The Chemistry of Stellar and Planetary Formation Eric Herbst Departments of Physics, Astronomy, and Chemistry The Ohio State University The Center of the Milky Way 100,000 lt yr Andromeda: a “nearby” spiral galaxy The Eagle Nebula: active star forming region in our galaxy The Horsehead Nebula (also in our galaxy – Orion) Dense Interstellar Cold Core 10 K 10(4) cm-3 H2 dominant sites of star formation 0.5 lt yr 500 lt yr away Extinction consistent with size distribution from 5-250 nm. Dust constitutes 1% of mass in a cloud. IR spectral studies yield information about cores of dust particles (silicates, carbon) as well as icy mantles Dominant Mantle Species: water, CO2, CO, CH3OH Work-horse method for gas-phase molecules Must compare with results of laboratory spectra The soon-to-be Herschel Space Observatory Cold Core Low-mass Star Formation adiabatic collapse Protostar T = 10 K n = 104 cm-3 Molecule factory Star + Disk hot core 100 K Via high-resolution gas-phase analytical spectroscopy: 133 neutral molecules (February 2008) 18 molecular ions (main isotopes) 14 positive 4 negative H C, N, O S, Si, P, K, Na, Mg, Al, F Most in our own galaxy only. Gaseous interstellar molecules (151) N=2 N=3 N=4 N=5 N=6 N=7 N=8 N=9 N = 10 H2 AlCl CH2 C2S NH3 CH4 CH3OH CH3NH2 HCOOCH3 (CH3)2O (CH3)2CO CH PN H2S OCS H2CO SiH4 CH3SH CH3CCH CH3C2CN C2H5OH CH3C4CN NH SiN NH2 MgCN H2CS CH2NH C2H4 CH3CHO HC6H C2H5CN CH3CH2CHO OH SiO H2O MgNC H2CN C5 H2C4 c-CH2OCH2 C7H CH3C4H (CH2OH)2 O2(?) SiS HNO NaCN l-C3H l-C3H2 CH3CN CH2CHCN HOCH2CHO C8H HF PO C2H SO2 c-C3H c-C3H2 CH3NC HC4CN CH3COOH HC6CN C2 SH HCN N2O HCCH H2CCN NH2CHO C6H H2CCCHCN CH3CONH2 N = 11 CN AlF HNC SiCN HNCO H2NCN H2CCHO H2CCHOH H2C6 CH2CHCH3 HC8CN CO FeO HCO SiNC HNCS CH2CO C5H CH2CHCHO CS SiC c-SiC2 CCP HCCN HCOOH C5N C2H6 CH3C6H CP MgCN C2CN C4H HC4N NO MgNC C3O HC2CN C5S(?) N = 12 NS AlNC C3S HC2NC HC4H C6H6 SO HCP H3+ c-SiC3 C4Si CH2CNH HCl CH+ C3 HCO+ C3N- HNCCC HC2CHO NaCl CO+ C2O HOC+ H3O+ CNCHO c-C3H2O KCl SO+ CO2 N2H+ HCNH+ H2COH+ N2(?) CF+ HCS+ HOCO+ C4H- N = 13 HC10CN HC3NH+ C6H- C8H- The Chemistry of Cold Cores • Do chemical reactions take place under low density and low temperature conditions? • Collision interval = 1 day to 1 millenium k(T) = A(T)exp(-Ea/RT) • How can we convert atoms into molecules? • H+H H+H POTENTIAL ENERGY OF REACTION activation energy typical neutral reactions radical-radical reactions A+B ion-molecule reactions k(T) = A(T) exp(-Ea /kT) C+ D Cosmic rays produce ions T = 10-20 K Gould & Salpeter FORMATION OF GASEOUS WATER IN COLD CORES H2 + COSMIC RAYS H2+ + e H2+ + H2 H3+ + H H3+ + O OH+ + H2 OHn+ + H2 OHn+1+ + H H3O+ + e H2O + H; OH + 2H, etc + longer pathways to unsaturated organic species…… Formation of Ices In Cold Cores H O OH H H2O Other ices formed: methane, ammonia, CO, CO2, formaldehyde, methanol (all confirmed by experiments at low temperature.) What is a model? • Simulates chemistry in the gas and on surfaces • 6000 gas-phase reactions; 200 surface reactions • Physical conditions can be homogeneous and timeindependent, or can be heterogeneous and/or time dependent • Molecular concentrations can be calculated. Comparison with observation yields physical conditions and history of object. • Cold cores (gas + ices) fit best at age of 105 yr (80% of molecules fit to within observational error). • Can even simulate what ices look like! Development of ice mantle in cold interstellar core Cuppen & Herbst, 2007 Hot Core Chemistry 100-300 K evaporation 10 K Cold phase +accretion + surface chemistry (Hrich) Surface chemistry involving heavy radicals (photochemistry) Saturated organic molecules such as ethers, alcohols Garrod & Herbst (2006) ORGANIC MOLECULES PREDICTED IN HOT CORES • Dimethyl ether, methyl formate, formic acid, glycolaldehyde, acetic acid, ethanol, acetaldehyde, ketene, acetone, ethylene glycol • Methyl amine, urea, formamide, acetamide, methoxyamine, hydroxymethylamine • Garrod, Widicus Weaver, & Herbst (2008) Protoplanetary Disk Cosmic rays UV X-ray midplane UV 500 AU T Tauri star – 106 yr old 0.01-0.1 M0 Keplerian rotation ALMA: the future……. http://www.physics.ohio-state.edu/~eric/ Vertical Distribution 70 T [K] density 50 40 30 densiy [cm-3] 60 109 9 10 cm-3 temperature 108108 10710 7 10 106 6 105 105 20 0 20 40 60 80 R = 105 AU photodissociation 100 Z(AU) accretion Too detailed for observers Icy Molecular Layer Layer PDR HOT CORE IN ORION Molecular inventory contains gaseous saturated (H-rich) “normal” molecules, not detected in colder regions. Ice mantles no longer exist. Negative Ions in Clouds • Herbst (1982) considered the possible abundance of anions in cold regions of the ISM based on radiative attachment mechanism: • A + e → A- + hn • and estimated their maximum abundance to be 1% of the neutral counterparts.