重力磁共振和引力波

M. Ruggiero, A. Ortolan
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引用次数: 0

摘要

引力波通常用一个横向无迹(TT)张量来描述,这允许引入所谓的TT坐标。然而,另一种可能的方法是基于费米坐标系的使用,在任意在时空中移动的观察者的世界线附近定义。特别是,费米坐标具有直接的操作意义,因为它们是观测者用来进行空间和时间测量的坐标;实际上,使用这些坐标,度量张量只包含(直到所需的近似水平)在参考系内部的坐标变换下不变的量。使用这种方法可以很容易地强调,观察者所测量的内容既取决于他移动的背景场,也取决于他的运动类型。这与我们在非惯性系中学习经典力学时所发生的情况非常相似:惯性力的出现,取决于惯性系相对于惯性系的特殊运动。我们证明了使用费米坐标,平面引力波的效应可以用重力电磁场来描述:换句话说,波场相当于重力电场和重力磁场的作用,它们与传播方向是横向的,彼此正交。特别地,重力磁场作用于自旋粒子,我们表明,由于引力波场的作用,可能会出现重力磁共振。我们给出了这一现象的经典和量子描述,并认为它可以作为一种新型引力波探测器的基础。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Gravitomagnetic resonance and gravitational waves
Gravitational waves are usually described in terms of a transverse and traceless (TT) tensor, which allows to introduce the so-called TT coordinates. However, another possible approach is based on the use of a Fermi coordinates system, defined in the vicinity of the world-line of an observer arbitrarily moving in spacetime. In particular, Fermi coordinates have a direct operational meaning, since they are the coordinates an observer would use to perform space and time measurements; indeed, using these coordinates the metric tensor contains (up to the required approximation level) only quantities that are invariant under coordinate transformations internal to the reference frame. Using this approach it is simple to emphasise that what an observer measures depends both on the background field where he is moving and, also, on his kind of motion. This is quite similar to what happens when we study classical mechanics in non inertial frames: inertial forces appear, depending on the peculiar motion of the frame with respect to an inertial one. We show that using Fermi coordinates the effects of a plane gravitational wave can be described by gravitoelectromagnetic fields: in other words, the wave field is equivalent to the action of a gravitoelectric and a gravitomagnetic field, that are transverse to the propagation direction and orthogonal to each other. In particular, the gravito-magnetic field acts on spinning particles and we show that, due to the action of the gravitational wave field a gravitomagnetic resonance may appear. We give both a classical and a quantum description of this phenomenon and suggest that it can be used as the basis for a new type of gravitational wave detectors.
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