Sper Scientific 840026 Radiation Detection Meter User Manual

Page 10

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given off from natural radioactive minerals in the earth's

crust is a major constituent of background radiation. For the

most part, it is quite low, due to the long time required for

the remaining radioisotopes to decay. In atomic reactions

(either natural or forced by man) the decay process is sped

up by the effect of neutrons given off in the fission process

interacting with more unstable isotopes to cause immediate

decay. While this allows the energy of the isotope to be

harvested in a conveniently short time, the unstable decay

products produced generally have short half-lives, on the

order of seconds to centuries, and are very radioactive. As

a result of this process, considerable larger quantities of

short half-life (high decay rate) isotopes become a part of

the world we live in. This is the basis for the controversy

and concerns on the subject of nuclear power generation,

waste disposal, and nuclear weapons.

INTERACTION OF RADIATION WITH MATTER

The particles and photons that result from nuclear decay

carry most of the energy released from the original unsta-

ble nucleus. The value of this energy is expressed in elec-

tron Volts, or eV. The energy of beta and alpha rays is in-

vested in the particles' speed. A typical beta particle from

Cesium-137 has an energy of about 500,000 eV, and a

speed that approaches that of light. Beta energies can

cover a wide range, and many radioisotopes are known to

emit betas at energies in excess of 10 million eV. The

penetration range of typical beta particles is only a few mil-

limeters in human skin.

Alpha particles have even shorter penetration ranges than

beta particles. Typical alpha energies are on the order of 5

million eV, with ranges so short that they are extremely dif-

ficult to measure. Alphas are stopped by a ~nin sheet of

paper, and in air only travel a few inches at most before

coming to a stop. Therefore, alpha particles cannot be de-

tected without being in close contact with the source, and

even then only the alphas coming from the surface of the

source can be detected. Alphas generated within the

source are absorbed before reaching the surface. Due to

short range, alpha particles are not a serious health hazard

unless they are emitted from within the body when their

high energy, in close contact with sensitive living tissue, is

an extreme hazard. Fortunately, almost all alpha-emitting

substances also emit gamma rays, allowing for their detec-

tion.

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