Research Article

Occurrence Characteristics and Threshold Pore Throat Radius of Movable Fluids for Dolomite Intercrystalline Pores of Lacustrine Carbonate Rocks

Table 2

Variation of porosity component during NMR centrifugal process.

SamplePore typeCentrifugal force (MPa)NMR porosity component (%)
0.01 ms-0.1 ms0.1 ms-1 ms1 ms-10 ms10 ms-100 ms>100 ms

24Intercrystalline poreBefore centrifugation0.1791.0894.1910.8570.008
240.1440.1791.0893.7430.8330.008
240.2880.1711.0873.6510.6730.008
240.5760.1661.0553.5670.5290.007
241.440.1651.0543.4130.4600.007

Variation of porosity component0.0140.0350.7790.3970.001
26Intercrystalline poreBefore centrifugation0.0051.82511.4790.0000.000
260.1440.0011.72710.4070.0000.000
260.2880.0001.5509.8120.0000.000
260.5760.0001.4398.5380.0000.000
261.440.0001.4217.5040.0000.000

Variation of porosity component0.0050.4053.9750.0000.000
S12Intercrystalline dissolved poreBefore centrifugation0.2671.7394.3360.4770.061
S120.1440.2621.7382.2070.0620.034
S120.2880.2611.6551.4030.0840.034
S120.5760.2591.5891.0300.0800.032
S121.440.2561.5600.8930.0790.032

Variation of porosity component0.0110.1793.4430.3980.029
27Intercrystalline dissolved poreBefore centrifugation0.2442.4334.1021.3120.000
270.1440.2442.4073.1511.1830.000
270.2880.2392.3672.6260.2750.000
270.5760.2312.2902.2300.1410.000
271.440.2252.1391.0560.1010.000

Variation of porosity component0.0190.2953.0471.2110.000