I tiakina i:
| Kaituhi matua: | |
|---|---|
| Hōputu: | Recurso digital |
| Reo: | Ingarihi |
| I whakaputaina: |
Zenodo
2026
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| Ngā marau: | |
| Urunga tuihono: | https://doi.org/10.5281/zenodo.18944179 |
| Ngā Tūtohu: |
Tāpirihia he Tūtohu
Kāore He Tūtohu, Me noho koe te mea tuatahi ki te tūtohu i tēnei pūkete!
|
Rārangi ihirangi:
- <h3><strong>FORTHCOMING UPDATE: V7 (FULL MATHEMATICAL DERIVATIONS)</strong></h3> <p><strong>NOTICE:</strong> A comprehensive technical update (<strong>V7</strong>) is currently in preparation and will be uploaded shortly to this DOI. In response to recent interest and peer-discussion, this upcoming version will provide the <strong>complete mathematical framework</strong> for the Passive Inductive Body (PIB) model, specifically:</p> <ul> <li> <p><strong>Lorentz Force Derivations:</strong> Full calculus of <span>$\vec{F}_L = q(\vec{v} \times \vec{B})$</span> applied to porous metallic aggregate cores.</p> </li> <li> <p><strong>Thermal Energetics:</strong> Quantitative modeling of eddy current dissipation and nickel vaporization thresholds at 3.88 AU.</p> </li> <li> <p><strong>Kinematic Alignment:</strong> Finalized mathematical fit between the PIB model and post-March 17, 2026, observation data (Jupiter/Eupheme flyby).</p> </li> </ul> <p><strong>Major updates in this V6 (Final Submission Alignment):</strong></p> <ul> <li><strong>Official AAS Submission:</strong> This version is identical to the manuscript submitted to the <em>Research Notes of the AAS</em> (RNAAS) under reference <strong>AAS74885</strong>.</li> <li><strong>Technical Corrections:</strong> * Updated the <strong>porosity ratio to 5:1</strong> for the metallic aggregate core, ensuring physical consistency with the Passive Inductive Body (PIB) model.</li> <ul> <li>Corrected the nomenclature for the <strong>Eupheme</strong> probe (Eupheme/60P flyby) to match current mission data.</li> </ul> <li><strong>Formatting:</strong> Clean version for publication (removed line numbers) and finalized bibliography.</li> <li><strong>Theoretical Refocusing:</strong> The interpretation remains centered on the geophysics of differentiated planetary core remnants, providing a robust natural framework for observed kinematic anomalies in 1I/'Oumuamua and 3I/Atlas.</li> <li><strong>Fragmentation Mechanisms:</strong> Clarification of thermo-mechanical stresses and the 120-degree symmetry induced by eddy current heating within the metallic core.</li> </ul> <p>This document serves as the formal baseline for the PIB model and its falsifiable predictions ahead of the <strong>March 17, 2026</strong>, observation window.</p>