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Improved understanding of sublevel blasting Determination of the extent of the compacted zone, its properties and the effects on caving Nikolaos Petropoulos May 16, 2018

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Improved understanding of sublevel blasting

Determination of the extent of the compacted zone, its properties and the effects on caving

Nikolaos Petropoulos

May 16, 2018

Background

2

Underground Blasting

in SLC

Background

2

Confining

material

Burden

Background

2

Confining

material

Background

2

Blast direction

Confining

material

Small-scale blast

tests

Laboratory impact

tests

Background

2

Confining

material

Pillar tests &

Full-scale tests

Aims

•To study the interaction between the confining

material and the burden

•How the properties of the materials change during

blasting

3

Small-scale blast tests

4

Used Instrumentation:

• Accelerometers

• Draw wire

• Custom-made incremental displacement sensor

Laboratory impact tests

5

Pillar tests

6

Full-scale tests (On-going work)

7

TDR cables

Live systems (accelerometers)

Draw wire

Inspection/back up holes

✓ ✓

Level 1022 block 26

Results

The results are based on:

•8 small scale blast tests

•43 impact tests

•2 pillar tests

•2 full-scale tests (yet to be analyzed, blasted 9th of May)

8

Results-Impact tests

9

𝐷𝑖𝑠𝑝𝑙𝑎𝑐𝑒𝑚𝑒𝑛𝑡 = 𝑒𝑎+𝑏∙𝑑𝑖𝑠𝑡𝑎𝑛𝑐𝑒 𝑓𝑟𝑜𝑚 𝑏𝑢𝑟𝑑𝑒𝑛

Wet

Dry

Results – Pillar tests

10

Fine

Coarse

𝐷𝑖𝑠𝑝𝑙𝑎𝑐𝑒𝑚𝑒𝑛𝑡 = 𝑒𝑎+𝑏∙𝑑𝑖𝑠𝑡𝑎𝑛𝑐𝑒 𝑓𝑟𝑜𝑚 𝑏𝑢𝑟𝑑𝑒𝑛

Results – Small scale blast & Pillar tests

Burden movement

Blasting action

Burden movement

Confining material reaction

Results – Full-scale tests (preliminary results)

12

Pulling velocity ≈ 80 m/sTrue time 55 ms

Conclusions

Confining material behavior

• Particle-to-particle interactions

• Elasto-plastic behavior of the particles without breakage

• Over-compaction when water and fine particles are present

• Tensile strength is introduced

• An inverse exponential function can describe the extent of the compaction zone

Burden behavior

• Limited movement

• Burden seems intact even if the fracture network was developed

• Backward burden movement due to relaxation forces from the confining material

• Burden erosion material appears in the gap between the blasted and intact rock13

Acknowledgements

Supervisors: Assoc. Prof. Daniel Johansson &

Prof. Erling Nordlund

Financial Support

Thank you very much!