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"I have heard of a future possibility of mining asteroids for minerals. How would one go about finding asteroids that have important minerals?"
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Formation of Planetesimals in a Dynamically Evolving Nebula
Project Investigators: Nader Haghighipour
Summary
The current model of the formation of planetesimals through gravitational instability cannot account for the growth of particles from a few mm to several cm in size. The shear-induced turbulence in such systems prevents small solid objects to accumulate and grow larger. The focus of this project is to show that the appearance of gas density/pressure enhanced regions will facilitate this process and speed up the growth of small solid objects.
Astrobiology Roadmap Objectives:
Project Progress
It has been suggested that km-sized objects can form through the fragmentation of a gravitationally unstable layer of solid materials in a nebula. However, the difference between the rotational velocities of gas and dust particles in a gaseous disk produces a shear between these layers, which in turn results in turbulence. This turbulence and prevents solid objects from accumulating and increasing their local density to the necessary value for starting gravitational instability. To overcome this problem, models of gravitational instability consider objects with initial sizes larger than 50 cm and do not account for the growth of mm-sized particles (which are formed though hitting and sticking of micron-sized objects) to several cm in size. In this project, we have shown that the key in resolving this issue and filling the gap between mm-sized particles and 50 cm-sized objects is the interactions of dust particles with gas in the vicinity of pressure-enhanced regions. The combined effect of gas-drag and pressure-gradients causes micron-sized dust particles to migrate towards pressure-enhanced regions, while growing to a few millimeter in size (Figure 1).
Growth of a 10 micron dust particle to a few cm in size in the vicinity of a pressure enhanced region.These objects accumulate in the location of the maximum gas pressure, where gas and dust rotate with similar Keplreian velocity and no shear-induced turbulence exists. Settling dust particles in the location of maximum gas pressure form clumps of several centimeter in size (Figure 2).
Settling and accumulation of cm-sized objects in the region of maximum gas pressure (the red dashed line). No shear-induced turbulence exists in this region.The appearing and disappearing of pressure enhancements attracts these clumps and forms larger accumulations. These large accumulations, in turn form km-sized bodies by coalescing with one another and/or undergoing gravitational instability.
Publications
Haghighipour, N. (2007). Planetesimal Formation via Gravitational Instability in Gas-Density Enhanced Regions. Gordon Research Conference, Origins of Solar Systems. Mount Holyoky, Connecticut.
Haghighipour, N. (2008). Gas Density/Pressure Enhanced Regions as Favorable Places for the Formation of Planetesimals via Gravitational Instability. Workshop on Planet Formation Processes and the Development of Prebiotic Conditions. Caltech, Pasadena, California.
![Other Projects](https://webarchive.library.unt.edu/eot2008/20090825142332im_/http://astrobiology.nasa.gov/img/text/hd_other_projects_sa.gif)
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- A search for Main Belt Comets in Pan-STARRS 1
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- A spectroscopically unique Main Belt asteroid: 10537 (1991 RY16)
- A Supertree Analysis of the Metazoan Phylogeny
- Acquisition and Installation of a new Cameca ims 1280 ion microprobe
- Acquisition and Installation of Witec Confocal Raman microscope scanning system
- Amorphization of Crystalline Water Ice in the Solar System
- Assessing the likelihood of supernova impact of protoplanetary disks
- Carbonate Lithologies on Devon Island, Canada
- Chemistry and biology of ultramafic-hosted alkaline springs
- Chemistry of the NH3/H2O system
- DIVERSITY AND BIOGEOGRAPHY OF THE UNIQUE TROPICAL PHYLUM PLACOZOA
- Dynamical Evolution of Astroid Belt and the Parent Bodies of Iron Meteorites
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- FMARS Long Duration Mission: a simulation of manned Mars exploration in an analogue environment, Devon Island, Canada
- Formation and Detection of Hot-Earth Objects in Systems with Close-in Jupiters
- Formation and the Prospects of the Detection of Habitable Planets in Extreme Planetary Systems
- Formation of Molecular Hydrogen via Interaction of Ionizing Radiation with Hydrocarbon Ices in the Interstellar Medium
- Formation of Planetesimals in a Dynamically Evolving Nebula
- FU ORIONIS ERUPTIONS
- Ice Ages on Mars
- Ice at the Mars Phoenix Landing Site
- Ice on Main Belt Comets
- Icelandic subglacial lakes
- Mechanisms of Marine Microbial Community Structuring
- Mechanistical Studies on the Non-Equilibrium Chemistry of Unusual Carbon Oxide in Solar System Ices
- Modeling grain surface reaction pathways for large organic molecules
- Molecular Deuteration on grain surfaces
- NEWBORN BINARIES
- Observations and Models of comet 17P/Holmes
- Origin and Activation Mechanism of Main Belt Comets
- Origin of Irregular Satellites
- Recovery of comet 85P/Boethin for the Deep Impact Extended Mission
- Sediment-buried basement deep biosphere
- Serpentinazation and abiogenic methane in the Mariana Forearc
- Sleeping through the Arctic Martian Sol
- Spectropolarimetric studies of stars with hot jupiters
- TES study of intracrater low albedo deposits, Amazonis Planitia, Mars
- The delivery of short-lived radionucleides to the solar system
- The effect of lunar-like satellites on the orbital infrared lightcurves of Earth-analog planets
- The Main Belt distribution of basaltic asteroids
- The Size Distribution of Small KBOs
- THE VYSOS PROJECT
- Ultra-violet processing of ices in the Rosette Nebula
- Unveiling the evolution and interplay of ice and gas in quiescent clouds
- Variable Young Stellar Objects Survey (VYSOS)
- Water on Mars
- X-ray- and UV-bright low-mass stars in the solar neighborhood