Measuring method of liquid full pressure gradient-flow relation in low-permeability reservoir
A technology of pressure gradient and measurement method, which is used in measurement devices, permeability/surface area analysis, suspension and porous material analysis, etc. Measure core starting pressure and other issues to achieve accurate measurement and accurate flow characteristics
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Embodiment 1
[0065] A method for accurately measuring the total pressure gradient-flow relationship of a low-permeability rock core, comprising the following steps and results as follows:
[0066] A rock core (diameter 25mm, length 80mm) with a permeability of 20 millidarcy is measured with a static method measuring device, and the starting pressure gradient is measured to be 0.006MPa / m with salinity water;
[0067] The rock core is measured by the steady-state method to obtain the pressure gradient-flow data of water, and the measured starting pressure gradient is 0.05MPa / m.
[0068] Combining the starting pressure gradient data obtained by the static method and the relationship between the pressure gradient and the flow rate obtained by the steady state method, the Figure 5 , that is, the pressure gradient-flow relationship of the salinity water flowing in the low-permeability core under the full pressure gradient is obtained.
Embodiment 2
[0070] A rock core (diameter 25mm, length 60mm) with a permeability of 0.611 millidarcy is measured with a static method measuring device, and the starting pressure gradient is measured to be 0.05MPa / m with salinity water;
[0071] The rock core is measured by the steady-state method to obtain the pressure gradient-flow data of water, and the measured starting pressure gradient is 0.40MPa / m.
[0072] Combining the starting pressure gradient data obtained by the static method and the relationship between the pressure gradient and the flow rate obtained by the steady state method, the Image 6 , that is, the pressure gradient-flow relationship of the salinity water flowing in the low-permeability core under the full pressure gradient is obtained.
Embodiment 3
[0074] A rock core (diameter 25mm, length 60mm) with a permeability of 0.611 mD is measured with a static method, and the starting pressure gradient is 0.09MPa / m measured with silicone oil;
[0075] The rock core is measured by the steady-state method to obtain the pressure gradient-flow data of the oil, and the measured starting pressure gradient is 1.35MPa / m.
[0076] Combining the starting pressure gradient data obtained by the static method and the relationship between the pressure gradient and the flow rate obtained by the steady state method, the Figure 7 , that is, the pressure gradient-flow relationship of the salinity water flowing in the low-permeability core under the full pressure gradient is obtained.
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