How Is the Strong Equivalence Principle Stronger Than the Weak One?
At a glance
- 1. Start with free fall
The weak equivalence principle says that test bodies fall alike, regardless of their composition.
- 2. Include self-gravity
The strong principle also covers bodies whose own gravitational binding energy is significant.
- 3. Include gravity experiments
It extends local position and Lorentz invariance to experiments involving gravity itself.
- 4. Compare the predictions
Look for differences in how self-gravitating bodies fall or how local gravitational experiments behave.
The strong equivalence principle (SEP) is stronger because it applies not only to ordinary test objects, but also to bodies whose own gravity contributes significantly to their mass. It also places restrictions on local experiments involving gravity itself. The weak equivalence principle (WEP) concerns the universality of free fall for test bodies whose self-gravity is negligible.
This distinction matters when comparing theories of gravity. A theory can make ordinary materials fall at the same rate and still predict different behavior for strongly self-gravitating objects, or allow local gravitational measurements to depend on where or how they are performed.
The weak equivalence principle
In its usual form, the WEP says that two test bodies released at the same place and with the same initial velocity have the same acceleration in a gravitational field, independent of their composition. “Test body” here means an object small enough that its own gravity and its effect on the surrounding field can be neglected.
For example, in a vacuum, a piece of lead and a piece of aluminum should fall with the same acceleration near Earth. The WEP is often expressed as equality between inertial mass and passive gravitational mass: the property determining resistance to acceleration matches the property determining response to an external gravitational field.
The WEP does not, by itself, say that every possible experiment behaves as it would in special relativity in a freely falling laboratory. Nor does its usual test-body formulation settle how a body’s own gravitational binding energy affects its motion.
What the strong principle adds
The terminology is often presented as a hierarchy:
| Principle | What it covers |
|---|---|
| WEP | Universal free fall of test bodies with negligible self-gravity |
| Einstein equivalence principle (EEP) | WEP, plus local Lorentz invariance and local position invariance for nongravitational experiments |
| SEP | Extends the EEP’s local-independence idea to gravitational experiments and includes self-gravitating bodies |
Local Lorentz invariance means that the outcome of a local nongravitational experiment does not depend on the freely falling laboratory’s velocity. Local position invariance means it does not depend on the laboratory’s location or time. The SEP applies these requirements more broadly, to experiments whose physics involves gravity, and requires universal free fall to extend to bodies with appreciable gravitational self-energy.
“Local” is essential: a sufficiently small freely falling laboratory can eliminate a nearly uniform external gravitational field, but not tidal effects caused by variations in that field across the laboratory. The principles concern the ideal local limit, not the claim that gravity can be eliminated everywhere or over an arbitrarily large region.
A worked comparison: Earth and a neutron star
A rough way to see why self-gravity changes the test is to estimate a body’s gravitational binding energy. For a uniform sphere in Newtonian gravity, its binding energy has magnitude . As a fraction of its rest energy, this is
where is the body’s mass, its radius, the gravitational constant, and the speed of light.
For Earth, substituting kg and m gives a fraction of about . Earth’s gravitational binding energy is tiny compared with its rest energy, so ordinary laboratory tests of free fall are essentially tests of the WEP for bodies with negligible self-gravity.
For a rough neutron-star example, take times the Sun’s mass and km. The same formula gives a fraction near . This is only an order-of-magnitude illustration: a neutron star is relativistic and not a uniform Newtonian sphere. Still, it shows that self-gravity can be a substantial part of a compact body’s energy, unlike for Earth.
A theory might therefore predict that a neutron star and a weakly self-gravitating body respond slightly differently to an external gravitational field, even if it predicts no measurable composition-dependent difference between lead and aluminum. Such a theory could pass ordinary WEP tests while violating the SEP.
How violations are tested
One example is the Nordtvedt effect: if gravitational binding energy contributes differently to a body’s gravitational response and inertial mass, bodies with different self-energy fractions may fall differently toward the same source. The Earth and Moon have different internal structures and self-energy fractions, so lunar laser ranging can test whether they fall identically toward the Sun. This probes an aspect of the SEP that a standard laboratory comparison of materials does not directly isolate.
Other tests examine whether local gravitational measurements depend on the surrounding gravitational environment. General relativity satisfies the SEP in its usual classical formulation, while many alternative theories satisfy the WEP but violate the SEP. The SEP is thus a more demanding condition on a theory, not simply another name for universal free fall.
Common mistakes
- Treating “strong” as a reference to the strong nuclear force. It means the principle has a broader scope, not that it concerns that force.
- Saying the WEP covers every body without qualification. Standard WEP tests use bodies whose own gravity is negligible; SEP tests address significant self-gravity.
- Equating the SEP with the EEP. The EEP concerns local nongravitational experiments; the SEP extends the requirements to gravitational experiments and self-gravitating bodies.
- Assuming freely falling frames remove all gravity. They remove the locally uniform part of a field, but tidal effects remain across a finite region.
References
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