Geology Reference
In-Depth Information
G
molar free energy
p
i
partial pressure
of component
i
in a gas mixture
G
universal gravitational constant (when printed
bold in this topic).
P
load pressure, in pascals (Pa), megapascals
(MPa = 10
6
Pa) or gigapascals (GPa = 10
9
Pa)
Ga
'giga-annum' = 1 billion years = 10
9
years
pH
= −log
10
a
H
+
(measure of acidity/alkalinity)
h
height in m
p
H
2
O
partial pressure
of H
2
O in a gas mixture (e.g.
air), in same units as
P
H
molar enthalpy
k
rate constant
q
ionic charge, measured as a multiple of the
charge on an electron
K
equilibrium constant
K
i
A
partition coefficient
describing the distribution
of element
i
between melt and mineral A.
See Box 9.1*
r
(a) radial co-ordinate; (b) ionic radius (Box 2.6),
in pm (picometres = 10
-12
m)
S
molar entropy
L
litre (see dm
3
)
t
time, in seconds, minutes, years (a), thousands
of years (ka) or millions of years (Ma)
L
length of guitar string (Equation 5.1)
ln
natural logarithm = log
e
t
1/2
half-life
m
mass
T
temperature, in °C or kelvins (K)
Ma
'mega-annum' = 1 million years = 10
6
years
v
velocity
meq
milliequivalents
x
spatial co-ordinate
n+
nominal cation charge in atomic charge units*
x
a
the mass proportion (0 <
x
a
< 1.00) of component
(e.g. mineral)
a
in a mixture
n
D
number of daughter nuclei present in a
sample*
X
(a) composition in general terms; (b) composi-
tion of a mineral expressed in molar propor-
tions of its end-members*
n
P
number of parent (radionuclide) nuclei present
in a sample*
N
neutron number (Box 10.1)*
y
years
N
c
co-ordination number (Table 7.1)*
y
spatial co-ordinate, transverse displacement of
guitar string (Equation 5.1)
p
number of non-bridging oxygens per silicon
atom in a silicate crystal structure - a measure
of polymerization*
z
spatial co-ordinate
Z
atomic number*
*Dimensionless quantity.
Greek and other symbols (in Greek alphabet order)
α
alpha
notional stirring rate in heterogeneous kinetics experiment (Equation 3.4)
α
2
+
alpha-particle
4
He nucleus, consisting of 2 protons and 2 neutrons
β
-
beta
beta-particle = high-energy electron emitted from a nucleus
β
+
positron (
antimatter
particle equivalent to electron)
δ
18
O
delta
18
O
18
O/
16
O ratio in a mineral or rock, expressed as the positive or negative deviation in parts
per thousand (‰ = 'per mil') from the
18
O
16
O value in a reference material (see Glossary)
Δ
G
delta
†
-
G
free energy change accompanying a reaction
Δ
H
delta
†
-
H
ethalpy change accompanying a reaction
Δ
S
delta
†
-
S
entropy change accompanying a reaction
Δ
T
delta
†
-
T
temperature change, degree of supercooling (=T −
T
solidus
) in °C
η
eta
viscosity (Equations 3.14 and 3.15)
λ
lamda
(a) wavelength; (b) radioactive decay constant
v
nu
neutrino
v
nu-bar
anti-neutrino (antimatter particle)
†
These are the capital forms of the relevant Greek letter.
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