3700 Geowilliams

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3700 Geowilliams
Discovery [1]
Discovered by C. Shoemaker
E. Shoemaker
Discovery site Palomar Obs.
Discovery date23 October 1984
Designations
(3700) Geowilliams
Named after
George E. Williams [1]
(Australian geologist)
1984 UL2 ·1973 YF2
1977 UJ
main-belt [1] [2]  ·(inner) [3]
background [4]
Orbital characteristics [2]
Epoch 23 March 2018 (JD 2458200.5)
Uncertainty parameter 0
Observation arc 43.54 yr (15,902 d)
Aphelion 2.9602 AU
Perihelion 1.8695 AU
2.4148 AU
Eccentricity 0.2258
3.75 yr (1,371 d)
293.18°
0° 15m 45.36s / day
Inclination 12.121°
289.16°
153.06°
Physical characteristics
Mean diameter
7.712±0.130  km [5]
7.74±1.83 km [6]
7.753±0.152 km [7]
8.70±0.30 km [8]
8.82±0.86 km [9]
8.97 km(calculated) [3]
14.383±0.0183  h [10]
14.387±0.003 h [lower-alpha 1]
0.20(assumed) [3]
0.227±0.045 [9]
0.23±0.13 [6]
0.233±0.033 [8]
0.2970±0.0516 [5]
SMASS = S k [2]
12.443±0.002(R) [10]
12.50 [5] [8] [9]
12.6 [2] [3]
12.89 [6]
12.94±0.46 [11]

    3700 Geowilliams, provisional designation 1984 UL2, is a stony background asteroid from the inner regions of the asteroid belt, approximately 8 kilometers (5 miles) in diameter. It was discovered on 23 October 1984, by American astronomer couple Carolyn and Eugene Shoemaker at the Palomar Observatory in California, United States. [1] The S k-subtype has a rotation period of 14.38 hours. It was named for Australian geologist George E. Williams. [1]

    Contents

    Orbit and classification

    Geowilliams is a non-family asteroid from the main belt's background population. [4] It orbits the Sun in the inner main-belt at a distance of 1.9–3.0  AU once every 3 years and 9 months (1,371 days; semi-major axis of 2.41 AU). Its orbit has an eccentricity of 0.23 and an inclination of 12° with respect to the ecliptic. [2] The body's observation arc begins with its first observation as 1973 YF2 at Crimea-Nauchnij in December 1973, almost 11 years prior to its official discovery observation at Palomar. [1]

    Physical characteristics

    In the SMASS classification, Geowilliams is a Sk-subtype that transitions between the common S-type asteroid and the K-type asteroid. The latter spectral type is often found among members of the Eos family. [2]

    Rotation period

    In January 2008, a rotational lightcurve of Geowilliams was obtained from photometric observations by Australian amateur astronomer David Higgins at the Hunters Hill Observatory ( E14 ). Lightcurve analysis gave a well-defined rotation period of 14.387 hours with a brightness variation of 0.40 magnitude ( U=3 ). [lower-alpha 1] In July 2010, a similar period of 14.383 hours and an amplitude of 0.42 was measured at the Palomar Transient Factory in California ( U=2 ). [10]

    Diameter and albedo

    According to the surveys carried out by the Japanese Akari satellite and the NEOWISE mission of NASA's Wide-field Infrared Survey Explorer, Geowilliams measures between 7.712 and 8.82 kilometers in diameter and its surface has an albedo between 0.227 and 0.297. [5] [6] [7] [8] [9]

    The Collaborative Asteroid Lightcurve Link assumes a standard albedo for a stony asteroid of 0.20, and calculates a diameter of 8.97 kilometers based on an absolute magnitude of 12.6. [3]

    Naming

    This minor planet was named after Australian geologist George E. Williams who discovered the Acraman crater when he worked for BHP in South Australia. The old 90-kilometer impact structure is one of the largest meteorite impact craters known on Earth and the largest one on the Australian continent. [1] The official naming citation was published by the Minor Planet Center on 2 February 1988 ( M.P.C. 12810). [12]

    Notes

    1. 1 2 David Higgins (2011): rotation period 14.387±0.003 hours with a brightness amplitude of 0.40±0.02 mag. Quality code is 3. Summary figures for (3700) Geowilliams at the LCDB and archived website of the Hunters Hill Observatory by David Higgins.

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    References

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