The real secret of turbulence is the sequential , and thus discrete nature of it . It is quite clear that a streamline oscillates after impacting a density and lubricity/ viscosity region. This oscillation is generated along and at the boundary between the different regional substances. While it is easy to overlook it is plain to see that vortices not only dance around each other they oscillate sequentially relative to each other. This sequence is given the name phase which obscures its function. The sequential process is to seed, grow and protect the formation of a regional vortex until it is given birth to by reason of exceeding its dynamic boundary conditions, at the same time as this grows , the protecting vortex is shed by a thinning umbilical cord which is eventually and rapidly drawn into the anti flow around the developing vortex and becomes the seed for another anti vortex to grow and repeat the cycle.
The drive for this cyclical vortex production is the head pressure of the flow, but the inherent vorticity shapes the dynamics through the density and viscosit/ lubricity profiles. In a fluid, rigidity drops off on a sliding scale. Thus a rigid rotational description is misleading. The rotation of a fluid is easily shaped on its boundary. Thus to draw a line of circulation around a vortex is erroneous, while rotation implies a closed loop it does not imply a continuous boundary. In fact the boundary is best described as a collection of arcs. The nature of these arcs could be quite arbitrary, but observation suggests trochoids as good approximations or splines. Thus we may define a circulation boundary as an intersection of trochoidal arcs and the vorticity as the sum of the vorticity of the trochoids.
This then leaves sections of the circulation amenable to interaction, so that a powerful contra trochoid can knock out a circulation spline, but still. Lose the loop. The reduction in the circulation this implies can lead to a vortex core with higher vorticity peeling off and running against the unravelling circulation boundary.
The collapse of the outer boundary allows pressure deformations to seed a contra vortex
The determination of the rotational profile can be modelled by the winding of a piece of elastic. The tension that moves the fluid behaves like a compression or stress front that travels at a fixed speed along a spiral surface rotating out against a spiral surface being dragged in and thus creating another compression or stress front between successive layers of the first. This continues until as many interleaved spiral urfaces as can be supported are achieved and the whole fluid is subject to these cylindrical stress surfaces. The vortex movement is then block like but not rigid. Individual sheets may reach fracture points a and shear away from the elastic like sheet allowing local turbulence to develop. This may grow and lead to a collapse of the sheets dependent on it, or form a trapped bubble that rotates in the vortex, depending on the local density, lubricity and viscosity. These bubbles may be long lasting , intermittent or explosive.
The behaviour of fluids is certainly very interesting and capable of all inconceivable motions! …