arXiv:2610.39221
Spatial-Mode Selection for Local Mineral Absorption Spectroscopy
Qipeng Qian, Jialiang Jin, Shihao Wang, Yuntao Qian
Abstract
Absorption-band depth measures the fractional decrease in mineral reflectance below its local continuum. Recovering this feature strength for a small mineral region supports quantitative comparisons between regions, but diffraction mixes its light with the surroundings. Conventional spectral fitting can separate mean contributions; it cannot remove background photon noise already recorded. We develop a quantum-inspired measurement framework that uses spatial-mode demultiplexing (SPADE) to retain the target absorption response while reducing background acceptance before detection. The framework connects finite mineral-region geometry and reference spectra to estimation precision. A loss-dependent design condition identifies when adding SPADE exposure improves on direct imaging (DI) under fixed-response Poisson measurements with unknown scene parameters. Joint inference from initial DI observations and both mode ports estimates target depth together with an unknown, spatially shared background spectrum. In equal-time simulations that include localization uncertainty, alignment time, calibration, and detector costs, this acquisition reduces depth root-mean-square error (RMSE) by 14\%--26\% across five absorption strengths relative to all-pixel DI with the same background freedom. These results use a supplied target feature shape and geometry, with target continuum slope fitted and curvature fixed. The analysis separates optical selectivity from parameter ambiguity and acquisition cost, providing a quantitative basis for spatial-mode receiver design in local mineral spectroscopy.
AI Summary
The paper asks whether optical spatial-mode selection can improve estimation of a small mineral patch’s absorption-band depth when diffraction mixes its light with an extended background. It models finite, spatially incoherent reflecting regions using reference spectra and wavelength-dependent diffraction, comparing all-pixel direct imaging (DI) with initial DI localization followed by binary spatial-mode demultiplexing (SPADE). Both mode ports and the initial DI data are fitted jointly, including an unknown background spectrum shared across space. Fisher-information analysis separates background shot noise from ambiguity involving brightness, position, and spectral parameters. For fixed-response Poisson measurements, it specializes local optimal-design theory to give a necessary and sufficient condition for beneficial SPADE exposure: loss-adjusted SPADE information along DI’s least-distinguishable depth–nuisance direction must exceed the displaced DI information. In the calcite/dolomite example, the transmission threshold is 0.4559; transmission 0.70 permits a maximum 35.8% information increase. Complete simulated 10-second acquisitions include localization uncertainty, alignment time, calibration, and detector noise. Across five depths, 400 trials per receiver give 14–26% lower depth RMSE than DI with identical background freedom. A separate supplied-spectrum benchmark covering 24 material/geometry conditions gives a geometric-mean RMSE ratio of 0.884. The results assume supplied target geometry and feature shape, fitted continuum slope but fixed curvature, accurately executed alignment, and spatially shared background spectra. Unknown curvature substantially reduces absolute information. Spatial composition mismatch can reverse the advantage: one gradient test gives an adaptive/DI RMSE ratio of 1.88. Broadband sorter performance remains experimentally untested; quantum optimality is not established.
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