Method for determining pore structure through classifying isothermal adsorption curve of mud shale
A technology of isotherm adsorption curve and pore structure, applied in permeability/surface area analysis, suspension and porous material analysis, measurement device, etc., which can solve the problem that the pore structure of shale cannot be effectively judged, and the difference between different isotherm adsorption curves cannot be highlighted. and other issues to achieve the effect of diversifying types, promoting inference, and avoiding high costs
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specific Embodiment 1
[0041] Specific embodiment 1: combine Figure 8 Isotherm adsorption curves of shale samples in the Sichuan Basin and Figure 9 Figure 8 As shown in the frequency histogram of the middle sample, the D11 sample, that is, the mud shale sample in the Sichuan Basin, is classified according to the mud shale isotherm adsorption curve classification method as the W8 type, which is a medium wedge-shaped small hole. From the pore frequency distribution diagram, it can be seen that the pores with a pore diameter of 10-20nm in the D11 sample account for the largest pore volume, and it can be preliminarily inferred that the sample is dominated by small pores; the peak of the sample pore diameter is obvious, but the percentage of the total volume of the pore where the peak is located Not high, only about 16%, the aperture frequency at the right end of the peak value decreases in turn and tends to be stable to about 6%, which can be seen in the sorting process.
specific Embodiment 2
[0042] Specific embodiment 2: combine Figure 10 Isotherm adsorption curves of shale samples in the Sichuan Basin and Figure 11 Figure 10 As shown in the frequency histogram of the middle sample, the classification result of the D10 sample, that is, the mud shale sample in the Sichuan Basin, is W9 type, which is a well-sorted wedge-shaped small hole. From the pore frequency distribution diagram, we can see that the pores with 18-24nm pore size occupy the most of the total volume of the sample. It is judged that the sample is dominated by small pores; About 27%, the frequency on the right side of the peak is stable, about 5%, it can be seen that the sorting is very good.
[0043] The method disclosed in the present invention for judging the pore structure by classifying the isothermal adsorption curves of mud shale is to classify the isothermal adsorption curves of the bedrock standard samples of mud shale through the pore shape, pore size and pore throat sorting, that is, ...
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