Asteroid Tracking and Spectroscopy

Overview

Project Advisors: Dr. Sarah Sonnett, Dr. George Chartas

Conducted research on the detection of the presence of hydrated minerals on C-type and S-type asteroids in the Hilda and Cybele clusters. For this project, I utilized Fast Fourier Transforms (FFTs), Hanning smoothing functions, Gaussian fitting, and signal normalization techniques to turn raw standard star and asteroid data obtained from Las Cumbres Observatory (LCO) telescopes into spectroscopic data with asteroid chemical signatures. Data was obtained using diffraction grating and spectrometer data in the infrared and visible wavelength regime. Additionally, I scheduled the observations by generating ephemerides using the JPL Small Body Database, local atmospheric conditions, asteroid tracker maps.

Observation

Asteroids to be observed were selected through a filtering process on the JPL Small Bodies database and nearby solar analog stars were selected through the SIMBAD database. Dark frames were taken first, followed by observations of planetary nebula, solar analog stars, and the asteroid targets. Asteroid and star images were taken using the SA-200 diffraction grating to obtain spectral data on the Rita Hollings Observatory telescope, with other data coming from collaborators at LCO telescopes in Australia and Hawaii.

Centroiding and Rotation

Asteroid and star location within the frame was determined by planetary nebula observation. The zeroth and end of first order spectral pixel coordinates were calculated using circular regions to centroid them in DS9 software. Dark-subtracted images were rotated by the angle based on the location of the values from the centroiding process. This allowed us to properly align the spectrometer image data (the bright line), coming from the asteroid (bright dot in the circle).

Wavelength Calibration

The detector gives an output of what CCD pixel a photon interacted with, not wavelength. We implemented a linear fit of pixel position from the known spectral lines of a planetary nebula observed that night. The slope value is used to calibrate pixel position to wavelength values for both the solar analog and the target spectra.

Planetary nebula strong spectral lines used for calibration (Meinel et al., 1975)

Spectrum of the planetary nebula IC 4997

Cross Correlation

The solar analog spectrum is divided from the asteroid spectrum to obtain the corrected spectrum of the asteroid. If the centroiding is off by a few pixels, anomalies can appear in the corrected spectra. We calculated and shifted the star spectrum by the lag between the sharp telluric (i.e. atmospheric) features present in both spectra.

Results

Hydrated minerals were not detected on Hebe or Mnemosyne, but other previously undiscovered absorption features were detected that could possibly indicate other forms of water on the asteroid. The novel application of the cross correlation shift to the interpolated spectrum we believe can greatly improve the accuracy of results in many types of spectroscopy research. Solar corrected asteroid spectra displayed wavelength to detector counts typical of S-type asteroids, with less counts in bluer wavelengths.