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PreprintCC BY 4.0arXiv

Explicit Coleman integration over finite extensions of ℚp

Abstract

Coleman integration is an important computational ingredient of the Chabauty--Coleman method and its extensions. We extend the Balakrishnan--Tuitman algorithm to general smooth projective curves with good reduction over arbitrary finite extensions of ℚp, allowing both ramification and nontrivial residue degree. Given a suitable plane model and integral bases, we provide explicit precision bounds and an accompanying Magma implementation. As an application, a single-prime computation at p=19 over the unramified quadratic extension ℚ192/ℚ19 recovers all $35$ affine sporadic quadratic divisors on $X(s3,ns5)$ over ℚ(√5). Completeness is proved in an appendix using symmetric Chabauty and a Mordell--Weil sieve.

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BibTeX
@misc{cai2026explicit,
  title = {{Explicit Coleman integration over finite extensions of $\mathbbQ_p$}},
  author = {Yulin Cai and Timo Keller},
  howpublished = {arXiv},
  year = {2026},
  month = oct,
  doi = {10.48550/arxiv.2610.33970},
  eprint = {2610.33970},
  archivePrefix = {arXiv},
  url = {https://arxiv.org/abs/2610.33970},
  note = {CC BY 4.0},
}
RIS
TY  - UNPB
TI  - Explicit Coleman integration over finite extensions of ℚ_p
AU  - Yulin Cai
AU  - Timo Keller
PY  - 2026
DA  - 2026/10/25
PB  - arXiv
DO  - 10.48550/arxiv.2610.33970
UR  - https://arxiv.org/abs/2610.33970
AB  - Coleman integration is an important computational ingredient of the Chabauty--Coleman method and its extensions. We extend the Balakrishnan--Tuitman algorithm to general smooth projective curves with good reduction over arbitrary finite extensions of ℚ_p, allowing both ramification and nontrivial residue degree. Given a suitable plane model and integral bases, we provide explicit precision bounds and an accompanying Magma implementation. As an application, a single-prime computation at p=19 over the unramified quadratic extension ℚ_19^2/ℚ_19 recovers all $35$ affine sporadic quadratic divisors on $X(s3,ns5)$ over ℚ(√5). Completeness is proved in an appendix using symmetric Chabauty and a Mordell--Weil sieve.
ER  -