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DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

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energy grade line A visual representation of<br />

the energy in a flow. Indicates the sum of the<br />

velocity head, V 2 /2g, elevation, <strong>and</strong> pressure<br />

head, p/γ, for the flow, where V is the flow<br />

speed,g is the acceleration of gravity,p is pressure,<br />

<strong>and</strong> γ is the unit weight (weight per unit<br />

volume) of the fluid.<br />

energy-momentum relations — special<br />

relativity In special relativity physical laws<br />

must be the same in reference systems moving<br />

uniformly with respect to each other; that<br />

is, they must be invariant under Lorentz Transformations.<br />

In special relativity time is not an<br />

absolute variable, <strong>and</strong> therefore special relativity<br />

is mathematically described through a fourdimensional<br />

spacetime with time as the first coordinate<br />

in addition to the three spatial coordinates.<br />

In order for the Lorentz electromagnetic<br />

force to be incorporated into a law of mechanics<br />

that is invariant under Lorentz transformations,<br />

<strong>and</strong> for the mechanics law to also reduce<br />

to Newton’s law at low velocities, a fourcomponent<br />

relativistic momentum vector is defined<br />

such that the first component equals the<br />

energy of a given particle <strong>and</strong> the other three<br />

components equal the momentum components<br />

oftheparticle. Sincethefour-vectorscalarproduct<br />

is invariant under Lorentz transformations,<br />

one obtains the relativistic relationship between<br />

the energy <strong>and</strong> the momentum of a particle by<br />

calculating the four-vector scalar product of the<br />

four-vector momentum with itself.<br />

energy per unit length (cosmic string) In<br />

the framework of a cosmological model with<br />

the generation of topological defects, a cosmic<br />

string is an approximation of a vacuum vortex<br />

defect in terms of a line-like structure, confined<br />

to a two-dimensional world sheet. For a complete<br />

macroscopic description (as opposed to<br />

microscopic, in terms of relevant fields like the<br />

Higgs field <strong>and</strong> other microscopic fields coupled<br />

to it) we need to know quantities such as the<br />

string tension T <strong>and</strong> the energy per unit length<br />

U (often denoted µ in the literature). For a microscopic<br />

model, specified by its Lagrangian,<br />

we can compute its energy-momentum tensor<br />

T µν by st<strong>and</strong>ard methods. Given the cylindrical<br />

symmetry of the string configuration, the energy<br />

© 2001 by CRC Press LLC<br />

per unit length is calculated as<br />

<br />

U = 2π rdrT tt ,<br />

entropy<br />

where T tt is the time-time component of the<br />

energy-momentum tensor. See equation of state<br />

(cosmic string), Goto–Nambu string, tension<br />

(cosmic string), wiggle (cosmic string).<br />

enthalpy An extensive thermodynamic potential<br />

H given by<br />

H = U − PV ,<br />

where U is the internal energy, P is the pressure,<br />

<strong>and</strong> V is the volume of the system. The<br />

change of the enthalpy is the maximum work<br />

that can be extracted from a reversible closed<br />

system at constant P . For a reversible process<br />

at constant S <strong>and</strong> P , work stored as enthalpy can<br />

be recovered completely.<br />

entrainment Jets <strong>and</strong> plumes, moving<br />

through fluid at rest, have the tendency to entrain<br />

ambient fluid into the flow. The rate ∂Q/∂x<br />

[m 2 s −1 ], at which the volume flow Q [m 3 s −1 ]<br />

increases per unit distance x [m], is called the entrainment<br />

rate. The most customary parameterization<br />

of the entrainment rate is ∂Q/∂x = ERu<br />

(Morton, 1959), where R <strong>and</strong> u are circumference<br />

<strong>and</strong> velocity of the flow Q. The nondimensional<br />

proportionality factor E is called<br />

the entrainment coefficient, which increases as<br />

the gradient Richardson number Ri decreases.<br />

This implies that entrainment is more efficient<br />

for large velocity differences <strong>and</strong> small density<br />

differences. Often entrainment involves the<br />

transport of one substance in another, such as<br />

suspended particles in a current, or parcels of<br />

moist air in dry winds.<br />

entropy That thermodynamic potential defined<br />

by the exact differential<br />

dS = dQ/T ,<br />

where dQ is a reversible transfer of heat in a<br />

system, <strong>and</strong> T is the temperature at which the<br />

transfer occurs. Entropy is conceptually associated<br />

with disorder; the greater the entropy the<br />

less ordered energy is available.<br />

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