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Physics News Update
Number 433, June 15, 1999 by Phillip F. Schewe and Ben Stein

ZERO-POINT MOTION IN A BOSE-EINSTEIN CONDENSATE has been quantitatively measured for the first time, allowing researchers, in effect, to study matter at a temperature of absolute zero. According to quantum mechanics, objects cooled to absolute zero do not freeze to a complete standstill; instead they jiggle around by some minimum amount. MIT researchers (Wolfgang Ketterle, 617-253-6815) measured such "zero-point motion" in a sodium BEC, a collection of gas atoms that are collectively in the lowest possible energy state (Update 233). According to Ketterle, "the condensate has no entropy and behaves like matter at absolute zero." The MIT physicists measured the motion (or lack thereof) by taking advantage of the fact that atoms absorb light at slightly lower (higher) frequencies if they are moving away from (towards) the light. To determine these Doppler shifts (100 billion times smaller than those of moving galaxies), the researchers used a technique known as Bragg scattering. In this technique, atoms absorb photons at one energy from a laser beam and are stimulated by a second laser to emit a photon at another energy which can be shifted upward or downward depending on the atoms' motion towards or away from the lasers. Measuring the range in energies of the emitted photons allowed the researchers to determine the range of momentum values in the condensate. Multiplying this measured momentum spread (Dp) by the size of the condensate (Dx) gave an answer of approximately h-bar (Planck's constant divided by 2p)--the minimum value allowed by Heisenberg's uncertainty relation and quantum physics. While earlier BECs surely harvested this zero-point motion, previous measurements of BEC momentum spreads were done with exploding condensates having energies larger than the zero-point energy. (J. Stenger et al., Physical Review Letters, 7 June 1999.)

ACOUSTIC-DEPENDENT FRICTION. Studies of friction are often carried out at modest relative speeds: the two moving surfaces in question typically slide past each other at 1 cm/s. However, researchers at UCLA (Anders Johansen, 310-825-2863) wondered if new mechanisms might appear when surfaces slide against each other at higher velocities, such as those associated with friction between tectonic plates during earthquakes. Observing the jerky "stick-slip" motion of a steel block riding on a rotating steel table, the researchers carefully measured the friction forces for relative velocities up to 0.35 m/s, by monitoring the expansion and compression in a spring attached to the steel block. At these high velocities, they noted that the significantly increased production of sound waves (largely neglected in past analyses) dissipates a large amount of energy, stealing away some of the energy of motion required for two surfaces to slide past each other and thereby amounting to an increase in friction. This suggests that the generation of sound waves between two sliding fault surfaces during an earthquake may provide a significant feedback mechanism that mitigates a quake's effects, by converting energy of motion (friction which might otherwise have caused fracturing in the Earth) into sound energy. ( Johansen and Sornette, Physical Review Letters, 21 June 1999.)