We present a study of the magnetic properties of the superparamagnetic
ferritin system by employing zero-field (ZF) and longitudinal-field (
LF) mu(+)SR measurements. Two mu(+) fractions with different depolaris
ation behaviour are detected, one arising from muons stopped in the or
ganic shell and one from muons stopped in the mineral core. The freezi
ng of the superparamagnetic moments is evident in the temperature evol
ution of the ZF relaxation rates of both fractions. It occurs graduall
y below approximate to 60 K and is essentially complete at approximate
to 11 K. The results are consistent with a distribution of blocking t
emperatures which in turn reflects the distribution of core sizes.