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The neutron porosity is usually abbreviated NPHI or PHIN  on log panels and denoted as 

LaTeX Math Inline
body\phi_n
  in equations.


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anchor1
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N_n = \phi N_f + V_{sh} N_{sh} + V_m N_m

which can be re-arranged as:

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anchor1
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N_n = N_m  + V_{sh} \cdot (N_{sh} -N_m) + \phi \cdot (N_f - V_{sh} N_m)


The key measurement is compensated neutron log  

LaTeX Math Inline
bodyN_n
 (log name CNL) from Compensated Neutron Tool.

The key model parameters are:

LaTeX Math Inline
bodyN_m

rock matrix CNL

LaTeX Math Inline
bodyN_{sh}

shale CNL

LaTeX Math Inline
bodyN_f

pore-saturating fluid CNL

LaTeX Math Inline
bodyN_{mf}

mud filtrate CNL

LaTeX Math Inline
body\{ N_w, \, N_o, \, N_g \}

formation water, oil, gas CNL

LaTeX Math Inline
bodys_{xo}

a fraction of pore volume invaded by mud filtrate

LaTeX Math Inline
body\{ s_w, \, s_o, \, s_g \}

original water, oil, gas reservoir saturations

LaTeX Math Inline
bodys_w + s_o + s_g = 1



The values of 

LaTeX Math Inline
bodyN_m
 and 
LaTeX Math Inline
bodyN_{sh}
 are calibrated for each lithofacies individually and can be assessed as vertical axis cut-off on 
LaTeX Math Inline
bodyN_{log}
 cross-plot against the lab core porosity 
LaTeX Math Inline
body\phi_{\rm air}
 and shaliness 
LaTeX Math Inline
bodyV_{sh}

The model also accounts for saturating rock fluids with fluid CNL value 

LaTeX Math Inline
bodyN_f
.

In overbalance drilling across permeable rocks the saturating fluid is usually mud filtrate

In underbalance drilling the saturating fluid is identified from resistivity logs.  


The total neutron porosity 

LaTeX Math Inline
body\phi_n
 equation is:

LaTeX Math Block
anchorphie_rhob
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\phi_n = \frac{N_n - N_m}{N_f-V_{sh}N_m}


The effective neutron porosity 

LaTeX Math Inline
body\phi_{en}
 equation is:

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anchorphie_rhob
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\phi_{en} = \phi_n -  \frac{N_{sh}-N_m}{N_f - V_{sh}N_m} \cdot V_{sh}


The fluid density 

LaTeX Math Inline
bodyN_f
 is calculated in-situ using the following equation:

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anchorBL8T4
alignmentleft
N_f = s_{xo} \rho_{mf} + (1-s_{xo}) ( s_w N_w + s_o N_o + s_g N_g )


The matrix CNL is calculated from the following equation:

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N_m = \sum_i V_{m,i} N_{m,i}

where 

LaTeX Math Inline
bodyV_{m,i}
 – volume share of the i-th matrix component,

LaTeX Math Inline
bodyN_{m,i}
 – density of the i-th matrix component,

LaTeX Math Inline
body\sum_i V_{mi} =1
.


See also

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Petrophysics / Volumetric Rock Model