
The Basics of Blasting Vibrations and Noise
Highway construction projects; placement
of sewer, water, gas and electrical services; residential and commercial
building projects; and mining frequently require the use of explosives.
In these applications, rock must be broken loose from the ground
and blasting is the only practical way to accomplish this task.
Unfortunately, the public has many misconceptions about the use
of explosives.
Blasting agents, a type of explosives, are preferred
in most situations because they are economical and safe. ANFO, a
mixture of fuel oil and ammonium nitrate (the same compound as commercially-available
fertilizer), is the blasting agent most commonly used. Dynamite
is seldom used today, and similar high-energy explosives are needed
only in small quantities.
Explosives manufacturers have done extensive
research on ways to improve their products, with the most important
goals being enhanced safety and efficiency. As a result, it now
takes only about 8 ounces of explosives to break loose a ton of
rock (an impressive 4,000 to 1 ratio).
The first step in using explosives to break
rock is drilling a series of holes, usually 3-6 inches in diameter,
in which to place the blasting agent. Careful planning goes into
determining a precise pattern for these holes since this is a major
factor in achieving desirable results. Before a blasting agent is
placed in a hole, it is preceded by a small booster charge.
A booster provides just enough energy to detonate
the blasting agent. Boosters in each hole are detonated individually
by blasting caps that have built-in time delays. Using delays just
thousands of a second apart is enough to greatly disperse the energy
released by the total amount of explosives involved. To an observer,
a blast seems to happen instantaneously. What actually takes place,
however, is a rapid progression of smaller explosions.
More than 90 percent of a blasts energy
is consumed as it fractures the rock. This efficiency is achieved
by adjusting the amount of explosives detonated per delay interval,
which is also important in minimizing ground vibration. Its
possible to have a 100-hole blast, for example, create the same
ground vibration as a 50-hole blast, even though theres twice
as much explosives involved in the 100-hole blast.
Only the remaining energy not used up
as it breaks rock is capable of causing ground vibration.
Ground vibration caused by any source rapidly decreases as the distance
from the source increases. Advance planning of the amount of explosives
used and the time delays employed is remarkably effective in controlling
the amount of vibration that will occur from a blast. However, quarries
and other users of explosives often use seismographs that measure
ground vibration to verify their predictions. These sensitive instruments
are placed on the surface of the ground, where the most intense
vibration from blasting occurs.
Studies by government agencies, universities
and engineering firms have investigated the effects of ground vibrations
on residential structures. Criteria derived from these studies are
an invaluable reference tool. Companies using explosives in populated
areas typically establish a self-imposed margin of safety to insure
that vibrations are well below intensities that create slight cosmetic
damage to even the weakest type of structure.
Research has shown that the first evidence of
damage to a structure from vibration is hairline cracks in plaster.
This component of a homes construction is brittle and has
the lowest structural strength. Drywall and sheetrock would be next,
followed by brick and mortar. Poured concrete is the strongest of
allit can withstand high vibration levels with no effects.
Blast vibrations intense enough to crack a homes foundation
or patio would cause profound effects on other components.
It was pointed out earlier that blast vibrations
are the most intense on the earths surface. Therefore, underground
objects such as wells, pipelines, swimming pools and septic tanks
are subjected to less vibration than objects sitting on top of the
ground. When explosives are detonated, vibrations measured 150 feet
below the surface, for example, are typically 15 percent of the
intensity at ground level. Its a common misconception that
well casings, because they are underground, are easily damaged by
blasting vibrations, but overwhelming research and field evidence
has proven that there is no justification for this concern. It is
possible for people with shallow wells to notice a slight, temporary
increase in water turbidity after a blast. This is caused by fine
sediment becoming dislodged from around the well casing, which may
occur a low vibration levels.
Research has also shown that the denser a material
is (rock compared to soil, for example), the less efficient it is
at transmitting vibrations. A homeowner with a foundation embedded
in the same shelf of rock being mined as a nearby quarry operation
has no reason to be concerned that the home will experience more
vibration than other homes with foundations in soil that are the
same distance from the blasting.
Airblast is a term commonly used
to describe excess energy that is released into the atmosphere as
a result of explosives detonation. A more correct term for it is
overpressure. Although this pressure change traveling
through the air transmits noise from a detonation, most of the energy
is below the frequency range of human hearing. The lower frequency
air pressure may cause windows to rattle, which is noise caused
by the glass shifting in a slightly loose window frame.
Natural phenomena that influences overpressure
are wind and variations in temperature at different heights in the
atmosphere. Therefore, the effects of overpressure may be less or
more noticeable in different days. Although overpressure is often
what causes people to be aware of the use of explosives at a quarry
or construction project, it has virtually no likelihood of damaging
a structure (including windows).
Overpressure from a detonation, by the way,
is transmitted through the air about 10 times slower than vibration
is transmitted through the ground. Although traveling faster, ground
vibration dissipates more rapidly than overpressure. This means
people can often hear a detonation at greater distances than they
can detect ground vibration from it.
Even when blasting practices are followed that
produce effects far below that which may cause structural damage,
it is still possible for a detonation to be noticed by people some
distance away. The reasons for this are that: (1) Vibration is perceptible
to humans at surprisingly low levels and (2) Air pressure changes,
such as overpressure, are dissipated relatively slowly. The noise
of a blast, rattling windows or a slight vibration may startle some
people, but it is extremely rare that any type of damage is occurring.
It is possible for a houses structural
components, or some of the items it contains, to harmlessly resonate
at nearly the same vibration frequency that is caused by blasting.
This may cause slightly more noticeable effects, such as rattling
dishes. Since the duration is so short, it does not damage the structure
or anything within it. Granted, it is conceivable that a precariously
balanced dish on a wall shelf may fall in such a circumstance. However,
it is more likely to be dislodged by other activities in the home.
People are usually surprised to learn that slamming
doors, truck traffic, children running and hammering nails produce
much greater vibration effects in a home than those produced by
the nearby use of explosives. These activities do not cause as much
concern as blasting because they are expected and routine.
Environmental forces also contribute a surprising
amount of stress to a home. These forces include soil settling,
wetting/drying of soil (causing expansion and contraction around
the foundation), humidity, temperature changes and wind. The Effects
of Vibrations and Environmental Forces: A Guide for the Investigation
of Structures states that environmental strains might be 50 to 100
times greater than the level of blasting vibration that is noticed
by humans. Sooner or later, every home will show the effects of
natural elements. Common effects are cracked plaster and concrete,
which homeowners sometimes mistakenly attribute to blasting.
Explosives must be used to provide some of the
products that are necessary for our society. The crushed stone industry,
for example, must use explosives as the first step in the production
of construction aggregates. These aggregates are needed for every
residential, commercial and infrastructure project. While using
explosives, its always a high priority for our industry to
take whatever precautions are necessary to protect the publics
safety and property.
Note: This information is based in part on interviews
with Rodger Bayer, Vibra-Tech Engineers, Inc., Florissant, Mo.,
and Randall Wheeler, White Industrial Seismology, Inc., Joplin,
Mo. Both have extensive knowledge of blast vibration analysis and
many years of experience in this field working for a variety of
clients. Another source used is The Effects of Vibrations and Environmental
Forces: A Guide for Investigation of Structures by Lewis Oriard
(International Society of Explosives Engineers, 1999)
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Missouri Limestone Producers Association
P.O. Box 1725
Jefferson City, MO 65102
Phone: 573-635-0208
Fax: 573-634-8006
Steve Rudloff
Executive Manager
steve@molimestone.com

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