第十七章。物理天文学研究

J. Lubbock
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摘要

我补充一些关于月球理论的进一步发展,我认为最好详细说明,以节省计算器的麻烦,避免出错的危险,尽管它们可以通过我为此目的而提供的表格非常方便和方便地获得。一方面,通过完善建立在行星理论中所使用的各种方程的综合基础上的月球理论,似乎有必要给物理天文学引入更大程度的统一性;另一方面,在行星理论中完成迄今为止只应用于周期内等式的方法,似乎也同样重要。到目前为止,干扰函数中引起长期不等式的那些项已经被分离出来,系统的稳定性是通过对某些方程的积分来推断的,这些方程在忽略偏心率的高次幂时是线性的,并且是从建立在椭圆常数变化基础上的考虑中推断出来的。我认为,系统的稳定性也可以从微分方程直接积分的表达式中推断出来。事实上,为了使系统稳定,必须确保正弦或余弦符号下的角都不是虚数,否则这些项就会被转换成指数,并受到无限递增的影响。在月球理论中,用这种观点确定的任意量,按照这里给出的方法,所引入的角度可以归结为太阳和月球的平均运动之差、它们的平均异常和月球的纬度之差。
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XVII. Researches in physical astronomy
I SUBJOIN some further developments in the Theory of the Moon, which I have thought it advisable to give at length, in order to save the trouble of the calculator and to avoid the danger of mistake, although they may be ob­ tained with great readiness and facility by means of the Table which I have given for the purpose. While on the one hand it seems desirable to introduce into the science of Physical Astronomy a greater degree of uniformity, by bringing to per­ fection a Theory of the Moon, founded on the integration of the equations which are used in the planetary theory, it seems also no less important to complete in the latter the method hitherto applied solely to the periodic in­ equalities. Hitherto those terms in the disturbing function which give rise to the secular inequalities have been detached, and the stability of the system has been inferred by means of the integration of certain equations, which are linear when the higher powers of the eccentricities are neglected, and from consi­ derations founded on the variation of the elliptic constants. The stability of the system may, I think, also be inferred from the expres­ sions which result at once from the direct integration of the differential equa­ tions. In fact, in order that the system may be stable, it is necessary that none of the angles under the sign sine or cosine be imaginary, which terms would then be converted into exponentials, and be subject to indefinite in­ crease. In the lunar theory, the arbitrary quantities being determined with that view, according to the method here given, the angles which are intro­ duced may be reduced to the difference of the mean motions of the sun and moon, their mean anomalies and the argument of the moon’s latitude *.
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