Title: The Little Spacecraft That Could. Subject(s): MOON -- Exploration; LUNAR Prospector (Artificial satellite) Source: Scientific American, Jun99, Vol. 280 Issue 6, p20, 2p, 1 diagram Author(s): Alpert, Mark Abstract: Discusses the scientific mission of the Lunar Prospector spacecraft to gauge the size of the moon's core. Details on the process of measurement; Theories on the moon's origin; Plans for its use in the study of the moon's polar regions. AN: 1893291 ISSN: 0036-8733 Note: Tucson-Pima Public Library subscribes to this magazine. Database: MasterFILE Elite Section: SCIENCE AND THE CITIZEN ASTRONOMY THE LITTLE SPACECRAFT THAT COULD After a string of remarkable discoveries, Lunar Prospector prepares for a spectacular finale Lunar Prospector is not an impressive-looking spacecraft. Shaped like a soup can with its ends cut off, the 295-kilogram (650-pound) orbiter is not much larger than a washing machine. But as it nears the end of its 18-month mission, the plucky vessel continues to provide revealing glimpses of the composition and structure of the moon. The spacecraft first grabbed the public's attention in early 1998, when its instruments detected evidence of ice in the perpetually shadowed areas near the moon's poles. Now mission investigators have announced another important finding: measurements indicating that the moon has a relatively tiny core. The new data reinforce the theory that the moon was created by a cataclysmic collision between Earth and another body more than four billion years ago. The investigators gauged the size of the moon's core in two ways. Because of the Doppler effect, which shifts the frequency of Lunar Prospector's radio signal as the spacecraft moves toward or away from Earth, researchers were able to identify slight variations in the craft's velocity as it orbited the moon. By carefully recording these variations, the scientists mapped the lunar gravitational field and calculated the moon's moment of inertia, which revealed the distribution of the body's mass. Assuming that the moon's core, like Earth's, is composed mostly of iron, researchers estimated that its radius must be between 220 and 450 kilometers (140 to 280 miles). The radius of the moon as a whole is 1,738 kilometers. "It's an indirect measurement, with a lot of uncertainties," says Alan B. Binder, the principal investigator for Lunar Prospector. But Binder and his colleagues had an ingenious plan for refining the estimate. Although the moon's core does not generate a planetary magnetic field, as Earth's does, Lunar Prospector's magnetometer was able to measure the weak field induced in the moon's core when the body passed through the tail of Earth's magnetosphere. From these data, the scientists calculated a core radius of between 300 and 425 kilometers. At this size, the moon's core would contain only about 2 percent of the body's mass. In contrast, Earth's core--which has a radius of about 3,400 kilometers--comprises about 30 percent of the planet's mass. The relative puniness of the moon's core suggests that the moon was born with a severe iron deficiency. Astronomers have theorized that about 4.5 billion years ago a rogue protoplanet, probably two or three times as massive as Mars, slammed into Earth and blasted a huge amount of debris into space. According to this theory, some of the debris clumped together to form the moon. Binder believes the impact occurred after most of Earth's iron had sunk to the planet's core. In that case, the debris expelled into space would have been mostly iron-poor rock from Earth's mantle and from the mantle of the protoplanet. Lunar Prospector may find additional clues to the moon's origins in the last months of its mission. Earlier this year the spacecraft dropped from its 100-kilometer-high mapping orbit to a low elliptical orbit that brings it as close as seven kilometers to the moon's surface. The lower altitude allows the craft to take more accurate readings, although it must fire its thruster every four weeks to avoid hitting the moon. A crash landing, however, is the craft's ultimate fate. On July 31 the mission runs out of funding, and eventually the orbiter will run out of fuel. But even the smashup may yield a scientific return: investigators hope to maneuver Lunar Prospector for an impact in one of the moon's permanently shadowed polar regions. Some scientists are still skeptical about the presence of ice in these areas; to strengthen the evidence, Binder and his colleagues would like to analyze the plume of material that would be ejected by the spacecraft's swan dive. Observatories in Earth orbit, including the Hubble Space Telescope, might be able to see traces of water vapor in the plume. "That would be an absolute confirmation of water," Binder says. Officials at the National Aeronautics and Space Administration have not yet approved the impact experiment. MOON'S CORE DIAGRAMS: Holds only 2 percent of the body's mass (left), whereas Earth's core contains nearly one third of the planet's mass (below). ~~~~~~~~ By Mark Alpert _________________ Copyright of Scientific American is the property of Scientific American Inc. and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. Source: Scientific American, Jun99, Vol. 280 Issue 6, p20, 2p, 1 diagram. Item Number: 1893291