28.19: Observaons Of Comet C/2007 (lulin) Before And During Its PerihelionAuthor Block: Gian-Paolo Tozzi 1 , J. R. Brucato 1 , P. Patriarchi 1 , J. Licandro 2 , E. Mazzoa Epifani 3 , C. Snodgrass 4 , J. Vincent 41 INAF Osservatorio Astrofisico di Arcetri, Italy, 2 IAC, Spain, 3 INAF, Italy, 4 M PS, Germany.Presentaon Time: 10/4/2010 4:36 PM - 4:38 PMLocaon: Exhibit Hall<strong>Abs</strong>tract.<strong>Abs</strong>tract: Comet Lulin was observed in July 2008, when the comet was in-bound at 1.7 AU from the Sun. Analysis of the images showed that the comethad a very intense and anomalous enhancement of the column density of the solid components in the inner coma. This effect was before interpreted as due tothe presence of sublimang grains (Tozzi et al, 2004, AA, 424, 325; 2007, 476, 979) or, more recently, to a developing coma expanding very slowly (few meters persecond, Tozzi et al. 2010, submied). To disentangle the two phenomena the comet was re-observed in two epochs around its perihelion (Jan - Mar. 2009), whenit was at about 1.40 AU from the Sun and at about 0.4 AU from the Earth. In this case the enhancement in the inner coma had disappeared, showing only a widebut less intense enhancement at about 20000-30000 km of projected distance. A possible contaminaon of gas, that would produce a similar effect, has beenexcluded by spectra and observaons with narrow band filters centred in spectral regions without gas emission. In the presentaon the results of the analysiswith possible interpretaons will be given.28.20: A Study of Water in Comet C/2007 N3 (Lulin)Author Block: Emily Sudholt 1 , B. P. Bonev 2 , E. L. Gibb 1 , M. A. DiSan 3 , G. Villanueva 3 , M. J. Mumma 3 , K. Magee-Sauer 41 University of Missouri - St. Louis, 2 Catholic University of America, 3 NASA Goddard Space Flight Center, 4 Rowan University.Presentaon Time: 10/4/2010 4:38 PM - 4:40 PMLocaon: Exhibit Hall<strong>Abs</strong>tract: We conducted a sensive search for HDO and detected H 2 O and OH in the spectra of comet C/2007 N3 (Lulin) obtained by NIRSPEC at the Keck IItelescope atop Mauna Kea, Hawaii. OH prompt emission is a direct proxy of H 2 O producon and eliminates “inter-seng” calibraon uncertaines in evaluangthe HDO/H 2 O rao. We report an upper limit for HDO/H 2 O, and spaal profiles, rotaonal temperatures, and producon rates for H2O. The work ofundergraduate student E. Sudholt was supported over 12 months by NSF Grant AST- 0807939 (PI/Co-PI Bonev/Gibb) and by the Goddard Center for Astrobiology (PIMumma). Co-authors gratefully acknowledge support from the NSF Astronomy and Astrophysics Research Grants Program, and by the NASA’s PlanetaryAstronomy, Planetary Atmospheres, and Astrobiology Programs.28.21: Detecons of Ethane (C 2 H 6 ), Methane (CH 4 ), and Carbon Monoxide (CO) in the Coma of Comet C/2006 W3 (Christensen) at 3.25 AU from The SunAuthor Block: Boncho Bonev 1 , H. Böhnhardt 2 , M. J. Mumma 3 , M. A. DiSan 3 , G. L. Villanueva 1 , M. Lippi 2 , E. L. Gibb 41 The Catholic Univ. of America / Goddard Center for Astrobiology, 2 Max-Planck Instute for Solar System Research, Germany, 3 NASA Goddard Space FlightCenter / Goddard Center for Astrobiology, 4 Univ. of Missori - St. Louis / Goddard Center for Astrobiology.Presentaon Time: 10/4/2010 4:40 PM - 4:42 PMLocaon: Exhibit Hall<strong>Abs</strong>tract: We report high-resoluon spectroscopic observaons of comet C/2006 W3 (Christensen) using the Cryogenic Infrared Echelle Spectrograph at theVery Large Telescope Observatory atop Cerro Paranal, Chile. We detected the “hypervolales” C 2 H 6 , CH 4 , and CO in the coma observed at heliocentric distance of3.25 AU. We also detected CO at 4.03 AU from the Sun. This presentaon will report spaal profiles, rotaonal temperature, and producon rates of the threedetected species. We compare our results with the radio detecon of CO (Bockelee-Morvan et al. A&A, 518, L149) and other parent volales at 3.20 and 3.32 AUto achieve an overall measure of the volale composion of this comet. The apparent enrichment in the coma of “hypervolales” will be discussed in terms offraconaon of nave ices within the nucleus. We gratefully acknowledge support from the NSF Astronomy and Astrophysics Research Grants Program (PI/co-PIBonev/Gibb), by the NASA’s Planetary Astronomy (PI Mumma; PI DiSan), Planetary Atmospheres (PI DiSan; PI Villanueva), and Astrobiology (PI Mumma)Programs, and by the German-Isreal Foundaon for Scienfic Research and Development (PI Böhnhardt).28.22: The Molecular Composion of Comet C/2007 W1 (Boani): Evidence of a Peculiar Outgassing and Rich ChemistryAuthor Block: Geronimo Villanueva 1 , M. A. DiSan 1 , M. J. Mumma 1 , B. P. Bonev 2 , E. L. Gibb 3 , K. Magee-Sauer 4 , G. A. Blake 51 NASA's GSFC, 2 Catholic University of America, 3 University of Missouri, 4 Rowan University, 5 Caltech.Presentaon Time: 10/4/2010 4:42 PM - 4:44 PMLocaon: Exhibit Hall<strong>Abs</strong>tract.<strong>Abs</strong>tract: We report observaons of comet C/2007 W1 (Boani) performed using the long-slit high-resoluon echelle grang spectrograph at Keck-2(NIRSPEC) on July 9 and 10 of 2008. We present results for 10 volale species (H2O, OH*, C2H6, CH3OH, H2CO, CH4, HCN, C2H2, NH3, CO), the ortho-para raosof H2O and CH4, and an upper-limit of the water D/H rao in comet Boani. We observe important differences in the spaal profiles of the detected species,with the majority of the polar volales showing very asymmetric profiles. We present emission profiles for all observed volales along the cometary coma anddiscuss different producon scenarios necessary to explain these. Ulmately, we compare all measured cosmogonic indicators and relate these to a possibleformaon path for this comet. We acknowledge support from the NASA Planetary Atmospheres, Planetary Astronomy, Astrobiology Programs, and the NSFAstronomy and Astrophysics Research Grants Program.28.23: Searching for Gas Emission through Visible Spectroscopy of Large Perihelia (>5AU) CometsAuthor Block: Sean Mossman 1 , L. M. Woodney 1 , Y. R. Fernandez 21 California State Univ. San Bernardino, 2 University of Central Florida.Presentaon Time: 10/4/2010 4:44 PM - 4:46 PMLocaon: Exhibit Hall<strong>Abs</strong>tract: We present spectroscopic observaons of several comets with perihelia beyond 5 AU. In recent years many large perihelia comets have beendiscovered with acve dust comae. The gas, which must be driving the dust producon, is rarely detected. These objects are not close enough to the sun forwater sublimaon to be responsible for coma producon, so sublimaon of other volales (CO, CO2) or phase changes in water-ice likely drive the acvity. Theyrepresent a class of comets less altered from their original states than those that regularly pass through the water sublimaon zone and therefore can be used toaddress quesons of cometary composion and disentangle evoluonary effects.We used the LRIS spectrometer (0.3 Å spectral resoluon) on the Keck 10 m telescope atop Mauna Kea, Hawaii in hopes of detecng fluorescence from some ofthe commonly observed visible gas species such as CN, C2 or CO+. Our targets were three Centaurs - 95P/Chiron, 29P/Schwassmann-Wachmann 1 and C/ 2001M10 (NEAT) - and one long-period comet - C/2003 O1 (LINEAR). We present upper limits of gas species producon rates and the gas-to-dust mass loss rao.28.24: Dynamics of Crystalline Silicates in the Coma of Comet 9P/Tempel and the Deep Impact EjectaAuthor Block: Michael S. Kelley 1 , D. H. Wooden 2 , S. S. Lindsay 3 , D. E. Harker 4 , C. E. Woodward 5
1 Univ. of Maryland, 2 NASA Ames, 3 New Mexico State Univ., 4 UCSD/CASS, 5 Univ. of Minnesota.Presentaon Time: 10/4/2010 4:46 PM - 4:48 PMLocaon: Exhibit Hall<strong>Abs</strong>tract: Mid-infrared spectra have revealed the presence of crystalline silicates in the dust of comet 9P/Tempel, both before and aer the Deep Impactcratering experiment (Wooden et al. 2010, <strong>42nd</strong> <strong>DPS</strong> Meeng). The spectra of the Deep Impact ejecta reveal strong silicate emission features, includingresonances from Mg-rich crystalline silicates (forsterite and enstate), reminiscent of spectra of comet C/1995 O1 (Hale-Bopp). In constrast, spectra of theambient coma appears to be that of a typical eclipc comet: a weak 10 micron silicate plateau with subtle features aributable to forsterite. Wooden et al. (2010)examine the me evoluon of archival Spitzer Space Telescope spectra of the Deep Impact ejecta and find that crystalline silicates are present in the ejecta aslate as 40 hours post-impact. They also find that the spectra at these late epochs have the same spectral shapes as the ambient coma. Thus, the slower movingejecta and the ambient coma are both composed of large porous aggregates containing crystalline silicates. We examine the dynamics of dust ejected by DeepImpact and find that this slower moving ejecta is at least 10 microns in size. This result implies that the ambient coma of 9P/Tempel is dominated by grains withsizes of order 10 microns. If we generalize our results, we conclude that many eclipc comets may be dominated by large porous grains with high crystallinefracons, approximately 40% by mass, despite their weak silicate emission features.This research is supported by NASA's Planetary Atmospheres Program.28.25: Using Imaging of Mulple Outbursts to Invesgate the Behavior and Nucleus Properes of Comet 29P/Schwassmann-Wachmann 1Author Block: Yanga R. Fernandez 1 , N. H. Samarasinha 2 , B. E. A. Mueller 2 , L. M. Woodney 31 Univ. of Central Florida, 2 PSI, 3 Cal State U.-San Bernardino.Presentaon Time: 10/4/2010 4:48 PM - 4:50 PMLocaon: Exhibit Hall<strong>Abs</strong>tract.<strong>Abs</strong>tract: We present an analysis of the dynamic dust coma of comet 29P/Schwassmann-Wachmann 1 (SW1), a comet with a long record of observedoutbursts. We have obtained R-band CCD imaging of SW1's dust coma in 2002, 2003, 2005, 2008, and 2010, and at every epoch, the comet was fortuitously inoutburst, showing dust jets, spirals, and/or shells. This gives us a significant and growing database of these events with which we can study properes of SW1'sdust and nucleus, and their me evoluon. As an outburst evolves, our data show that the near-nucleus dust brightness and dust morphology change on daily andweekly mescales. Moreover, not all outbursts have the same strength; in parcular our 2010 imaging shows evidence of a mini-outburst of shorter duraon andsmaller magnitude than the others. In this presentaon we will follow up earlier analyses of the dust coma [1,2], and we will present preliminary results frommodeling the dust seen in specific outbursts. We are using a Monte Carlo dust model [3] that reproduces the features seen in the coma and thereby constrainsproperes such as outburst ming, spin state, and source regions. References: [1] Ellis, C.E., et al. 2004, BAAS 36, 1146. [2] Fernandez, Y.R., et al. 2008, IAUC8991. [3] Samarasinha 2000, ApJ 529, L107.28.26: Visible-wavelength Observaons of Jupiter-family Comet Nuclei as Part of Seppcon.Author Block: Jana Pichova 1 , S. C. Lowry 2 , R. Laird 2 , M. F. A’Hearn 3 , J. M. Bauer 4 , H. Campins 5 , Y. Fernández 5 , A. Fitzsimmons 6 , O. Groussin 7 , H. Hsieh 6 , M.Kelley 3 , P. Lamy 7 , J. Licandro 8 , C. M. Lisse 9 , K. J. Meech 1 , W. T. Reach 10 , C. Snodgrass 11 , I. Toth 12 , H. A. Weaver 9 , P. Weaissman 41 Univ. of Hawaii, 2 Centre for Astrophysics and Planetary Sciences, University of Kent, United Kingdom, 3 Dept. of Astronomy, Univ. of Maryland, 4 NASA/JPL,5 Physics Dept., Univ. of Central Florida, 6 Astrophysics Research Centre, Queens Univ. Belfast, United Kingdom, 7 Laboratoire d’Astrophysique de Marseille, CNRS& Université de Provence, France, 8 Instuto de Astrosica de Canarias, Spain, 9 Johns Hopkins Univ. Applied Physics Lab., 10 SOFIA/USRANASA Ames ReseachCenter, 11 Max Planck Instute for Solar System Research, Germany, 12 Konkoly Obs., Hungary.Presentaon Time: 10/4/2010 4:50 PM - 4:52 PMLocaon: Exhibit Hall<strong>Abs</strong>tract: We present the latest analysis and results from SEPPCoN (Survey of Ensemble Physical Properes of Cometary Nuclei). This on-going survey involvesstudying 100 JFCs - about 25% of the known populaon - at both mid-infrared and visible wave-lengths to constrain the distribuons of sizes, shapes, spins, andalbedos of this populaon. Having earlier reported results from measuring thermal emissions of our sample nuclei [1,2,3,4], we report here progress on thevisible-wavelength observaons that we have obtained at many ground-based facilies in Chile, Spain, and the United States. To date we have aemptedobservaons of 91% of our sample of 100 JFCs, and at least 64 of those were successfully detected. In most cases the comets were at heliocentric distancesbetween 3.0 and 6.5 AU so as to decrease the odds of a comet having a coma. Of the 64 detected comets, 48 were apparently bare, having no extendedemission. Our datasets are further augmented by archival data and photometry from the NEAT program [5]. An important goal of SEPPCoN is to accumulate alarge comprehensive set of high quality physical data on cometary nuclei in order to make accurate stascal comparisons with other minor-body populaonssuch as Trojans, Centaurs, and Kuiper-belt objects. Informaon on the size, shape, spin-rate, albedo and color distribuons is crical for understanding theirorigins and evoluonary processes affecng them.This work was supported in part by grants from NASA (NNX09AB44G) and NSF (AST-0808004).[1] Fernandez, Y., et al. 2008, Asteroids Comets Mete-ors 2008, LPI Co. No. 1405, paper id. 8307.[2] Kelley, M., et al. 2008, Asteroids Comets Meteors 2008, LPI Co. No. 1405, paper id. 8272.[3] Groussin, O., et al. 2009, Icarus 199, 568.[4] Licandro, J., et al. 2009, A&A 507, 1667.[5] Bauer, J., et al. 2010, AAS Meeng 216, paper 409.01.28.27: Whither Cometary Dust?Author Block: Carey M. Lisse 11 Johns Hopkins Univ..Presentaon Time: 10/4/2010 4:52 PM - 4:54 PMLocaon: Exhibit Hall<strong>Abs</strong>tract: In this paper I will discuss recent findings that have important implicaons for our understanding of the formaon and evoluon of primive solarsystem dust, including:- Nesvorny et al. (2010), following up on their dynamical analyses of the zodiacal dust bands as sourced by the breakup of the Karin (5Mya) and Veritas (8Mya)asteroid families, argue that over 90% of the interplanetary dust cloud at 1 AU comes from JFC comets with near-circularized, low inclinaon orbits. This impliesthat the noted IPD collecons of anhydrous and hydrous dust parcles are likely to be from Oort cloud and JFC comets, respecvely, not from asteroids andcomets as thought in the past. Hydrous dust parcles from comets like 85P/Wild2 and 9P/Tempel 1 would be consistent with results from the STARDUST and DeepImpact experiments.- Esmates of the dust parcle size distribuons (PSDs) in the comae of 85P/Wild2 (Green et al. 2004, 2007) and 73P/SW-3 (Sitko et al. 2010, Vaubaillon & Reach2010) and in the trails of comets (Reach et al. 2007) have broken power law structure, with a plateau enhancement of parcles of 1 mm - 1 cm in size. This size is
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References:[1] NRC, Europa Science
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most asteroids, at least in an exte