E I N S T E I N I A N G R A V I T A T I O N
137
a(r) = GM
G
/r
2
. (8.2)
Galileo had, of course, previously shown that objects made from different materials
fall with the same acceleration in the gravitational field at the surface of the Earth, a result
that implies m
G
∝ m
I
. This is the Newtonian Principle of Equivalence.
Einstein used this Principle as a basis for a new Theory of Gravitation! He extended the
axioms of Special Relativity, that apply to field-free frames, to frames of reference in “free
fall”. A freely falling frame must be in a state of unpowered motion in a uniform
gravitational field . The field region must be sufficiently small for there to be no
measurable variation in the field throughout the region. If a field gradient does exist in
the region then so called “tidal effects” are present, and these can, in principle, be
determined (by distorting a liquid drop, for example). The results of all experiments
carried out in ideal freely falling frames are therefore fully consistent with Special
Relativity. All freely-falling observers measure the speed of light to be c, its constant free-
space value. It is not possible to carry out experiments in ideal freely-falling frames that
permit a distinction to be made between the acceleration of local, freely-falling objects,
and their motion in an equivalent external gravitational field. As an immediate
consequence of the extended Principle of Equivalence, Einstein showed that a beam of
light would be observed to be deflected from its straight path in a close encounter with a
sufficiently massive object. The observers would, themselves, be far removed from the
gravitational field of the massive object causing the deflection. Einstein’s original
calculation of the deflection of light from a distant star, grazing the Sun, as observed here
on the Earth, included only those changes in time intervals that he had predicted would