Every term you will meet on a monitoring job, explained in one sentence first. Tap a term anywhere on the site to see it.
How the ground moves
Pure tone
Ground moving back and forth in one smooth, steady rhythm.
Picture itA child on a swing: same height each time, same time for each swing, over and over.
PreciselyA single sine wave with one frequency and one amplitude. Real blast vibration is many tones at once; the pure tone is the building block we use to explain them.
On siteThe concept pages and the vibration calculator use a pure tone so the numbers can be checked by hand.
Picture itIf displacement is where the ground is, velocity is how fast that is changing, and acceleration is how fast the speed is changing. Same motion, three views.
PreciselyThe instantaneous rate of change of a quantity with respect to time. Velocity is the derivative of displacement; acceleration is the derivative of velocity.
On siteThe platform converts between g and mm/s using this relationship at a given frequency.
Far enough from the blast that the shaking is small and smooth.
Picture itStanding across the road from a concert rather than beside the speakers.
PreciselyDistances at which vibration is low-frequency, low-amplitude and dominated by surface waves, as opposed to the near field close to the charge.
On siteNeighbour monitoring is far-field. Near-field records need a wider range.
Picture itGravel versus boulders from the same bench.
PreciselyThe size distribution of the broken rock, estimated from powder factor, rock type and pattern (Kuz-Ram), and reported as a mean size and the size 80 % passes.
On siteFiner costs more explosive; coarser costs more at the crusher.
PreciselyRock projected from the face or the collar, with a range that grows with charge per metre and shrinks with burden and stemming; exclusion zones are set as multiples of it.
On siteShort stemming and thin burden are the usual causes.