magh Spectro-Polarimetry as a potentially powerful tool for A rbser vat O asteroid studies INAF --Osservatorio Astrofisico di Torino . ry A. Cellino & S. Bagnulo - Helsinki, 19-21/08/2013 Asteroid Spectroscopy and Spectrophotometry (From Bus et al. 2002) magh Spectro-Polarimetry as a potentially powerful tool for A rbser vat O asteroid studies INAF --Osservatorio Astrofisico di Torino A. Cellino & S. Bagnulo - Helsinki, 19-21/08/2013 Asteroid taxonomy has been traditionally based on spectrophotometric properties, in the wavelength range covering UBVRI colors. The distribution of different taxonomic classes as a function of heliocentric distance is related to the general composition gradient of our Solar System . ry magh Spectro-Polarimetry as a potentially powerful tool for A rbser vat O asteroid studies INAF --Osservatorio Astrofisico di Torino A. Cellino & S. Bagnulo - Helsinki, 19-21/08/2013 The mineralogical interpretation of reflectance spectra E, M and P classes are characterized by very different albedo . ry magh Spectro-Polarimetry as a potentially powerful tool for A rbser vat O asteroid studies INAF --Osservatorio Astrofisico di Torino . ry A. Cellino & S. Bagnulo - Helsinki, 19-21/08/2013 Some fundamental problems in current asteroid science: The determination of asteroid masses and densities The measurement of asteroid sizes and shapes The determination of the relation between composition and taxonomic classification The physical characterization of potential Earth impactors In all the above problems a crucial role is played by the problem of determining asteroid albedos magh Spectro-Polarimetry as a potentially powerful tool for A rbser vat O asteroid studies INAF --Osservatorio Astrofisico di Torino . ry A. Cellino & S. Bagnulo - Helsinki, 19-21/08/2013 log(D) 3.1236 0.2H 0.5 log( pV ) Is a fundamental relation in asteroid science, where: D is the equivalent diameter in km. 3.1236 is a wavelength-dependent constant (the indicated value is for V colour) pv is the geometric albedo in V. It is defined as the ratio between the object brightness at zero phase angle and that of an ideal, flat and perfectly Lambertian disk, having the same projected surface of the object. The albedo is an important physical parameter, being related to surface composition, texture and more in general to the history of the object. H is the absolute magnitude in V, that is the apparent brightness that would be measured at unit distance from the Sun and the observer, and at zero phase angle. It varies at different solar oppositions of the same object. magh Spectro-Polarimetry as a potentially powerful tool for A rbser vat O asteroid studies INAF --Osservatorio Astrofisico di Torino Thermal Radiometry A. Cellino & S. Bagnulo - Helsinki, 19-21/08/2013 . ry magh Spectro-Polarimetry as a potentially powerful tool for A rbser vat O asteroid studies INAF --Osservatorio Astrofisico di Torino A. Cellino & S. Bagnulo - Helsinki, 19-21/08/2013 Thermal radiometry results, particularly for albedo, are model-dependent and suffer from poor knowledge of the value to assign to the absolute magnitude H. Radiometric albedoes for small asteroids observed in one single IR band have intrinsic uncertainties up to 60%, due to the uncertainty in the thermal model to be applied in different cases. Akari versus Wise albedoes . ry magh Spectro-Polarimetry as a potentially powerful tool for A rbser vat O asteroid studies ry A. Cellino & S. Bagnulo - Helsinki, 19-21/08/2013 INAF --Osservatorio Astrofisico di Torino Asteroid Polarimetry: What do we measure ? 1 Ceres ( I I // ) Pr ( I I // ) Partial linear polarization and polarization – phase curves. (%) Plane of th e sky I Scat t ering body I Scat t ering plane, SP . Eart h Sun Presence of a “Negative polarization branch” Curve described by a few parameters magh Spectro-Polarimetry as a potentially powerful tool for A rbser vat O asteroid studies INAF --Osservatorio Astrofisico di Torino . ry A. Cellino & S. Bagnulo - Helsinki, 19-21/08/2013 The derivation of the Albedo from polarimetric properties: the “slope – albedo law”. log pV = C1 log (h) + C2 Log(pV) = (-1.035 ± 0.090) log(h) – (1.724 ± 0.104) Improvement of the calibration of the slope-albedo relation needed: work curretly in progress magh Spectro-Polarimetry as a potentially powerful tool for A rbser vat O asteroid studies INAF --Osservatorio Astrofisico di Torino . ry A. Cellino & S. Bagnulo - Helsinki, 19-21/08/2013 Pros: Polarimetry is in principle an excellent technique to derive the albedoes of main belt asteroids and NEOs of all sizes. No dependence on absolute magnitude! Used in the past in asteroid taxonomy to distinguish between E, M, P classes. Cons: Time consuming! You need weeks to get a satisfactory coverage of the phase- polarization curve of a main belt asteroid! (much less time is needed for near-Earth asteroids). magh Spectro-Polarimetry as a potentially powerful tool for A rbser vat O asteroid studies ry A. Cellino & S. Bagnulo - Helsinki, 19-21/08/2013 INAF --Osservatorio Astrofisico di Torino Courtesy of I.N. Belskaya C-type . S-type E-type NEA Polarimetry Presence of a wide branch of positive polarization with a maximum near 90°polarimetry is inherently NEO efficient, since the rate of variation of the phase angle is fast for these objects, and a polarimetric slope can be obtained in a short time. Interesting for the purposes of ESA SSA program Even a single measurement of polarization at phase > 40 deg can be sufficient to obtain an overall albedo estimation! Very small (faint) NEAs are observable with the VLT (as shown by the case of Apophis). magh Spectro-Polarimetry as a potentially powerful tool for A rbser vat O asteroid studies INAF --Osservatorio Astrofisico di Torino . ry A. Cellino & S. Bagnulo - Helsinki, 19-21/08/2013 First results about wavelength dependence of linear polarization Opposite behaviour among moderate-albedo and lowalbedo asteroids. Similar effects observed also for comets. Belskaya et al., Icarus 199, 97-105 (2009) Full spectro-polarimetry never attempted so far for asteroids! UBVRI Itokawa observations at CASLEO magh Spectro-Polarimetry as a potentially powerful tool for A rbser vat O asteroid studies INAF --Osservatorio Astrofisico di Torino EXAMPLE: POLARIMETRIC OBSERVATIONS OF (25143) ITOKAWA AT LARGE PHASE ANGLES in 2004 at CASLEO Linear fits of UBVRI data obtained in five colors in consecutive nights, covering a large interval of phase angles A. Cellino & S. Bagnulo - Helsinki, 19-21/08/2013 . ry magh Spectro-Polarimetry as a potentially powerful tool for A rbser vat O asteroid studies INAF --Osservatorio Astrofisico di Torino . ry A. Cellino & S. Bagnulo - Helsinki, 19-21/08/2013 The preliminary results obtained so far, if confirmed, would imply that one single spectro-polarization measurement obtained at different wavelengths either at large phase angles (> 20o) or at a phase angle around 10o could be sufficient to distinguish between asteroids belonging to different albedo and taxonomic classes. Stay tuned! We have been awarded the first observing run of asteroid spectro-polarimetry at VLT in the next observing semester ! magh Spectro-Polarimetry as a potentially powerful tool for A rbser vat O asteroid studies INAF --Osservatorio Astrofisico di Torino . ry A. Cellino & S. Bagnulo - Helsinki, 19-21/08/2013 Other interesting targets for observations: the “Barbarians” future Known objects: 234 (Ld - class), 172, 236, 387, 980 (L – class) 679 (K - class) Unusual spectra, presence of CAI compounds on the surfaces. Possible association with some dynamical families. Masiero and Cellino (2009) (dashed and dotted lines show, for a comparison, typical polarizationphase curves for B-type ((24) Themis) and L-type ((12) Victoria) asteroids, respectively) magh Spectro-Polarimetry as a potentially powerful tool for A rbser vat O asteroid studies A. Cellino & S. Bagnulo - Helsinki, 19-21/08/2013 INAF --Osservatorio Astrofisico di Torino Asteroid polarimetry as a support to space missions: the examples of Steins and Lutetia 0.0 1.5 21 Lutetia 2867 Steins -0.5 1.0 K 0.5 Pmin (%) Polarization degree (%) 2867E E AR -1.0 0.0 F F -1.5 -0.5 Sw V SSw Sq-SSS SKS SSSS SSS M M M M B C -2.0 -1.0 -1.5 -2.5 0 5 10 15 20 Phase angle (deg) 25 30 12 Courtesy of I.N. Belskaya 16 21 Cx ChCh Ch C Ch Ch Ch Cqh Ch Cgh Ch 20 inv(deg) L 24 28 . ry magh Spectro-Polarimetry as a potentially powerful tool for A rbser vat O asteroid studies INAF --Osservatorio Astrofisico di Torino A. Cellino & S. Bagnulo - Helsinki, 19-21/08/2013 Thank you . ry