阅读说明：本技术 一种气体突破压力测定方法和校正方法 (Gas breakthrough pressure measuring method and correcting method ) 是由 肖玉峰 王红岩 姜振学 葛新民 于 2021-01-22 设计创作，主要内容包括：本发明实施例提供了一种气体突破压力测定方法和校正方法。所述气体突破压力测定方法包括：准备岩样；测量干燥岩样的核磁共振衰减曲线,根据该曲线计算干燥岩样的核磁共振T2谱；测量饱水岩样的核磁共振衰减曲线,根据该曲线计算饱水岩样的核磁共振T2谱；根据所述饱水岩样的核磁共振T2谱和干燥岩样的核磁共振T2谱,计算气体突破压力值。本发明能够快速精确的得到页岩气体突破压力值,为页岩油气储层的评价和表征提供依据。(The embodiment of the invention provides a gas breakthrough pressure measuring method and a gas breakthrough pressure correcting method. The gas breakthrough pressure determination method comprises the following steps: preparing a rock sample; measuring the nuclear magnetic resonance attenuation curve of the dried rock sample, and calculating the nuclear magnetic resonance T2 spectrum of the dried rock sample according to the curve; measuring a nuclear magnetic resonance attenuation curve of the water-saturated rock sample, and calculating a nuclear magnetic resonance T2 spectrum of the water-saturated rock sample according to the curve; and calculating the gas breakthrough pressure value according to the nuclear magnetic resonance T2 spectrum of the water-saturated rock sample and the nuclear magnetic resonance T2 spectrum of the dry rock sample. The method can quickly and accurately obtain the shale gas breakthrough pressure value, and provides a basis for evaluation and characterization of the shale oil and gas reservoir.)

1. A method of determining a breakthrough pressure of a gas, comprising:

preparing a rock sample;

measuring the nuclear magnetic resonance attenuation curve of the dried rock sample, and calculating the nuclear magnetic resonance T2 spectrum of the dried rock sample according to the curve;

measuring a nuclear magnetic resonance attenuation curve of the water-saturated rock sample, and calculating a nuclear magnetic resonance T2 spectrum of the water-saturated rock sample according to the curve;

and calculating the gas breakthrough pressure value according to the nuclear magnetic resonance T2 spectrum of the water-saturated rock sample and the nuclear magnetic resonance T2 spectrum of the dry rock sample.

2. The method of claim 1, wherein calculating a gas breakthrough pressure value from the nuclear magnetic resonance T2 spectrum of the water-saturated rock sample and the nuclear magnetic resonance T2 spectrum of the dry rock sample comprises:

according to the nuclear magnetic resonance T2 spectrum of the water-saturated rock sample and the nuclear magnetic resonance T2 spectrum of the dry rock sample, calculating the geometric mean value of an intrinsic nuclear magnetic resonance T2 spectrum and an intrinsic nuclear magnetic resonance T2 spectrum;

calculating the proportion of small holes of the rock sample according to the intrinsic nuclear magnetic resonance T2 spectrum;

and calculating the gas breakthrough pressure value of the rock sample according to the geometric mean value of the intrinsic nuclear magnetic resonance T2 spectrum and the proportion of the small holes.

3. The method of claim 2, wherein calculating an intrinsic nuclear magnetic resonance T2 spectrum from the nuclear magnetic resonance T2 spectrum of the water-saturated rock sample and the nuclear magnetic resonance T2 spectrum of the dry rock sample comprises:

intrinsic nmr T2 spectrum-nmr T2 spectrum of water-saturated rock sample-nmr T2 spectrum of dry rock sample.

4. The method of claim 2, wherein the calculating the pore fraction of the rock sample from the intrinsic nmr T2 spectrum comprises:

the proportion of the small holes is the proportion of the area of the small holes in the intrinsic nuclear magnetic resonance T2 spectrum to the total area of the intrinsic nuclear magnetic resonance T2 spectrum;

wherein S is_microporeIs the proportion of the small holes,

the small pore area in the intrinsic nuclear magnetic resonance T2 spectrum,

the total area of the intrinsic nuclear magnetic resonance T2 spectrum.

5. The method according to claim 2 or 4,

the pores are pores with a relaxation time of less than a threshold time in the intrinsic nmr T2 spectrum, the threshold time preferably being 2 ms.

6. The method according to claim 2, wherein the gas breakthrough pressure value P is calculated according to the geometric mean of the intrinsic NMR T2 spectrum and the small hole ratio_b：

Wherein a, b and c are fitting coefficients,

S_microporeis the proportion of the small holes,

T_2gmthe geometric mean of the spectrum of intrinsic nuclear magnetic resonance T2.

7. The method of claim 1, wherein the preparing the rock sample comprises:

obtaining a downhole plunger-like rock sample.

8. The method of claim 1,

measuring a nuclear magnetic resonance attenuation curve of the rock sample by using a rock core nuclear magnetic resonance analyzer; and

the nuclear magnetic resonance attenuation curve is a transverse macroscopic magnetization vector attenuation curve.

9. The method of claim 1, wherein said calculating a nuclear magnetic resonance T2 spectrum for a dry rock sample from said curve and said calculating a nuclear magnetic resonance T2 spectrum for a water-saturated rock sample from said curve comprise

And carrying out inversion calculation on the nuclear magnetic resonance attenuation curve.

10. The method of claim 1,

the preparation process of the water-saturated rock sample comprises the step of putting the rock sample into a high-pressure rock core saturator to enable the pores of the rock sample to completely saturate formation water.

11. A method of gas breakthrough pressure correction, comprising: a method of determining gas breakthrough pressure according to any one of claims 1 to 10, obtaining a gas breakthrough pressure measurement;

fitting to form a linear relation between the real value of the gas breakthrough pressure and the measured value of the gas breakthrough pressure by utilizing a plurality of gas breakthrough pressure measured values corresponding to a plurality of rock samples;

and substituting the measured value of the gas breakthrough pressure into the linear relation to obtain the true value of the gas breakthrough pressure.

Technical Field

The invention belongs to the field of geophysical logging, and particularly relates to a gas breakthrough pressure measuring method and a gas breakthrough pressure correcting method.

Background

The gas breakthrough pressure is a key parameter for evaluating unconventional reservoirs such as shale oil gas and the like and representing the sealing performance of a cover layer, and is generally obtained by a core scale logging method at present. The conventional data such as sound wave time difference, resistivity and the like are mostly adopted in the existing logging calculation model, the characteristics such as the micro-pore structure of rock and the like cannot be reflected, the calculation precision of gas breakthrough pressure is low, and the gas breakthrough pressure period tested by using a breakthrough pressure tester is too long.

Disclosure of Invention

The embodiment of the invention aims to provide a gas breakthrough pressure measuring method and a gas breakthrough pressure correcting method, which can quickly and accurately obtain a shale gas breakthrough pressure value and provide a basis for evaluation and characterization of a shale oil-gas reservoir.

The inventor of the invention discovers through research that in the prior art method, the gas breakthrough pressure is measured mainly through a breakthrough pressure experimental instrument, the test process is complicated, and the test period is long. The low-field nuclear magnetic resonance technology plays an important role in petrophysics and well logging, and the measurement signal is only related to formation hydrogen nuclei, so that information such as a reservoir pore structure, fluid components and the like can be effectively represented. The inventor of the invention further researches and can quickly and accurately obtain the gas breakthrough pressure value according to the nuclear magnetic resonance T2 spectrum of the water-saturated rock sample and the nuclear magnetic resonance T2 spectrum of the dry rock sample.

In order to achieve the above object, an embodiment of the present invention provides a gas breakthrough pressure measurement method and a calibration method, the method including: preparing a rock sample; measuring the nuclear magnetic resonance attenuation curve of the dried rock sample, and calculating the nuclear magnetic resonance T2 spectrum of the dried rock sample according to the curve; measuring a nuclear magnetic resonance attenuation curve of the water-saturated rock sample, and calculating a nuclear magnetic resonance T2 spectrum of the water-saturated rock sample according to the curve; and calculating the gas breakthrough pressure value according to the nuclear magnetic resonance T2 spectrum of the water-saturated rock sample and the nuclear magnetic resonance T2 spectrum of the dry rock sample.

Optionally, the method further includes: according to the nuclear magnetic resonance T2 spectrum of the water-saturated rock sample and the nuclear magnetic resonance T2 spectrum of the dry rock sample, calculating a gas breakthrough pressure value comprises the following steps: according to the nuclear magnetic resonance T2 spectrum of the water-saturated rock sample and the nuclear magnetic resonance T2 spectrum of the dry rock sample, calculating the geometric mean value of an intrinsic nuclear magnetic resonance T2 spectrum and an intrinsic nuclear magnetic resonance T2 spectrum; calculating the proportion of small holes of the rock sample according to the intrinsic nuclear magnetic resonance T2 spectrum; and calculating the gas breakthrough pressure value of the rock sample according to the geometric mean value of the intrinsic nuclear magnetic resonance T2 spectrum and the proportion of the small holes.

Optionally, the calculating an intrinsic nmr T2 spectrum according to the nmr T2 spectrum of the water-saturated rock sample and the nmr T2 spectrum of the dry rock sample includes: intrinsic nmr T2 spectrum-nmr T2 spectrum of water-saturated rock sample-nmr T2 spectrum of dry rock sample.

Optionally, the calculating the pore proportion of the rock sample according to the intrinsic nuclear magnetic resonance T2 spectrum includes: the proportion of the small holes is the proportion of the area of the small holes in the intrinsic nuclear magnetic resonance T2 spectrum to the total area of the intrinsic nuclear magnetic resonance T2 spectrum;

wherein S is_microporeIs the proportion of the small holes,

the small pore area in the intrinsic nuclear magnetic resonance T2 spectrum,

the total area of the intrinsic nuclear magnetic resonance T2 spectrum.

Optionally, the small hole is a pore with a relaxation time in the intrinsic nmr T2 spectrum smaller than a threshold time, which is preferably 2 ms.

Optionally, the gas breakthrough pressure value P is calculated according to the geometric mean of the intrinsic nuclear magnetic resonance T2 spectrum and the proportion of the small holes_b：

Wherein a, b and c are fitting coefficients,

S_microporeis the proportion of the small holes,

T_2gmthe geometric mean of the spectrum of intrinsic nuclear magnetic resonance T2.

Optionally, the preparing the rock sample comprises: obtaining a downhole plunger-like rock sample.

Optionally, measuring a nuclear magnetic resonance attenuation curve of the rock sample by using a rock core nuclear magnetic resonance analyzer; and the nuclear magnetic resonance attenuation curve is a transverse macroscopic magnetization vector attenuation curve.

Optionally, the calculating a nuclear magnetic resonance T2 spectrum of the dry rock sample according to the curve and the calculating a nuclear magnetic resonance T2 spectrum of the water-saturated rock sample according to the curve include performing inversion calculation on the nuclear magnetic resonance attenuation curve.

Optionally, the preparation process of the water-saturated rock sample includes placing the rock sample into a high-pressure core saturator, so that the pores of the rock sample completely saturate formation water.

Correspondingly, the embodiment of the invention also provides a gas breakthrough pressure correction method, which comprises the following steps: a method of determining gas breakthrough pressure according to any one of claims 1 to 10, obtaining a gas breakthrough pressure measurement; fitting to form a linear relation between the real value of the gas breakthrough pressure and the measured value of the gas breakthrough pressure by utilizing a plurality of gas breakthrough pressure measured values corresponding to a plurality of rock samples; and substituting the measured value of the gas breakthrough pressure into the linear relation to obtain the true value of the gas breakthrough pressure.

According to the technical scheme, the rock sample is prepared; measuring the nuclear magnetic resonance attenuation curve of the dried rock sample, and calculating the nuclear magnetic resonance T2 spectrum of the dried rock sample according to the curve; measuring a nuclear magnetic resonance attenuation curve of the water-saturated rock sample, and calculating a nuclear magnetic resonance T2 spectrum of the water-saturated rock sample according to the curve; and calculating the gas breakthrough pressure value according to the nuclear magnetic resonance T2 spectrum of the water-saturated rock sample and the nuclear magnetic resonance T2 spectrum of the dry rock sample. The method can solve the problem that the influence of a pore structure on the breakthrough pressure cannot be considered by adopting conventional logging data such as sound waves, resistivity and the like, effectively improves the calculation precision of the gas breakthrough pressure, can quickly and accurately obtain the shale gas breakthrough pressure value, and has important significance on evaluation and comprehensive characterization of shale oil gas.

Additional features and advantages of embodiments of the invention will be set forth in the detailed description which follows.

Drawings

The accompanying drawings, which are included to provide a further understanding of the embodiments of the invention and are incorporated in and constitute a part of this specification, illustrate embodiments of the invention and together with the description serve to explain the embodiments of the invention without limiting the embodiments of the invention. In the drawings:

FIGS. 1, 2, 3 and 4 are schematic flow diagrams of a gas breakthrough pressure determination method of the invention;

FIG. 5 is a nuclear magnetic resonance T2 spectrum of a dried rock sample according to the invention;

FIG. 6 is a nuclear magnetic resonance T2 spectrum of a water-saturated rock sample according to the invention;

FIG. 7 is a spectrum of intrinsic NMR T2 of the present invention;

FIG. 8 is a graph of gas breakthrough pressure versus geometric mean of intrinsic NMR T2 spectra;

FIG. 9 is a graph of gas breakthrough pressure versus orifice ratio;

FIG. 10 is a linear plot of predicted gas breakthrough pressure versus measured gas breakthrough pressure.

Detailed Description

The following detailed description of embodiments of the invention refers to the accompanying drawings. It should be understood that the detailed description and specific examples, while indicating embodiments of the invention, are given by way of illustration and explanation only, not limitation.

FIG. 1 is a schematic flow diagram of a method for determining breakthrough gas pressure according to the present invention. As shown in fig. 1, the method for determining gas breakthrough pressure according to the embodiment of the invention may include the following steps:

step S101, preparing a rock sample, including obtaining a downhole plunger-like rock sample. The rock sample is preferably shale. The method comprises the steps that a worker obtains a shale sample with a specific depth in a well, the shale sample is processed into a plunger sample by adopting a linear cutting technology, and the length, the diameter and the weight of the shale sample are measured after the shale sample is dried. Preferably, the plug-like rock sample has a length of 2.54 cm and a diameter of 2.54 cm.

Step S102, calculating the nuclear magnetic resonance T2 spectrum of the dried rock sample. And measuring the nuclear magnetic resonance attenuation curve of the rock sample by using a rock core nuclear magnetic resonance analyzer, and calculating the nuclear magnetic resonance T2 spectrum of the dry rock sample according to the nuclear magnetic resonance attenuation curve, wherein the nuclear magnetic resonance attenuation curve is a transverse macroscopic magnetization vector attenuation curve. And calculating the nuclear magnetic resonance T2 spectrum of the dry rock sample according to the curve, wherein the nuclear magnetic resonance attenuation curve is subjected to inversion calculation.

The nuclear magnetic resonance analyzer mainly applies nuclear magnetic resonance working technology. The nuclear magnetic resonance technology is to detect various substances by utilizing resonance phenomenon caused by interaction of nuclear magnetic atoms and an external magnetic field, wherein among elements contained in a stratum, the magnetic rotation ratio of hydrogen nuclei is the largest and the abundance is higher, and the fluid quantity and the fluid type in rock pores and the binding force between the surfaces of fluid and rock pore solids are rapidly detected by detecting nuclear magnetic resonance signals of the hydrogen nuclei, so that the physical property parameters, the pore structure distribution, the movable fluid distribution, the oil-water distribution in different pores of the rock and the like are obtained. Preferably, the main frequency of the core nuclear magnetic resonance instrument is 21 MHz.

And step S103, calculating a nuclear magnetic resonance T2 spectrum of the water-saturated rock sample. The rock sample saturated with water is placed into a rock core nuclear magnetic resonance analyzer, the nuclear magnetic resonance attenuation curve of the rock sample saturated with water is measured, the nuclear magnetic resonance T2 spectrum of the rock sample saturated with water is calculated according to the curve, and the nuclear magnetic resonance attenuation curve is a transverse macroscopic magnetization vector attenuation curve. The preparation process of the water-saturated rock sample comprises the steps of putting the rock sample into a high-pressure rock core saturator, and enabling the pores of the rock sample to completely saturate formation water, wherein the formation water is saline water with the salinity equivalent to that of the formation water. And calculating the nuclear magnetic resonance T2 spectrum of the saturated rock sample according to the curve, wherein the nuclear magnetic resonance attenuation curve is subjected to inversion calculation.

And step S104, calculating a gas breakthrough pressure value. And calculating the gas breakthrough pressure value according to the nuclear magnetic resonance T2 spectrum of the water-saturated rock sample and the nuclear magnetic resonance T2 spectrum of the dry rock sample. When gas forms a continuous mobile phase in a liquid saturated rock sample under the action of a certain pressure difference, the corresponding pressure difference value of the inlet end and the outlet end is rock gas breakthrough pressure, and the gas breakthrough pressure is a key parameter for evaluating unconventional reservoirs such as shale oil gas and the like and characterizing the closure performance of a cover layer.

Fig. 2 is a specific embodiment of step S102. According to this embodiment, the nuclear magnetic resonance T2 spectrum of the dried rock sample is calculated, including:

step S201, drying the rock sample, wherein the processing mode includes but is not limited to drying and air drying;

step S202, measuring a nuclear magnetic resonance attenuation curve of the dried rock sample, setting appropriate measurement parameters (waiting time, echo interval, scanning times, gain and the like) for the analyzer by putting the dried rock sample into a rock core nuclear magnetic resonance analyzer, and measuring the nuclear magnetic resonance attenuation curve of the dried rock sample;

in step S203, the nuclear magnetic resonance T2 spectrum of the dried rock sample is calculated according to the curve. And calculating the nuclear magnetic resonance T2 spectrum of the dry rock sample according to the curve, wherein the nuclear magnetic resonance attenuation curve is subjected to inversion calculation. And (3) an inversion process: the nuclear magnetic resonance T2-signal amplitude spectrum is obtained by inverting the nuclear magnetic resonance attenuation signal amplitude spectrum (T2-the sum of the amplitudes of the signal amplitude spectrum is equal to the first point of the attenuation signal spectrum). Inversion methods include, but are not limited to, non-negative least squares, singular value decomposition, transform inversion algorithms, and the like. The nuclear magnetic resonance attenuation curve is a transverse macroscopic magnetization vector attenuation curve. The nuclear magnetic resonance attenuation curve is a transverse macroscopic magnetization vector attenuation curve. FIG. 5 is a nuclear magnetic resonance T2 spectrum of a dried rock sample of the present invention, and as shown in the figure, the main peak of the nuclear magnetic resonance T2 spectrum of the dried rock sample is distributed around 0.2 milliseconds, which mainly reflects the background signal of shale.

Fig. 3 is a specific embodiment of step S103. According to this embodiment, the calculation of the nuclear magnetic resonance T2 spectrum of the water-saturated rock sample includes:

s301, carrying out water saturation treatment on a rock sample, wherein the preparation process of the water-saturated rock sample comprises the step of putting the rock sample into a high-pressure rock core saturator to enable the pores of the rock sample to completely saturate formation water. Preferably, the pressure of the high-pressure core saturator is 30 MPa and the time is 48 hours. The formation water is saline water with the mineralization degree equivalent to that of the formation water;

step S302, measuring a nuclear magnetic resonance attenuation curve of a water-saturated rock sample, setting appropriate measurement parameters (waiting time, echo interval, scanning times, gain and the like) for an analyzer by putting the water-saturated rock sample into a rock core nuclear magnetic resonance analyzer, and measuring the nuclear magnetic resonance attenuation curve of the water-saturated rock sample;

and S303, calculating a nuclear magnetic resonance T2 spectrum of the water-saturated rock sample according to the curve, and calculating a nuclear magnetic resonance T2 spectrum of the water-saturated rock sample according to the curve, wherein the nuclear magnetic resonance attenuation curve is subjected to inversion calculation. FIG. 6 is a nuclear magnetic resonance T2 spectrum of the water-saturated rock sample, as shown in the figure, the nuclear magnetic resonance T2 spectrum is changed from single peak to double peak, the amplitude of the left peak is obviously increased, the right peak is distributed in about 5 milliseconds, the amplitude of the left peak is obviously larger than that of the right peak, and the nuclear magnetic resonance T2 spectrum of the water-saturated rock sample in FIG. 6 is obviously different from the nuclear magnetic resonance T2 spectrum of the dry rock sample in FIG. 5.

Fig. 4 is a specific embodiment of step S104. According to this embodiment, calculating the gas breakthrough pressure value comprises:

s401, acquiring a nuclear magnetic resonance T2 spectrum of a water-saturated rock sample and a nuclear magnetic resonance T2 spectrum of a dry rock sample; when the rock sample is subjected to water saturation and drying treatment, the rock sample is preferably dried, so that formation water is completely saturated in rock sample pores during the water saturation treatment of the rock sample;

step S402, calculating an intrinsic nuclear magnetic resonance T2 spectrum, wherein the step of calculating the intrinsic nuclear magnetic resonance T2 spectrum according to the nuclear magnetic resonance T2 spectrum of the water-saturated rock sample and the nuclear magnetic resonance T2 spectrum of the dried rock sample comprises the following steps: the intrinsic nuclear magnetic resonance T2 spectrum is the nuclear magnetic resonance T2 spectrum of a water-saturated rock sample-the nuclear magnetic resonance T2 spectrum of a dried rock sample, and the intrinsic nuclear magnetic resonance T2 spectrum can reflect the pore structure of the rock sample.

Fig. 7 is a spectrogram of intrinsic nmr T2 of the present invention, and as shown in the figure, the intrinsic nmr T2 spectrum is scaled to porosity, which is 5.65%, and the liquid-measured porosity of the rock sample is 5.42%, and the difference between the two is small, so that the intrinsic nmr T2 spectrum can be obtained to reflect the pore fluid information. Wherein the nuclear magnetic porosity is measured as: 1) the calibration process comprises the steps of measuring a standard sample with known porosity to obtain a transverse macroscopic magnetization vector attenuation curve, determining the maximum signal amplitude (all water signals) of a first point of the transverse macroscopic magnetization vector attenuation curve, dividing the maximum signal amplitude by the volume of the standard sample to obtain a signal value of a unit volume, and establishing a relation with the porosity (the volume of water in the unit volume of the core) of the standard sample; 2) and (3) measuring the sample, measuring the volume and the attenuation spectrum of the rock core sample, finding out the maximum value (all water signals) of the first point of the attenuation spectrum, dividing the maximum value by the volume to obtain the water signal of unit volume, and obtaining the porosity through the relationship established in the first step. The T2 magnitude spectrum is converted to a porosity component spectrum: (T2 spectrum signal amplitude/T2 spectrum amplitude sum) porosity, the porosity components are summed, i.e. porosity;

and S403, calculating the geometric mean value of the intrinsic nuclear magnetic resonance T2 spectrum according to the intrinsic nuclear magnetic resonance T2 spectrum. Fig. 8 is a graph of the relationship between the gas breakthrough pressure and the geometric mean of the intrinsic nuclear magnetic resonance T2 spectrum, as shown in the figure, the gas breakthrough pressure and the geometric mean of the intrinsic nuclear magnetic resonance T2 spectrum show an obvious power exponential relationship, the gas breakthrough capacity is inversely proportional to the pore diameter, and as the geometric mean of T2 increases, the breakthrough pressure decreases, and the gas breakthrough difficulty decreases;

step S404, calculating a rock sample small hole proportion according to an intrinsic nuclear magnetic resonance T2 spectrum, wherein the small hole proportion is the proportion of the area of the small holes in the intrinsic nuclear magnetic resonance T2 spectrum to the total area of the intrinsic nuclear magnetic resonance T2 spectrum;wherein S is_microporeIs the proportion of the small holes,the small pore area in the intrinsic nuclear magnetic resonance T2 spectrum,the total area of the intrinsic nuclear magnetic resonance T2 spectrum. The small hole is a pore with a relaxation time in the intrinsic nuclear magnetic resonance T2 spectrum smaller than a threshold time, wherein the threshold time is preferably 2ms, and the relaxation time represents the time required by the system to approach a stable fixed state from an unstable fixed state. FIG. 9 is a diagram of the proportional relationship between the gas breakthrough pressure and the aperture, as shown in the figure, the gas breakthrough pressure and the aperture proportion are in a proportional relationship, and the higher the aperture proportion is, the higher the gas breakthrough pressure is, and the greater the gas breakthrough difficulty is;

step S405, according to intrinsic nuclear magnetismCalculating a gas breakthrough pressure value according to the geometric mean value of the resonance T2 spectrum and the proportion of the pores, and calculating the gas breakthrough pressure value according to the geometric mean value of the intrinsic nuclear magnetic resonance T2 spectrum and the proportion of the pores:wherein a, b and c are fitting coefficients, are small hole ratios and are geometric mean values of intrinsic nuclear magnetic resonance T2 spectrums. The fitting coefficients relate to the investigation region, horizons etc.

Fig. 10 is a linear relationship diagram of the predicted gas breakthrough pressure and the actually measured gas breakthrough pressure, and as shown in the figure, the linear error between the predicted gas breakthrough pressure and the actually measured gas breakthrough pressure is 5.3%, and the overall linearity is good, which confirms that the gas breakthrough pressure measured by the present application has high accuracy. The measured gas breakthrough pressure is measured in a breakthrough pressure tester through a saturated rock sample. According to the gas breakthrough pressure measuring method provided by the invention, a gas breakthrough pressure measured value is obtained; fitting to form a linear relation between the real value of the gas breakthrough pressure and the measured value of the gas breakthrough pressure by utilizing a plurality of gas breakthrough pressure measured values corresponding to a plurality of rock samples; and substituting the measured value of the gas breakthrough pressure into the linear relation to obtain the true value of the gas breakthrough pressure, thereby realizing the correction of the gas breakthrough pressure.

Although the embodiments of the present invention have been described in detail with reference to the accompanying drawings, the embodiments of the present invention are not limited to the details of the above embodiments, and various simple modifications can be made to the technical solutions of the embodiments of the present invention within the technical idea of the embodiments of the present invention, and the simple modifications all belong to the protection scope of the embodiments of the present invention.

It should be noted that the various features described in the above embodiments may be combined in any suitable manner without departing from the scope of the invention. In order to avoid unnecessary repetition, the embodiments of the present invention do not describe every possible combination.

In addition, any combination of various different implementation manners of the embodiments of the present invention is also possible, and the embodiments of the present invention should be considered as disclosed in the embodiments of the present invention as long as the combination does not depart from the spirit of the embodiments of the present invention.