Abstract
In this chapter, we obtain the equations of motion that govern the simplest, non-trivial, deformable dynamics of an ellipsoidal body. We will employ volume averaging (also known as the method of moments or the virial method) to this end.
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Notes
- 1.
Further support for analyses that assume that granular minor planets deform in an affine manner will be found from results in plasticity theory (Sect. 4.4), and when comparing the predictions of such investigations with simulations and observation in the coming chapters.
- 2.
In fact, if we had retained \({\mathsf {B}}_S\) and \({\mathsf {B}}_P\) in their entirety when computing \({\mathbf {F}}_S\) and \({\mathbf {F}}_P\), then the formulae derived in Sect. 3.4 for \({\mathbf {F}}_S\) and \({\mathbf {F}}_P\) obey Newton’s third law, i.e., yield forces that are equal and opposite. This is proved as follows. From Maciejewski (1995), the total force exerted by the primary on the secondary, \({\mathbf {F}}_S = -\rho ''\rho 'G\int _{V''}\int _{V'}\frac{\overline{\mathbf {x}}_S - \overline{\mathbf {x}}_P}{\left| \overline{\mathbf {x}}_S - \overline{\mathbf {x}}_P\right| ^3}\mathrm{{d}}V' \mathrm{{d}}V''\), where \(\overline{\mathbf {x}}_S = {\mathbf {r}}_S + {\mathbf {x}}_S\) and \(\overline{\mathbf {x}}_P= {\mathbf {r}}_P + {\mathbf {x}}_P\) locate with respect to the mass center C material points in the primary and the secondary, respectively; see Fig. 3.1. The force \({\mathbf {F}}_P\) has the same formula, but with minus sign, so that \({\mathbf {F}}_S = -{\mathbf {F}}_P\). From Chandrasekhar (1969, p. 48, Theorem 7), \(-\rho 'G\int _{V'}\frac{\overline{\mathbf {x}}_S - \overline{\mathbf {x}}_P}{\left| \overline{\mathbf {x}}_S - \overline{\mathbf {x}}_P\right| ^3}\mathrm{{d}}V' = -2\pi \rho 'G{\mathsf {B}}_P\cdot {\mathbf {d}}_S\) , as it is the force per unit mass exerted at \({\mathbf {d}}_S\) by the primary; see Fig. 3.1. Similarly, \(-\rho ''G\int _{V''}\frac{\overline{\mathbf {x}}_P - \overline{\mathbf {x}}_S}{\left| \overline{\mathbf {x}}_P - \overline{\mathbf {x}}_S\right| ^3}\mathrm{{d}}V'' = -2\pi \rho ''G{\mathsf {B}}_S\cdot {\mathbf {d}}_P\). Thus, \({\mathbf {F}}_S = \rho ''\int _{V''}\left( -2\pi \rho 'G{\mathsf {B}}_P\cdot {\mathbf {d}}_S\right) \mathrm{{d}}V'' \) and \({\mathbf {F}}_P = \rho '\int _{V'}\left( -2\pi \rho ''G{\mathsf {B}}_S\cdot {\mathbf {d}}_P\right) \mathrm{{d}}V'\), which are exactly the formulae obtained in Sect. 3.4; see equations before (3.39) and (3.44). Clearly, \({\mathbf {F}}_S = -{\mathbf {F}}_P\).
- 3.
In a contact binary, the primary and the secondary touch each other. There may or may not be significant contact forces present. In this book, we will assume that the contact forces, if any, are insignificant compared to other forces present. The extent to which this assumption is valid will often be revealed by the mismatch of our predictions with observations; see, e.g., applications to binary near-Earth binaries in Sect. 10.8.
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Sharma, I. (2017). Affine Dynamics. In: Shapes and Dynamics of Granular Minor Planets. Advances in Geophysical and Environmental Mechanics and Mathematics. Springer, Cham. https://doi.org/10.1007/978-3-319-40490-5_3
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