Solution

ID: past-exam-of-the-mathematics-course-of-the-university-of-cambridge/2004/iii/paper-63/3/solution

For Roche-lobe overflow, . Cubing the Roche lobe approximation and using the donor's mass-radius relation gives
Kepler's third law therefore yields the Roche-lobe period-mass relation for a linear donor radius law:
The component distances from the centre of mass are and . Summing their angular momenta gives the circular-binary orbital angular momentum
During conservative binary mass transfer, and . Logarithmic differentiation at constant angular momentum gives . Thus the Roche-lobe radius response exponent gives
Their difference is . Since the donor loses mass, this is positive for : the donor shrinks relative to its Roche lobe, so transfer shuts off without an external driver. The Roche lobe itself expands only for ; for it shrinks more slowly than the donor.
Gravitational-wave emission from a binary system provides such a driver: the orbit emits gravitational waves carrying energy and angular momentum, and the shrinking Roche lobe can maintain contact. Allowing , the binary mass-transfer contact equation becomes
It gives a negative transfer rate for .
For the classical nova, assume isotropic re-emission from a binary star: ejecta carry the accretor's specific angular momentum . The eruption lasts many orbital periods, so the orbit responds approximately adiabatically and remains nearly circular; an instantaneous asymmetric kick would be a different model. To first order,
Differentiating the circular-binary orbital angular momentum formula during the ejection gives
The accompanying Roche lobe change is therefore
The donor does not change mass in the eruption and moves inside its expanded Roche lobe: this is nova-induced binary detachment.
Put for the constant external loss. During detachment the component masses are fixed, so the Roche lobe shrinks at fractional rate . Closing the fractional gap takes . During the subsequent semidetached binary phase, the binary mass-transfer contact equation gives , so accumulating the next eruption's mass takes . Consequently
Both times are evaluated to first order in , with the same equilibrium donor mass-radius relation; changes of and the transfer rate within one cycle affect higher orders.

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