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@wikipedia


Motivation

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The pipeline and wellbore flow simulations require a model of static fluid pressure
 

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 variation as a function of elevation
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:

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p = p(z)


Output

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bodyp(z)

Fluid pressure 

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Input

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bodyz

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body\rho_0

Fluid density at Logging reference point 

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Logging reference point (usually at surface)

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bodyc_0

Fluid Compressibility at Logging reference point 

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bodyz_0

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bodyg

Standard gravity constant



Equation

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The static balance equation for fluid column is:

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\frac{dp}{dz}= \rho(p) \cdot g


Approximations

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fluid

Ideal Gas

(Barometric formula)

Full-range model


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p(z) = p_0 + \rho_0 \cdot g \cdot (z-z_0)

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p(z) = p_0 \cdot \exp \left[ - \frac{

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\rho_0 \, g}{

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p_0} \cdot (z-z_0) \right]

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\frac{1+ c_0 \, p(z)}{1 + c_0 \, p_0} = \exp \left[ \frac{ с_0 \cdot \rho_0 \cdot g \cdot (z-z_0)}{1+c_0 \, p_0} \right]

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p_2 - p_1 = \rho_0 \cdot g \cdot (z_2-z_1)



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p_2 - p_1  = p_1  \cdot \left( \exp \left[ \frac{  \rho_0 \cdot g \cdot (z_2-z_1)} {p_0}  \right] - 1 \right) 

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LaTeX Math Block
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p_2 - p_1  = \frac{ (1+c_0 \, p_1)}{c_0}  \cdot \left( \exp \left[ \frac{ с_0 \cdot \rho_0 \cdot g \cdot (z_2-z_1)}{1+c_0 \, p_0} \right] - 1 \right) 



See also

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Physics / Mechanics / Continuum mechanics / Fluid Mechanics / Fluid Statics

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