Research Article

Experimental Study on Seepage Anisotropy of a Hexagonal Columnar Jointed Rock Mass

Table 2

The fitting parameters of the Izabsh equation.

Sample numberMaximum principal stress σ1 (MPa)Fitting coefficient λFitting coefficient mCoefficient of determination R2

SS0°19.326 E + 130.850.9975
29.744 E + 130.890.9992
39.798 E + 130.920.9995
41.072 E + 140.890.9995
51.140 E + 140.820.9984
69.529 E + 130.840.9993

SS15°19.895 E + 130.800.9892
21.142 E + 140.790.9898
31.139 E + 140.770.9914
41.067 E + 140.780.9945
51.006 E + 140.750.9966
67.177 E + 130.770.9988

SS30°11.043 E + 140.810.9930
21.229 E + 140.780.9928
31.353 E + 140.760.9888
41.395 E + 140.690.9833
51.266 E + 140.680.9847
69.560 E + 130.710.9921

SS45°11.140 E + 140.780.9864
21.117 E + 140.820.9900
31.100 E + 140.750.9908
46.255 E + 130.850.9992
55.451 E + 130.870.9993
64.901 E + 130.860.9993

SS60°11.069 E + 140.780.9954
21.202 E + 140.860.9983
31.226 E + 140.890.9974
41.207 E + 140.870.9983
51.188 E + 140.800.9989
69.357 E + 130.830.9989

SS7515.369 E + 131.020.9863
26.519 E + 131.020.9944
37.757 E + 130.990.9950
49.339 E + 130.950.9919
51.100 E + 140.960.9959
61.496 E + 140.930.9928
SS90°15.618 E + 131.000.9903
28.247 E + 130.910.9978
39.540 E + 130.930.9982
49.515 E + 130.980.9977
51.364 E + 140.830.9857
61.497 E + 140.830.9877