Lunar Dynamics And A Search For Objects Near the Earth-Moon Lagrangian Points Jill Eymann Abstroct. For the Saint Mary's College Summer Research Project, I propose performing a CD imaging search of the Earth-Moon Lagrangian positions, including the solar-synchronized positions in the stable L4/15 libration orbits. Observations using the 0.5-m SC telescope at the SMC Norma Geissberger Observatory will span 60" along the lunar orbital plane x 5' around Earth-Moon 15, 45" x 5' around 14. Limiting magnitude for the detection of libration objects near 14, and L5 is assumed to be 17-l-9th magnitude, the fainter limit depending on superior observing conditions. An automated search of selected priority will be attempted using the Faint Object Classification and Analysis System (FOCAS) software package from the National Optical Astronomy Observatories. Background. ln astronomy, the adjective 'trojan' refers to a minor planet or natural satellite (moon) that shares an orbit with a larger planet or moon, but does not collide with it because it orbits around one of the two Lagrangian points of stability, L4 and 15, which lie 60' ahead of and behind the larger body. The term originally referred to the Trojan asteroids orbiting Jupiter's Lagrangian points, as shown in the figure below. Subsequently, objects have been found orbiting the Lagrangian points of Neptune as well as Mars. ln addition, trojan moons are known to orbit the Lagrangian points of two of Saturn's mid-sized moons. With this in mind, my project will explore the Lagrangian Points in the Earth-Moon system in an attempt to discover natural satellites in those regions. The Lagrangian points, are the five positions in an orbital configuration where a small object affected only by gravity can theoretically be stationary relative to two larger objects (such as a satellite with respect to the Earth and Moon). The Lagrange points mark positions where the combined gravitational pull of the two large masses provides precisely the centripetal force required to rotate with them. They are analogous to geostationary orbits in that they allow an object to be in a "fixed" position in space rather than an orbit in which its relative position changes continuously. +12 Moon xLl \ i Earth I s' I ''''...-''geostationdrY J orbil i I I l \ ,l \ Moon's orbit \\-a\\- .-*-'*-*"**L3* A more precise but technical definition is that the Lagrangian points are the stationary solutions of the circular restricted three-body problem in gravitational physics. For example, given two massive bodies in circular orbits around their common center of mass, there are five positions in space where a third body, of comparatively negligible mass, could be placed which would then maintain its position relative to the two massive bodies. As seen in a rotating reference frame with the same period as the two coorbiting bodies, the gravitational fields of two massive bodies combined with the centrifugal force are in balance at the Lagrangian points, allowing the third body to be stationary with respect to the first two bodies. Lagrangian satellite searches may be useful in detecting captured asteroidal bodies or impact ejecta from the lunar surface; this unique and accessible material is important for astro-geological study and could also help confirm theoretical predictions in the four-body problem in celestial mechanics. Also, determining whether or not the stable libration orbits are clear of large obstacles is practical because of the potential future use of these orbits for global telecommunication satellite systems and solar deepspace telemetry networks, space manufacturing facilities utilizing lunar or asteroidal raw materials, large optical and radio telescope arrays, and/or as part of a comprehensive SETI (Search for Extraterrestrial lntelligence) search for possible alien artifacts in the Solar System (Freitas, 1980). The current observational status of the triangular libration orbits and L4/15 is sporadic with limits of L2- 14th magnitude (Freitas and Valdes, 1980); even after almost 20 years, the existence of material at these points remains controversial. No searches for material at Earth-Moon L3 have been reported in the literature. The lunar halo survey near Earth-M oon LL/L2 involves an investigation of the same orbital space examined during previous searches for selenocentric satellites. The best modern effort encompasslng was byTombaugh et al. (1959), who achieved a limit of 11-12th magnitude in the region No environment. the L1/12 halo orbits and 13-14th magnitude for most of the rest of the lunar satellite have been reported in the searches for discrete objects fainter than 14th magnitude near sun-Earth L2 literature. lt is time to revisit the problem and to renew a search with modern experimental facilities. OBSERVING PROGRAM objects in the The observing program, with the major goal of obtaining maximum sensitivity to discrete lunar orbital plane, will pursue five distinct objectives as follows. (tracked Eorth-Moon L4/15 Libration orbit objects. My highest priority will be to obtain pairs of images The telescope and sidereal) at the unique solar-synchronized stable phases in the L4/15 libration orbits. methods drive will be adjusted to track the predicted stable libration orbital positions computed by the erred described in Freitas and Valdes (1980). Previous observers (e.g., Bruman, 1969) have sometimes the lunar drastically by using a simple 1-/6 Moon phase formula and then neglecting to take into account orbital eccentricity and the fact that each lunar ephemeris tabulated in the Nautical Almanac in incorporates the heliocentric motion of the observer, all of which can cause pointing inaccuracies predicted to be dynamically excess of 10.. Though the Lagrangian points L4 and L5 are themselves Each CCD unstable, a third CCD image pair will be taken at both L4 and L5 tracked at the lunar rate. image will be a sky-limited exposure determined by nightly conditions. Eorth-Moon L4/15 Libration Orbit Survey. The degree of stability and the mechanics of trapping objects in precisely the theoretical libration orbit and phase are unknown. Oscillations around the ideal stable locations (in the Earth-Moon plane) are likely for natural objects injected into such orbits with arbitrary initial conditions; in which case possible trapped bodies may deviate significantly from the solarless synchronized positions. Also, the extent of out-of-plane motion is thought to be a few degrees or (Roosen eI al., !967;Schechter, 1968; Schutz and Tapley ,1970), but is, at present, undetermined by reliable theoretical computations. Consequently, a series of CCD images spanning more than the entire 45. libration orbit regions with 0.5" overlap will be tracked at the lunar rate. Survey images on successive nights will be overlapped to compensate for possible diurnal object movement. The choice of observing time is dictated by a number of factors that serve to maximize the probability of detection of faint libration objects with known or anticipated orbital characteristics. To obtain the maximum reflected brightness from bodies trapped near L4 and 15, the following conditions need to be satisfied: (1) end of astronomical twilight; (2) end of lunar twilight; (3) maximum lunar declination for a (5) minimum zenith angle for L4 or L5; (4) maximum elongation angle of solar-synchronized objects; minimum reflection angle ensuring "full" phase of possible targets; (6) maximum distance from the (15) Milky Way background for L4 and L5; and (7) maximum post-moonset (14) or pre-moonrise (5) and (7) observing time. For libration orbit objects the best compromise between requirements places the Moon no more than 95' (7.4 days lunar phase) from the Sun. Hence a four-night observation schedule is best completed over the lunar-phase Days 5-8 for L4 and Days21'-24 for 15. t REFERENCES BREAKWELL, J. V. AND J. V. BROWN (1979). The 'halo' family of 3-dimensional periodic orbits in the Earth-Moon restricted 3-body problem. Celest. Mech. 20,389-404. BRUMAN, J. R. (1969). A lunar libration point experiment. lcarus 10,197-200. FARQUHAR, R. W. (1970). The Moon's influence on the location of the Sun-Earth exterior libration point. Celest. Mech. 2, 13I-133. FRE1TAS, R. A., JR. (1980). lnterstellar probes:A new approach to SETI. i. Brit. lnterplanet. Soc.33,95- 100. FRE;TAS, R. A., JR., AND F. VALDES (1980). A search for natural or artificial objects located at the Earth- Moon libration points. lcarus 42,442-447. JARV|S, J. F., AND J. A. TYSON (1930). FOCAS: Faint Object Classification and Analysis System. Astron. J. 86,476-495. ROOSEN, R. G., R. S. HARRTNGTON, W. H. JEFFREYS, J. W. SIMPSON, AND R. G. MILLER (1967]'. Doubt about liberation clouds. Phys. Today 20(5), 10-15. SCHECHTER, H. B. (1968). Three-dimensional nonlinear stability analysis of Sun-perturbed Earth-Moon equilateral points. AIAA J. 6,1223-1228. SCHUTZ, B. E., AND B. D. TAPLEY (1970). Numerical studies of solar influenced particle motion near the triangular Earth-Moon libration points. ln Periodic Orbits, Stability and Resonances (G. Ed.), pp. !28-1,42. Reidel, Dordrecht. E. 0. Giacaglia, VALDES, F. (1932). Faint Object Classification and Analysis System. Kitt Peak National Observatory, Computer Support Group, Tucson, Arizona. I
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