Production, Transport, and Destruction of Dust in the Kuiper Belt: The Effects of Refractory and Volatile Grain Compositions

The Venetia Burney Student Dust Counter (SDC) on board the New Horizons spacecraft measures the spatial and size distributions of dust along its trajectory. Models based on early SDC measurements predicted a peak dust number density at a heliocentric distance of ∼40 au, followed by a rapid decline....

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Main Authors: Thomas Corbett, Alex Doner, Mihály Horányi, Pontus Brandt, Will Grundy, Carey M. Lisse, Joel Parker, Lowell Peltier, Andrew R. Poppe, Kelsi N. Singer, S. Alan Stern, Anne J. Verbiscer
Format: Article
Language:English
Published: IOP Publishing 2025-01-01
Series:The Astrophysical Journal Letters
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Online Access:https://doi.org/10.3847/2041-8213/adab75
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author Thomas Corbett
Alex Doner
Mihály Horányi
Pontus Brandt
Will Grundy
Carey M. Lisse
Joel Parker
Lowell Peltier
Andrew R. Poppe
Kelsi N. Singer
S. Alan Stern
Anne J. Verbiscer
author_facet Thomas Corbett
Alex Doner
Mihály Horányi
Pontus Brandt
Will Grundy
Carey M. Lisse
Joel Parker
Lowell Peltier
Andrew R. Poppe
Kelsi N. Singer
S. Alan Stern
Anne J. Verbiscer
author_sort Thomas Corbett
collection DOAJ
description The Venetia Burney Student Dust Counter (SDC) on board the New Horizons spacecraft measures the spatial and size distributions of dust along its trajectory. Models based on early SDC measurements predicted a peak dust number density at a heliocentric distance of ∼40 au, followed by a rapid decline. Instead, SDC observed dust fluxes 2–3 times higher than predicted between 40 and 60 au. One potential explanation for this discrepancy is that SDC may be encountering icy grains with different dynamical behavior than previously modeled silicate grains. Due to ultraviolet photosputtering, water–ice grains rapidly erode and migrate outward, significantly contributing to the measured dust number densities only at distances ≳40 au. We present a model of silicate and ice grain dynamics in the outer solar system, considering gravitational and radiation forces and grain erosion. Using SDC data, we estimate that the mass production rate of ice grains between 0.1 and 10 μ m in the Kuiper Belt (KB) would need to be 20–70 times higher than that of silicate grains. However, KB grains are expected to be refractory/volatile mixtures rather than pure silicate or ice. Thus, we briefly explore simple models of more realistic mixed-grain cases to further gauge the effects of grain composition on the equilibrium dust distribution. Future SDC measurements at greater distances will test the model predictions and further constrain silicate and ice grain production rates in the KB.
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spelling doaj-art-ce96a1778a5643c49fa819854972c12b2025-01-30T18:15:10ZengIOP PublishingThe Astrophysical Journal Letters2041-82052025-01-019792L5010.3847/2041-8213/adab75Production, Transport, and Destruction of Dust in the Kuiper Belt: The Effects of Refractory and Volatile Grain CompositionsThomas Corbett0https://orcid.org/0009-0004-3314-2870Alex Doner1https://orcid.org/0000-0001-7065-3224Mihály Horányi2https://orcid.org/0000-0002-5920-9226Pontus Brandt3https://orcid.org/0000-0002-4644-0306Will Grundy4https://orcid.org/0000-0002-8296-6540Carey M. Lisse5https://orcid.org/0000-0002-9548-1526Joel Parker6https://orcid.org/0000-0002-3672-0603Lowell Peltier7https://orcid.org/0000-0002-9179-8323Andrew R. Poppe8https://orcid.org/0000-0001-8137-8176Kelsi N. Singer9https://orcid.org/0000-0003-3045-8445S. Alan Stern10https://orcid.org/0000-0001-5018-7537Anne J. Verbiscer11https://orcid.org/0000-0002-3323-9304Laboratory for Atmospheric and Space Physics, University of Colorado , Boulder, CO, USA ; Thomas.Corbett@lasp.colorado.edu; Department of Physics, University of Colorado , Boulder, CO, USALaboratory for Atmospheric and Space Physics, University of Colorado , Boulder, CO, USA ; Thomas.Corbett@lasp.colorado.edu; Department of Physics, University of Colorado , Boulder, CO, USALaboratory for Atmospheric and Space Physics, University of Colorado , Boulder, CO, USA ; Thomas.Corbett@lasp.colorado.edu; Department of Physics, University of Colorado , Boulder, CO, USAThe Johns Hopkins University Applied Physics Laboratory , Laurel, MD, USALowell Observatory , Flagstaff, AZ, USAThe Johns Hopkins University Applied Physics Laboratory , Laurel, MD, USASouthwest Research Institute , Boulder, CO, USANational Research Council of Canada , Herzberg Astronomy and Astrophysics Research Centre, Victoria, BC, Canada; Department of Physics and Astronomy, University of Victoria , Victoria, BC, CanadaSpace Sciences Laboratory, University of California , Berkeley, CA, USASouthwest Research Institute , Boulder, CO, USASouthwest Research Institute , Boulder, CO, USADepartment of Astronomy, University of Virginia , Charlottesville, VA, USAThe Venetia Burney Student Dust Counter (SDC) on board the New Horizons spacecraft measures the spatial and size distributions of dust along its trajectory. Models based on early SDC measurements predicted a peak dust number density at a heliocentric distance of ∼40 au, followed by a rapid decline. Instead, SDC observed dust fluxes 2–3 times higher than predicted between 40 and 60 au. One potential explanation for this discrepancy is that SDC may be encountering icy grains with different dynamical behavior than previously modeled silicate grains. Due to ultraviolet photosputtering, water–ice grains rapidly erode and migrate outward, significantly contributing to the measured dust number densities only at distances ≳40 au. We present a model of silicate and ice grain dynamics in the outer solar system, considering gravitational and radiation forces and grain erosion. Using SDC data, we estimate that the mass production rate of ice grains between 0.1 and 10 μ m in the Kuiper Belt (KB) would need to be 20–70 times higher than that of silicate grains. However, KB grains are expected to be refractory/volatile mixtures rather than pure silicate or ice. Thus, we briefly explore simple models of more realistic mixed-grain cases to further gauge the effects of grain composition on the equilibrium dust distribution. Future SDC measurements at greater distances will test the model predictions and further constrain silicate and ice grain production rates in the KB.https://doi.org/10.3847/2041-8213/adab75Interplanetary dustAstrophysical dust processes
spellingShingle Thomas Corbett
Alex Doner
Mihály Horányi
Pontus Brandt
Will Grundy
Carey M. Lisse
Joel Parker
Lowell Peltier
Andrew R. Poppe
Kelsi N. Singer
S. Alan Stern
Anne J. Verbiscer
Production, Transport, and Destruction of Dust in the Kuiper Belt: The Effects of Refractory and Volatile Grain Compositions
The Astrophysical Journal Letters
Interplanetary dust
Astrophysical dust processes
title Production, Transport, and Destruction of Dust in the Kuiper Belt: The Effects of Refractory and Volatile Grain Compositions
title_full Production, Transport, and Destruction of Dust in the Kuiper Belt: The Effects of Refractory and Volatile Grain Compositions
title_fullStr Production, Transport, and Destruction of Dust in the Kuiper Belt: The Effects of Refractory and Volatile Grain Compositions
title_full_unstemmed Production, Transport, and Destruction of Dust in the Kuiper Belt: The Effects of Refractory and Volatile Grain Compositions
title_short Production, Transport, and Destruction of Dust in the Kuiper Belt: The Effects of Refractory and Volatile Grain Compositions
title_sort production transport and destruction of dust in the kuiper belt the effects of refractory and volatile grain compositions
topic Interplanetary dust
Astrophysical dust processes
url https://doi.org/10.3847/2041-8213/adab75
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