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On the Evolution of Dust Mineralogy, from Protoplanetary Disks to Planetary Systems

Oliveira, Isa and Olofsson, Johan and Pontoppidan, Klaus M. and van Dishoeck, Ewine F. and Augereau, Jean-Charles and Merín, Bruno (2011) On the Evolution of Dust Mineralogy, from Protoplanetary Disks to Planetary Systems. Astrophysical Journal, 734 (1). Art. No. 51. ISSN 0004-637X.

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Mineralogical studies of silicate features emitted by dust grains in protoplanetary disks and solar system bodies can shed light on the progress of planet formation. The significant fraction of crystalline material in comets, chondritic meteorites, and interplanetary dust particles indicates a modification of the almost completely amorphous interstellar medium dust from which they formed. The production of crystalline silicates, thus, must happen in protoplanetary disks, where dust evolves to build planets and planetesimals. Different scenarios have been proposed, but it is still unclear how and when this happens. This paper presents dust grain mineralogy (composition, crystallinity, and grain size distribution) of a complete sample of protoplanetary disks in the young Serpens cluster. These results are compared to those in the young Taurus region and to sources that have retained their protoplanetary disks in the older Upper Scorpius and η Chamaeleontis stellar clusters, using the same analysis technique for all samples. This comparison allows an investigation of the grain mineralogy evolution with time for a total sample of 139 disks. The mean cluster age and disk fraction are used as indicators of the evolutionary stage of the different populations. Our results show that the disks in the different regions have similar distributions of mean grain sizes and crystallinity fractions (~10%-20%) despite the spread in mean ages. Furthermore, there is no evidence of preferential grain sizes for any given disk geometry nor for the mean cluster crystallinity fraction to increase with mean age in the 1-8 Myr range. The main implication is that a modest level of crystallinity is established in the disk surface early on (≤1 Myr), reaching an equilibrium that is independent of what may be happening in the disk midplane. These results are discussed in the context of planet formation, in comparison with mineralogical results from small bodies in our own solar system.

Item Type:Article
Related URLs:
URLURL TypeDescription
Pontoppidan, Klaus M.0000-0001-7552-1562
van Dishoeck, Ewine F.0000-0001-7591-1907
Additional Information:© 2011 The American Astronomical Society. Received 2010 October 29; accepted 2011 April 5; published 2011 May 24. Astrochemistry at Leiden is supported by a Spinoza grant from the Netherlands Organization for Scientific Research (NWO) and by the Netherlands Research School for Astronomy (NOVA) grants. This work is based on observations made with the Spitzer Space Telescope, which is operated by the Jet Propulsion Laboratory, California Institute of Technology under a contract with NASA. Support for this work was provided by NASA through an award issued by JPL/Caltech.
Funding AgencyGrant Number
Nederlandse Organisatie voor Wetenschappelijk Onderzoek (NWO)UNSPECIFIED
Nederlandse Onderzoekschool voor de Astronomie (NOVA)UNSPECIFIED
Subject Keywords:circumstellar matter; infrared: stars; methods: statistical; protoplanetary disks; stars: pre-main sequence
Issue or Number:1
Classification Code:PACS: 96.30.Cw; 98.58.Db; 98.58.Ca; 97.10.Fy; 95.30.Ft; 96.55+z
Record Number:CaltechAUTHORS:20110613-082456139
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Official Citation:On the Evolution of Dust Mineralogy, from Protoplanetary Disks to Planetary Systems Isa Oliveira, Johan Olofsson, Klaus M. Pontoppidan, Ewine F. van Dishoeck, Jean-Charles Augereau and Bruno Merín doi: 10.1088/0004-637X/734/1/51
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:23979
Deposited By: Ruth Sustaita
Deposited On:13 Jun 2011 15:44
Last Modified:03 Oct 2019 02:51

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