arXiv subjects

Kevin Righter

Publications and source records attributed to Kevin Righter.

4 recordsLinked to original sources

arXiv2026

Ice Deposition Fronts In Porous Bodies From Transient Heating Events In a Protoplanetary Disk

Using a 1D mass and heat transport model, we numerically integrate heat flow and gas transport in a porous body exposed to a transient heating event while embedded in a protoplanetary disk. When small icy grains are heated, volatiles sublimate, enriching the disk with volatile gases. When a porous body enters this heated, volatile-rich environment, volatile gases diffuse throughout the cool, porous body and deposit ice where the partial pressure of a volatile exceeds its vapor pressure. We simulate sublimation and deposition fronts of water, carbon dioxide, and carbon monoxide. Our simulations show that an ice deposition front forms and moves deeper into the porous body as the body warms. The amount of nebular gas deposited in an initially dry body is usually extremely low; however, in an initially icy body, an ice deposition front contains locally sublimated volatiles. In this case, the front can increase the ice volume fraction (by a factor of 2) in a thin layer below the surface. We find that the propagation speed, propagation strength, and final depth of an ice deposition front primarily depend on pore size. We propose that nebular heating events can alter the subsurface morphology and physical properties of porous icy objects embedded in a protoplanetary disk.

astro-ph.EP↗

arXiv2025

A Pyroxenite Mantle on Mercury? Experimental Insights from Enstatite Chondrite Melting at Pressures up to 5 GPa

Enstatite chondrites (EC) are potential source material for the accretion of Mercury due to their reduced nature and enrichment in volatile elements. Understanding their melting properties is therefore important to better assess a scenario where Mercury formed from these chondrites. Here, we present experimental data on the partial melting of a modified EH4 Indarch EC, which was adjusted to have 18\% more metallic Si than SiO$_2$ in mass, yielding an oxygen fugacity of 3.7 below the iron--w\"ustite redox buffer and 12 wt\% Si in the metal. Experiments were performed from 0.5 to 5 GPa. Results indicate that the stability field of enstatite expands relative to olivine. This expansion is likely due to the presence of Ca--S and Mg--S complexes in the silicate melt, which enhance SiO$_2$ activity and promote enstatite crystallization. Additionally, sulfides show enrichment in Mg and Ca, up to 22 and 13 wt\% respectively, the main remaining cations being Fe, Cr, and Mn. These high Mg and Ca contents are observed at low temperatures and high silica content in the silicate melt, respectively. High-pressure melts (2 to 5 GPa, 160--400 km depth in Mercury) are Mg-rich, similar to those in Mercury's high-magnesium region (HMR), while low-pressure melts (0.5 to 1 GPa, 40--80 km depth) are Si-rich, comparable to the northern volcanic plains (NVP). Results suggest that a large fraction of Mercury's surface aligns compositionally with these melts, implying that Mercury's mantle could predominantly have a pyroxenitic composition. However, regions with differing compositions, such as aluminum-rich areas like the Caloris basin, suggest local variability in mantle geochemistry. Overall, our results show that if Mercury formed from materials similar to EC, batch melting of its primitive pyroxenite mantle would yield magmas with compositions resembling those of most rocks observed on the surface.

astro-ph.EP↗

arXiv2024

QRIS: A Quantitative Reflectance Imaging System for the Pristine Sample of Asteroid Bennu

The Quantitative Reflectance Imaging System (QRIS) is a laboratory-based spectral imaging system constructed to image the sample of asteroid Bennu delivered to Earth by the Origins, Spectral Interpretation, Resource Identification, and Security-Regolith Explorer (OSIRIS-REx) spacecraft. The system was installed in the OSIRIS-REx cleanroom at NASA's Johnson Space Center to collect data during preliminary examination of the Bennu sample. QRIS uses a 12-bit machine vision camera to measure reflectance over wavelength bands spanning the near ultraviolet to the near infrared. Raw data are processed by a calibration pipeline that generates a series of monochromatic, high-dynamic-range reflectance images, as well as band ratio maps, band depth maps, and 3-channel color images. The purpose of these spectral reflectance data is to help characterize lithologies in the sample and compare them to lithologies observed on Bennu by the OSIRIS-REx spacecraft. This initial assessment of lithological diversity was intended to help select the subsamples that will be used to address mission science questions about the early solar system and the origins of life and to provide important context for the selection of representative subsamples for preservation and distribution to international partners. When QRIS imaged the Bennu sample, unexpected calibration issues arose that had not been evident at imaging rehearsals and negatively impacted the quality of QRIS data. These issues were caused by stray light within the lens and reflections off the glovebox window and interior, and were exacerbated by the sample's extremely low reflectance. QRIS data were useful for confirming conclusions drawn from other data, but reflectance and spectral data from QRIS alone unfortunately have limited utility.

astro-ph.EP↗

arXiv2021

Origin of the Moon

The Earth-Moon system is unusual in several respects. The Moon is roughly 1/4 the radius of the Earth - a larger satellite-to-planet size ratio than all known satellites other than Pluto's Charon. The Moon has a tiny core, perhaps with only ~1% of its mass, in contrast to Earth whose core contains nearly 30% of its mass. The Earth-Moon system has a high total angular momentum, implying a rapidly spinning Earth when the Moon formed. In addition, the early Moon was hot and at least partially molten with a deep magma ocean. Identification of a model for lunar origin that can satisfactorily explain all of these features has been the focus of decades of research.

astro-ph.EP↗