The motion of charged particles in reconnecting current sheets can be
either chaotic or regular depending on the magnetic field structure wi
thin the current sheet, namely, relative transversal and longitudinal
components of the magnetic field. The nonzero transversal magnetic fie
ld is responsible for chaotic trajectories, whereas the appreciable lo
ngitudinal component suppresses the chaos. In high-temperature current
sheets typical for the solar atmosphere the threshold longitudinal co
mponent is by an order of magnitude lower than the principal (reconnec
ting) component. Variations of the longitudinal component may be respo
nsible for the existence of various regimes of electron acceleration o
bserved in solar flares.