2010 Annual Science Report
Rensselaer Polytechnic Institute Reporting | SEP 2009 – AUG 2010
Project 2: Processing of Precometary Ices in the Early Solar System
The discovery of numerous planetary systems still in the process of formation gives us a unique opportunity to glimpse how our own solar system may have formed 4.6 billion years ago. Our goal is to test the hypothesis that the building blocks of life were synthesized in space and delivered to the early Earth by comets and asteroids. We use computers to simulate shock waves that energize the gas and dust in proto-planetary disks and drive physical and chemical processes that would not otherwise occur. Our work seeks specifically to determine (i) whether asteroids and comets were heated to temperatures that favor prebiotic chemistry; and (ii) whether the requisite heating mechanisms operate in other planetary systems forming today.
Precometary Ices in Molecular Clouds and Cores – The 5-year objective of this project is to study thermal processing of precometary materials in the solar nebula and protoplanetary disks. In Year 2 we made important contributions to the physics of two heating mechanisms – multifluid, magnetohydrodynamic shock waves and a new electrodynamic process discovered by us.
a) Multifluid, Magnetohydrodynamic Shock Waves
Roberge, Ciolek, and grad student Max Katz modeled the dynamical effects of dust grains on multifluid MHD shock waves. Fig. 1 describes the shock produced when a 20 km/s protostellar jet impacts a molecular cloud core. The shock consists of a sharp discontinuity (J shock) in the neutral component of the plasma (magenta curve) plus smooth disturbances in the charged particles (red and blue symbols). The response of the charged particles is shown for two cases, where dust is either effectively absent (red) or present (blue). Multifluid shocks are heated primarily by friction associated with differential motions between charged and neutral particles. Consequently, the discrepancy between the red and blue solutions shows that models of shock heating require realistic treatments of grain dynamics. This result should have a large impact on studies of shock-heated molecules around protostars, e.g., by SOFIA.
b) Electrodynamic Heating in the Solar Nebula and Protoplanetary Disks
Roberge and grad student Raymond Menzel discovered a new mechanism for heating asteroids and planetesimals (Fig. 2). The motion of a large body through nearby plasma produces a shear layer near the solid surface. Magnetic field gradients inside the shear layer (vastly exaggerated in the figure) generate nonzero electric fields in an around the asteroid. Preliminary estimates of heating by the resulting electric currents (Joule heating) suggest that electrodynamic heating profoundly influenced the thermal histories of asteroids. This work is directly relevant to the prebiotic synthesis of amino acids and other biomolecules in the solar nebula.
PROJECT INVESTIGATORS:Wayne Roberge
PROJECT MEMBERS:Glenn Ciolek
RELATED OBJECTIVES:Objective 1.1
Formation and evolution of habitable planets.
Sources of prebiotic materials and catalysts
Origins and evolution of functional biomolecules