概括
与地球和金星相比,火星在其历史上产生的岩明显少,但比月球更多. 这表明相对于火星的大小和历史,火星上的火山活动较低.
科学领域:
- 行星科学 行星科学
- 火山学 火山学是一门学科.
- 地质物理学 地质物理学
背景情况:
- 了解行星进化需要量化岩生成速率.
- 火星展示了过去火山活动的证据,但它的总岩石产量并没有受到很好的约束.
研究的目的:
- 为了估计火星上在过去38亿年中产生的岩的总体体积和速度.
- 为了比较火星的岩生成率与地球,金星和月球的岩生成率.
主要方法:
- 利用现有的地质和地物理数据来建模岩生成.
- 计算出总的挤出和侵入性岩体积.
- 估计的年度岩生成速度.
主要成果:
- 火星上产生的总岩量估计为654×106立方公里.
- 火星的平均岩生成速度为0.17公里3/年.
- 火星的岩速率大大低于地球 (26-34公里/年) 和金星 (<20公里/年),但高于月球 (0.025公里/年).
- 当缩小到地球质量时,火星的速度小于地球和金星的速度,略小于月球的速度.
结论:
- 在地质时间尺度上,火星的磁性活动比地球和金星少得多.
- 缩放的岩生成速度表明陆地行星之间的内部热量和地质过程存在差异.
相关概念视频
Gravity between Spherical Bodies
Newton's law of gravitation describes the gravitational force between any two point masses. However, for extended spherical objects like the Earth, the Moon, and other planets, the law holds with an assumption that masses of spherical objects are concentrated at their respective centers.
This assumption can be proved easily by showing that the expression for gravitational potential energy between a hollow sphere of mass (M) and a point mass (m) is the same as it would be for a pair of extended...
This assumption can be proved easily by showing that the expression for gravitational potential energy between a hollow sphere of mass (M) and a point mass (m) is the same as it would be for a pair of extended...
Acceleration due to Gravity on Other Planets
The gravitational acceleration of an object near the Earth's surface is called the acceleration due to gravity. It can be measured by conducting simple experiments on Earth. However, such an experiment is impossible to conduct on the surface of other planets.
Astronomical observations are thus used to measure the acceleration due to gravity on other planets. This can be determined by observing the effect of a planet's gravity on objects close to it. The crucial factor that helps in this...
Astronomical observations are thus used to measure the acceleration due to gravity on other planets. This can be determined by observing the effect of a planet's gravity on objects close to it. The crucial factor that helps in this...
Circular Orbits and Critical Velocity for Satellites
The Moon orbits around the Earth. In turn, the Earth (and other planets) orbit the Sun. The space directly above our atmosphere is filled with artificial satellites in orbit. One can examine the circular orbit, the simplest kind of orbit, to understand the relationship between the speed and the period of planets and satellites with respect to their positions and the bodies that they orbit.
Nicolaus Copernicus (1473-1543) first suggested that the Earth and all other planets orbit the Sun in...
Nicolaus Copernicus (1473-1543) first suggested that the Earth and all other planets orbit the Sun in...
Kepler's Third Law of Planetary Motion
In the early 17th century, German astronomer and mathematician Johannes Kepler postulated three laws for the motion of planets in the solar system. In 1909, he formulated his first two laws based on the observations of his forebears, Nikolaus Copernicus and Tycho Brahe. However, in 1918, he published his third law of planetary motion, which gives a precise mathematical relationship between a planet's average distance from the Sun and the amount of time it takes to revolve around the Sun. It...
Tidal Forces
The origin of Earth's ocean tides has been a subject of continuous investigation for over 2000 years. However, the work of Newton is considered to be the beginning of the proper understanding of the phenomenon. Ocean tides are the result of gravitational tidal forces. These same tidal forces are present in any astronomical body; they are responsible for the internal heat that creates the volcanic activity on Io, one of Jupiter's moons, and the breakup of stars that get too close to black holes.
Gravitation
In the years before Newton, a general belief prevailed that different laws governed objects in the sky than objects on Earth. When Kepler wrote down the three laws of planetary motion, explaining in detail the geometrical properties of the planetary orbits around the Sun, there was no immediate idea to discern their connection with more fundamental laws. It was Isaac Newton who, in 1665–66, figured out the connection between planetary motion, the motion of the moon around the Earth, and the...


