We investigate the fossil magnetic field in the accretion and protoplanetary
discs using the Shakura and Sunyaev approach. The distinguishing feature of
this study is the accurate solution of the ionization balance equations and the
induction equation with Ohmic diffusion, magnetic ambipolar diffusion, buoyancy
and the Hall effect. We consider the ionization by cosmic rays, X-rays and
radionuclides, radiative recombinations, recombinations onto dust grains, and
also thermal ionization. The buoyancy appears as the additional mechanism of
magnetic flux escape in the steady-state solution of the induction equation.
Calculations show that Ohmic diffusion and magnetic ambipolar diffusion
constraint the generation of the magnetic field inside the dead' zones. The magnetic field in these regions is quasi-vertical. The buoyancy constraints the toroidal magnetic field strength close to the disc inner edge. As a result, the toroidal and vertical magnetic fields become comparable. The Hall effect is important in the regions close to the borders of the dead’ zones because
electrons are magnetized there. The magnetic field in these regions is
quasi-radial. We calculate the magnetic field strength and geometry for the
discs with accretion rates .
The fossil magnetic field geometry does not change significantly during the
disc evolution while the accretion rate decreases. We construct the synthetic
maps of dust emission polarized due to the dust grain alignment by the magnetic
field. In the polarization maps, the `dead’ zones appear as the regions with
the reduced values of polarization degree in comparison to those in the
adjacent regions.

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