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Physics News Update
Number 834, July 27, 2007 by Phil Schewe and Ben Stein

Hydrogen-Seven

An experiment at the GANIL facility in France is the first to make, observe, identify, and characterize the heaviest isotope yet of hydrogen, H-7, consisting of a lone proton and 6 neutrons. (An earlier experiment saw some inconclusive evidence for this state-see Korsheninnikov et al., Physical Review Letters, 8 Feb 2003.)

All of the lighter isotopes of hydrogen have previously been seen: H-1 (ordinary hydrogen), H-2 (deuterium), H-3 (tritium), and H-4 up to H-6. Technically speaking, the H-7 state (like H-4, H-5, and H-6) is not a fully bound nucleus. It is considered a resonance since (besides being very short lived) energy is required to force the extra neutron to adhere to the other nucleons.

In a proper nucleus energy is required to remove a neutron. In the GANIL experiment, a beam of helium-8 ions (themselves quite rare) is smashed into a carbon-12 nucleus residing in a gas of butane (see figure at http://www.aip.org/png/2007/283.htm). In a few rare occurrences, the He-8 gives one of its protons to the C-12, producing H-7 and N-13, respectively. The H-7 flies apart almost immediately into H-3 and 4 separate neutrons.

Meanwhile the N-13 is observed in the active-target MAYA detector (named after a cartoon character, Maya the Bee, whose honeycomb hive resembles the hexagonal cathode pads in the experiment), a device much like a bubble chamber, allowing its energy and trajectory to be deduced.

By taking the conservation of momentum and energy into account, the fleeting existence of the H-7 is extracted from the N-13 data (see the figure at www.aip.org/png). A total of 7 H-7 events was observed. A rough lifetime for H-7 of less than 10^-21 seconds can be inferred. The helium-8 nucleus (2 protons plus 6 neutrons) used to make the H-7 is interesting all by itself since it is believed to consist of a nuclear core with two “halo” neutrons orbiting outside.

This radioactive species must carefully be gathered up from carbon-carbon collisions (in a separate step) and then accelerated to participating in the H-7 experiment. One of the GANIL researchers, Manuel Caamaño Fresco (caamano@ganil.fr, 33-231-45-4435), says that one of the chief reasons for looking at H-7 is to get a better handle on exotic nuclear matter.

The H-7 nucleus, during its brief existence, might consist of a H-3 core and plus two 2-neutron outriders, or maybe even a single 4-neutron blob outside. Larger still hydrogen isotopes, such as H-8 or H-9, might be observable. (Caamaño et al., Physical Review Letters, upcoming article; PhD thesis at http://www.usc.es/genp/maya/)

Laser Icemaking

Physicists at the University of Goettingen have for the first time gotten supercooled water to freeze using pulses of laser light. Supercooling occurs when a sample of water is chilled down through its normal freezing point (0 C) without crystallization occurring.

This can happen in a small sample and if no “nucleation” site presents itself around which solid ice (a crystal structure) can form. The incoming laser pulse brings about an optical breakdown: some of the water molecules are ionized, creating a momentary plasma. The hot plasma expands and forms a vapor bubble that collapses very rapidly.

It is the pressure waves emitted by the tiny plasma and the bubble collapse which, the Goettingen scientists believe, trigger the rapid crystallization. Previously an acoustic equivalent of this process---sonocrystallization-had been seen, but this is the first time crystallization has been initiated by a laser pulse.

One of the researchers, Robert Mettin (R.Mettin@physik3.gwdg.de, +49-551-39-2285), suggests that laser icemaking can be extended to studying solidification of other materials. (Lindinger et al., Physical Review Letters, 27 July 2007

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