Encyclopedia of Environmental Science and Engineering, Volume I and II

(Ben Green) #1

INSTRUMENTATION: WATER AND WASTEWATER ANALYSIS 583


are illustrated. A single arm electrolytic cell is also avail-
able.^105 Unstable reagents, namely, bromine, dipositive silver,
titanium(III), chlorine, etc., can be conveniently generated and
utilized in this technique. In Table 11 a number of applications
are listed. The ability to utilize these unstable reagents expands
the horizon of tritrimetry and analytical methodology.

(3) Measurement of radioactivity 106 – 8
a. Introduction
Radioactive species in water and wastewater samples
arise from natural and anthropogenic sources. The radiation
emitted from radioisotopes is deleterious to all life forms
and has led to the development of a number of radiochemi-
cal methods. Standard Methods^2 includes procedures for
the detection of tritium, radium, and radioactive species of
cesium, iodine, strontium, and uranium, as well as, the gen-
eral measurement of the amount of ionizing radiation.
Several kinds of ionizing radiation emanate from
radioisotopes. They include gamma and x-rays, beta rays
(electrons and positrons), and alpha rays (helium nuclei).
Ionizing radiation, when penetrating matter, causes the
formation of ions that are dangerous to life forms leading
to cancer in people and animals. Gamma and x-rays are at
the high frequency ( 10 6 Hz) end of the electromagnetic
spectrum. The former arise from decay events occurring in
the nucleus and are more energetic higher frequency than

x-rays that arise from rearrangement of electrons surround-
ing the decaying nucleus. Both kinds of radiation are highly
penetrating due to their high energy, and therefore are quite
dangerous. Gamma and x-rays are emitted as continuous
spectra.
Beta particles are of two types; negatively charged
electrons or negatrons and positively charged positrons.
They arise from decay processes in nuclei. A positron has a
very short life time and is annihilated on collision with an
electron to form two gamma photons. Beta particles have
a greater penetrating ability than alpha particles and are
poorer at ionizing matter. Since beta particles are scattered
in air, their range is difficult to assess. Beta particles, emit-
ted during nuclear decay, yield a continuous spectrum of
particle energies.
Alpha particles are the nuclei of helium atoms and have
a positive charge of two. They are the product of the decay of
natural isotopes, such as uranium, radium, and others. Alpha
particles have high energies and, therefore, high ionizing
power. Their penetrability, however, is low, about 5–7 cm in
air. Alpha particles emitted from radioisotopes do not yield
continuous spectra. The particles are monoenergetic or have
a group of several discrete energies.

b. Instrumentation
Ionizing radiation interacting or colliding with matter
causes the production of charged particles or energetic spe-
cies; measurement of these entities is the basis of radiation
detectors. Two phenomena are utilized in detecting ionizing
radiation: namely, ionization of gases and solids to yield an
ion current pulse and the excitation of crystals to provide a
luminescence pulse. The ionization of gases is used in ion-
ization chambers, proportional counters, and GM (Geiger
Muller) tubes. Semiconductor radiation devices produce
electron–hole pairs on the impingement of ionizing radia-
tion. Crystal and liquid scintillation detectors are employed
for insoluble and soluble samples, respectively. An instru-
ment for radiation measurement consists of several modules:
namely, the detector responding to the radiation, circuits that
count pulses, and pulse height analysis circuits that discrimi-
nate between the energies of the pulses.
The nature of the pulse must be understood. In a number
of detectors the pulse height of the radiation event is pro-
portional to the energy of the particle or radiation and inde-
pendent of the applied potential, whereas in other detectors
the pulse height is independent of energy. The pulse of pho-
toelectrons or luminescence has a pulse width due to the
random nature of the collision process. This fact leads to
small statistical differences in the pulse heights for a series
of radiation events with the same energy. The smaller the
pulse width the greater the resolution of the detector.
Radiation detectors operate under two modes, pulse and
mean level. Of interest here is the pulse type that detects the
interaction of radiation with the detector as a unique event.
These pulses are counted and measured in counts per unit
time, usually, counts per minute, cpm. The type of radiation
(beta, gamma, etc.), the frequency or wavelength and the
intensity of the radiation can also be determined.

ANODE
DELIVERY
TIP

CATHODE
DELIVERY
TIP

GLASS WOOL

TO GENERATOR
ELECTROLYTE SUPPLY
RESERVOIR

PL ELECTRODES
(SPIRALLY WOUND)









FIGURE 37 Generator cell for external production of
titrants for coulometric titrantions. (Adapted with per-
mission for reference 104. Copyright 1931 American
Chemical Society.) For example in acid/base titrimetry: (a)
generation of OH at the cathode: 2H 2 O  2e → H 2 
2OH (b) generation of H at the anode: H 2 O → 1/2O 2 
2H  2e.

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