AD
Abbreviation
from
the Latin anno domini.
Denotes the time period after the birth of Christ.
A/m
Ampère
per metre. Unit of magnetisation
when expressed per unit of volume.
Typically, the natural
remanent magnetisation of a baked clay is in the
order of 1 A/m and of a sediment 10-3 A/m.
Am2
Ampère
times metres squared. Unit of the magnetic moment.
Am2/kg
Ampère
times metres squared per kilogram. Unit of magnetisation when expressed
per unit of weight.
Anhysteretic
remanent magnetisation (ARM)
Remanent
magnetisation imparted to a sample in the laboratory by applying a
decaying alternating
magnetic field in the
presence of a steady magnetic
field.
Anisotropy
of magnetic susceptibility (AMS)
Antiferromagnetism
(see also ferromagnetism). Form of
ferromagnetism in crystalline material with two oppositely and equally
magnetised sublattices. The
quantum mechanical exchange
interaction
at short distance between cations via an anion (indirect interaction)
favours an
antiparallel
alignment of the individual magnetic moments of atoms or ions. The
resulting magnetisation
is zero. The magnetic susceptibility is weak.
Antiferromagnetics become paramagnetic (see also paramagnetism) beyond
the Néel-Temperature.
Example: haematite.
Antiferromagnetics
often have ferromagnetic properties due to impurities (parasitic
ferromagnetism, e.g. in goethite,
haematite) or because of an imperfect
antiparallelism of the magnetic moments (canted antiferromagnetism,
e.g. haematite).
Archaeointensity
Archaeomagnetic dating
Archaeomagnetism
(see also
palaeomagnetism) For
the archaeologist a dating method based on the remanent magnetisation of baked clays.
Study of the magnetic properties
of archaeological materials (mainly baked clays) of historical or
pre-historical age.
Archaic Period
Cultural period
in Greece between 750 and 500 BC, subsequent to the Dark Ages and
followed by the Classical period.
This period is characterised by the
naturalistic representation of the human figure, the formation of
city-states and the rise the aristocracy.
Azimuth
Angle between
the vertical plane through the observation sight-of-line and the
geographic
meridial plane.