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DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

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operates between 115 <strong>and</strong> 1100 nm, offers spectral<br />

resolving power ranging from 150 to 100000<br />

<strong>and</strong> long slit capabilities.<br />

Hubble time Inverse of Hubble constant;<br />

H−1 o = 9.78h−1 × 109 years corresponding to<br />

the time it would take the universe to reach its<br />

present size exp<strong>and</strong>ing at constant rateHo. Here<br />

h=H0 (100 km/sec/Mpc). See Hubble radius.<br />

humic substance High molecular weight organic<br />

compounds resulting from plant decay, especially<br />

terrestrial plants; water-soluble soil humic<br />

substance imparts a yellow color to water.<br />

See also colored dissolved organic matter.<br />

hurricane Intense tropical cyclone of the<br />

Atlantic Ocean, Caribbean region, <strong>and</strong> on the<br />

northeastern coast of Australia. Similar types<br />

of tropical cyclone appearing over the western<br />

Pacific are called typhoons. A hurricane is a<br />

circulatory strong wind system (180 km/h or so)<br />

with low central pressure (below 950 mb), <strong>and</strong><br />

is confined to a few hundred kilometers. In the<br />

northern hemisphere the wind rotation is counterclockwise.<br />

Huygens principle In radiation fields, the<br />

phase front at any instant can be thought of as the<br />

locus of radiating sources, <strong>and</strong> the phase front at<br />

the next instant is obtained by a phase coherent<br />

addition of the radiation from all those sources.<br />

Hyades An open cluster of about 100 stars<br />

visible to the naked eye in the constellation of<br />

Taurus (45 parsecs from the sun, at right ascension<br />

4 h 27 m , declination +16 ◦ 0 ′ ). The Hyades<br />

cluster is about 600 million years old.<br />

hybrid topological defect Different symmetry<br />

breaking schemes in quantum field theory<br />

allow for the possibility of formation of various<br />

kinds of topological defects, like monopoles,<br />

cosmic strings, <strong>and</strong> domain walls, in the early<br />

universe. Realistic gr<strong>and</strong> unified models generally<br />

involve several phase transitions <strong>and</strong> therefore<br />

one type may become attached to another,<br />

<strong>and</strong> the system will end up, say, with<br />

walls bounded by strings or strings connecting<br />

monopoles. Such mixed configurations are<br />

calledhybridtopologicaldefects<strong>and</strong>aredynam-<br />

© 2001 by CRC Press LLC<br />

hydraulic depth<br />

ically unstable since no topological constraint<br />

can be applied on them. See cosmic phase transition,<br />

cosmic topological defect, gr<strong>and</strong> unification,<br />

Langacker–Pi mechanism.<br />

hydraulic head (piezometric head) The<br />

equivalent height of a fluid required to maintain<br />

a pressure hydrostatically. The hydraulic<br />

head is of practical meaning only when defined<br />

for a uniform fluid density. For a flow field with<br />

variable fluid density, a reference head is often<br />

defined using a reference density. Given density<br />

ρ, the hydraulic headh is defined as<br />

h= p<br />

ρg +z<br />

where p is fluid pressure, g is gravitational acceleration,<br />

<strong>and</strong> z is elevation measured from an<br />

arbitrary reference point. In groundwater hydrology,<br />

the hydraulic head is also called the<br />

piezometric head.<br />

hydraulic conductivity (K) The ability of a<br />

porous medium to transmit fluid is dependent on<br />

both the properties of the fluid <strong>and</strong> the medium:<br />

<br />

ρg<br />

K=κ<br />

µ<br />

where κ is the intrinsic permeability of the<br />

porous medium, ρg is the fluid weight, <strong>and</strong> µ<br />

is the viscosity of the fluid. Hydraulic conductivity<br />

is generally a tensor because of κ.<br />

It has the dimension of velocity. See Darcy’s<br />

law. The hydraulic conductivity of natural substances<br />

ranges over many orders of magnitude,<br />

from 10 −21 ms −1 for unfractured crystalline<br />

rock to 10 −2 ms −1 for karst limestone <strong>and</strong><br />

gravel. The hydraulic conductivity decreases<br />

very rapidly as the medium becomes unsaturated,<br />

because the larger pores of the subsurface<br />

become airfilled first, causing flow to occur<br />

in smaller pores which conduct water at much<br />

lower flow rates according to Poiseuille’s law.<br />

We therefore write the hydraulic conductivity in<br />

unsaturated systems as K(θ), indicating that it<br />

is a function of the volumetric moisture content.<br />

hydraulic depth The cross-sectional area of<br />

a free-surface flow (such as a river) divided by<br />

the top width of the flow.<br />

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