The Hafele-Keating experiment was a famous experiment conducted in 1971 to test the time dilation predicted by special relativity. In that experiment, atomic clocks were flown in airplanes traveling in opposite directions around the Earth. The experiment measured the difference in the time recorded by the clocks upon their return, comparing it to the time recorded by a stationary clock on the ground.
While it's not possible to recreate the exact Hafele-Keating experiment by simply spinning clocks in a lab, the principles behind the experiment can be demonstrated in simpler ways. Spinning a clock itself would not create a significant enough effect to measure time dilation. Instead, the experiment relied on the high speeds of the airplanes to produce measurable time differences.
To simulate the kinematic time dilation aspect of the Hafele-Keating experiment in a lab, you would need to create relative motion between two clocks at speeds comparable to a significant fraction of the speed of light. Achieving such speeds in a lab environment is not currently feasible for everyday experiments.
However, there are other experiments that can demonstrate the time dilation effects of special relativity in a laboratory setting. For instance, high-precision experiments with fast-moving particles, such as particle accelerators, can observe time dilation effects. Additionally, experiments with subatomic particles called muons, which are created in the upper atmosphere and decay rapidly, provide evidence for time dilation as they reach the Earth's surface.
In summary, while it is not possible to replicate the Hafele-Keating experiment by simply spinning clocks in a lab, there are other experiments that demonstrate the effects of time dilation in different ways, such as particle accelerators and muon experiments.