SPHEREx Pre-Perihelion Mapping of $\mathrm{H_2O}$, $\mathrm{CO_2}$, and $\mathrm{CO}$ in Interstellar Object 3I/ATLAS
Carey M. Lisse, Yoonsoo P. Bach, Brendan P. Crill, Phil M. Korngut, Ari J. Cukierman, Sean A. Bryan, Asantha Cooray, C. Darren Dowell, Michael W. Werner, Joseph L. Hora, Zafar Rustamkulov, Jeong-Eun Lee, Bumhoo Lim, Y. R. Fernandez, Volker Tolls, W. T. Reach, O. Doré, Michael Zemcov, James J. Bock, Yun-Ting Cheng, C. Champagne, Seungwon Choi, M. Connelley, J. P. Emery, Spencer Everett, Andreas L. Faisst, Jooyeon Geem, Howard Hui, Masateru Ishiguro, Sunho Jin, Hangbin Jo, Max Mahlke, Daniel C. Masters, Gary J. Melnick, Chi H. Nguyen, Roberta Paladini, M. L. Sitko, Yujin Yang
TL;DR
This study leverages SPHEREx's $R=40$–$130$ spectrophotometry over $0.7$–$5\,\mu$m to map H$_2$O, CO$_2$, and CO in interstellar object 3I/ATLAS during its pre-perihelion passage. The analysis detects robust water emission at 2.7–2.8 μm, a dominant CO$_2$-emission shell extending to at least several 10^5 km, and tentative CO/^{13}CO$_2$ signals, yielding gas production rates of $Q_{\mathrm{H_2O}}=3.2\times10^{26}$ s$^{-1}$, $Q_{^{12}\mathrm{CO_2}}=1.6\times10^{27}$ s$^{-1}$, $Q_{^{13}\mathrm{CO_2}}=1.3\times10^{25}$ s$^{-1}$, and $Q_{\mathrm{CO}}=1.0\times10^{26}$ s$^{-1}$. A 1.0–1.5 μm continuum image is unresolved, while the 1.5–4.0 μm continuum shows water-ice absorption features; radial profiles indicate CO$_2$ outflow declines faster than $1/\rho$, consistent with acceleration or destruction. The nucleus remains unresolved with an upper size limit of about $2.5$ km, and 3I displays comet-like activity reminiscent of 103P/Hartley 2, suggesting strong thermal processing prior to ejection and marking ISOs as often thermally evolved prior to interstellar transit. These findings support a picture in which ISOs are not uniformly primitive but instead exhibit a spectrum of thermal histories, with 3I lying toward the end of the active lifetime and CO$_2$-rich, CO-poor compositions. The results motivate population-wide SPHEREx ISO studies to test the prevalence of thermal processing in the ISO population and to refine models of ISO origin and evolution.
Abstract
From 01- to 15-Aug-2025 UT, the SPHEREx spacecraft observed interstellar object 3I/ATLAS. Using $R = 40$-$130$ spectrophotometry at $λ= 0.7$-$5μ$m, light curves, spectra, and imaging of 3I were obtained. From these, robust detections of water gas emission at $2.7$-$2.8\,μ$m and CO$_2$ gas at $4.23$-$4.27\,μ$m plus tentative detections of $^{13}$CO$_2$ and CO gas were found. A slightly extended H$_2$O coma was detected, and a huge CO$_2$ atmosphere extending out to at least $4.2\times10^{5}\,$km was discovered. Gas production rates for H$_2$O, $^{12}$CO$_2$, $^{13}$CO$_2$, and CO were $Q_{\mathrm{gas}} = 3.2\times10^{26} \pm 20\%$, $1.6\times10^{27} \pm 10\%$, $1.3\times10^{25} \pm 25\%$, and $1.0\times10^{26} \pm 25\%$, respectively. Co-addition of all $λ= 1.0$-$1.5\,μ$m scattered light continuum images produced a high SNR image consistent with an unresolved source. The scattered light lightcurve showed $\lesssim 15\%$ variability over the observation period. The absolute brightness of 3I at $1.0$-$1.5\,μ$m is consistent with a $< 2.5\,$km radius nucleus surrounded by a 100 times brighter coma. The $1.5$-$4.0\,μ$m continuum structure shows a strong feature commensurate with water ice absorption seen in KBOs and distant comets. The observed cometary behavior of 3I, including its preponderance of CO$_2$ emission, lack of CO output, small size, and predominance of large icy chunks of material in a flux-dominant coma is reminiscent of the behavior of short period comet 103P/Hartley 2, target of the NASA Deep Impact extended mission in 2010 and a ``hyperactive comet'' near the end of its outgassing lifetime. This correspondence places 3I closer to barely- or non-active 1I/Oumuamua than primitive, ice rich 2I/Borisov, suggesting that ISOs are often highly thermally processed before ejection into the ISM.
