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@wikipedia


Stationary Fluid flow when  with fluid pressure and temperature across reservoir do not change  pressure 

LaTeX Math Inline
bodyp(t, {\bf r})
 is not changing in time:

LaTeX Math Block
anchorp
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p(t, {\bf r}) = p({\rm const
\\[1.2ex]
Tbf r})

This immediately leads to stationary fluid velocity 

LaTeX Math Inline
body{\bf u}(t,

...

{\bf

...

r})

...

This automatically implies that fluid density also stay constant as soon as the flow is in thermodynamic quasistatic equilibrium:

mathblock
LaTeX Math Block
anchoru
alignmentleft
{\rhobf u}(t, {\bf r}) = {\bf u}({\rm const

Well production or injection resulting in steady state flow is characterized by 

constant rate:

bf r})



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Expand
titleDerivation


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In the most general case (both reservoir and pipelines) the fluid velocity is a function of pressure and pressure gradient and can be written as:

LaTeX Math Block
anchor1
alignmentleft
q
{\bf u}(t, {\bf r})= 
= q = \rm const

constant formation pressure 

LaTeX Math Block
alignmentleft
p_e(t) = p_e = \rm const

and constant bottom-hole pressure:

F({\bf r}, p, \nabla p)

with right side not dependent on time in stationary flow:

LaTeX Math Block
anchor1
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\frac{\partial {\bf u}(t, {\bf r})}{\partial t}= 0

which leads to

LaTeX Math Block Reference
anchoru
.



The fluid temperature 

LaTeX Math Inline
bodyT(t, {\bf r})
 is supposed to vary slowly enough to provide quasistatic equilibrium.


This flow regime is often observed in pipeline fluid flow and reservoir fluid flows.

See also

...

Physics / Fluid Dynamics 

Steady State Well Flow Regime (SS) ]

...

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