In this series, I’m discussing how ideas from calculus and precalculus (with a touch of differential equations) can predict the precession in Mercury’s orbit and thus confirm Einstein’s theory of general relativity. The origins of this series came from a class project that I assigned to my Differential Equations students maybe 20 years ago.
We have shown that the motion of a planet around the Sun, expressed in polar coordinates with the Sun at the origin, under general relativity is
,
where ,
,
is the semi-major axis of the planet’s orbit,
is the orbit’s eccentricity,
,
is the gravitational constant of the universe,
is the mass of the planet,
is the mass of the Sun,
is the planet’s perihelion,
is the constant angular momentum of the planet, and
is the speed of light.
The above function is maximized (i.e., the distance from the Sun
is minimized) when
is as large as possible. This occurs when
is a multiple of
.
Said another way, the planet is at its closest point to the Sun when . One orbit later, the planet returns to its closest point to the Sun when
We now use the approximation
;
this can be demonstrated by linearization, Taylor series, or using the first two terms of the geometric series . With this approximation, the closest approach to the Sun in the next orbit occurs when
,
which is coterminal with the angle
.
Substituting and
, we see that the amount of precession per orbit is
.
The units of are radians per orbit. In the next post, we will use Mercury’s data to find
in seconds of arc per century.

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