Abstract
CCD photometric observations of four main-belt and one near-Earth asteroid were made in 2019. Of these, the Vestoid 2602 Moore and Hungaria (27568) 2000 PT6 were confirmed to be binary asteroids. The Hungaria 3880 Kaiserman is a suspected binary. Near-Earth asteroid (142040) 2002 QE15 was found to have a long period (46.4 h). Re-evaluation of data for the asteroid from two previous apparitions found a secondary period that is consistent with the system being a candidate for the rare class of very wide binary asteroids. New analysis of the data from 2016 for Phocaea member 2937 Gibbs found two periods (the second being ambiguous). It could not be determined if the asteroid is binary or in a tumbling state.
CCD photometric observations of five asteroids were conducted in 2019 April-July as part of ongoing work at the Center for Solar System Studies (CS3) to find the rotation periods of asteroids. The primary targets are near-Earth asteroids but, when there are no such objects within reach of our instruments or they are poorly placed, we observe main-belts objects, concentrating on Jupiter Trojans, Hildas, and Hungarias.
Table I lists the telescopes and CCD cameras that are combined to make observations. Up to nine telescopes can be used for the campaign, although seven is more common. All the cameras use CCD chips from the KAF blue-enhanced family and so have essentially the same response. The pixel scales ranged from 1.24–1.60 arcsec/pixel. All lightcurve observations were unfiltered since a clear filter can result in a 0.1–0.3 magnitude loss. The exposures varied depending on the asteroid’s brightness and sky motion.
Table I.
List of available telescopes and CCD cameras at CS3. The exact combination for each telescope/camera pair can vary due to maintenance or specific needs.
| Telescopes | Cameras |
|---|---|
| 0.30-m f/6.3 Schmidt-Cass | FLI Microline 1001E |
| 0.35-m f/9.1 Schmidt-Cass | FLI Proline 1001E |
| 0.35-m f/11 Schmidt-Cass | SBIG STL-1001E |
| 0.4 0-m f/10 Schmidt-Cass | |
| 0.50-m f/8.1 Ritchey-Chretien |
Measurements were made using MPO Canopus. The Comp Star Selector utility in MPO Canopus found up to five comparison stars of near solar-color for differential photometry. Comp star magnitudes were taken from ATLAS catalog (Tonry et al., 2018), which has Sloan griz magnitudes that were derived from the GAIA and Pan-STARR catalogs, among others. The authors state that systematic errors are generally no larger than 0.005 mag, although they can reach 0.02 mag in small areas near the Galactic plane. BVRI magnitudes were derived by Warner using formulae from Kostov and Bonev (2017). The overall errors for the BVRI magnitudes, when combining those in the ATLAS catalog and the conversion formulae, are on the order of 0.04–0.05.
Even so, we found in most cases that nightly zero point adjustments on the order of only 0.02–0.03 mag were required during period analysis. There were occasional exceptions that required up to 0.10 mag. These may have been related in part to using unfiltered observations, poor centroiding of the reference stars, and not correcting for second-order extinction terms. Regardless, the systematic errors seem to be considerably less than other catalogs, which reduces the uncertainty in the results when analysis involves data from extended periods or the asteroid is tumbling.
Period analysis was done with MPO Canopus, which implements the FALC algorithm by Harris (Harris et al., 1989). The same algorithm is used in an iterative fashion when it appears there is more than one period. This works well for binary but not for tumbling asteroids.
In the plots below, the “Reduced Magnitude” is Johnson V. These have been converted from sky magnitudes to unity distance by applying −5*log (rΔ) with r and Δ being, respectively, the Sun-asteroid and Earth-asteroid distances in AU. The magnitudes were normalized to the phase angle in parentheses using G = 0.15. The X-axis is the rotational phase ranging from −0.05 to 1.05. If the plot includes an amplitude, it is for the Fourier model curve and not necessarily the adopted amplitude for the lightcurve.
Our initial search for previous results started with the asteroid lightcurve database (LCDB; Warner et al., 2009) found on-line at http://www.minorplanet.info/lightcurvedatabase.html. Readers are strongly encouraged to obtain, when possible, the original references listed in the LCDB.
2602 Moore.
Stephens observed this asteroid in 2019 April and May. Soon after the observations began, there were indications of attenuations that might be attributed to a satellite. An extensive campaign covered almost a month and confirmed the attenuations as being occultation and/or eclipses (mutual events) due to a satellite.
The three plots show the data without subtracting a second period followed by the results of the dual-period search. The depth of the attenuations ranged from 0.08–0.14 mag. Using the smaller value, we estimate an effective diameter ratio of satellite-to-primary Ds/Dp ≥ 0.28 ± 0.02. There were no previous lightcurve results posted in the LCDB.


2937 Gibbs.
There were several results posted in the LCDB for this 6-km Phocaea asteroid. Behrend (2005) reported 3.06153 h based on observations in 2005 August. His group observed again four months later and found a similar but less precise P = 3.06 h. Co-author Stephens (2017) found P = 3.189 h using data from 2016 December. This is similar to the Behrend results but differs by several sigma.
New observations made in 2019 June led to a significantly shorter period of 2.982 h. The new data could not be fit to the previous results. Given the large amplitude and relatively low solar phase angle, we adopted 2.982 h to be the true period and took another look at the data from 2016, forcing it to be near 2.98 h.

The “NoSub” plot shows what appear to be deviations in the lightcurve but the nosier data and smaller amplitude made those uncertain, at least to start. Our dual-period search found a very good fit to P1 = 2.984 h after subtracting each of several possible secondary periods, P2. Regardless of which secondary period was used, the result for P1 remained the same.

The period spectrum for the secondary period (“2016 P2”) showed four possibilities with the one near 11 hours being the half-period of the longest solution of about 22 hours.


We examined the solutions at 5.6 h, 7.49 h, and 22.43 h to see which would produce the most plausible result. At P2 = 5.62 h, the fit is acceptable given the scatter in the data set. It’s important to note that this P2 is not harmonically related to P1, i.e., they do not have an integer ratio.
On the other hand, the remaining two solutions have nearly integral ratios with P1. The lightcurve at P2 = 7.49 h is almost trimodal, which is possible because of the low amplitude (Harris et al., 2014). The lightcurve at P2 = 22.43 h is clearly wrong and simply a fit by exclusion, which is where the Fourier algorithm finds a local RMS minimum by minimizing the number of overlapping data points.
The harmonic relation between P1 and P2 = 7.49 h raises the possibility that the asteroid is in a low-level tumbling state where P1 = 2.984 h dominates the solution and a linear combination of rotation and precession frequencies produces a “beat frequency” that is n/7.49, with n being an integer value. This is not uncommon (see Harris et al., 2014; Pravec et al., 2014; 2005).
3880 Kaiserman.
We observed this Hungaria member twice before the latest observations. Warner (2012b) found a period of 5.270 h. In 2014 Warner (2015b) found a period of 5.227 h as well as indications of a secondary period of 22.16 h that was attributed to a possible satellite.

Our 2019 data also gave indications of a secondary period. The dual-period analysis found P1 = 5.271 h, in agreement with Warner (2012b), and P2 = 16.09 h. The lightcurve for P2 is low amplitude (0.05 mag) but appears to be bimodal and has a shape typically seen for elongated satellites that are tidally-locked to the orbital period.
(27568) 2000 PT6.
This was the fourth time we observed this Hungaria. Warner (2012a) reported a period of 3.624 h, but this was revised to 3.493 h after the data from observations in 2013 (Warner and Stephens, 2013) led to a period of 3.4885 h. They also reported the possibility of the asteroid being binary, with an orbital period of 16.353 h and estimated Ds/Dp of 0.22. Follow-up observations in 2014 (Warner, 2015a) found indications of a satellite but the orbital period was 11.73 h and there was no estimate of the effective diameters ratio.
The 2019 data leave little doubt that the asteroid is binary with an the satellite tidally-locked to an orbital period of 16.099 h. The satellite’s lightcurve shape indicates an elongated body. We estimate Ds/Dp ≥ 0.23 ± 0.04

(142040) 2002 QE15.
Pravec et al. (2002) observed this NEA in 2002 September-October and reported a period of 2.5811 h. When we observed it in 2015 (Warner, 2016) and 2017 (Warner, 2018), we did not think that our 3.88 h lightcurves were superimposed on a long period lightcurve. Then again, as we found we did in the past, the adjustments of the nightly zero points maybe have removed the traces of a long period.
We observed the asteroid again in 2019 May and June. With the ATLAS catalog (Tonry et al., 2018) and the higher confidence in nightly zero points, we found a P = 46.4 h. This made it a possible very wide binary asteroid (see, e.g., Warner and Stephens, 2019; and references therein). This rare class has about 30 candidates, some with very convincing evidence, that features a primary long primary period (> 24 h to 500+ h) with an underlying short period (usually 2–5 h) with a lightcurve that looks like a typical primary of an “ordinary” binary asteroid.

The data set in 2019 was too sparse and noisy to find a secondary period, especially if it had a particularly low amplitude. However, we returned to our previous data sets to see if we might have overlooked something. Part of this was to reset zero points and not change them significantly.
The new analysis of the 2015 data set found a low-amplitude (0.11 mag) lightcurve with a period of 47.1 h, which was in reasonable agreement with the 2019 result. Once that long period was subtracted in a dual-period search, we found a convincing solution of 3.891 h, which is close to what we found in the previous single period result. The 2017 data set provided a convincing case as well with the long-period lightcurve period of 48.1 h and a short period of 3.856 h, in reasonable agreement with the short period from the 2015 reanalysis and single period results.


Table II.
Observing circumstances. The phase angle (α) is given at the start and end of each date range. LPAB and BPAB are the average phase angle bisector longitude and latitude (see Harris et al., 1984). The additional lines after the first, complete line give the periods associated with a satellite or alternate solutions for a second period. The Grp column gives the family/group (Warner et al., 2009). H: Hungaria; MC: Mars-crosser; NEA: Near-Earth asteroid; V: Vestoid.
| Number | Name | 20xx/mm/dd | Phase | LPAB | BPAB | Period(h) | P.E. | Amp | A.E. | Grp |
|---|---|---|---|---|---|---|---|---|---|---|
| 2602 | Moore | 19/04/17–05/15 | 22.1, 27.1 | 164 | 2 | 3.46723 | 0.00003 | 0.43 | 0.01 | V |
| Satellite | 27.455 | 0.003 | 0.15 | 0.01 | ||||||
| 2937 | Gibbs | 16/12/17–12/19 | 8.8, 7.9 | 103 | −7 | 2.984 | 0.001 | 0.25 | 0.02 | MC |
| P2 Alt1 | 5.62 | 0.01 | 0.14 | 0.02 | ||||||
| P2 Alt2 | 7.49 | 0.01 | 0.14 | 0.02 | ||||||
| 3880 | Kaiserman | 19/07/01–07/07 | 11.9, 23.4 | 280 | 10 | 5.2694 | 0.0007 | 0.14 | 0.01 | H |
| Satellite? | 16.09 | 0.02 | 0.05 | 0.01 | ||||||
| 27568 | 2000 PT6 | 19/06/26–07/07 | 21.9, 43.4 | 268 | 31 | 3.5006 | 0.0003 | 0.25 | 0.02 | H |
| Satellite | 16.099 | 0.008 | 0.18 | 0.02 | ||||||
| 142040 | 2002 QE15 | 19/05/24–06/02 | 9.6, 11.7 | 245 | 15 | 46.4 | 0.2 | 0.19 | 0.03 | NEA |
| 142040 | 2002 QE15 | 15/07/14–07/21 | 51.7, 53.4 | 349 | 43 | 47.1 | 0.1 | 0.11 | 0.01 | |
| Satellite? | 3.891 | 0.001 | 0.15 | 0.02 | ||||||
| 142040 | 2002 QE15 | 17/08/21–08/29 | 46.6, 48.7 | 288 | 44 | 48.1 | 0.2 | 0.20 | 0.03 | |
| Satellite? | 3.856 | 0.003 | 0.11 | 0.02 |
Acknowledgements
Funding for observations at CS3 and work on the asteroid lightcurve database (Warner et al., 2009) and ALCDEF database (alcdef.org) are supported by NASA grant 80NSSC18K0851.
This work includes data from the Asteroid Terrestrial-impact Last Alert System (ATLAS) project. ATLAS is primarily funded to search for near earth asteroids through NASA grants NN12AR55G, 80NSSC18K0284, and 80NSSC18K1575; byproducts of the NEO search include images and catalogs from the survey area. The ATLAS science products have been made possible through the contributions of the University of Hawaii Institute for Astronomy, the Queen’s University Belfast, the Space Telescope Science Institute, and the South African Astronomical Observatory.
The authors gratefully acknowledge Shoemaker NEO Grants from the Planetary Society (2007, 2013). These were used to purchase some of the telescopes and CCD cameras used in this research.
Contributor Information
Brian D. Warner, Center for Solar System Studies / MoreData!, 446 Sycamore Ave., Eaton, CO 80615 USA
Robert D. Stephens, Center for Solar System Studies / MoreData!, Rancho Cucamonga, CA
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