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首页> 外文期刊>American journal of physics >Flying through polytropes
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Flying through polytropes

机译:穿越多向性

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Dropping objects into a tunnel bored through Earth has been used to visualize simple harmonic motion for many years, and even imagined for use as rapid transport systems. Unlike previous studies that assumed a constant density Earth, here we calculate the fall-through time of polytropes, models of Earth's interior where the pressure varies as a power of the density. This means the fall-through time can be calculated as the central condensation varies from one to large within the family of polytropes. Having a family of models, rather than a single model, helps to explore the properties of planets and stars. Comparing the family of phase space solutions shows that the fall-through time and velocity approach the limit of radial free-fall onto a point mass as the central condensation increases. More condensed models give higher maximum velocities but do not have the right global properties for Earth. The angular distance one can travel along the surface is calculated as a brachistochrone (path of least time) tunnel that is a function of the depth to which the tunnel is bored. We also show that completely degenerate objects, simple models of white dwarf stars supported by completely degenerate electrons, have sizes similar to Earth but their much higher masses mean a much larger gravitational strength and a shorter fall-through time. Numerical integrations of the equations describing polytropes and completely degenerate objects are used to generate the initial models. Analytic solutions and numerical integration of the equations of motion are used to calculate the fall-through time for each model, and numerical integrations with analytic approximations at the boundaries are used to calculate the brachistochrones in the polytropes. Scaling relationships are provided to help use these results in other planets and stars. (C) 2016 American Association of Physics Teachers.
机译:多年以来,人们一直将物体掉入穿过地球的隧道中,以可视化简单的谐波运动,甚至可以想象用作快速运输系统。与以前的假设地球密度恒定的研究不同,这里我们计算多向性的下降时间,即地球内部模型,其中压力随密度的变化而变化。这意味着在多向性家族中,中心凝结从一个变化到较大变化,可以计算出下降时间。拥有一个模型家族,而不是一个模型,有助于探索行星和恒星的特性。比较一系列相空间解表明,随着中心凝结度的增加,下降时间和速度接近径向自由落体到点质量的极限。压缩模型越多,最大速度越高,但地球没有正确的全局属性。可以沿地面行进的角距离被计算为腕形(最小时间路径)隧道,该隧道是隧道掘进深度的函数。我们还表明,完全退化的物体,由完全退化的电子支撑的白矮星的简单模型,具有与地球相似的大小,但是它们的质量更高,则意味着更大的引力强度和更短的下降时间。描述多变量和完全退化对象的方程的数值积分用于生成初始模型。运动方程的解析解和数值积分被用来计算每个模型的下降时间,边界处带有解析近似的数值积分被用来计算多向性中的腕足钟。提供比例关系以帮助在其他行星和恒星中使用这些结果。 (C)2016年美国物理教师协会。

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