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316                                               Advanced Mine Ventilation

         handheld pump were used for this purpose, but now electrochemical cells have become
         available for this purpose. When NO, NO 2 , or even CO enter a special cell; they react
         with the electrolyte and create a light signal, “a photon.” A bank of photomultiplier
         tubes picks up the signal and translates it into specific gas concentrations. The preci-
         sion of such instruments is quite good at   1 ppm.
            Earlier instruments were bulky, such as Ecolysers [2], and were difficult to carry,
         but new instruments are light and can be handheld. An instrument named “Passport”
         can measure five gases in a single unit as listed below.
            CO (1e50 ppm)
            O 2 (1%e20%)
            CH 4 (1%e5%)
            NO (1e25 ppm) and
            NO 2 (1e5 ppm).
            It is strongly advised that for conclusive results, all gas samples must be analyzed in
         a laboratory by trained technicians using a GC.


         19.1.5   Radon

         Radon is a gaseous, chemically inert, radioactive product of the disintegration of
         radium. Found primarily in uranium mines, although present in trace amounts in
         several coal mines, radon diffuses from the rock strata into the mine environment,
         where the decay process continues. Table 19.2 gives the disintegration process for
         uranium-238 to become lead-206. Shown in this table is the type of radiation given
         off by each decay process and the half-life of each element in the series. The half-
         life of a radioactive substance is the time required for a given amount of that substance
         to lose one half of its radioactivity. The half-life of uranium-238 is approximately 4.5
         billion years; radium, 1622 years; and radon, 3.8 days.
            Once radon is released into the mine environment, the decay process continues
         with the formation of radium A, which decays to radium B, which produces radium
         C, and so forth. The products formed by the decay of radon are referred to as radon
         daughters. The radon daughter products are atoms of solid matter having relatively
         short half-lives. During the decay process, either alpha or beta particles are emitted.
         These emissions may also be accompanied by gamma ray activity. It is the short-
         lived alpha particles and potential alpha emitters such as radon and its daughters
         that are of prime concern to the ventilation engineer. Because it is a gas and has
         a relatively long half-life, inhaled radon is exhaled before large amounts of alpha
         particles are emitted. The daughter products, however, attach themselves to the
         dust that is present in the environment and when inhaled, tend to be deposited in
         the respiratory system. It has been estimated that when both radon and radon
         daughters are inhaled, only about 5% of the alpha radiation received is contributed
         by the radon [3].
            During radioactive decay, the individual members in the series are decaying and be-
         ing formed at the same time. At some point in time, equilibrium is reached, and the
         quantity of each member in the series remains constant. At this time, each member
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