Sample
In archaeomagnetism,
a piece or fragment of baked material taken
in an in-situ
baked structure.
Secular variation
The interior
geomagnetic field is
also a function of time. The field slowly
changes its direction and intensity. This
temporal change is known as secular variation.
The secular variation has been discovered by the English
mathematician and astronomer H. Gellibrand (1597-1637) in 1634.
The secular variation can be graphically represented in a
Bauer-plot (inclination vs. declination), named
after L.A. Bauer (1865
- 1920). Basis of
archaeomagnetic
dating.
Specimen
Cylindrical or cubic piece cut from a
sample by drilling or sawing, respectively.
Spherical harmonics
Spinner magnetometer
Instrument to measure
the remanent
magnetisation of rocks based
on the dynamo principle. The sample is rotated in the
centre of a coil. During rotation the field
lines of the magnetic
moment of the sample cut the coil and
induce in it an electromagnetic force (signal) according to the
law of Faraday. The amplitude of the signal is proportional to
the magnetic moment of the sample and its phase
determines the direction of the magnetic
moment.
SQUID-sensor
The SQUID sensor
or Superconducting Quantum Interference
Device can be regarded as a ring with
superconducting properties. Once a circulating
current I is stimulated in
the ring, it flows for ever as the resistivity is
nearly zero and the current can only be changed
through an external magnetic field (from a sample). When
the external magnetic field is strong enough, the
circulating current reaches a critical
value Ic,
the SQUID becomes resistive, magnetic flux enters the ring and
the current drops by quantised values ΔI = nΦ0 (nΦ0 denotes multiples of
the flux quantum Φ0 = ħ/2e
= 2.07 ( 10-15, ħ
= Planck’s constant and e = electron charge) below Ic. As the current
dropped below Ic,
the superconducting state is achieved again. Further
increase of the external magnetic field yield multiple flux
changes. A critical current equal to 0.75Φ0, causes the
circulating current to change polarity. The number of polarity
changes is proportional of the magnetic
field produced by the sample and
hence to its remanent magnetisation.
Stokehole
Part of a kiln. A hollow dug into
the
ground from which fuel was put into the fire burning in the
combustion chamber.
Also called stoke-pit. If the kiln is
built at the surface one can speak about a stoking area.
Stone-age
Denotes a time period
in the early development of the human society before the
use of metals, Weapons and tools were made from stone. Began
in Europe around 2 million years ago and ended around 4000 BC.
It can be subdivided in three periods Palaeolithic,
Mesolithic and Neolithic.
Superparamagnetism
Ferromagnetism of very small particles (in the order of 30
nm and smaller) that have relaxation
times on the laboratory time scale.
Superstructure
Free-standing temporary or permanent walling of the kiln above
the ground, this term applies also to the kiln structure above
the level of the raised oven-floor.
Support
Protruding, recessed or raised structure, temporary or
inbuilt located in the combustion chamber of a kiln, to
support the mechanical stability of the
overlying raised oven-floor. If located in the
centre of
the kiln as single standing element, also called pedestal.