FIELD: mining industry.
SUBSTANCE: invention relates to the determination of the characteristics of formation fluids simultaneously located in the pore space of a rock sample. When implementing the method, several naturally saturated samples of rock belonging to the same formation are selected, so that there are 2 samples per one place of collection. Samples from the first group are crushed and pieces larger than 3 mm in size are selected. The volume of the solid phase Vsol.ph.1i is determined on each selected sample of crushed rock using a helium porosimeter. The apparent volume of pore fluids Vf.ap.1i is determined by nuclear magnetic resonance (hereinafter – NMR) at HI=1. The crushed sample is placed in prepared cups made of a filter paper. The cups with the sample are placed in Soxhlet apparatuses for cleaning samples by extraction in an alcohol-benzene mixture. After the extraction, the sample cups are dried, desalted in distilled water if necessary, and re-dried, at a temperature of 105ºC. The volume of the solid phase Vsol.ph.2i is determined using a helium porosimeter. The apparent volume of pore fluids Vf.ap.2i is determined by NMR at HI=1. The true volume of fluids that occupied the pore space is calculated, according to a given mathematical dependence. Then the apparent volume of fluids, which occupied the pore space, is calculated at HI=1 according to a given mathematical dependence. Next, the effective hydrogen index of the fluids located in the pores of naturally saturated samples is calculated. The samples are then placed under a layer of fluid in the form of kerosene or a model of formation water and kept under vacuum until the release of air bubbles stops, after which the samples are placed in a saturator, where they are kept for at least 2 hours with an excess pressure of 15 MPa. The apparent coefficient of total porosity Cp100app is determined by NMR at 100% filling of the pore space with fluids. The hydrogen index of the fluid HIfl.sat with which the samples were saturated with is determined. The effective hydrogen index of all fluids in the pore space is calculated for samples in a naturally saturated state with pre-saturation with fluid, followed by the calculation of the true coefficient of total porosity of samples pre-saturated with kerosene.
EFFECT: increased information content and reliability of the definition is achieved.
1 cl, 3 tbl
Title | Year | Author | Number |
---|---|---|---|
METHOD FOR DETERMINING THE TOTAL POROSITY OF NATURALLY SATURATED ROCK SAMPLES USING THE NMR METHOD | 2021 |
|
RU2780988C1 |
METHOD FOR DETERMINATION OF PETROLEUM-WATER SATURATION OF SPECIMEN ROCKS | 2000 |
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RU2574329C1 |
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RU2818048C1 |
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RU2662055C1 |
METHOD FOR DETERMINING A COEFFICIENT OF RESIDUAL WATER SATURATION OF ROCKS | 2017 |
|
RU2650706C1 |
METHOD FOR DETERMINING POROSITY OF ROCKS | 0 |
|
SU1728751A1 |
METHOD AND DEVICE FOR DETERMINATION OF CHARACTERISTICS OF FORMATION FLUID DURING NUCLEAR MAGNETIC LOGGING | 2006 |
|
RU2393509C2 |
METHOD OF DETERMINING EFFECTIVE POROSITY COEFFICIENT OF GAS-SATURATED FORMATIONS | 0 |
|
SU825879A1 |
Authors
Dates
2021-06-01—Published
2020-07-16—Filed