Charged particle motion in reconnecting current sheets (CS) can be bot
h regular and chaotic, depending on the values of transverse (perpendi
cular to the CS plane) and longitudinal (parallel to the electric fiel
d inside the CS) components of the magnetic field. The non-zero transv
erse field gives rise to chaos, whereas a sufficiently large longitudi
nal field tends to stabilize the motion. The longitudinal field change
in time may be the cause of different regimes of electron acceleratio
n in solar flares and magnetospheric substorms.