当地的星际尘埃流的偏移由太阳辐射压力
M Landgraf1, K Augustsson, E Grün
1NASA Johnson Space Center, Mailcode SN2, Houston, TX 77058, USA. mlandgra@esoc.esa.de
概括
由于太阳辐射压力,星际尘埃粒在2-4AU之间不太常见. 这种压力是太阳引力的1.4-1.8倍,影响酸盐和有机耐火粒.
科学领域:
- *行星科学和天体物理学
- * 宇宙尘埃动力学
背景情况:
- * 了解星际尘埃的组成和分布对于行星的形成和进化至关重要.
- *以前的研究表明,太阳系内的尘埃种群存在差异.
研究的目的:
- * 为了研究在2~4 AU的日中心距离范围内观测到的星际尘埃颗粒的缺陷.
- * 确定负责观察到的尘埃粒分布的力量.
主要方法:
- *分析Ulysses和利略航天器上的尘埃探测器数据.
- * 模拟太阳辐射压力和太阳重力对各种组成和大小的尘埃粒的影响.
主要成果:
- *在4AU以外的区域相比,在2AU至4AU之间检测到显著的星际尘埃颗粒 (质量为1×10−17至3×10−16公斤) 缺乏.
- *太阳辐射压力需要是太阳引力的1.4到1.8倍,以转移这些粒.
- * 这些比率与天文酸盐,有机耐火材料和纯石墨颗粒 (直径为0.2-0.4微米) 的光学特性保持一致.
结论:
- *太阳辐射压力在塑造太阳系内部星际尘埃分布方面起着至关重要的作用.
- *观察到的尘埃缺陷与作用于酸盐,有机和石墨尘埃颗粒的力量一致.
- * 这一发现提供了对尘埃动态及其与星际环境中的恒星辐射相互作用的见解.
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...
Variation in Acceleration due to Gravity near the Earth's Surface
An object's apparent weight is its weight measured by a spring balance at its location. It is different from its true weight, the force with which the Earth pulls it, because of the Earth's rotation. Mathematically, an object's apparent weight equals its true weight minus the centripetal force that keeps it in a circular motion along with the Earth's surface every 24 hours.
The difference between the true and apparent weights is proportional to the square of the Earth's angular speed. Since the...
The difference between the true and apparent weights is proportional to the square of the Earth's angular speed. Since the...
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.
Momentum And Radiation Pressure
An object absorbing an electromagnetic wave would experience a force in the direction of propagation of the wave. This force occurs because electromagnetic waves contain and transport momentum. The force accounts for the wave's radiation pressure exerted on the object. Maxwell's prediction was confirmed in 1903 by Nichols and Hull by precisely measuring radiation pressures with a torsion balance. The measuring instrument had mirrors suspended from a fiber kept inside a glass container. Nichols...
Radiation Pressure: Problem Solving
The radiation pressure applied by an electromagnetic wave on a perfectly absorbing surface equals the energy density of the wave. The wave's momentum also gets transferred to the surface when an electromagnetic wave is entirely absorbed by it. The rate at which momentum is transmitted to an absorbing surface perpendicular to the propagation direction equals the force on the surface.
The average value of the rate of momentum transfer divided by the absorbing area represents the average force per...
The average value of the rate of momentum transfer divided by the absorbing area represents the average force per...
Variation of Atmospheric Pressure
Change in atmospheric pressure with height is particularly interesting. The decrease in atmospheric pressure with increasing altitude is due to the decreasing gravitational force per unit area as we move away from the surface of the earth.
Assuming the air temperature is constant at a given altitude and that the ideal gas law of thermodynamics describes the atmosphere to a good approximation, one can find the variation of atmospheric pressure with height.
Let p(y) be the atmospheric pressure at...
Assuming the air temperature is constant at a given altitude and that the ideal gas law of thermodynamics describes the atmosphere to a good approximation, one can find the variation of atmospheric pressure with height.
Let p(y) be the atmospheric pressure at...


