METHODS AND SYSTEMS FOR DETERMINING BULK DENSITY, POROSITY, AND PORE SIZE DISTRIBUTION OF SUBSURFACE FORMATIONS
First Claim
1. A non-transitory computer-readable medium having computer executable instructions that trigger a computer to perform the operations of:
- receiving in-air mass of a fluid-saturated sample of the subsurface formation, wherein the in-air mass comprises mass of matrix or grains of the sample, mass of a fluid surrounding the sample, and mass of the fluid inside the sample, the in-air mass of the fluid-saturated sample, ms, given by the formula;
ms=Vmρ
m+(Vϕ
+Vsur)ρ
l where ρ
m is a density of the matrix of the subsurface formation, ρ
l is a density of the fluid inside and surrounding the sample, Vm is a volume of the matrix, Vϕ
is a volume of the fluid inside the sample, and Vsur is a volume of the fluid surrounding the sample;
determining volume of the fluid inside the sample, Vϕ
, and volume of the fluid surrounding the sample, Vsur, using nuclear magnetic resonance (NMR);
receiving mass of the fluid-saturated sample in a weighing fluid;
determining mass of the fluid-saturated sample without the surrounding fluid in the weighing fluid, mf, given by the formula;
mf=Vmρ
m+Vϕ
ρ
l−
Vcρ
f where ρ
f is the density of the weighing fluid; and
determining a volume of the fluid-saturated sample without the surrounding fluid, Vc, using the formula;
Vc=(ms−
mf−
Vsurρ
l)/ρ
f.
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Accused Products
Abstract
Herein methods and systems for determining matrix or grain density of a subsurface formation are described. This includes measuring in-air mass of a fluid-saturated sample of the subsurface formation, wherein the in-air mass comprises mass of matrix or grains of the sample, mass of a fluid surrounding the sample, and mass of the fluid inside the sample. The volume of the fluid inside the sample, Vϕ, and volume of the fluid surrounding the sample, Vsur, are determined using nuclear magnetic resonance (NMR). The fluid-saturated sample can then be submerged in a predetermined volume of a weighing fluid and mass of the fluid-saturated sample without the surrounding fluid in the weighing fluid, mf is measured. Using the measured and determined values one can determine the volume of the sample without the surrounding fluid, Vc, the bulk density of the fluid-saturated sample without the surrounding fluid, ρb, the volume of the matrix, Vm, and the matrix or grain density of the subsurface formation, ρm.
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Citations
4 Claims
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1. A non-transitory computer-readable medium having computer executable instructions that trigger a computer to perform the operations of:
-
receiving in-air mass of a fluid-saturated sample of the subsurface formation, wherein the in-air mass comprises mass of matrix or grains of the sample, mass of a fluid surrounding the sample, and mass of the fluid inside the sample, the in-air mass of the fluid-saturated sample, ms, given by the formula;
ms=Vmρ
m+(Vϕ
+Vsur)ρ
lwhere ρ
m is a density of the matrix of the subsurface formation, ρ
l is a density of the fluid inside and surrounding the sample, Vm is a volume of the matrix, Vϕ
is a volume of the fluid inside the sample, and Vsur is a volume of the fluid surrounding the sample;determining volume of the fluid inside the sample, Vϕ
, and volume of the fluid surrounding the sample, Vsur, using nuclear magnetic resonance (NMR);receiving mass of the fluid-saturated sample in a weighing fluid; determining mass of the fluid-saturated sample without the surrounding fluid in the weighing fluid, mf, given by the formula;
mf=Vmρ
m+Vϕ
ρ
l−
Vcρ
fwhere ρ
f is the density of the weighing fluid; anddetermining a volume of the fluid-saturated sample without the surrounding fluid, Vc, using the formula;
Vc=(ms−
mf−
Vsurρ
l)/ρ
f. - View Dependent Claims (2, 3, 4)
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Specification