.benchmark --deg 8 --seed 123 --trials 100

API

• series_solve_all(coeffs, max_order=32, boots=3, tol=1e-12, max_deflation=None, verbose=False)
• series_one_root(coeffs, center=None, max_order=32, boots=3, tol=1e-14)
• sympy_solve(poly) — lightweight SymPy integration (if SymPy is installed).

How it works (short)

Let p(x) be a degree-n polynomial. We recenter around x = μ and expand q(y) = p(μ + y) = a0 + a1 y + a2 y^2 + .... If a1 ≠ 0, solve q(y)=0 by compositional inversion of F(y) = y + β2 y^2 + β3 y^3 + ... with βk = ak/a1. Lagrange inversion gives the inverse coefficients {g_m} of F, and the nearby root is y ≈ Σ_{m≥1} g_m t^m, with t = -a0/a1. Update μ ← μ + y (bootstrap) and repeat a few times; then deflate and continue.

This repo implements the coefficient formula g_m = (1/m) * [y^{m-1}] (1 / F'(y))^m using truncated series arithmetic. No derivatives of p beyond a1 = q'(0) are used.

Caveats

• Multiple or nearly-multiple roots are ill-conditioned for any method. We switch to a guarded Durand–Kerner step when |a1| is tiny.
• Convergence radius depends on the local analytic structure; bootstrap helps.

License

MIT

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New in this build

Friendlier API

from geodepoly import solve_poly, solve_all, solve_one
roots = solve_poly(coeffs, method="hybrid", resum="pade")

Methods: hybrid (series seeds + Aberth), aberth, dk, numpy (companion).
Resummation: None, "pade", "borel", "borel-pade".

SymPy integration

from geodepoly.sympy_plugin import sympy_solve
roots = sympy_solve(x**8 - 3*x + 1, method="hybrid", resum="pade")

Mathematica / Maple bridge (JSON CLI)

python bridges/geodepoly_cli.py <<'JSON'
{"coeffs":[-6,11,-6,1],"kwargs":{"method":"hybrid","resum":"pade"}}
JSON

In Mathematica:

payload = ExportString[<|"coeffs"->{-6,11,-6,1},"kwargs"-><|"method"->"hybrid","resum"->"pade"|>|>,"JSON"];
res = RunProcess[{"python","bridges/geodepoly_cli.py"}, "StandardInput"->payload, "StandardOutput"];
ImportString[res, "JSON"]

Benchmarks

python -m geodepoly.scripts.bench_compare --deg 8 --trials 50 --out bench_deg8.csv

Paper skeleton

See paper/GeodePoly_MVP.md.

Hyper-Catalan API (S[t2,t3,...])

Utilities based on the paper's multivariate series:

from geodepoly import evaluate_hyper_catalan, evaluate_quadratic_slice, catalan_number

# Quadratic slice (Catalan series)
t2 = 0.05
alpha_approx = evaluate_quadratic_slice(t2, max_weight=20)
catalan_series = sum(catalan_number(n) * (t2**n) for n in range(12))

# Multivariate evaluation (truncated by weighted degree)
alpha_multi = evaluate_hyper_catalan({2: 0.05, 3: 0.01}, max_weight=12)

See docs/paper_guide.md for how the paper maps onto the codebase.