BANK • PEŁNY PODGLĄD
mapy-i-podróże: Asteroid
Historia brzmi jak fake • wikipedia-seeded
ŹRÓDŁA I DOWODY
11 zapisanych źródełEvidence: 69 • authority: 72
The asteroid belt is a torus-shaped region in the Solar System, centered on the Sun and roughly spanning the space between the orbits of the planets Jupiter and Mars. It contains a great many solid, irregularly shaped bodies called asteroids or minor planets. The identified objects are of many sizes, but much smaller than planets, and, on average, are about one million kilometers (or six hundred thousand miles) apart. This asteroid belt is also called the main asteroid belt or main belt to distinguish it from other asteroid populations in the Solar System. The asteroid belt is the innermost and smallest circumstellar disc in the Solar System. Its total mass is estimated to be 3% that of the…
Otwórz źródło ↗Evidence: 41 • authority: 72
In astrodynamics and aerospace, a delta-v budget is an estimate of the total change in velocity (delta-v) required for a space mission. It is calculated as the sum of the delta-v required to perform each propulsive maneuver needed during the mission. As input to the Tsiolkovsky rocket equation, it determines how much propellant is required for a vehicle of given empty mass and propulsion system. Delta-v is a scalar quantity dependent only on the desired trajectory and not on the mass of the space vehicle. For example, although more fuel is needed to transfer a heavier communication satellite from low Earth orbit to geosynchronous orbit than for a lighter one, the delta-v required is the sam…
Otwórz źródło ↗Evidence: 41 • authority: 92
Impactor relics of CI-like chondrites in Chang'e-6 lunar samples.. The impact history of the Moon provides the opportunity to better understand mass transfer in the Solar System. While Earth's meteorite collection serves as a key reference for material flux in the Earth-Moon system, it suffers from profound biases arising from Earth's orbital dynamics and atmospheric filtering. Systematic identification and classification of meteorites on the airless Moon thus provide additional critical constraints for reconstructing the primordial accretion history and impactor population of the inner Solar System. However, identifying impactors on the Moon remains challenging due to their vaporization up…
Otwórz źródło ↗Evidence: 31 • authority: 72
The Earth is unique among known planets in having oceans of liquid water on its surface. It was long thought that Earth's water did not originate from the planet's region of the protoplanetary disk. Instead, it was hypothesized that water and other volatiles must have been delivered to Earth from the outer Solar System later in its history. Recent research, however, indicates that hydrogen inside the Earth played a role in the formation of the ocean. The two ideas are not mutually exclusive, as there is also evidence that water was delivered to Earth by impacts from icy planetesimals similar in composition to asteroids in the outer edges of the asteroid belt. Liquid water, necessary for all…
Otwórz źródło ↗Evidence: 31 • authority: 80
Earth–Moon Separation Problem In The Motion Of Near Earth Asteroids
Otwórz źródło ↗Evidence: — • authority: 72
In astronomy, planetary mass is a measure of the mass of a planet-like astronomical object. Within the Solar System, planets are usually measured in the astronomical system of units, where the unit of mass is the solar mass (M☉), the mass of the Sun. In the study of extrasolar planets, the unit of measure is typically the mass of Jupiter (MJ) for large gas giant planets, and the mass of Earth (M🜨) for smaller rocky terrestrial planets. The mass of a planet within the Solar System is an adjusted parameter in the preparation of ephemerides. There are three variations of how planetary mass can be calculated: If the planet has natural satellites, its mass can be calculated using Newton's law o…
Otwórz źródło ↗Evidence: — • authority: 72
The following is a collection of lists of asteroids of the Solar System that are exceptional in some way, such as their size or orbit. For the purposes of this article, "asteroid" refers to minor planets out to the orbit of Neptune, and includes the dwarf planet Ceres, the Jupiter trojans and the centaurs, but not trans-Neptunian objects (objects in the Kuiper belt, scattered disc or inner Oort cloud). For a complete list of minor planets in numerical order, see List of minor planets. Asteroids are given minor planet numbers, but not all minor planets are asteroids. Minor planet numbers are also given to objects of the Kuiper belt, which is similar to the asteroid belt but farther out (arou…
Otwórz źródło ↗Evidence: — • authority: 72
The two moons of Mars are Phobos and Deimos. They are irregular in shape. Both were discovered by American astronomer Asaph Hall in August 1877 and are named after the Greek mythological twin characters Phobos (fear and panic) and Deimos (terror and dread) who accompanied their father Ares (Mars in Roman mythology, hence the name of the planet) into battle. Compared to the Earth's Moon, the moons Phobos and Deimos are very small. Phobos has a diameter of 22.2 km (13.8 mi) and a mass of 1.08×1016 kg, while Deimos measures 12.6 km (7.8 mi) across, with a mass of 1.5×1015 kg. Phobos orbits closer to Mars, with a semi-major axis of 9,377 km (5,827 mi) and an orbital period of 7.66 hours; while…
Otwórz źródło ↗Evidence: — • authority: 72
The Moon is the only natural satellite of Earth. It orbits Earth in an elliptical path, at a distance that varies over the year, averaging around 378,000 kilometers (235,000 mi). It completes an orbit (lunar month) in relation to Earth and the Sun (synodically) every 29.5 days. The Moon and Earth are bound by gravitational attraction, which is stronger on the sides facing each other. The resulting tidal forces are the main driver of Earth's tides, and have pulled the Moon to always face Earth with the same near side. This tidal locking effectively synchronizes the Moon's rotation period (lunar day) to its orbital period (lunar month). In geophysical terms, the Moon is a planetary-mass objec…
Otwórz źródło ↗Evidence: — • authority: 92
BroadSCOPE: An Optical Broadband Seismic Sensor for Planetary Exploration.. Seismology is crucial for the geologic and interior exploration of planetary bodies. High signal-to-noise (SNR) instruments are required to record low amplitude seismic events such as deep moonquakes. Here we describe the Broadband Seismic Characterization using Optics for Planetary Exploration ("BroadSCOPE") sensor, a broadband planetary seismometer built by Silicon Audio and the Lunar and Planetary Laboratory at the University of Arizona. Our laser interferometer design offers high sensitivity and a high tilt tolerance, while maintaining low power and mass. Our self-noise floor is targeted at 10-9ms-2/Hz at freque…
Otwórz źródło ↗Evidence: — • authority: 72
An asteroid is a minor planet that orbits within the inner Solar System or is co-orbital with Jupiter (Trojan asteroids). These objects are larger than a meteoroid (thus 1 meter or larger) and are neither a planet nor an identified comet. Asteroids are rocky, metallic, or icy bodies with no atmosphere, and are broadly classified into C-type (carbonaceous), M-type (metallic), or S-type (silicaceous). The size and shape of asteroids vary significantly, ranging from small rubble piles under a kilometer across to Ceres, a dwarf planet almost 1000 km in diameter. A body is classified as a comet, not an asteroid, if it shows a coma (tail) when warmed by solar radiation, although recent observatio…
Otwórz źródło ↗