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Blast vibration has long been associated with quarries, but separating
fact from fiction has often been a problem. Blasting is necessary
to break rock from the ground, prior to it being taken for processing.
In the early days of aggregate quarrying, explosives were not used
particularly scientifically although some attempts were made to
optimise use to minimise cost and maximise output. In most cases,
high explosives would be detonated instantaneously — either packed
into near vertical drill holes or occasionally into horizontal
tunnels running into the face from quarry floor level. The latter
could take six months to excavate and the blasting events were such big occasions that
the local populace would turn out to watch. They were also the subject
of reports in the national trade press. These methods would generate
both considerable ground vibration and air blast ('overpressure')
often perceived over a wide area. Indeed the residents on the higher
ground on the outskirts of Bath, often reported hearing blasts
from Emborough and Vobster, seven or eight miles away!
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For safety, environmental
and economic reasons blasting techniques have changed out of all
recognition over the last 30 years. Instead of instantaneous detonation,
explosives in each drill hole are initiated in a predetermined
sequence so that there are delays of a few milliseconds between
each activation. The shock waves generated not only direct much
more energy into breaking up the stone effectively (and less into
sound and air vibration), they create much lower levels of ground
vibration in the surrounding area. The explosives used are now
far safer to handle. Blocks which were initially too large to go
through the crusher used to be broken up by secondary blasting
which was particularly noisy and potentially very dangerous. This
is now done by 'drop balling' or using jib-mounted breakers.
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