Orbital angular momentum carried by the wind. Use a circular orbit of separation , and write and . The donor's distance from the center of mass is . With spins neglected, its specific orbital angular momentum is , while the circular-binary orbital angular momentum is
A fast spherically symmetric stellar wind has no net extra angular momentum in the donor's rest frame and escapes with mean specific orbital angular momentum . Thus Jeans-mode mass loss gives
Initially take negligible wind capture by the companion, so , and the total mass derivative is . Logarithmic differentiation of gives
Combining the two expressions yields , so is constant. Kepler's third law then gives . Hence
These are secular relations for slow changes of the orbit through nearly circular states. A wind being fast compared with orbital speed does not mean its mass-loss timescale is shorter than an orbital period; impulsive removal would require a different orbital calculation.
Whether wind drives contact. Ignore nuclear expansion on the stated short evolutionary timescale. With and , wind alone gives
Because , the ratio increases precisely when
This is wind-driven Roche-lobe overflow: the escaping wind makes the donor expand relative to its lobe and drives a separate transfer stream. It is not the slow-wind capture mechanism called Wind Roche-lobe overflow. If the inequality is reversed, the donor recedes inside its expanding lobe and detaches; wind loss alone does not maintain a Roche-lobe transfer stream. At equality it gives no leading-order change of overfill, so additional evolution or higher-order changes decide the outcome.
Contact rate and its stability. Now let the transfer stream be accreted conservatively by star 2 while the separate wind still escapes at rate . Denote the stream rate by . Then
Only the wind removes orbital angular momentum; internal transfer redistributes it. Using the same wind-loss law and differentiating gives
Substitute this into the donor and lobe radius derivatives. The overfill evolves as
Maintaining contact sets the left side to zero and gives the contact transfer rate with Jeans-mode wind loss,
When the wind-drive condition holds, its numerator is positive. If , the denominator is also positive and the stream rate is positive; increasing transfer reduces overfill and can balance the wind driver.
If instead , positive transfer increases overfill, which drives still more transfer. The formal contact formula would demand a negative stream rate and is not a physical steady solution. The system develops unstable, runaway mass transfer on the timescale appropriate to the assumed donor response. For a giant with an adiabatically responding envelope, this can lead to a common envelope and rapid orbital evolution, rather than the stable contact sequence; the eventual outcome requires physics beyond these radius laws. At , transfer gives no linear restoring effect, and a nonzero wind driver cannot be balanced by a finite rate within this approximation.
An intrinsic S-type star is a thermally pulsing AGB star whose third dredge-up exposes carbon and products of the slow neutron-capture process. An extrinsic S-type star has similar surface pollution but no current internal source; it received the material from a former AGB companion. A barium star is the warmer main-sequence or giant counterpart, recognized particularly through strong barium and other slow-neutron-capture elements.
This interpretation predicts a white dwarf companion, the remnant of the former AGB donor. Barium and extrinsic S-type stars are indeed binaries, often with periods long enough that the donor could not have undergone ordinary Roche-lobe overflow. Their abundance patterns, white-dwarf companions, and wide or eccentric orbits therefore point to wind mass transfer in a binary star.
The Bondi–Hoyle accretion estimate treats the companion as moving through a locally uniform wind with relative speed , sound speed , and density . Gravity focuses gas from the accretion radius
giving
For a roughly spherical donor wind, and combines wind and orbital velocities. This supplies an order-of-magnitude accreted fraction; wind acceleration, density gradients, orbital deflection, and Wind Roche-lobe overflow can substantially change it.
For initial masses and , increasing the initial period gives three broad channels:
The transition periods are set by the primary's maximum radius relative to its Roche lobe, and their exact values depend on mass-transfer efficiency, wind speed, and common-envelope energy formalism.
A fast escaping Jeans-mode mass loss wind can drive a giant into Roche-lobe overflow because its radius changes as it loses mass, even though the wind itself is not substantially captured. This differs from slow Wind Roche-lobe overflow. For and , wind alone gives , where and is the escaping wind rate. The displayed inequality is exactly the condition that overfill increases.