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ericm1234
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Can anyone point me to a derivation of the navier stokes equations in polar? I don't see where the single derivative in theta terms are coming from in the first 2 components.
ericm1234 said:the equations are not derived in the link you gave; my own derivation fails to see where the last terms in those 2nd and 3rd equations in that link are coming from.
The Navier-Stokes equation in polar coordinates is a mathematical formula that describes the motion of a fluid in terms of its velocity, pressure, and other properties. It is a fundamental equation in fluid mechanics and is used to model a wide range of physical phenomena.
The Navier-Stokes equation can be derived from the fundamental principles of conservation of mass, momentum, and energy. In polar coordinates, the equations of motion are written in terms of the radial and tangential components of velocity, which are related to the Cartesian components through a transformation.
The derivation of the Navier-Stokes equation in polar coordinates assumes that the fluid is incompressible, Newtonian (exhibiting constant viscosity), and inviscid (no friction or viscosity forces). Additionally, it assumes that the fluid is in steady state, meaning that the properties of the fluid do not change with time.
The Navier-Stokes equation in polar coordinates is a powerful tool for understanding and predicting fluid behavior. It is used in a wide range of applications, from studying the flow of air around an airplane wing to modeling ocean currents. It also has important implications for fields such as weather forecasting, aerodynamics, and hydrodynamics.
While the Navier-Stokes equation in polar coordinates is a useful and widely used tool, it does have some limitations. For example, it assumes that the fluid is in a steady state, which may not always be the case in real-world situations. It also does not take into account certain complexities, such as turbulence, which can significantly affect fluid behavior. Therefore, it should be used with caution and in conjunction with other models and techniques.