![\begin{figure}
\par\includegraphics[width=8.8cm]{Gf012_f1.eps} \end{figure}](/articles/aa/full/2004/32/aagf012/Timg12.gif) |
Figure 1:
A top view of the solar nebula illustrating the various regions of
the viscosity. Inner region: MRI (magnetorotational
instability) survives due to the thermal ionization. High
viscosity, high radial inflow velocity, and short inflow time.
Intermediate region: MRI is suppressed. Low viscosity, low
inflow velocity, and long inflow time. Outer region: MRI
survives due to the ionization by cosmic rays. High viscosity,
high inflow velocity, and short inflow time. The material tends to
accumulate in the Jupiter-Saturn region due to the difference of
the inflow velocity between the intermediate and outer regions.
The gas inflow time in Jupiter-Saturn region is long enough that
they have time to capture the gas. |