(SR) 5. Geomechanics

The pillar stability factor is more than 0.7 in Smoky River as per Analysis of Retreat Mining Pillar Stability (ARMPS).

(SR) 5.1 Rock Propaties

The following strength properties are reported by Dr. C. Mark. However, on many occasions, he has quoted Dr. P. Cain's earlier publications on the strata surrounding the 5B-4 Mine.

Rock type

Test type

Strength (MPa)

Sandstone

Unconfined Compressive Strength

104.1 (Average)

Siltstone

Unconfined Compressive Strength (Lab.)

70.00 ~ 120.00

Grey Siltstone

Diametral Point Load Test

24.60

Grey Siltstone

Axial Point Load Test

103.00

Mudstone

Diametral Point Load Test

0.33

Mudstone

Axial Point Load Test

28.50

 

The following strength data (in MPa) are provided by the Smoky River Mine:

Rock type

Is(50) diametrical

Is(50) axial

Ax.:Dia. Ratio

UCS(Calc.)

UCS(test)

Carbonaceous Mudstone

0.19

-

-

32.97

-

Fissile Mudstone

0.05

-

-

-

37.72

Mudstone

0.77

1.78

2.31

27.94

-

Grey Mudstone with Siltstone

0.92

-

-

-

-

33% Silt

0.22

3.07

13.95

48.19

-

50% Silt

0.68

4.96

7.29

77.86

15.70

70% Silt

-

-

-

-

-

Grey Siltstone

1.23

5.13

4.17

80.53

-

Iron Nodule

2.57

-

-

-

-


(SR) 5.2 Roof Rating

The following rockmass classification ratings for Smoky River Coalfield are reported by Dr. C. Mark (unless otherwise notified) on the 5B-4 Mine:

Rock type

Classification type

Rating (Overall)

Weak Siltstone and thick Mudstone

CMRR

50 (Normal case), 40 (Fracture zone)

Siltstone and Mudstone*

RMR

35 (Roof)


(SR) 5.3 In Situ Stresses

The Smoky River area has clearly been subjected to intense horizontal tectonic pressures, as evidenced by the pervasive thrust faulting. In 1985, Jeremic reported that one underground observation at the #2 Mine had the maximum stress oriented approximately N35°E.

At present, there is little evidence of horizontal stress underground. Dr. C. Mark reports that in one location near the outcrop, a few large roof "pots" are indicative of a N30°E horizontal stress. It is possible that as mining progresses into the ridge towards deeper area, the horizontal stress may increase and rotate towards the regional stress orientation. The estimated in situ vertical stress is proportional to the cover depth and the horizontal stresses are 1/3 to 1 time of the vertical stress.