Depletion of Moderately Volatile Elements by Open-system Loss in the Early Solar Nebula

1,2,3Debanjan Sengupta,1Paul R. Estrada,1Jeffrey N. Cuzzi,4Munir Humayun
The Astrophysical Journal 932, 82 Open Access Link to Article [DOI 10.3847/1538-4357/ac6dcc]
1NASA Ames Research Center; Mail Stop 245-3, Moffett Field, CA 94035, USA
2Universities Space Research Association; 7178 Columbia Gateway Drive, Columbia, MD 21046, USA
3NASA Postdoctoral Program (NPP) Fellow
4National High Magnetic Field Laboratory and Department of Earth, Ocean and Atmospheric Science, Florida State University, 1800 E. Paul Dirac Drive, Tallahassee, FL, 32310, USA

Rocky bodies of the inner solar system display a systematic depletion of “moderately volatile elements” (MVEs) that correlates with the expected condensation temperature of their likely host materials under protoplanetary nebula conditions. In this paper, we present and test a new hypothesis in which open-system loss processes irreversibly remove vaporized MVEs from high nebula altitudes, leaving behind the more refractory solids residing much closer to the midplane. The MVEs irreversibly lost from the nebula through these open-system loss processes are then simply unavailable for condensation onto planetesimals forming even much later, after the nebula has cooled, overcoming a critical difficulty encountered by previous models of this type. We model open-system loss processes operating at high nebula altitudes, such as resulting from disk winds flowing out of the system entirely, or layered accretion directly onto the young Sun. We find that mass-loss rates higher than those found in typical T-Tauri disk winds, lasting short periods of time, are most satisfactory, pointing to multiple intense early outburst stages. Using our global nebula model, incorporating realistic particle growth and inward drift for solids, we constrain how much the MVE-depletion signature in the inner region is diluted by the drift of undepleted material from the outer nebula. We also find that a significant irreversible loss of the common rock-forming elements (Fe, Mg, Si) can occur, leading to a new explanation of another long-standing puzzle of the apparent “enhancement” in the relative abundance of highly refractory elements in chondrites.


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