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DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

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Herbig–Haro object An object that is apparently<br />

a forming star, surrounded by still accreting<br />

matter. These objects have strong stellar<br />

winds, <strong>and</strong> mass loss including jets. Herbig–<br />

Haro objects are powerful emiters of infrared radiation;<br />

thespectrumconsistsofstrongemission<br />

lines presumably produced by internal shocks<br />

within protostellar jets or winds.<br />

herringbone burst See type II radio burst.<br />

Hertz (Hz) Unit of frequency equal to s −1 .<br />

Hertzsprung Gap The region on a<br />

Hertzsprung–Russell Diagram between the<br />

main sequence <strong>and</strong> red giant branches in which<br />

relatively few stars are found. The reason is that<br />

stars evolve across the gap (at roughly constant<br />

luminosity) very quickly because the hydrogen<br />

fuel in their cores has been exhausted <strong>and</strong> the<br />

hydrogen around the core is not yet hot enough<br />

to fuse. Thus, the only energy source is gravitational<br />

potential energy from core contraction,<br />

some of which is used up in simultaneously exp<strong>and</strong>ing<br />

the outer layers of the star. The gap<br />

is particularly conspicuous in the HR diagram<br />

of a young open cluster of stars, where all the<br />

stars are the same age. See Hertzsprung–Russell<br />

diagram, main sequence star, open cluster, red<br />

giant.<br />

Hertzsprung–Russell diagram See HR diagram.<br />

Hesperian Geophysical epoch on the planet<br />

Mars, 1.8 to 3.5 Gy BP. Channels on Mars give<br />

evidence of large volumes of water flow at the<br />

end of the Hesperian <strong>and</strong> the beginning of the<br />

Amazonian epoch.<br />

H I 21-cm line Spectral line emitted in the<br />

radio domain, at a wavelength of 21 cm (corresponding<br />

to a frequency of 1420 GHz), due<br />

to the hyperfine transition between two energy<br />

states in the ground level of the hydrogen atom,<br />

the lower state with electron spin <strong>and</strong> proton spin<br />

anti-parallel, the higher state with the two spins<br />

parallel. The HI 21-cm emission line was first<br />

detected in 1951; since then it has been used to<br />

map the distribution of neutral hydrogen within<br />

the galaxy, <strong>and</strong> in external galaxies, with radio<br />

© 2001 by CRC Press LLC<br />

high-pressure <strong>and</strong> high-temperature experiment<br />

telescopes <strong>and</strong> interferometers. See forbidden<br />

lines.<br />

Higgs mechanism Mechanism responsible<br />

for the existence of massive particles in the st<strong>and</strong>ard<br />

model of quantum field theory. The mechanism<br />

arises in a spontaneous breakdown of symmetry.<br />

For instance, far before a gauge U(1)<br />

symmetry the symmetry breakdown (i.e., at high<br />

temperatures), we have a complex scalar fieldφ<br />

<strong>and</strong> a massless gauge field A µ (like the photon,<br />

for example) with two degrees of freedom<br />

(two polarizations). As the temperature lowers,<br />

φ selects one possible phase in the range<br />

[0 − 2π]. This is called spontaneous symmetry<br />

breakdown. After the breakdown, φ represents<br />

a massive scalar field <strong>and</strong>A µ becomes a massive<br />

gauge field (three degrees of freedom), totaling<br />

again exactly four degrees of freedom as before<br />

the transition. Such events were presumably important<br />

in the very early universe. See Abelian<br />

Higgs model, cosmic topological defect, Goldstone<br />

model, spontaneous symmetry breaking.<br />

higher derivative theories Theories of gravity<br />

in which the equations of motion contain<br />

higher than second derivatives of the basic variables<br />

(the potentials) of the theory.<br />

highl<strong>and</strong>s, lunar See lunar highl<strong>and</strong>s.<br />

high-pressure <strong>and</strong> high-temperature experiment<br />

An experiment to measure density of<br />

rocks <strong>and</strong> minerals, velocity of elastic waves <strong>and</strong><br />

elastic modulus, <strong>and</strong> to investigate materials,<br />

phases, <strong>and</strong> melting, realizing the high-pressure<br />

<strong>and</strong> high-temperature state of the Earth’s interior.<br />

There are two kinds of high-pressure apparatuses:<br />

a dynamic high-pressure apparatus<br />

utilizing shock waves <strong>and</strong> a static high-pressure<br />

apparatus applying constant load. For the former,<br />

it is possible to produce pressure of several<br />

hundred gigaPascals (GPa) instantaneously, corresponding<br />

to the pressure at the Earth’s core.<br />

However, because of the short reaction time<br />

<strong>and</strong> inaccuracies of the estimate of temperature,<br />

other approaches are being used, such as piston<br />

cylinder apparatus which is able to produce pressure<br />

<strong>and</strong> temperature characteristic of the uppermost<br />

mantle (up to 6 GPa <strong>and</strong> 2,800 K), multianvil<br />

type apparatus which can produce pres-<br />

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