Hydrodynamical shear mixing in subsonic boundary layers and its role in the thermonuclear explosion of classical novae

Open Access

Fig. 4.

Initial mass fractions of ¹H, ¹²C, ¹⁴N and ¹⁶O at the WD envelope. The variable q is a mass variable defined as q = 1 − M_int/M_WD, where M_int is the interior mass (q = 0 denotes the outermost envelope layers – i.e. WD surface). The profiles for models 080COSHIVA, 080COcarb are plotted in panel (a) and the ones for models 125COSHIVA and 125COcarb are plotted in panel (b).

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