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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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charge exchange<br />

an ordinary differential equation problem. The<br />

solution may be obtained graphically or by numerical<br />

techniques. Used in the study of open<br />

channel flow <strong>and</strong> elsewhere.<br />

charge exchange An atomic process that<br />

may occur when a fast ion collides with a neutral<br />

atom, in which an electron is transferred from<br />

the atom to the ion. As a result, the atom becomes<br />

a slow ion, while the ion becomes an energetic<br />

neutral atom (ENA). It strongly depends<br />

on energy (also on the type of ion) <strong>and</strong> is much<br />

more pronounced around 5 keV than at 50 keV.<br />

Charge exchange is believed to be the major<br />

mechanism by which ions produced in a magnetic<br />

storm are lost, leading to the decay of the<br />

enhanced ring current associated with the storm.<br />

Ionsofthatringcurrentaremagneticallytrapped<br />

by the Earth, but if they change into ENAs, the<br />

magnetic field no longer affects them, <strong>and</strong> they<br />

move in straight lines, making them a possible<br />

means of remotely sensing the ring current.<br />

Charles’ Law At constant pressure, the volume<br />

of an ideal gas is directly proportional to<br />

the absolute temperature of that gas.<br />

Charon Moon of Pluto, although it is close<br />

enough in size to Pluto to be considered a double<br />

planet. It was discovered by Christy in 1978. Its<br />

orbithasaneccentricityof0.0001, aninclination<br />

of 98.3 ◦ , <strong>and</strong> a semimajor axis of 1.96 ×10 4 km.<br />

Both Pluto <strong>and</strong> Charon rotate in such a way as to<br />

always keep the same face towards each other.<br />

Its radius is not well determined, with measurements<br />

giving between 590 <strong>and</strong> 630 km. Its mass<br />

<strong>and</strong> density are not well known. Its geometric<br />

albedo is 0.36, <strong>and</strong> it orbits every 6.387 Earth<br />

days.<br />

chemically peculiar star A star whose surface<br />

composition deviates from the st<strong>and</strong>ard set<br />

by the sun (3/4 hydrogen, 1/4 helium, a few percent<br />

of everything else in st<strong>and</strong>ard proportions:<br />

See cosmic abundance). This happens for one of<br />

three reasons: (1) products of nuclear reactions<br />

in the star itself have been mixed to the surface<br />

(as in carbon stars or R Coronae Borealis stars),<br />

(2) products of nuclear reactions in a companion<br />

star have been transferred to the observed,<br />

or (3) a combination of radiation pressure <strong>and</strong><br />

© 2001 by CRC Press LLC<br />

a very steady atmosphere has separated out unusual<br />

atoms, often in regions of strong magnetic<br />

fields. Europium <strong>and</strong> strontium are among the<br />

elements sometimes greatly overabundant in the<br />

third sort of star, called an Ap star (A for its spectral<br />

type, p for peculiar).<br />

chenier Beach ridge.<br />

Chezy coefficient, Chezy equation The<br />

Chezy equation is used to relate flow speed to<br />

flow geometry <strong>and</strong> other parameters. The equation<br />

is V =C RSf , where V is flow speed,<br />

C is the Chezy coefficient, R =A/P = hydraulic<br />

radius, <strong>and</strong> Sf is friction slope (head<br />

loss per unit length). The Chezy coefficient is<br />

determined primarily by channel roughness but<br />

decreases with increasing roughness. An alternative<br />

to the Manning equation.<br />

chlorinity The concentration of chloride ions<br />

by mass in seawater (g/kg). Typical ocean chlorinity<br />

is of order 19 g/kg of seawater. There is<br />

an observed constant ratio of chlorinity to salinity:<br />

Salinity in parts per thous<strong>and</strong> = (1.80655)<br />

(chlorinity in parts per thous<strong>and</strong>). See salinity.<br />

chlorophyll Chemical compounds occurring<br />

in plants that enable radiant energy to be converted<br />

to chemical energy in the process of photosynthesis;<br />

there are several types (e.g., denoted<br />

as chl a, b, etc.) with chl a typically the<br />

most abundant.<br />

chondrite A relatively abundant stony meteorite<br />

characterized by the presence of small<br />

(∼ 1 mm) glassy spherical inclusions called<br />

chondrules. Chondrites are further subdivided<br />

into ordinary, carbonaceous, <strong>and</strong> enstatite chondrites,<br />

depending on details of composition <strong>and</strong><br />

thermal processing.<br />

chondrite, carbonaceous A form of chondrite<br />

with high abundances of water, organic,<br />

<strong>and</strong> other volatile materials. This, <strong>and</strong> the fact<br />

that the heavier elements are present in roughly<br />

solar proportions, indicates that these bodies<br />

have been little processed. These meteorites<br />

are further classified by their volatile content<br />

into CI (or C1), which are most nearly solar in<br />

composition, CII (CM) <strong>and</strong> CIII (CO or CV),

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