Stability Graph Method#
The Stability Graph Method was developed by Mathews et al. (1980) [1] as a modification of the Q rock mass classification system by Barton (1974) [2]. It provides an empirical approach for assessing stope wall stability in underground mining.
The method relates a Stability Number \(N'\) to the Hydraulic Radius of a stope wall through stability charts. The stability number is defined as:
where:
\(A\) (Factor A) is a stress factor
\(B\) (Factor B) is a rock defect orientation factor
\(C\) (Factor C) is a design surface orientation factor
\(Q'\) is a modified NGI rock mass parameter:
Here, \(RQD\), \(J_n\), \(J_r\), \(J_a\), and \(J_w\) are terms from Barton’s classification, with the stress reduction factor (SRF) omitted to better represent conditions in open stopes.
Factor A (Stress Factor) Accounts for the ratio of intact rock strength to induced stress at the stope surface. - Intact strength is typically measured by the uniaxial compressive strength (UCS). - Induced stress corresponds to the maximum tangential stress acting parallel to the stope wall. This factor is estimated either through numerical modelling or from empirical charts (Mathews et al., 1981).
Application The method distinguishes between three primary stability domains: 1. Stress-controlled failure 2. Structurally controlled failure 3. Combined stress and structural failure
These zones are separated by transition areas and are defined using case histories from mining operations.