Mechanical Modification of Chondrule Fine-grained Rims by Dusty Nebular Shocks
نویسندگان
چکیده
Abstract The mechanical processes that convert an initially fluffy chondrule fine-grained rim (FGR) into a more compact structure remain poorly characterized. Given the presence of shocks in protoplanetary disks, we use numerical simulations to test hypothesis dust-laden solar nebula contributed FGR modification. We iSALE2D shock physics code model collision dusty nebular fronts (which term “dust clouds”) surfaces host porous FGR. In our simulations, dust particles are modeled as dunite disks. radii follow Mathis–Rumpl–Nordsieck distribution interstellar grains. Chondrules rectangular slabs. vary impact speed v imp , fractional abundance f cloud grains impacting shock, and pre-existing thus compute temperatures pressures resulting from collisions, well net mass accretion by FGRs. Dust increase upon impact, depending on kinetic energy . rims with higher heat up than those lower possibly important implications for composition Maximum Fine-grained can experience gain cloud, but some instances, is lost rim. find qualitative similarities topography FGR–chondrule interface between petrographic analyses Paris CM chondrite other authors.
منابع مشابه
Evaporation of nebular fines during chondrule formation
Studies of matrix in primitive chondrites provide our only detailed information about the fine fraction (diameter <2 μm) of solids in the solar nebula. A minor fraction of the fines, the presolar grains, offers information about the kinds of materials present in the molecular cloud that spawned the Solar System. Although some researchers have argued that chondritic matrix is relatively unaltere...
متن کاملA nebular origin for chondritic fine-grained phyllosilicates.
Hydrated minerals occur in accretionary rims around chondrules in CM chondrites. Previous models suggested that these phyllosilicates did not form by gas-solid reactions in the canonical solar nebula. We propose that chondrule-forming shock waves in icy regions of the nebula produced conditions that allowed rapid mineral hydration. The time scales for phyllosilicate formation are similar to the...
متن کاملChondrules and Nebular Shocks
Beneath the fusion-encrusted surfaces of the most primitive stony meteorites lies not homogeneous rock, but a profusion of millimeter-sized igneous spheres. These chondrules, and their centimeter-sized counterparts, the calcium-aluminum-rich inclusions, comprise more than half of the volume fraction of chondritic meteorites. They are the oldest creations of the solar system. Their chemical comp...
متن کاملEvaporation/condensation of Chondritic Chondrule Precursors in Nebular
Introduction: The origin of chondrules remains one of the great enigmas in meteoritics. Under the canonical formation conditions of low pressures, high temperatures and moderate cooling rates (10-1000 K/hr), some evaporation at least of the moderately volatile elements is expected. Chondrules are depleted in moderately volatile elements, but they do not have the systematic isotopic fractionatio...
متن کاملCHONDRULE FORMATION IN NEBULAR SHOCK WAVES GENERATED BY PLANETESIMALS PASSING THROUGH JOVIAN RESONANCES: RELATIVE IMPORTANCE OF BOW SHOCKS AND IMPACT SHOCKS. L. L. Hood
PASSING THROUGH JOVIAN RESONANCES: RELATIVE IMPORTANCE OF BOW SHOCKS AND IMPACT SHOCKS. L. L. Hood 1 , F. J. Ciesla 2 , N. A. Artemieva 3,4 , F. Marzari 5 , and S. J. Weidenschilling 4 , 1 Lunar and Planetary Laboratory, Univ. of Arizona, Tucson, Arizona 85721, [email protected], 2 Dept. of Geophysical Sciences, Univ. of Chicago, Chicago, Illinois 60637, 3 Institute for Dynamics of Geospheres...
متن کاملذخیره در منابع من
با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید
ژورنال
عنوان ژورنال: The planetary science journal
سال: 2023
ISSN: ['2632-3338']
DOI: https://doi.org/10.3847/psj/acd758