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Rock Mechanics.pdf - Mining and Blasting

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BACKFILL PROPERTIES AND PLACEMENT<br />

Table 14.1 Size analyses of s<strong>and</strong>fills prepared from mill tailings (from Thomas et al. 1979).<br />

Size<br />

fraction<br />

(m) Weight %<br />

Mine 1 Mine 2 Mine 3 Mine 7 Mine 8 Mine 9<br />

+3340 0.0 0.00 0.0 0.00 0.07 0.00<br />

2360–3340 0.0 0.00 0.0 0.00 1.09 0.00<br />

1180–2360 0.0 0.00 0.0 0.00 9.01 0.00<br />

850–1180 0.0 0.00 0.0 0.00 8.16 0.13<br />

600–850 0.0 0.00 0.0 0.00 11.00 1.39<br />

425–600 0.7 0.05 0.0 0.20 8.28 6.02<br />

300–425 2.5 0.21 0.0 0.59 6.44 12.86<br />

212–300 8.3 1.62 0.8 3.16 6.37 19.73<br />

150–212 15.7 2.33 3.2 8.69 7.08 18.88<br />

106–150 17.1 11.08 17.2 22.50 5.71 18.33<br />

75–106 20.9 11.67 22.8 17.30 4.79 10.04<br />

53–75 11.0 20.52 13.2 17.53 3.57 4.90<br />

40–53 7.5 9.32 14.9 6.78 1.17 4.04<br />

30–40 7.1 14.25 14.9 15.93 3.36 1.09<br />

20–30 2.4 15.72 8.0 5.14 4.04 0.69<br />

15–20 1.4 7.91 2.2 1.11 4.39 0.43<br />

10–15 0.8 1.32 0.6 0.30 2.88 0.23<br />

–10 4.8 4.01 2.2 0.79 12.60 1.25<br />

silt <strong>and</strong> fine s<strong>and</strong>. On average, the proportion of – 10 m material is less than 4%, so<br />

that, by inference, the clay-size fraction is very low. Natural s<strong>and</strong>s which have been<br />

used or considered for use as mine backfill are generally coarser than artificial s<strong>and</strong>s.<br />

Particle sizes are concentrated in the range 150–600 m, corresponding to a medium<br />

s<strong>and</strong>.<br />

The permeability of a fill mass determines the drainage condition it experiences<br />

internally under imposed surface load. Investigations by McNay <strong>and</strong> Corson (1975)<br />

indicate that successful s<strong>and</strong>fills have a permeability coefficient in the range 7 × 10 −8 –<br />

7.8 × 10 −5 ms −1 . These values correspond to soil gradings of medium slit to coarse<br />

s<strong>and</strong>, which are consistent with the classifications defined by the particle size data.<br />

Common mining practice is to specify fill drainage properties in terms of percolation<br />

rate, using a st<strong>and</strong>ard percolation tube test. The percolation rate (measured in<br />

mm h −1 ) is essentially equivalent to the permeability of the fill as measured under<br />

a gravity gradient close to unity. Mitchell (1983) proposes that the percolation rate<br />

(P) of fill in situ may be estimated from percolation tube test results <strong>and</strong> in situ <strong>and</strong><br />

measured void ratios of fill using the relation<br />

Pcorrected = Pmeasured(ein situ/emeasured) 2<br />

(14.1)<br />

A percolation rate of 25 mm hr −1 (equivalent to a permeability coefficient of 7 ×<br />

10 −6 ms −1 ) is recommended to provide a free-draining fill, <strong>and</strong> to ensure that placed<br />

fill will be free of ponded surface water a couple of shifts after placement.<br />

At the base of a stope, where the water flow is choked through the filled drawpoint<br />

<strong>and</strong> bulkhead, the permeability Pd of the fill must be higher than in the fill mass in<br />

411

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