Fig. 9
Aspect ratio as a function of orbital distance for the discs with high α-viscosity values (top left), namely α = 10−2, 5 × 10−3 and low α-viscosity values (bottom left), namely α = 10−3, 5 × 10−4 and 5 ×10−4, for the two grain size distributions (BOD in dark blue, MRN in reddish pink). The iceline moves inwards as α decreases, due to reduced viscous heating. The wiggles that can be seen in parts of the low α discs are caused by convection. Right plots: temperature as a function of orbital distance for the discs with high α-viscosity values (top), namely α = 10−2, 5 × 10−3 and for low α-viscosity values (bottom), namely α = 10−3, 5 × 10−4 and 10−4.
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