摘要: With high-resolution narrowband He I 10830 \r{A} filtergrams from GST, we
give an extensive analysis for 4 granular sized microeruptions which appear as
the gentle ejection of material in He I 10830 \r{A} band. The analysis was
aided with the EUV data from AIA and line-of-sight magnetograms from HMI on
board SDO. The microeruptions are situated on magnetic polarity inversion lines
(PILs), and their roots are accurately traced down to intergranular lanes.
Their durations are different, two microeruptions are repetitive microjets,
lasting ~ 50 and 27 minutes respectively, while the other two events are
singular, lasting ~ 5 minutes. For the two microjets, they are continuous and
recurrent in He I 10830 \r{A} band, and the recurrence is quasi-periodic with
the period of ~ 5 minutes. We found that only transient co-spatial EUV
brightenings are observed for the longer duration microjets and EUV
brightenings are absent for the two singular microeruptions. What is essential
to the longer duration microjets is that granules with the concentration of
positive magnetic field persistently transport the magnetic field to the PILs,
canceling the opposite magnetic flux and making the base of the two microjets
and the underlying granules migrate with the speed of ~ 0.25 and 1.0 km/s. The
observations support the scenario of magnetic reconnection for the
quasi-periodic microjets and further show that the reconnection continuously
generates multi-temperature components, especially the cool component with
chromospheric temperature. In addition, the ongoing reconnection is modulated
by p-mode oscillations inside the Sun.