Number 623, February 5,2003
by Phil Schewe, James Riordon, and Ben Stein
New Superburst Theory
When a neutron star pulls matter from a nearby companion onto itself,
powerful x-ray bursts, visible to telescopes in Earth orbit, can result.
Some astronomers believe the bursts leave behind an ocean of debris,
heavy nuclei mostly, on the neutron star's surface.
Occasionally much larger "superbursts," with up to 1000 times
the amount of x rays than other bursts, can flare up. Henrik
Schatz of Michigan State University (517-333-6397) and his collaborators
Lars Bildsten from UCSB and Andrew Cumming of UCSC believe that an energy
blitz is generated when high energy photons strike the heavy nuclei
in the debris ocean, springing free either a proton, neutron, or alpha
particle, which then recombine with the residual nuclei forming lighter,
stronger bound nuclei and free energy. This photodisintegration process
is triggered by the thermonuclear explosion of a small amount of carbon,
but may then proceed subject to positive feedback: the warmer the surface
temperature the more disintegration, which in turn leads to warmer temperatures.
The runaway production of energy through the conversion of heavy nuclei
into lighter nuclei could be unique in astrophysics: all other thermonuclear
energy generation (such as those inside our sun) proceeds by fusing
lighter nuclei into heavier nuclei. (Schatz
et al., Astrophysical Journal Letters, 3 January 2003;
see also http://groups.nscl.msu.edu/nero/)
Lorentz Violations? Not Yet
Lorentz invariance, the idea that the result of a physics experiment
should stay the same whether the apparatus is motionless or traveling
at some great constant speed relative to a reference point, is taken
for granted in the theory of special relativity. Yet in recent years
some scientists have come to question this pillar of physics, and to
suggest theoretical models (called "standard model extensions,"
or SMEs ) incorporating Lorentz violations and experimental ways of
settling the matter (see Update
578). In these models, the speed of light is not universal but will
have extra terms dependent on the speed or orientation of the apparatus
(see http://media4.physics.indiana.edu/~kostelec/faq.html
). Even before the advent of Einstein's relativity, the Michelson-Morley
experiment tried to perceive (unsuccessfully) a difference in the speed
of light when the Earth was traveling in two different directions in
space while on opposite sides of its orbit around the sun. Now scientists
have to be more subtle in their approach. In one new laboratory experiment,
just completed by Stanford physicists (John
Lipa, 650-723-4562) microwaves in two resonant cavities (one oriented
east-west, the other pointing vertically) are monitored as the Earth
sweeps around the sun. Any orientation- or speed-dependent changes in
the speed of light would alter the resonant conditions of the cavities
in a measurable way. The geometry of the experiment gives it optimal
sensitivity to a number of coefficients in a generalized SME. The Stanford
group sees no such anisotropy at the level of 10-13 for velocity-independent
terms, and at the 10-9 level for velocity-dependent terms.
(Lipa et
al., Physical Review Letters, 14 February 2003.)
Ground Temperatures Since the Year 1500
Ground Temperatures Since the year 1500 can be read back by examining
the temperatures in deep boreholes. Temperatures in the Earth's crust
are determined by a combination of surface climate effects and internal
heat flow. The general trend is a linear rise in temperature with depth,
but this is modulated by heat perturbations which act in a nonlinear
way; typically perturbations penetrate about 20 meters of depth per
year or about 150 m in 100 years. Hugo Beltrami (St. Francis Xavier
University in Nova Scotia) has examined temperature-depth profiles from
826 places around the world. Taking into account the known temperature
anomalies, he is able to work out the average surface energy flux and
temperature for many localities and for the world as a whole back for
a period of 500 years. Beltrami (902-867-2326)
finds that global average surface temperature has increased by 0.45
K in the last 200 years. During this time, however, some places have
experienced more dramatic average temperature swings: for example, parts
of Africa show a cooling while northern Canada is warmer (3-4 K) during
the same period. (Geophysical Research Letters, vol 29, 23, 2111;
also see http://geophysics.stfx.ca/public/index.html)