u du= − μ
dx x2

(15)

whence

u2 = + C.
x

(16)

In the case of a particle falling directly towards the earth from rest at a very great distance we have C = 0 and, by Newton’s Law of Gravitation, μ/a2 = g, where a is the earth’s radius. The deviation of the earth’s figure from sphericity, and the variation of g with latitude, are here ignored. We find that the velocity with which the particle would arrive at the earth’s surface (x = a) is √(2ga). If we take as rough values a = 21 × 106 feet, g = 32 foot-second units, we get a velocity of 36,500 feet, or about seven miles, per second. If the particles start from rest at a finite distance c, we have in (16), C = − 2μ/c, and therefore

dx= u = − √ { 2μ (c − x)},
dt cx

(17)

the minus sign indicating motion towards the origin. If we put x = c cos2 1⁄2φ, we find

t = c3/2(φ + sin φ),
√(8μ)