A method for predicting forced self-absorption in shale reservoirs
A technology of shale reservoir and prediction method, which is applied to measurement devices, soil material testing, instruments, etc., can solve the problems of forced external force and calculation result error without considering the sliding effect of fracturing fluid in capillary shape.
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[0342] The experimental rock samples and fluid basic parameters used for self-priming calculation are shown in Table 1:
[0343] Table 1 Basic parameters of rock samples and test fluids
[0344]
[0345] (1) Comparison of self-priming length
[0346] Such as figure 1As shown, among the two types of pores, organic pores and inorganic (clay) mineral pores, the self-absorption length of clay pores is the largest. That is, at the same time, the water self-imbibition invades the deepest clay pores; judging from different self-imbibition depths, the self-imbibition process of shale rocks is not piston displacement, but non-uniform advancement. This is mainly due to the fact that the self-priming force of clay pores is not only affected by forced self-priming force and capillary force, but also by osmotic pressure; at the same time, the wettability of organic pores is poor, and capillary force is small; The difference in pore morphology is also part of the reason.
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