Myslius said:
So how fast the Earth is moving in space and what is our time dilation?
Rasalhague said:
The problem with this is that we can do it at will for any object! For anything--the earth, the sun, the center of the galaxy--we can define an inertial frame of reference in which the object is (at least momentarily) at rest.
Myslius said:
You see, you can't take any point as inertial frame of reference.
In the case of an accelerating object, including objects moving at a constant speed but changing direction, we can define an instantaneous rest frame as an inertial frame of reference as one having the velocity that the object has at a particular instant. The object will only be at rest in that frame of reference for that instant though. There's no one inertial reference frame in which an accelerating object remains at rest.
In special relativity, as in Newtonian mechanics, there's no absolute state of rest (so there's no answer to your question "how fast is the Earth moving?"), but there is an absolute state of non-acceleration. In Einstein's words, we have
nicht die Bevorzugung eines bestimmtes Bewegungszustandes sondern nur die Bevorzugung eines bestimmtes Beschleunigungszustandes (not the favoring of a particular state of motion but only the favoring of a particular state of acceleration).
The kind of time effect being measured in the Hafele-Keating experiment is the kind of absolute difference that arises from differences in acceleration, as in the twin "paradox", the kind I labelled type 2. I'm guessing your unease with this comes from reading descriptions of the Hafele-Keating experiment purely in terms of a difference in velocity, which has led you to think of it as being like the symmetrical time effects of type 1. These symmetrical/reciprocal effects can be thought of as effects of perspective, analogous to the way that an object looks different when viewed from different angles. You can no more what is the velocity-induced time dilation of the Earth than what is the distortion of, say, France, due to the angle that it's at. In either case, there's no absolute answer, only relative answers, given some arbitrary position (point of view), in the case of distortion due to angle of view, or some arbitrary standard of rest ("velocity of view"), in the case of time dilation.
But the planes in the Hafele-Keating experiment are distinguished by more than relative velocity. They differed in their states of acceleration, one having a greater angular speed, and therefore a greater linear acceleration than the other, relative to the approximately inertial centre of the earth.
Myslius said:
All I'm saying that by comparing time dilation of clocks you can find inertial frame where there is no time dilation (at least it is very small - approximation
The time dilation formula tells you how, given a time interval between two events that happen at the same place (along some spatial axis) in one inertial frame of reference, you can work out the time interval between those same events according to another inertial frame of reference moving at some velocity (along that axis) relative to the first. Inertial frames of reference where these events happen at the same place might seem like a natural choice of absolute rest,
but in any such frame of reference there will be inflinitely many pairs of events which don't happen at the same place (along that axis), for which the "frame of maximum time" between them is another frame of reference. Since our choice of events, and of orientation (hence spatial axis), was arbitrary, there's nothing uniquely "rest-like / motionless-like" about that first frame of reference; we could just as well have picked another inertial frame of reference, and another pair of events by which to define "at rest".
Myslius said:
sqrt(1 - (v/c)^2)
by taking v you're taking velocity difference between two "events". But this function isn't linear, so we can determine the exact speeds.
I don't understand this point. Nonlinear functions can have exact solutions.
http://www.quickmath.com/webMathematica3/quickmath/page.jsp?s1=equations&s2=solve&s3=basic