Radioactive Investigations of Oil and Gas Wells 1965
DOI: 10.1016/b978-0-08-010001-2.50007-2
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Methods of Well Radiometry

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“…There are many methods and algorithms to calculate total porosity, like a combination of neutron‐density cross plot, cores and density log. Among these, estimation from density log ( ρ b , RHOB) is preferred if fluid and matrix densities are known (Anselmetti & Eberli, 1999; Asquith, 1985; Larionov, 1969). This relationship is written as ϕtotalbadbreak=ϕD0.33emgoodbreak=ρnormalm0.33em0.33emρbρnormalm0.33em0.33emρf,$$\begin{equation}{\phi }_{{\rm{total}}} = {\phi }_{\rm{D}}\ = \frac{{{\rho }_{{\rm{m}}\ - \ }{\rho }_{\rm{b}}}}{{{\rho }_{{\rm{m}}\ - }\ {\rho }_{\rm{f}}}},\end{equation}$$where ρ m is the matrix density, ρ f is the fluid density, and ρ b is the bulk density (measured density log data).…”
Section: Methodsmentioning
confidence: 99%
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“…There are many methods and algorithms to calculate total porosity, like a combination of neutron‐density cross plot, cores and density log. Among these, estimation from density log ( ρ b , RHOB) is preferred if fluid and matrix densities are known (Anselmetti & Eberli, 1999; Asquith, 1985; Larionov, 1969). This relationship is written as ϕtotalbadbreak=ϕD0.33emgoodbreak=ρnormalm0.33em0.33emρbρnormalm0.33em0.33emρf,$$\begin{equation}{\phi }_{{\rm{total}}} = {\phi }_{\rm{D}}\ = \frac{{{\rho }_{{\rm{m}}\ - \ }{\rho }_{\rm{b}}}}{{{\rho }_{{\rm{m}}\ - }\ {\rho }_{\rm{f}}}},\end{equation}$$where ρ m is the matrix density, ρ f is the fluid density, and ρ b is the bulk density (measured density log data).…”
Section: Methodsmentioning
confidence: 99%
“…There are various methods for obtaining shale volume, and in this research, we followed the method of Larionov's equations. Larionov (1969) introduced a method for shale volume calculation in tertiary or younger rocks using the following equations: IGRbadbreak=GRlogGRminGRmaxGRmin,$$\begin{equation}{I}_{{\rm{GR}}} = \frac{{{\rm{GR}}_{{\rm{log}}} - {\rm{GR}}_{{\rm{min}}}}}{{{\rm{GR}}_{{\rm{max}}} - {\rm{GR}}_{{\rm{min}}}}},\end{equation}$$ Vshbadbreak=0.33em0.33()2false[2IGRfalse]10.16emfor0.16emolder0.16emrocks,$$\begin{equation}{V}_{{\rm{sh}}} = \ 0.33\left( {{2}^{[2{I}_{{\rm{GR}}}]} - 1} \right)\,{\rm{for}}\,{\rm{older}}\,{\rm{rocks,}}\end{equation}$$ Vshbadbreak=0.33em0.083()2false[3.7IGRfalse]10.16emfor0.16emyounger0.16emrocks,$$\begin{equation}{V}_{{\rm{sh}}} = \ 0.083\left( {{2}^{[3.7{I}_{{\rm{GR}}}]} - 1} \right)\,{\rm{for}}\,{\rm{younger}}\,{\rm{rocks,}}\end{equation}$$where I GR is the gamma ray index, GR log is the measured gamma‐ray, GR min and GR max are observed minimum and maximum gamma‐ray, or clean rock and shaly (non‐organic) interval, respectively.…”
Section: Methodsmentioning
confidence: 99%
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