Resumo Executivo
Applied orbital spectroscopy for geothermal alteration cap mapping, microseepage identification, and pipeline corridor terrain stability. We demonstrate how narrow SWIR ammonium illite signatures and thermal inertia anomalies pinpoint blind hydrothermal reservoirs without destructive surface disruption.
Principais Descobertas Metodológicas
Ammonium illite absorption at 2.120 µm reliably marks high-temperature boiling zones and geothermal upflow channels.
Surface mineral alteration induced by reducing hydrocarbon microseepage exhibits detectable bleaching of hematite and anomalous clay recrystallisation.
Diurnal thermal inertia modeling maps subterranean void formations and moisture emergence along 200+ km pipeline corridors.
Física e Metodologia de Inversão
Combines multi-temporal shortwave infrared absorption mapping with diurnal day/night thermal infrared pairs normalized by broadband surface albedo to isolate subsurface thermal conductivity anomalies.
Janelas Espectrais Diagnósticas
| Band Regime | Wavelength Range | Physical / Chemical Feature |
|---|---|---|
| SWIR-2 | 2.11 – 2.13 µm | NH4+ ammonium illite substitution diagnostic envelope |
| TIR | 8.00 – 12.00 µm | Diurnal surface thermal inertia and silica emissivity variation |
Citação e Identificador de Objeto Digital (DOI)
@techreport{axine_the_spectral_advantage_in_energy_2026,
author = {Axine Labs Research},
title = {The Spectral Advantage in Energy},
institution = {Axine Labs Technical Whitepaper Series},
number = {2},
year = {2026},
doi = {pending (Zenodo, 2026)},
url = {https://axinelabs.com/papers/the-spectral-advantage-in-energy}
}