We start by selecting a spherical control volume dV. As shown in the figure below, this is given by
where r, θ, and φ stand for the radius, polar, and azimuthal angles, respectively. The azimuthal angle is also referred to as the zenith or colatitude angle.
The differential mass is
We will represent the velocity field via
In an Eulerian reference frame mass conservation is represented by accumulation, net flow, and source terms in a control volume.
AccumulationThe accumulation term is given by the time rate of change of mass. We therefore haveThe net flow through the control volume can be divided into that corresponding to each direction.
Radial FlowStarting with the radial direction, we haveThe inflow area Ain is a trapezoid whose area is given by
The key term here is the sine term. Note that the mid segment is the average of the bases (parallel sides). Upon expansion of Ain, and in the limit of vanishing dθ, we have
substitution into Ain yields
where high order terms have been dropped.
The outflow in the radial direction is
but
where
and
By only keeping the lowest (second & third) order terms in the resulting expression, we have
Note, that in the expression for Aout, we kept both second order and third order terms. The reason for this is that this term will be multiplied by "dr" and therefore, the overall order will be three. In principle, one must carry all those terms until the final substitution is made, and only then one can compare terms and keep those with the lowest order.
At the outset, the net flow in the radial direction is given by
Polar Flow (θ)The inflow in the polar direction iswhere
The outflow in the θ direction is
where
Upon expansion, and keeping both second and third order terms, we get
Finally, the net flow in the polar direction is
Azimuthal Flow (φ)The inflow in the azimuthal direction is given bywith
while the outflow is
and
At the outset, the net flow in the polar direction is
Continuity EquationNow, by collecting all mass fluxes we havewhich, upon dividing by dV and combining terms, reduces to
which is the continuity equation in spherical coordinates
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derivation of pedal equation
There are basically SEVERAL continuity equations, one for each conserved quantity. The equations themselves are simply statements that matter (in the example of conservation of mass) will not appear out of nothing, or suddenly teleport to a far-away place.
http://en.wikipedia.org/wiki/Navier-Stokes_equations Please go to this page.
They could be the coordinates of a straight line equation
Yes if it is a straight line equation