Table 4 Differential response of rock permeability performance.

From: Investigation of change coal seam floor permeability based on pressurized water testing

 

P-Q curve type

Absolute change in permeability(\(\:{q}_{\text{P}5}-{q}_{\text{P}1}\))

(Lu)

k

\(\:{k}_{\text{Y}1}/{k}_{\text{Y}2}\)

(Calculation result after removing * data)

Y1

Y2

Y1

Y2

Y1

Y2

Carbonaceous mudstone

A

-

1.43

-

86.72%

-

-

A

-

1.04

-

90.53%

-

Bauxite mudstone

A

D

0.47

16.85

94.55%

11.32%

−29.59

(8.52)

A

D

0.17

17.25

98.16%

−17.83%*

Fine sandstone

D

E

0.33

0.00

96.35%

100.00%

1.20

A

D

−1.11

0.00

113.45%

100.00%

D

A

−0.88

0.15

112.31%

98.09%

C-E

E

1.34

0.00

85.79%

100.00%

C-E

D

−0.46

3.04

111.92%

48.21%

-

E

-

1.08

-

73.07%

Benxi limestone

C

B-D

0.19

2.75

88.34%

20.06%

4.92

(1.27)

E

A

−5.64

−0.11

594.74%*

118.64%

Coal No.10

A

B-E

−0.39

0.00

105.34%

100.00%

1.05

Bauxite rock

A

D

0.08

3.61

99.06%

38.01%

2.09

D

D

−0.29

2.77

103.70%

55.82%

D

D

0.00

3.48

100.00%

39.70%

D

D

−0.24

3.67

104.71%

60.37%

D

-

0.00

-

100.00%

 

Ordovician limestone

D

D

0.00

8.88

100.00%

4.37%

4.59

D

D

0.00

8.35

100.00%

5.86%

D

D

0.00

6.04

100.00%

33.84%

D

D

0.00

5.85

100.00%

43.04%