Method for determining gas saturation of tight reservoir

Abstract

The present invention a method for determining the gas saturation of a tight reservoir. The method comprises the steps of: determining the pore size distribution of the tight reservoir rock sample, and calculating the free water saturation; calculating the water-membrane water saturation; calculating the corner water saturation; calculating the gas saturation of the tight reservoir rock sample according to the following equation: Sg=100−Sw wherein Sw is the water saturation in %; Sw is the sum of the free water saturation, the water saturation and the corner water saturation; Sg is the gas saturation in %. The method for determining the gas saturation of a tight reservoir uses model calculations, which avoids errors in the determination results of the gas saturation caused by water volatilization, surface adsorption, and observation of water flow during experiments.

Description

CROSS-REFERENCE TO RELATED APPLICATIONS

This application claims priority to Chinese Patent Application No. 201910104816.1, filed on Feb. 1, 2019, which is hereby incorporated by reference in its entirety.

TECHNICAL FIELD

The present invention relates to a method for determining the gas saturation of a tight reservoir, which belongs to the technical field of oil and gas determination.

BACKGROUND

The natural gas content of underground rocks is usually calculated using a volume method, which requires four key parameters: gas saturation, porosity, rock density, and formation factor. Among them, the gas saturation varies widely. At present, the gas saturation of a tight reservoirs is measured by natural gas injection in a lab. Natural gas is injected into the rock with saturated water while maintaining a certain filling pressure. When it is observed that the water no longer flows out of the outlet, the rock core is taken out, followed by weighing the reduced mass of the rock core before and after the experiment to calculate the injected gas volume, and its ratio to the pore volume is the gas saturation. By changing different injection pressures, the gas saturation under different filling pressure conditions can be obtained.

Tight reservoirs have low porosity, are easily affected by experimental conditions, and have increased errors. Specifically, this method has the following disadvantages: 1. during the experiment, the liquid measurement is not accurate, the tight reservoir itself has low porosity, and the water content of the rock is small, which is easily affected; if the processes of sample loading, sampling and weighing take a long time, the water in the rock is volatile, resulting in a low water content; the adsorption of water on the surface of the rock tends to increase the water content; 2. the end condition of the experiment is to observe no more water flowing out of the outlet, the water existing in the pipeline cannot be observed, and the filled water cannot be seen in the pipeline, leading to the end of the experiment in advance, and a smaller gas saturation; 3. to determine the gas saturation at multiple pressure points, one need to take a sample to determine the gas saturation at each pressure point, then saturate water again and determine the saturation corresponding to the next pressure point; the sample is repeated for a long time and the process is tedious; 4. repetitive filling of rocks and saturating water can easily change the pore structure of rocks, such as resulting in micro-fractures; 5. repetitive filling of wet rocks and saturating water can easily change the wettability of rocks, for example, if becoming from hydrophilic to hydrophobic, it is easy to form dominant channels, resulting in incomplete gas filling; 6. it is difficult to fully achieve the temperature and pressure conditions in the experiment, the fluid pressure is less than 70 MPa and the temperature is less than 200° C.; 7. only a single value for total gas saturation can be determined.

SUMMARY

In order to solve the above technical problems, an object of the present invention is to provide a method for determining the gas saturation of a tight reservoir, which can overcome the disadvantages of the methods in the prior art, such as complexity, inaccurate results, difficulty in meeting underground high temperature and high-pressure geological conditions, etc.

In order to achieve the above object, the present invention provides a method for determining the gas saturation of a tight reservoir, comprising:

a free water saturation calculation step: determining the pore size distribution of the tight reservoir rock sample, and calculating the free water saturation of the tight reservoir rock sample from the pore size distribution;

a water-membrane water saturation calculation step: calculating the water-membrane water saturation of the tight reservoir rock sample;

a corner water saturation calculation step: calculating the corner water saturation of the tight reservoir rock sample;

a gas saturation calculation step: calculating the gas saturation of the tight reservoir rock sample according to the following equation:S_g=100−S_w

wherein S_w is the water saturation in %; the water saturation is the sum of the free water saturation, the water-membrane water saturation and the corner water saturation;

S_g is the gas saturation in %.

The determination method provided in the present invention is based on assuming that the reservoir rock contains only two fluids, formation water and natural gas, and the gas saturation is directly affected by the rock water saturation; if the reservoir water saturation is obtained, the gas saturation can be obtained; the size and stacking relationship of the rock-forming mineral particles determine the geometry and spatial distribution of the fluid storage space; the formation water exists in rocks in three main forms: (1) free water: pore water that cannot be expelled by natural gas, occupying small pore throats that cannot be filled, and its saturation is affected by natural gas filling pressure and pore throat capillary force; (2) water-membrane water: adsorbed on the pore wall in the form of a thin membrane, its saturation is related to the surface area of the pore wall and the thickness of the water-membrane; (3) corner water: existing in the corners that are difficult to displace among the particles, and its saturation is affected by the size and the contact relationship of the rock particles.

In the above method, the pore size distribution of the tight reservoir rock sample can be determined by mercury porosimetry, nuclear magnetic resonance method, etc., but it is not limited to the above two methods. The basic principle of rock pore diameter measurement using the mercury porosimetry is that mercury does not wet the rock surface and is a non-wetting phase, and the air in the rock pores is a wetting phase. The process of mercury injection into rock pores is to displace the wetting phase with a non-wetting phase. Due to the effect of the capillary pressure at the pore throat, mercury cannot enter the pores when the pressure is low. Only when the injection pressure exceeds the capillary pressure, mercury can enter the pore throat of the rock sample. The injection pressure at this time is the capillary pressure. The capillary radius corresponding to the capillary pressure is equivalent to the pore throat radius, and the volume of mercury entering the pores is the pore volume. The injection pressure is increased such that mercury enters the pores controlled by a smaller throat. In this manner, by continuously increasing the injection pressure, the relationship between the injection pressure, that is, the capillary pressure, and the pore volume can be obtained. The gas saturation of the wetting phase can be calculated from the volume of mercury injected and the pore volume of the tight reservoir rock sample, and then the curve of the pore size distribution of different pore throat radius ranges and the capillary pressure can be obtained. In the free water saturation calculation step, the data of the pore size distribution includes data of pore spaces corresponding to different pore throat radii.

In the above method, preferably, in the free water saturation calculation step, the data of pore spaces corresponding to different pore throat radii includes the pore throat radii corresponding to the pore spaces with different radii and the percentages of pore volumes occupied by the pore spaces with different radii.

In the above method, preferably, in the free water saturation calculation step, the pore size distribution of the tight reservoir rock sample is determined by the mercury porosimetry as follows:

injecting mercury into rock pores to displace air in rock pores;

when the injection pressure exceeds the capillary pressure, mercury entering the pore throat of the rock sample, and at this time, the injection pressure being the capillary pressure, the capillary radius corresponding to the pressure is equivalent to the pore throat radius, and the volume of mercury entering the pores being the pore volume;

increasing the injection pressure such that mercury enters the pores controlled by a smaller throat, to obtain the pore throat radius and the pore volume corresponding to the smaller throat; and repeatedly increasing the injection pressure to obtain the pore throat radii and the pore volumes corresponding to different throats.

In the above method, since the surface tension of the fluid system in the laboratory is different from that of the oil reservoir system, it is necessary to convert the laboratory's capillary pressure data into the oil reservoir capillary pressure. Assuming that the “J” function is a parameter of rock characteristics and does not change from the laboratory to the gas reservoir, the mercury porosimetry curve can be converted into the relationship between the water saturation and the filling pressure (e.g., FIG. 3), according to the actual gas reservoir conditions. In the free water saturation calculation step, the free water saturation of the tight reservoir rock sample is calculated from the pore size distribution as follows:

(1) obtaining the relationship between the injection pressure and the pore volume from the pore throat radii and the pore volumes corresponding to different throats in the tight reservoir rock sample;

$P_{\mathrm{mercury}-\mathrm{air}}=\frac{2{\sigma }_{\mathrm{mercury}-\mathrm{air}}\cos {\theta }_{\mathrm{mercury}-\mathrm{air}}}{r}$

wherein P_mercury-air is the capillary pressure in 10⁶ Pa; σ_mercury-air is the fluid interfacial tension between mercury and air in mN/m; θ_mercury-air is the wet contact angle between mercury and air in °; r is the capillary radius in 10⁻⁹ m; in the mercury porosimetry, σ_mercury-air=480 mN/M, θ_mercury-air=140°;

(2) calculating the gas saturation from the volume of mercury injected and the pore volume of the tight reservoir rock sample, and then obtaining the curve of the pore size distribution of different pore throat radius ranges and the capillary pressure:

$P_{\mathrm{filling}}=\frac{2{\sigma }_{\mathrm{gas}-\mathrm{water}}\cos {\theta }_{\mathrm{gas}-\mathrm{water}}}{r}$

σ_gas-water is the interfacial tension in mN/m; preferably, the gas-water interfacial tension G_gas-water=20 mN/m;

θ_gas-water is the gas-water contact angle; preferably, θ is 0, and cos θ=1;

P_filling is the gas-water filling pressure in MPa;

r is the capillary radius in 10⁻⁹ m;

(3) converting the curve of the pore size distribution of different pore throat radius ranges and the capillary pressure into the relationship curve of free water saturation and capillary pressure; obtaining the free water saturation from the filling pressure, that is, calculating the corresponding pore throat radius from the filling pressure, and summing the pore volumes larger than this radius, the percentage of this sum to the total pore volumes being the free water saturation.

In the above method, preferably, the water-membrane water saturation calculation step is performed as follows:

(1) it is inappropriate for the irreducible water saturation method to regard the thickness of the water-membrane in the reservoir as a constant value, and the thickness of the water-membrane in the reservoir cannot be the lower limit of the available pore throat radius in the reservoir (see FIG. 1). Using Dlvo theory, the calculation equation of the water-membrane thickness is given, that is, calculating the water-membrane thicknesses in the pore spaces corresponding to different pore throat radii according to the following equation:

$h={\left(\frac{a·r}{\sigma }\right)}^{1/3}$

wherein, a is a constant; the more hydrophilic the reservoir is, the greater is its value, which is preferably 1.18×10⁻⁷; h is the water-membrane thickness in μm; σ is the fluid interfacial tension in mN/m; r is the pore throat radius in 10⁻⁹ m;

(2) as seen from the above, a layer of water-membrane will leave after uniform oil and water displacement in a single pipe; the water-membrane is an integral part of the irreducible water; the thickness of the water-membrane will become thinner as the surface tension increases, and will gradually increase as the pore size becomes larger; the volume occupied by the water-membrane is compared with the capillary volume to calculate the irreducible water saturation of the water-membrane, that is, calculating the water-membrane saturation according to the following equation:

$S_{wmi}=\frac{V_{\mathrm{water}-\mathrm{membrane}}}{V_{sum}}=\frac{r^2-{\left(r-h\right)}^2}{r^2}$

wherein S_wmi is water-membrane water saturation of the pore space corresponding to the i-th pore throat radius;

r is the pore throat radius which corresponds to the pore space corresponding to the i-th pore throat radius;

h is the water-membrane thickness which corresponds to the pore space corresponding to the i-th pore throat radius.

In the above method, the corner water saturation of the reservoir is affected by the shape of the pores. In ideal cases, such as regular arrangement of spherical particles, triangular arrangement of spherical particles, regular triangle pores, square pores, regular hexagonal pores, the water saturation values can be calculated. For specific reservoirs, a simpler method can be used for the calculation of corner water saturation by observing the pore structure of the reservoir and directly determining the corner water saturation, or by counting the proportions of different types of pore structure, and determining the corner water saturation by weighted average. Preferably, the corner water saturation calculation step is performed by one of:

(1) observing the pore structure of the reservoir and directly determining the corner water saturation;

(2) counting the proportions of corner water corresponding to different types of pore structure, and determining the corner water saturation by weighted average;

(3) the pressure of the water-membrane on the surface of the particles is unstable, and it will gather towards the corner. In the particle model, most of the irreducible water is distributed in the corners between the particles (see FIG. 2), forming corner water. The water saturation equation of the particle model is as follows, and the corner water saturation can be calculated according to the following equation:

$S_{\mathrm{wyi}}=\frac{A_3}{A_2+A_3}=\frac{4}{4-\pi }\left[\sqrt{{\left(\frac{r}{R}\right)}^2+2\frac{r}{R}}-\arccos \left(\frac{R}{R+r}\right)-{\left(\frac{r}{R}\right)}^2\mathrm{arc}\sin \left(\frac{R}{R+r}\right)\right]$

wherein, A2 is the circular cross-sectional area of the air-water interface;

A3 is the cross-sectional area of the corner water;

r is the arc radius of air-water interface, that is, the pore throat radius,

$r=\frac{2\sigma }{p_{\mathrm{filling}}}$ in 10⁻⁹ m;

R is the particle radius of the tight reservoir rock sample in 10⁻⁹ m;

S_wyi is water saturation of the pore space corresponding to the i-th pore throat radius;

P_filling is the filling pressure in MPa;

σ is the fluid interfacial tension in mN/m.

In the above method, preferably, the gas saturation calculation step is performed as follows:

(1) calculating the water saturation according to the following equation:

$S_w=\sum _{i=1}^n{\lambda }_i\left(S_{wyi}+S_{wmi}\right)+S_{wz}$

wherein S_w is the water saturation;

λ_i is the percentage of pore volume occupied by the pore space corresponding to the i-th pore throat radius;

S_wyi is the corner water saturation in the pore space corresponding to the i-th pore throat radius;

S_wmi is the water-membrane water saturation in the pore space corresponding to the i-th pore throat radius;

S_wz is the free water saturation, that is, the proportion of pore volume occupied by free water pore space;

(2) calculating the gas saturation of the tight reservoir rock sample according to the following equation:S_g=100−S_w

wherein S_w is water saturation in %; the water saturation is the sum of the free water saturation, the water-membrane water saturation and the corner water saturation;

S_g is the gas saturation in %.

According to a specific embodiment of the present invention, preferably, the method provided in the present invention comprises the following steps:

a free water saturation calculation step:

determining the pore size distribution of the tight reservoir rock sample by mercury porosimetry; when the injection pressure exceeds the capillary pressure, mercury entering the pore throat of the rock sample, and at this time, the injection pressure being the capillary pressure, the capillary radius corresponding to the capillary pressure being equivalent to the pore throat radius, and the volume of mercury entering the pores being the pore volume;

increasing the injection pressure such that mercury enters the pores controlled by a smaller throat, to obtain the corresponding pore throat radius and pore volume;

continuously increasing the injection pressure to obtain the relationship between the injection pressure, that is, the capillary pressure, and the pore volume;

calculating the gas saturation from the volume of mercury injected and the pore volume of the tight reservoir rock sample, and then obtaining the curve of the pore size distribution of different pore throat radius ranges and the capillary pressure;

converting the pore size distribution data of the tight reservoir rock sample into the capillary pressure of oil reservoir; and converting the mercury porosimetry curve into the relationship of water saturation according to the displacement pressure difference, in consideration of the interfacial tension and the contact angle under the conditions of actual gas reservoir temperature and pressure:

$P_{\mathrm{filling}}=\frac{2{\sigma }_{\mathrm{gas}-\mathrm{water}}\cos {\theta }_{\mathrm{gas}-\mathrm{water}}}{r}$

converting the curve of pore size distribution data and capillary pressure of the tight reservoir rock sample into the curve of free water saturation and capillary pressure, to obtain the filling pressure, so as to obtain the free water saturation; that is, calculating the corresponding pore throat radius from the filling pressure, and summing the pore volumes larger than this radius, the percentage of this sum to the total pore volumes being the free water saturation.

σ_gas-water is the interfacial tension in mN/m; preferably, the gas-water interfacial tension σ_gas-water=20 mN/m;

θ_gas-water is the gas-water contact angle; preferably, θ is 0, and cos θ=1;

P_filling is the filling pressure in MPa;

r is the capillary radius in 10⁻⁹ m;

a water-membrane water saturation calculation step:

calculating the water-membrane thicknesses in the pore spaces corresponding to different pore throat radii according to the following equation:

$h={\left(\frac{a·r}{\sigma }\right)}^{1/3}$

wherein a is a constant; the more hydrophilic the reservoir is, the greater is its value, which is preferably 1.18×10⁻⁷; h is the water-membrane thickness in μm; σ is the fluid interfacial tension in mN/m; r is the pore throat radius in 10⁻⁹ m;

calculating the water-membrane saturation according to the following equation:

$S_{wmi}=\frac{V_{\mathrm{water}-\mathrm{membrane}}}{V_{sum}}=\frac{r^2-{\left(r-h\right)}^2}{r^2}$

wherein S_wmi is the water-membrane water saturation of the pore space corresponding to the i-th pore throat radius;

r is the pore throat radius which corresponds to the pore space corresponding to the i-th pore throat radius;

h is the water-membrane thickness which corresponds to the pore space corresponding to the i-th pore throat radius;

a corner water saturation calculation step:

calculating the corner water saturation according to the following equation:

$S_{\mathrm{wyi}}=\frac{A_3}{A_2+A_3}=\frac{4}{4-\pi }\left[\sqrt{{\left(\frac{r}{R}\right)}^2+2\frac{r}{R}}-\arccos \left(\frac{R}{R+r}\right)-{\left(\frac{r}{R}\right)}^2\mathrm{arc}\sin \left(\frac{R}{R+r}\right)\right]$

wherein r is the arc radius of air-water interface, that is, the pore throat radius,

$r=\frac{2\sigma }{p_{\mathrm{filling}}}$ in 10⁻⁹ m;

R is the particle radius of the tight reservoir rock sample in 10⁻⁹ m;

S_wyi is the water saturation of the pore space corresponding to the i-th pore throat radius;

P_filling is the filling pressure in MPa;

σ is the fluid interfacial tension in mN/m;

a gas saturation calculation step:

calculating the water saturation according to the following equation:

$S_w=\sum _{i=1}^n{\lambda }_i\left(S_{\mathrm{wyi}}+S_{\mathrm{wmi}}\right)+S_{wz}$

wherein S_w is the water saturation;

λ_i is the percentage of pore volume occupied by the pore space corresponding to the i-th pore throat radius;

S_wyi is the corner water saturation in the pore space corresponding to the i-th pore throat radius;

S_wmi is the water-membrane water saturation in the pore space corresponding to the i-th pore throat radius;

S_wz is the free water saturation, that is, the proportion of pore volume occupied by the free water pore space;

then calculating the gas saturation of the tight reservoir rock sample according to the following equation:S_g=100−S_w

wherein S_w is the water saturation in %; the water saturation is the sum of the free water saturation, the water-membrane water saturation and the corner water saturation; S_g is the gas saturation in %.

The method for determining gas saturation of a tight reservoir provided in the present invention has the following beneficial effects:

1. using model calculations to avoid errors in the determination results of the gas saturation caused by water volatilization, surface adsorption, and observation of water flow during experiments;

2. avoiding the effect of repeated rock filling on the pore structure and wettability;

3. directly obtaining the gas saturation at multiple pressure points, which is simple and fast;

4. meeting the conditions of underground temperature and pressure, where the fluid pressure can be greater than 70 MPa, and the temperature can be greater than 200° C.;

5. separately obtaining the saturation and proportion of three kinds of water: free water, water-membrane and corner water;

6. not only determining the single value of total gas saturation, but also giving the gas saturation distribution at different pore sizes.

As compared with the existing method, the determination method of the present invention has shorter test time, requires less sample, has no requirements on the shape of the sample (either core plunger or rock cuttings), is safe and environmentally friendly, can use no mercury (e.g., Examples 2 and 3), and saves test gas. By subdividing the irreducible water saturation of the prior art into water-membrane water saturation and corner water saturation, the method of the present invention can overcome the disadvantages of the methods in prior art, such as complexity, inaccurate results caused by insufficient filling time, difficulty in meeting underground high temperature and high pressure geological conditions, etc, while it avoids errors in determination results of the gas saturation caused by water volatilization, surface adsorption, and observation of water flow during experiments.

BRIEF DESCRIPTION OF THE DRAWINGS

FIG. 1 is a schematic diagram of water-membrane water saturation calculation.

FIG. 2 is a schematic diagram of corner water calculation in a particle model.

FIG. 3 is a relationship diagram between the filling pressure and the gas saturation in Example 1.

FIG. 4 is a relationship diagram between the filled pore throat radius and the gas saturation in Example 1.

FIG. 5 is a relationship diagram between the filling pressure and the gas saturation in Example 2.

FIG. 6 is a relationship diagram between the filled pore throat radius and the gas saturation in Example 2.

FIG. 7 is a relationship diagram between the filling pressure and the gas saturation in Example 3.

FIG. 8 is a relationship diagram between the filled pore throat radius and the gas saturation in Example 3.

DETAILED DESCRIPTION

In order to have a clearer understanding of the technical features, objectives, and beneficial effects of the present invention, the technical solutions of the present invention will now be described below in detail, but cannot be understood as limiting the implementable scope of the present invention.

Example 1

This example provides a method for determining the gas saturation of a tight reservoir, which can theoretically be used for different types of rock samples. In this example, a Sandstone 1 sample is used for illustration. For different samples, input parameters are different, and the corresponding results will be different. The method includes the following steps.

The pore size distribution of the sample is measured using high-pressure mercury porosimetry, and the results are shown in Table 1.

TABLE 1
The pore size distribution of the Sandstone 1 sample
No., i	Pore throat radius ri, μm	λi, %
1	2.931	0.00
2	1.909	5.22
3	1.228	12.77
4	0.952	6.83
5	0.621	8.90
6	0.399	7.30
7	0.256	7.35
8	0.206	3.37
9	0.134	6.73
10	0.089	6.32
11	0.056	6.71
12	0.037	5.12
13	0.024	5.41
14	0.015	4.96
15	0.012	2.40
16	0.010	2.17
17	0.008	2.15
18	0.007	2.24
19	0.005	1.69
20	0.004	1.50
21	0.004	0.84

(1) Free Water Saturation:

the pore size distribution data are converted to the capillary pressure of oil reservoir. The mercury porosimetry curve is converted into the relationship between water saturation and displacement pressure difference, in consideration of the interfacial tension, contact angle, and the like, under the conditions of actual gas reservoir temperature and pressure:

$P_{\mathrm{filling}}=\frac{2{\sigma }_{\mathrm{gas}-\mathrm{water}}\cos {\theta }_{\mathrm{gas}-\mathrm{water}}}{r}$

The curve of pore size distribution data and capillary pressure measured in the laboratory is converted into the curve of free water saturation and capillary pressure, to obtain the filling pressure, and thus the free water saturation.

σ_gas-water is the interfacial tension in mN/m; in this example, the gas-water interfacial tension σ_gas-water=20 mN/m;

θ_gas-water is the gas-water contact angle, θ is 0, and thus cos θ=1;

P_filling is the gas-water filling pressure in MPa;

r is the capillary radius in 10⁻⁹ m;

(2) Water-Membrane Water Saturation:

The water-membrane thicknesses in the pore spaces corresponding to different pore throat radii is calculated according to the following equation:

$h_i={\left(\frac{1.18\times 10^{-4}{r}_i}{\sigma }\right)}^{1/3}$

wherein h_i is the water-membrane thickness which corresponds to the pore space corresponding to the i-th pore throat radius in μm; σ is the fluid interfacial tension in mN/m; r_i is the pore throat radius which corresponds to the pore space corresponding to the i-th pore throat radius; in this example, i is 1-20, and specific data are shown in Table 1;

the water-membrane saturation is calculated according to the following equation:

$S_{\mathrm{wmi}}=\frac{V_{\mathrm{water}\mathrm{film}}}{V_{\mathrm{sum}}}=\frac{r_i^2-{\left(r_i-h_i\right)}^2}{r_i^2}$

wherein S_wmi is the water-membrane water saturation of the pore space corresponding to the i-th pore throat radius;

r_i is the pore throat radius which corresponds to the pore space corresponding to the i-th pore throat radius; in this example, i is 1-20, and specific data are shown in Table 1;

h_i is the water-membrane thickness which corresponds to the pore space corresponding to the i-th pore throat radius;

(3) Corner Water Saturation:

The corner water saturation is calculated according to the following equation (see FIG. 2):

$S_{\mathrm{wyi}}=\frac{A_3}{A_2+A_3}=\frac{4}{4-\pi }\left[\sqrt{{\left(\frac{r_i}{R_i}\right)}^2+2\frac{r_i}{R_i}}-\arccos \left(\frac{R_i}{R_i+r_i}\right)-{\left(\frac{r_i}{R_i}\right)}^2\mathrm{arc}\sin \left(\frac{R_i}{R_i+r_i}\right)\right]$

wherein r_i is the arc radius of air-water interface, that is, the pore throat radius,

$r_i=\frac{2\sigma }{P_{\mathrm{filling}i}}$ in 10⁻⁹ m;

R_i is the particle radius of the tight reservoir rock sample in 10⁻⁹ m;

S_wyi is the water saturation of the pore space corresponding to the i-th pore throat radius;

P_{filling i} is the filling pressure of the pore space corresponding to the i-th pore throat radius in MPa;

σ is the fluid interfacial tension in mN/m;

(4) Gas Saturation:

The water saturation is calculated according to the following equation:

$S_w=\sum _{i=1}^n{\lambda }_i\left(S_{\mathrm{wyi}}+S_{\mathrm{wmi}}\right)+{\lambda }_z{S}_{\mathrm{wz}}$

wherein S_w is the water saturation;

λ_i is the percentage of pore volume occupied by the pore space corresponding to the i-th pore throat radius;

λ_z is the proportion of pore volume occupied by free water pore space;

S_wyi is the corner water saturation in the pore space corresponding to the i-th pore throat radius;

S_wmi is the water-membrane water saturation in the pore space corresponding to the i-th pore throat radius;

S_wz is the free water saturation, which has not been filled and is 100%.

The relationship between the filling pressure and the gas saturation is shown in FIG. 3, and the relationship between the filled pore throat radius and the gas saturation is shown in FIG. 4.

The gas saturation of the tight reservoir rock sample is then calculated according to the following equation:S_g=100−S_w

wherein S_w is the water saturation in %; the water saturation is the sum of the free water saturation, the water-membrane water saturation and the corner water saturation;

S_g is the gas saturation in %.

The parameters of this example are shown in Table 2.

TABLE 2
Parameters of this example
					Water				Water	Gas
	Pore throat				membrane		Particle		saturation	saturation
	radius r,	λi	Pfilling	Swmi	thickness h,	Swyi	radius R	Swz	Sw	Sg
No., i	μm	%	MPa	%	μm	%	μm	%	%	%
1	2.931	0.00	0.14	0.00	0.026	0.00	7.08	100	100	0
2	1.909	5.22	0.21	0.12	0.022	0.94	4.61	95	95	5
3	1.228	12.77	0.33	0.40	0.019	2.29	2.97	82	83	17
4	0.952	6.83	0.42	0.25	0.018	1.23	2.30	75	76	24
5	0.621	8.90	0.64	0.44	0.015	1.60	1.50	66	68	32
6	0.399	7.30	1.00	0.48	0.013	1.31	0.96	59	61	39
7	0.256	7.35	1.56	0.64	0.011	1.32	0.62	52	55	45
8	0.206	3.37	1.94	0.34	0.011	0.61	0.50	48	52	48
9	0.134	6.73	2.99	0.90	0.009	1.21	0.32	42	46	54
10	0.089	6.32	4.49	1.09	0.008	1.13	0.22	35	41	59
11	0.056	6.71	7.12	1.55	0.007	1.20	0.14	28	36	64
12	0.037	5.12	10.87	1.54	0.006	0.92	0.09	23	32	68
13	0.024	5.41	16.83	2.11	0.005	0.97	0.06	18	29	71
14	0.015	4.96	25.83	2.46	0.005	0.89	0.04	13	26	74
15	0.012	2.40	32.21	1.34	0.004	0.43	0.03	11	25	75
16	0.010	2.17	39.70	1.36	0.004	0.39	0.02	8	25	75
17	0.008	2.15	49.45	1.50	0.004	0.39	0.02	6	24	76
18	0.007	2.24	61.45	1.72	0.003	0.40	0.02	4	23	77
19	0.005	1.69	74.94	1.35	0.003	0.30	0.01	2	23	77
20	0.004	1.50	93.78	1.20	0.003	0.27	0.01	1	23	77
21	0.004	0.84	112.55	0.67	0.003	0.15	0.01	0	23	77

As can be seen from the above, in the method for determining gas saturation of a tight reservoir provided in Example 1, model calculations are used to avoid errors in the determination results of the gas saturation caused by water volatilization, surface adsorption, and observation of water flow during experiments, and also to avoid the effect of repeated rock filling on the pore structure and wettability. This method directly measures at 21 pressure points and directly obtains the gas saturation at multiple pressure points, which is simple and fast. This method can not only determine the single value of total gas saturation, but also give the gas saturation distribution at different pore sizes.

Example 2

In this example, the pore size distribution of a Sandstone 2 sample is determined by NMR, wherein the T2_i relaxation time and the ratio λi are obtained by T2 NMR spectrum measurement, and the pore throat radius is calculated by the formula r_i=3·ρ·T2_i, where ρ is the rock surface relaxation rate in μm/ms. The results are shown in Table 3.

TABLE 3
The pore size distribution of the Sandstone 2 sample
		T2i relaxation		Pore throat
	No., i	time (ms)	λi, %	radius ri, μm
	1	24.03	0.00	3.605
	2	18.02	0.10	2.704
	3	14.42	0.14	2.163
	4	13.11	0.10	1.966
	5	12.02	0.10	1.802
	6	11.09	0.07	1.664
	7	9.61	0.21	1.442
	8	8.01	0.14	1.202
	9	7.21	0.14	1.082
	10	6.01	0.31	0.901
	11	5.55	0.28	0.832
	12	5.15	0.31	0.773
	13	4.81	0.28	0.721
	14	3.60	0.76	0.541
	15	2.88	1.39	0.433
	16	2.40	1.53	0.361
	17	2.06	3.05	0.309
	18	1.80	5.90	0.270
	19	1.60	5.69	0.240
	20	1.44	6.91	0.216
	21	1.31	8.40	0.197
	22	1.20	7.70	0.180
	23	1.03	11.97	0.155
	24	0.90	8.75	0.135
	25	0.80	1.87	0.120
	26	0.72	1.53	0.108
	27	0.60	2.46	0.090
	28	0.55	0.73	0.083
	29	0.51	0.97	0.077
	30	0.48	0.69	0.072
	31	0.45	0.83	0.068
	32	0.42	1.01	0.064
	33	0.40	0.80	0.060
	34	0.38	0.49	0.057
	35	0.36	0.52	0.054
	36	0.29	3.05	0.043
	37	0.24	2.53	0.036
	38	0.21	2.05	0.031
	39	0.18	1.77	0.027
	40	0.16	1.91	0.024
	41	0.14	1.01	0.022
	42	0.13	1.15	0.020
	43	0.12	1.21	0.018
	44	0.10	1.60	0.015
	45	0.09	1.15	0.014
	46	0.08	1.49	0.012
	47	0.07	0.76	0.011
	48	0.07	0.80	0.010
	49	0.06	0.56	0.009
	50	0.06	0.59	0.008
	51	0.05	0.42	0.008
	52	0.05	0.59	0.007
	53	0.05	0.28	0.007
	54	0.04	0.28	0.006
	55	0.04	0.21	0.006
	56	0.04	0.24	0.006
	57	0.04	0.21	0.005

(1) Free Water Saturation:

The pore size distribution data are converted to the capillary pressure of oil reservoir. The mercury porosimetry curve is converted into the relationship between water saturation and displacement pressure difference, in consideration of the interfacial tension, contact angle, and the like, under the conditions of actual gas reservoir temperature and pressure:

$P_{\mathrm{filling}}=\frac{2{\sigma }_{\mathrm{gas}-\mathrm{water}}\cos {\theta }_{\mathrm{gas}-\mathrm{water}}}{r}$

The curve of pore size distribution data and capillary pressure measured in the laboratory is converted into the curve of free water saturation and capillary pressure, to obtain the filling pressure, and thus the free water saturation.

σ_gas-water is the interfacial tension in mN/m; in this example, the gas-water interfacial tension σ_gas-water=50 mN/m;

θ_gas-water is the gas-water contact angle, θ is 0, and thus cos θ=1;

P_filling is the gas-water filling pressure in MPa;

r is the capillary radius in 10⁻⁹ m;

(2) Water-Membrane Water Saturation:

The water-membrane thicknesses in the pore spaces corresponding to different pore throat radii is calculated according to the following equation:

$h_i={\left(\frac{1.18\times 10^{-4}{r}_i}{\sigma }\right)}^{1/3}$

wherein h_i is the water-membrane thickness which corresponds to the pore space corresponding to the i-th pore throat radius in μm; σ is the fluid interfacial tension in mN/m; r_i is the pore throat radius which corresponds to the pore space corresponding to the i-th pore throat radius; in this example, i is 1-57, and specific data are shown in Table 1;

the water-membrane saturation is calculated according to the following equation:

$S_{\mathrm{wmi}}=\frac{V_{\mathrm{water}\mathrm{film}}}{V_{\mathrm{sum}}}=\frac{r_i^2-{\left(r_i-h_i\right)}^2}{r_i^2}$

wherein S_wmi is the water-membrane water saturation of the pore space corresponding to the i-th pore throat radius;

r_i is the pore throat radius which corresponds to the pore space corresponding to the i-th pore throat radius; in this example, i is 1-57, and specific data are shown in Table 1;

h_i is the water-membrane thickness which corresponds to the pore space corresponding to the i-th pore throat radius;

(3) Corner Water Saturation:

The corner water saturation is calculated according to the following equation:

(1) observing the pore structure of the reservoir and directly determining the corner water saturation; this method is suitable for reservoir samples capable of image observation;

(2) according to Table 4, counting the proportions of corner water corresponding to different types of pore structure, and determining the corner water saturation as 28.45 by weighted average;S_wyi=31.2×75%+39.57×5%+21.5×10%+9.35×10%=28.45%

TABLE 4
Corner water statistics of the Sandstone 2 sample
	Regular	Triangular			Regular
	arrangement	arrangement	Regular		hexag-
Pore	of spherical	of spherical	triangle	Square	onal
structure	particles	particles	pores	pores	pores
corner water	31.2	53.34	39.57	21.5	9.35
saturation (%)
proportion (%)	75	0	5	10	10

(4) Gas Saturation:

The water saturation is calculated according to the following equation:

$S_w=\sum _{i=1}^n{\lambda }_i\left(S_{\mathrm{wyi}}+S_{\mathrm{wmi}}\right)+{\lambda }_z{S}_{\mathrm{wz}}$

wherein S_w is the water saturation;

λ_i is the percentage of pore volume occupied by the pore space corresponding to the i-th pore throat radius;

λ_z is the proportion of pore volume occupied by free water pore space; S_wyi is the corner water saturation in the pore space corresponding to the i-th pore throat radius;

S_wmi is the water-membrane water saturation in the pore space corresponding to the i-th pore throat radius;

S_wz is the free water saturation, which has not been filled and is 100%.

The relationship between the filling pressure and the gas saturation is shown in FIG. 5, and the relationship between the filled pore throat radius and the gas saturation is shown in FIG. 6.

The gas saturation of the tight reservoir rock sample is then calculated according to the following equation:S_g=100−S_w

wherein S_w is the water saturation in %; the water saturation is the sum of the free water saturation, the water-membrane water saturation and the corner water saturation;

S_g is the gas saturation in %.

The parameters of this example are shown in Table 5, and the physical simulation results corresponding to this example are shown in Table 6.

TABLE 5
Parameters of this example
			Water-membrane		Particle		Gas saturation
	Pfilling	Swmi	thickness h,	Swyi	radius R	Swz	Sw
No. i	MPa	%	μm	%	μm	%	%
1	0.03	0.00	0.020	0.00	8.71	100	0
2	0.04	0.00	0.019	0.03	6.53	100	0
3	0.05	0.00	0.017	0.04	5.22	100	0
4	0.05	0.00	0.017	0.03	4.75	100	0
5	0.06	0.00	0.016	0.03	4.35	100	0
6	0.06	0.00	0.016	0.02	4.02	99	0
7	0.07	0.00	0.015	0.06	3.48	99	1
8	0.08	0.00	0.014	0.04	2.90	99	1
9	0.09	0.00	0.014	0.04	2.61	99	1
10	0.11	0.01	0.013	0.09	2.18	99	1
11	0.12	0.01	0.013	0.08	2.01	98	1
12	0.13	0.01	0.012	0.09	1.87	98	1
13	0.14	0.01	0.012	0.08	1.74	98	2
14	0.18	0.03	0.011	0.21	1.31	97	2
15	0.23	0.06	0.010	0.39	1.04	96	3
16	0.28	0.08	0.009	0.43	0.87	94	4
17	0.32	0.18	0.009	0.86	0.75	91	6
18	0.37	0.37	0.009	1.65	0.65	85	10
19	0.42	0.39	0.008	1.59	0.58	79	14
20	0.46	0.50	0.008	1.93	0.52	73	18
21	0.51	0.65	0.008	2.35	0.47	64	23
22	0.55	0.63	0.008	2.16	0.44	56	28
23	0.65	1.08	0.007	3.35	0.37	45	36
24	0.74	0.86	0.007	2.45	0.33	36	41
25	0.83	0.20	0.007	0.52	0.29	34	43
26	0.93	0.17	0.006	0.43	0.26	32	43
27	1.11	0.32	0.006	0.69	0.22	30	45
28	1.20	0.10	0.006	0.20	0.20	29	45
29	1.30	0.14	0.006	0.27	0.19	28	46
30	1.39	0.10	0.006	0.19	0.17	27	46
31	1.48	0.13	0.005	0.23	0.16	27	47
32	1.57	0.16	0.005	0.28	0.15	26	47
33	1.66	0.13	0.005	0.22	0.15	25	48
34	1.76	0.08	0.005	0.14	0.14	24	48
35	1.85	0.09	0.005	0.15	0.13	24	48
36	2.31	0.62	0.005	0.86	0.10	21	50
37	2.78	0.58	0.004	0.71	0.09	18	51
38	3.24	0.52	0.004	0.57	0.07	16	52
39	3.70	0.48	0.004	0.50	0.07	14	53
40	4.17	0.56	0.004	0.53	0.06	13	54
41	4.63	0.32	0.004	0.28	0.05	12	54
42	5.08	0.38	0.004	0.32	0.05	10	55
43	5.56	0.43	0.003	0.34	0.04	9	55
44	6.49	0.61	0.003	0.45	0.04	8	56
45	7.41	0.47	0.003	0.32	0.03	6	56
46	8.33	0.66	0.003	0.42	0.03	5	56
47	9.26	0.36	0.003	0.21	0.03	4	56
48	10.20	0.40	0.003	0.22	0.02	3	57
49	11.11	0.29	0.003	0.16	0.02	3	57
50	12.05	0.32	0.003	0.17	0.02	2	57
51	12.99	0.24	0.003	0.12	0.02	2	57
52	13.89	0.35	0.003	0.17	0.02	1	57
53	14.71	0.17	0.003	0.08	0.02	1	57
54	15.63	0.17	0.002	0.08	0.02	1	57
55	16.67	0.13	0.002	0.06	0.01	0	57
56	17.54	0.16	0.002	0.07	0.01	0	57
57	18.52	0.14	0.002	0.06	0.01	0	57

TABLE 6
Physical simulation results corresponding to this example
Pfilling MPa Gas saturation Sw %
0            0
0.4          28
0.45         31
0.57         33
0.73         35
0.83         36
1.06         38
1.46         41
1.95         43
2.46         50
2.97         53

As can be seen from the above, model calculations are used in the method for determining the gas saturation of a tight reservoir provided in Example 2. As compared with Example 1, the pore throat radius distribution of the sandstone sample was measured by NMR experiments, and the proportion of corner water is obtained by observing the pore type and weighted calculation. In order to verify the validity of the method, it is compared with actual physical simulation experiments. The filling results are consistent with the results calculated by this method, and the physical simulation experimental data is relatively low, because that the experimental time is limited and the actual underground gas reservoir charging time cannot be reached. Therefore, the incomplete charging results in low results. However, because the physical simulation experiment can only reach a lower filling pressure, it can only be verified in the lower filling pressure range, but the above content is sufficient to prove the technical effect of the technical solution of the present invention.

Example 3

The sample in this example is a Sandstone 3 sample having large pores, and the pore size distribution of the Sandstone 3 sample is determined by NMR, wherein the T2_i relaxation time and the ratio λ_i are obtained by T2 NMR spectrum measurement, and the pore throat radius is calculated by the equation r_i=3·ρ·T2_i, where ρ is the rock surface relaxation rate in μm/ms. The results are shown in Table 7.

TABLE 7
The pore size distribution of the Sandstone 3 sample
		T2i relaxation		Pore throat
	NO., i	time (ms)	λi, %	radius ri, μm
	1	10000.00	0.00	1448.825
	2	8697.49	0.00	1351.653
	3	7564.63	0.00	1260.998
	4	6579.33	0.00	1176.423
	5	5722.37	0.00	1097.521
	6	4977.02	0.00	1023.911
	7	4328.76	0.00	955.238
	8	3764.94	0.00	891.170
	9	3274.55	0.00	831.400
	10	2848.04	0.00	775.638
	11	2477.08	0.00	723.616
	12	2154.43	0.00	675.084
	13	1873.82	0.00	629.806
	14	1629.75	0.00	587.565
	15	1417.47	0.00	548.157
	16	1232.85	0.01	511.393
	17	1072.27	0.02	477.094
	18	932.60	0.03	445.095
	19	811.13	0.04	415.243
	20	705.48	0.04	387.393
	21	613.59	0.05	361.411
	22	533.67	0.05	337.171
	23	464.16	0.05	314.557
	24	403.70	0.05	293.460
	25	351.12	0.05	273.777
	26	305.39	0.10	255.415
	27	265.61	0.17	238.285
	28	231.01	0.24	222.303
	29	200.92	0.31	207.393
	30	174.75	0.37	193.484
	31	151.99	0.43	180.507
	32	132.19	0.50	168.400
	33	114.98	0.56	157.106
	34	100.00	0.62	146.569
	35	86.97	0.68	136.738
	36	75.65	0.73	127.567
	37	65.79	0.79	119.012
	38	57.22	0.84	111.029
	39	49.77	0.89	103.583
	40	43.29	0.93	96.635
	41	37.65	0.96	90.154
	42	32.75	0.99	84.108
	43	28.48	1.01	78.467
	44	24.77	1.04	73.204
	45	21.54	1.06	68.294
	46	18.74	1.08	63.714
	47	16.30	1.10	59.440
	48	14.17	1.11	55.454
	49	12.33	1.12	51.734
	50	10.72	1.11	48.265
	51	9.33	1.10	45.028
	52	8.11	1.08	42.008
	53	7.05	1.05	39.190
	54	6.14	1.03	36.562
	55	5.34	1.01	34.110
	56	4.64	1.01	31.822
	57	4.04	1.03	29.688
	58	3.51	1.09	27.696
	59	3.05	1.17	25.839
	60	2.66	1.29	24.106
	61	2.31	1.44	22.489
	62	2.01	1.63	20.981
	63	1.75	1.86	19.574
	64	1.52	2.10	18.261
	65	1.32	2.35	17.036
	66	1.15	2.61	15.893
	67	1.00	2.87	14.828
	68	0.87	3.13	13.833
	69	0.76	3.35	12.905
	70	0.66	3.55	12.040
	71	0.57	3.71	11.232
	72	0.50	3.83	10.479
	73	0.43	3.90	9.776
	74	0.38	3.91	9.120
	75	0.33	3.85	8.509
	76	0.28	3.73	7.938
	77	0.25	3.54	7.406
	78	0.22	3.30	6.909
	79	0.19	3.02	6.446
	80	0.16	2.68	6.013
	81	0.14	2.32	5.610
	82	0.12	1.94	5.234
	83	0.11	1.57	4.883
	84	0.09	1.22	4.555
	85	0.08	0.91	4.250
	86	0.07	0.65	3.965
	87	0.06	0.44	3.699
	88	0.05	0.27	3.451
	89	0.05	0.16	3.219
	90	0.04	0.09	3.003
	91	0.04	0.04	2.802
	92	0.03	0.02	2.614
	93	0.03	0.01	2.439
	94	0.02	0.00	2.275
	95	0.02	0.00	2.123
	96	0.02	0.00	1.980
	97	0.02	0.00	1.847
	98	0.01	0.00	1.724
	99	0.01	0.00	1.608
	100	0.01	0.00	1.500

(1) Free Water Saturation:

The pore size distribution data are converted to the capillary pressure of oil reservoir. The mercury porosimetry curve is converted into the relationship between water saturation and displacement pressure difference, in consideration of the interfacial tension, contact angle, and the like, under the conditions of actual gas reservoir temperature and pressure:

$P_{\mathrm{filling}}=\frac{2{\sigma }_{\mathrm{gas}-\mathrm{water}}\cos {\theta }_{\mathrm{gas}-\mathrm{water}}}{r}$

The curve of pore size distribution data and capillary pressure measured in the laboratory is converted into the curve of free water saturation and capillary pressure, to obtain the filling pressure, and thus the free water saturation.

σ_gas-water is the interfacial tension, in mN/m; in this example, the gas-water interfacial tension σ_gas-water=50 mN/m;

θ_gas-water is the gas-water contact angle, θ is 0, and thus cos θ=1; P_filling is the filling pressure in MPa;

r is the capillary radius in 10⁻⁹ m;

(2) Water-Membrane Water Saturation:

The water-membrane thicknesses in the pore spaces corresponding to different pore throat radii is calculated according to the following equation:

$h_i={\left(\frac{1.18\times 10^{-4}{r}_i}{\sigma }\right)}^{1/3}$

wherein h_i is the water-membrane thickness which corresponds to the pore space corresponding to the i-th pore throat radius in μm; σ is the fluid interfacial tension in mN/m; r_i is the pore throat radius which corresponds to the pore space corresponding to the i-th pore throat radius; in this example, i is 1-57, and specific data are shown in Table 1;

the water-membrane saturation is calculated according to the following equation:

$S_{\mathrm{wmi}}=\frac{V_{\mathrm{water}-\mathrm{membrane}}}{V_{\mathrm{sum}}}=\frac{r_i^2-{\left(r_i-h_i\right)}^2}{r_i^2}$

wherein S_wmi is the water-membrane water saturation of the pore space corresponding to the i-th pore throat radius;

r_i is the pore throat radius which corresponds to the pore space corresponding to the i-th pore throat radius; in this example, i is 1-57, and specific data are shown in Table 1;

h_i is the water-membrane thickness which corresponds to the pore space corresponding to the i-th pore throat radius;

(3) Corner Water Saturation:

The corner water saturation is calculated according to the following equation (see FIG. 2):

$S_{\mathrm{wyi}}=\frac{A_3}{A_2+A_3}=\frac{4}{4-\pi }\hspace{1em}\left[\sqrt{{\left(\frac{r_i}{R_i}\right)}^2+2\frac{r_i}{R_i}}-\arccos \left(\frac{R_i}{R_i+r_i}\right)-{\left(\frac{r_i}{R_i}\right)}^2\mathrm{arc}\sin \left(\frac{R_i}{R_i+r_i}\right)\right]$

wherein r_i is the arc radius of air-water interface,

$r_i=\frac{2\sigma }{P_{\mathrm{filling}i}}$ in 10⁻⁹ m;

R_i is the particle radius of the tight reservoir rock sample in 10⁻⁹ m;

S_wyi is the water saturation of the pore space corresponding to the i-th pore throat radius;

P_{filling i} is the filling pressure of the pore space corresponding to the i-th pore throat radius in MPa;

σ is the fluid interfacial tension in mN/m;

the water saturation is calculated according to the following equation:

$S_w=\sum _{i=1}^n{\lambda }_i\left(S_{wyi}+S_{w\mathrm{mi}}\right)+{\lambda }_z{S}_{wz}$

wherein S_w is the water saturation;

λ_i is the percentage of pore volume occupied by the pore space corresponding to the i-th pore throat radius;

λ_i is the proportion of pore volume occupied by free water pore space;

S_wyi is the corner water saturation in the pore space corresponding to the i-th pore throat radius;

S_wmi is the water-membrane water saturation in the pore space corresponding to the i-th pore throat radius;

S_wz is the free water saturation, which has not been filled and is 100%.

The relationship between the filling pressure and the gas saturation is shown in FIG. 7, and the relationship between the filled pore throat radius and the gas saturation is shown in FIG. 8.

The gas saturation of the tight reservoir rock sample is then calculated according to the following equation:S_g=100−S_w

wherein S_w is the water saturation in %; the water saturation is the sum of the free water saturation, the water-membrane water saturation and the corner water saturation;

S_g is the gas saturation in %.

The parameters of this example are shown in Table 8, and the physical simulation results corresponding to this example are shown in Table 9.

TABLE 8
Parameters of this example
									Water
	pore throat				Water-membrane		Particle		saturation
	radius ri	λi	Pfilling	Swmi	thickness h,	Swyi	radius R	Swz	Sw
No. i	μm	%	MPa	%	μm	%	μm	%	%
1	1448.825	0.00	0.00	0.00	0.204	0.00	3499.58	100	0
2	1351.653	0.00	0.00	0.00	0.200	0.00	3264.86	100	0
3	1260.998	0.00	0.00	0.00	0.195	0.00	3045.89	100	0
4	1176.423	0.00	0.00	0.00	0.191	0.00	2841.60	100	0
5	1097.521	0.00	0.00	0.00	0.186	0.00	2651.02	100	0
6	1023.911	0.00	0.00	0.00	0.182	0.00	2473.21	100	0
7	955.238	0.00	0.00	0.00	0.178	0.00	2307.34	100	0
8	891.170	0.00	0.00	0.00	0.174	0.00	2152.58	100	0
9	831.400	0.00	0.00	0.00	0.170	0.00	2008.21	100	0
10	775.638	0.00	0.00	0.00	0.166	0.00	1873.52	100	0
11	723.616	0.00	0.00	0.00	0.162	0.00	1747.87	100	0
12	675.084	0.00	0.00	0.00	0.159	0.00	1630.64	100	0
13	629.806	0.00	0.00	0.00	0.155	0.00	1521.27	100	0
14	587.565	0.00	0.00	0.00	0.151	0.00	1419.24	100	0
15	548.157	0.00	0.00	0.00	0.148	0.00	1324.05	100	0
16	511.393	0.01	0.00	0.00	0.145	0.00	1235.25	100	0
17	477.094	0.02	0.00	0.00	0.141	0.00	1152.40	100	0
18	445.095	0.03	0.00	0.00	0.138	0.01	1075.11	100	0
19	415.243	0.04	0.00	0.00	0.135	0.00	1003.00	100	0
20	387.393	0.04	0.00	0.00	0.132	0.01	935.73	100	0
21	361.411	0.05	0.00	0.00	0.129	0.00	872.97	100	0
22	337.171	0.05	0.00	0.00	0.126	0.01	814.42	100	0
23	314.557	0.05	0.00	0.00	0.123	0.00	759.80	100	0
24	293.460	0.05	0.00	0.00	0.120	0.01	708.84	100	0
25	273.777	0.05	0.00	0.00	0.117	0.00	661.30	100	0
26	255.415	0.10	0.00	0.00	0.115	0.02	616.95	100	0
27	238.285	0.17	0.00	0.00	0.112	0.00	575.57	99	1
28	222.303	0.24	0.00	0.00	0.109	0.04	536.96	99	1
29	207.393	0.31	0.00	0.00	0.107	0.00	500.95	99	1
30	193.484	0.37	0.00	0.00	0.105	0.07	467.35	98	2
31	180.507	0.43	0.00	0.00	0.102	0.00	436.01	98	2
32	168.400	0.50	0.00	0.00	0.100	0.09	406.76	97	2
33	157.106	0.56	0.00	0.00	0.098	0.00	379.48	97	3
34	146.569	0.62	0.00	0.00	0.095	0.11	354.03	96	4
35	136.738	0.68	0.00	0.00	0.093	0.00	330.29	96	4
36	127.567	0.73	0.00	0.00	0.091	0.13	308.13	95	5
37	119.012	0.79	0.00	0.00	0.089	0.00	287.47	94	6
38	111.029	0.84	0.00	0.00	0.087	0.15	268.19	93	7
39	103.583	0.89	0.00	0.00	0.085	0.00	250.20	92	8
40	96.635	0.93	0.00	0.00	0.083	0.17	233.42	91	8
41	90.154	0.96	0.00	0.00	0.081	0.00	217.76	91	9
42	84.108	0.99	0.00	0.00	0.079	0.18	203.16	90	10
43	78.467	1.01	0.00	0.00	0.077	0.00	189.53	89	11
44	73.204	1.04	0.00	0.00	0.076	0.19	176.82	87	12
45	68.294	1.06	0.00	0.00	0.074	0.00	164.96	86	13
46	63.714	1.08	0.00	0.00	0.072	0.19	153.90	85	15
47	59.440	1.10	0.00	0.00	0.071	0.00	143.58	84	16
48	55.454	1.11	0.00	0.00	0.069	0.20	133.95	83	17
49	51.734	1.12	0.00	0.00	0.067	0.00	124.96	82	18
50	48.265	1.11	0.00	0.00	0.066	0.20	116.58	81	19
51	45.028	1.10	0.00	0.00	0.064	0.00	108.76	80	20
52	42.008	1.08	0.00	0.00	0.063	0.19	101.47	79	21
53	39.190	1.05	0.00	0.00	0.061	0.00	94.66	78	22
54	36.562	1.03	0.00	0.00	0.060	0.19	88.31	77	23
55	34.110	1.01	0.00	0.00	0.059	0.00	82.39	76	24
56	31.822	1.01	0.00	0.00	0.057	0.18	76.86	75	25
57	29.688	1.03	0.00	0.00	0.056	0.00	71.71	74	26
58	27.696	1.09	0.00	0.00	0.055	0.20	66.90	72	27
59	25.839	1.17	0.00	0.00	0.053	0.00	62.41	71	28
60	24.106	1.29	0.00	0.01	0.052	0.23	58.23	70	29
61	22.489	1.44	0.00	0.01	0.051	0.00	54.32	69	31
62	20.981	1.63	0.00	0.01	0.050	0.29	50.68	67	32
63	19.574	1.86	0.00	0.01	0.049	0.00	47.28	65	34
64	18.261	2.10	0.00	0.01	0.048	0.38	44.11	63	36
65	17.036	2.35	0.00	0.01	0.046	0.00	41.15	61	39
66	15.893	2.61	0.00	0.01	0.045	0.47	38.39	58	41
67	14.828	2.87	0.00	0.02	0.044	0.00	35.82	55	44
68	13.833	3.13	0.00	0.02	0.043	0.56	33.41	52	47
69	12.905	3.35	0.00	0.02	0.042	0.00	31.17	49	50
70	12.040	3.55	0.00	0.02	0.041	0.64	29.08	45	53
71	11.232	3.71	0.00	0.03	0.040	0.00	27.13	41	57
72	10.479	3.83	0.00	0.03	0.040	0.69	25.31	38	60
73	9.776	3.90	0.00	0.03	0.039	0.00	23.61	34	64
74	9.120	3.91	0.00	0.03	0.038	0.70	22.03	30	68
75	8.509	3.85	0.00	0.03	0.037	0.00	20.55	26	71
76	7.938	3.73	0.01	0.03	0.036	0.67	19.17	22	75
77	7.406	3.54	0.01	0.03	0.035	0.00	17.89	19	78
78	6.909	3.30	0.01	0.03	0.034	0.59	16.69	15	81
79	6.446	3.02	0.01	0.03	0.034	0.00	15.57	12	84
80	6.013	2.68	0.01	0.03	0.033	0.48	14.52	10	86
81	5.610	2.32	0.01	0.03	0.032	0.00	13.55	7	88
82	5.234	1.94	0.01	0.02	0.031	0.35	12.64	5	90
83	4.883	1.57	0.01	0.02	0.031	0.00	11.79	4	91
84	4.555	1.22	0.01	0.02	0.030	0.22	11.00	3	92
85	4.250	0.91	0.01	0.01	0.029	0.00	10.26	2	93
86	3.965	0.65	0.01	0.01	0.029	0.12	9.58	1	94
87	3.699	0.44	0.01	0.01	0.028	0.00	8.93	1	94
88	3.451	0.27	0.01	0.00	0.027	0.05	8.33	0	94
89	3.219	0.16	0.01	0.00	0.027	0.00	7.78	0	95
90	3.003	0.09	0.01	0.00	0.026	0.02	7.25	0	95
91	2.802	0.04	0.01	0.00	0.025	0.00	6.77	0	95
92	2.614	0.02	0.02	0.00	0.025	0.00	6.31	0	95
93	2.439	0.01	0.02	0.00	0.024	0.00	5.89	0	95
94	2.275	0.00	0.02	0.00	0.024	0.00	5.50	0	95
95	2.123	0.00	0.02	0.00	0.023	0.00	5.13	0	95
96	1.980	0.00	0.02	0.00	0.023	0.00	4.78	0	95
97	1.847	0.00	0.02	0.00	0.022	0.00	4.46	0	95
98	1.724	0.00	0.02	0.00	0.022	0.00	4.16	0	95
99	1.608	0.00	0.02	0.00	0.021	0.00	3.88	0	95
100	1.500	0.00	0.03	0.00	0.021	0.00	3.62	0	95

TABLE 9
Physical simulation results corresponding to this example
Pfilling MPa Gas saturation Sw %
0.1          21.41
0.2          50.12
0.3          57.54
0.4          65.46
0.5          70.96
0.6          78.24
0.7          84.50
0.8          86.98
0.9          90.94
1            92.51
1.1          93.37

As can be seen from FIG. 8, model calculations are used in the method for determining the gas saturation of a tight reservoir having large pores provided in Example 3, and compared with the physical simulation experiments. As compared with the actual physical simulation experiments, it is found that the final gas saturation data are consistent, but the experimental results at different pressure points are significantly different from those calculated by this method. The reason is analyzed to be that: when reaching a certain gas saturation condition, since the rock sample has large pores, the method of the present invention only needs to give a small pressure and can be completed in an infinite time in a gas reservoir; however, when reaching the same gas saturation condition, it is not easy to set a pressure of less than 0.01 MPa in the physical simulation experiment instrument, and it can only set a higher pressure than the method of the present invention. The consistency between the final gas saturation data demonstrates the accuracy of the method of the present invention from a certain aspect. Moreover, the method of the present invention has reached the low-pressure condition that is not easily reached by the physical simulation experimental instruments at present, which proves the technical advantages of the technical solution of the present invention.

Claims

1. A method for determining the gas saturation of a tight reservoir, comprising: a free water saturation calculation step: determining the pore size distribution of the tight reservoir rock sample, and calculating the free water saturation of the tight reservoir rock sample from the pore size distribution, wherein in the free water saturation calculation step, the pore size distribution of the tight reservoir rock sample is determined by mercury porosimetry as follows: injecting mercury into rock pores to displace air in rock pores;when the injection pressure exceeds the capillary pressure, mercury entering the pore throat of the rock sample, and at this time, the injection pressure being the capillary pressure, the capillary radius corresponding to the pressure is equivalent to the pore throat radius, and the volume of mercury entering the pores being the pore volume;increasing the injection pressure such that mercury enters the pores controlled by a smaller throat, to obtain the pore throat radius and the pore volume corresponding to the smaller throat; andrepeatedly increasing the injection pressure to obtain the pore throat radii and the pore volumes corresponding to different throats;a water-membrane water saturation calculation step: calculating the water-membrane water saturation of the tight reservoir rock sample;a corner water saturation calculation step: calculating the corner water saturation of the tight reservoir rock sample; anda gas saturation calculation step: calculating the gas saturation of the tight reservoir rock sample according to the following equation: Sg=100−Sw

2. The method according to claim 1, wherein in the free water saturation calculation step, the data of the pore size distribution includes data of pore spaces corresponding to different pore throat radii.

3. The method according to claim 2, wherein in the free water saturation calculation step, the data of pore spaces corresponding to different pore throat radii includes the pore throat radii corresponding to the pore spaces with different radii and the percentages of pore volume occupied by the pore spaces with different radii.

4. The method according to claim 1, wherein in the free water saturation calculation step, the free water saturation of the tight reservoir rock sample is calculated from the pore size distribution as follows: (1) obtaining the relationship between the injection pressure and the pore volume from the pore throat radii and the pore volumes corresponding to different throats in the tight reservoir rock sample;

5. The method according to claim 1, wherein the water-membrane water saturation calculation step is performed as follows: (1) calculating the water-membrane thicknesses in the pore spaces corresponding to different pore throat radii according to the following equation:

6. The method according to claim 1, wherein the corner water saturation calculation step is performed by one of: (1) observing the pore structure of the reservoir and directly determining the corner water saturation;(2) counting the proportions of corner water corresponding to different types of pore structure, and determining the corner water saturation by weighted average;(3) calculating the corner water saturation according to the following equation:

7. The method according to claim 1, wherein the gas saturation calculation step is performed as follows: (1) calculating the water saturation according to the following equation:

8. The method according to claim 1, comprising: a free water saturation calculation step:determining the pore size distribution of the tight reservoir rock sample by mercury porosimetry; when the injection pressure exceeds the capillary pressure, mercury entering the pore throat of the rock sample, and at this time, the injection pressure being the capillary pressure, the capillary radius corresponding to the capillary pressure being equivalent to the pore throat radius, and the volume of mercury entering the pores being the pore volume;increasing the injection pressure such that mercury enters the pores controlled by a smaller throat, to obtain the corresponding pore throat radius and pore volume;continuously increasing the injection pressure to obtain the relationship between the injection pressure, that is, the capillary pressure, and the pore volume;calculating the gas saturation from the volume of mercury injected and the pore volume of the tight reservoir rock sample, and then obtaining the curve of the pore size distribution of different pore throat radius ranges and the capillary pressure;converting the pore size distribution data of the tight reservoir rock sample into the capillary pressure of oil reservoir; and converting the mercury porosimetry curve into the relationship of water saturation according to the displacement pressure difference, in consideration of the interfacial tension and the contact angle under the conditions of actual gas reservoir temperature and pressure,

9. The method according to claim 1, wherein the method is based on the following premises: assuming that the reservoir rock contains only two fluids, formation water and natural gas, and the gas saturation is directly affected by the rock water saturation; if the reservoir water saturation is obtained, the gas saturation can be obtained;the size and stacking relationship of the rock-forming mineral particles determine the geometry and spatial distribution of the fluid storage space;the formation water exists in rocks in three main forms:(1) free water: pore water that cannot be expelled by natural gas, occupying small pore throats that cannot be filled, and its saturation is affected by natural gas filling pressure and pore throat capillary force;(2) water-membrane water: adsorbed on the pore wall in the form of a thin membrane, its saturation is related to the surface area of the pore wall and the thickness of the water-membrane;(3) corner water: existing in the corners that are difficult to displace among the particles, and its saturation is affected by the size and the contact relationship of the rock particles.