Mj. Dekkers et al., Magnetic properties of hydrothermally synthesized greigite (F3S4) - II. High- and low-temperature characteristics, GEOPHYS J I, 141(3), 2000, pp. 809-819
The magnetic behaviour of hydrothermally synthesized greigite was analysed
in the temperature range from 4 K to 700 degrees C. Below room temperature,
hysteresis parameters were determined as a function of temperature, with e
mphasis on the temperature range below 50 K. Saturation magnetization and i
nitial susceptibility were studied above room temperature, along with X-ray
diffraction analysis of material heated to various temperatures. The magne
tic behaviour of synthetic greigite on heating is determined by chemical al
teration rather than by magnetic unblocking. Heating in air yields more dis
criminative behaviour than heating in argon. When heated in air, the amount
of oxygen available for reaction with greigite determines the products and
magnetic behaviour. In systems open to contact with air, haematite is the
final reaction product. When the contact with air is restricted, magnetite
is the final reaction product. When air is excluded, pyrrhotite and magneti
te are the final reaction products; the amount of magnetite formed is deter
mined by the purity of the starting greigite and the degree of its surficia
l oxidation. The saturation magnetization of synthetic greigite is virtuall
y independent of temperature from room temperature down to 4 K. The saturat
ion remanent magnetization increases slowly by 20-30 per cent on cooling fr
om room temperature to 4 K. A broad maximum is observed at similar to 10 It
which may be diagnostic of greigite. The coercive and remanent coercive fo
rce both increase smoothly with decreasing temperature to 4 K. The coercive
force increases from similar to 50 mT at room temperature to approximately
100-120 mT at 4 K, and the remanent coercive force increases from approxim
ately 50-80 mT at room temperature to approximately 110-180 mT at 4 K.