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Physics-Based Modeling of Meteor Entry and BreakupA new research effort at NASA Ames Research Center has been initiated in Planetary Defense, which integrates the disciplines of planetary science, atmospheric entry physics, and physics-based risk assessment. This paper describes work within the new program and is focused on meteor entry and breakup.Over the last six decades significant effort was expended in the US and in Europe to understand meteor entry including ablation, fragmentation and airburst (if any) for various types of meteors ranging from stony to iron spectral types. These efforts have produced primarily empirical mathematical models based on observations. Weaknesses of these models, apart from their empiricism, are reliance on idealized shapes (spheres, cylinders, etc.) and simplified models for thermal response of meteoritic materials to aerodynamic and radiative heating. Furthermore, the fragmentation and energy release of meteors (airburst) is poorly understood.On the other hand, flight of human-made atmospheric entry capsules is well understood. The capsules and their requisite heatshields are designed and margined to survive entry. However, the highest speed Earth entry for capsules is 13 kms (Stardust). Furthermore, Earth entry capsules have never exceeded diameters of 5 m, nor have their peak aerothermal environments exceeded 0.3 atm and 1 kW/sq cm. The aims of the current work are: (i) to define the aerothermal environments for objects with entry velocities from 13 to 20 kms; (ii) to explore various hypotheses of fragmentation and airburst of stony meteors in the near term; (iii) to explore the possibility of performing relevant ground-based tests to verify candidate hypotheses; and (iv) to quantify the energy released in airbursts. The results of the new simulations will be used to anchor said risk assessment analyses. With these aims in mind, state-of-the-art entry capsule design tools are being extended for meteor entries. We describe: (i) applications of current simulation tools to spherical geometries of diameters ranging from 1 to 100 m for an entry velocity of 20 kms and stagnation pressures ranging from 1 to 100 atm; (ii) the influence of shape and departure of heating environment predictions from those for a simple spherical geometry; (iii) assessment of thermal response models for silica subject to intense radiation; and (iv) results for porosity-driven gross fragmentation of meteors, idealized as a collection of smaller objects. Lessons learned from these simulations will be used to help understand the Chelyabinsk meteor entry up to its first point of fragmentation.
Document ID
20150018060
Acquisition Source
Ames Research Center
Document Type
Conference Paper
Authors
Prabhu, Dinesh K.
(ERC, Inc. Moffett Field, CA, United States)
Agrawal, Parul
(ERC, Inc. Moffett Field, CA, United States)
Allen, Gary A., Jr.
(ERC, Inc. Moffett Field, CA, United States)
Bauschlicher, Charles W., Jr.
(NASA Ames Research Center Moffett Field, CA, United States)
Brandis, Aaron M.
(ERC, Inc. Moffett Field, CA, United States)
Chen, Yih-Kang
(NASA Ames Research Center Moffett Field, CA, United States)
Jaffe, Richard L.
(NASA Ames Research Center Moffett Field, CA, United States)
Palmer, Grant E.
(ERC, Inc. Moffett Field, CA, United States)
Saunders, David A.
(ERC, Inc. Moffett Field, CA, United States)
Stern, Eric C.
(ERC, Inc. Moffett Field, CA, United States)
Tauber, Michael E.
(ERC, Inc. Moffett Field, CA, United States)
Venkatapathy, Ethiraj
(NASA Ames Research Center Moffett Field, CA, United States)
Date Acquired
September 17, 2015
Publication Date
April 13, 2015
Subject Category
Astrodynamics
Report/Patent Number
ARC-E-DAA-TN21934
Meeting Information
Meeting: 2015 IAA Planetary Defense Conference
Location: Frascati
Country: Italy
Start Date: April 13, 2015
End Date: April 17, 2015
Sponsors: International Academy of Astronautics
Funding Number(s)
CONTRACT_GRANT: NNA10DE12C
Distribution Limits
Public
Copyright
Public Use Permitted.
Keywords
Near-Earth Asteroids
Atmospheric Entry
Energy Deposition
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