Abstract. Taylor's power law (TPL) describes the scaling relationship between
the temporal or spatial variance and mean of population densities by a
simple power law. TPL has been widely testified across space and time in
biomedical sciences, botany, ecology, economics, epidemiology, and other
fields. In this paper, TPL is analytically reconfirmed by testifying the
variance as a function of the mean of the released energy of earthquakes
with different magnitudes on varying timescales during the Wenchuan
earthquake sequence. Estimates of the exponent of TPL are approximately 2,
showing that there is mutual attraction among the events in the sequence. On
the other hand, the spatio-temporal distribution of the Wenchuan
aftershocks tends to be nonrandom but approximately definite and
deterministic, which highly indicates a stable spatio-temporally dependent
energy release caused by regional stress adjustment and redistribution
during the fault revolution after the mainshock. The effect of different
divisions on estimation of the intercept of TPL straight line has been
checked, while the exponent is kept to be 2. The result shows that the
intercept acts as a logarithm function of the time division. It implies that
the mean–variance relationship of the energy release from the earthquakes
can be predicted, although we cannot accurately know the occurrence time and
locations of imminent events.