Isotopes

Atoms of the same element, that is, atoms with the same number of

protons and electrons, may vary slightly in mass because of having

different numbers of neutrons. Since the chemical behavior of an element

depends upon its electrons’ electrical charges, extra neutrons (which do

not have an electrical charge) may affect the mass of an atom without

disturbing its chemical properties. Atoms having the same atomic number

but different atomic weights are called isotopes. For example, as shown

in Figure 8, the isotope ¹H, or ordinary hydrogen, consists of a nucleus

containing a proton (charge: +1; mass: 1) around which revolves an

electron (charge: -1; mass: negligible); ²H, known as deuterium,

contains an additional nuclear particle, a neutron (charge: 0; mass: 1);

³H, or tritium, contains two neutrons. Since the chemical behavior of an

element depends upon the number of its electrons, these three atoms,

although differing in weight, behave identically in chemical reactions.

For convenience, the atomic weight is written as a superscript to the

left of the element’s symbol. For instance ¹⁴C is the isotope of carbon

with an atomic weight of 14 (ordinary carbon is the isotope with an

atomic weight of 12, and it is written ¹²C).

[Illustration: Figure 8 _Isotopes of hydrogen._]

Hydrogen (¹H)

Deuterium (²H)

Tritium (³H)

Practically all elements have more than one isotope. There are two

general classes of isotopes, stable and radioactive. Stable isotopes

have no distinguishing characteristic other than their mass; radioactive

isotopes not only differ from their brothers in mass but also are

characterized by unstable nuclei. When the nucleus of an atom is

unstable, because of an unbalanced number of protons and neutrons, a

redistribution occurs sooner or later, and the atom decomposes

spontaneously and emits one of several kinds of radiations. Because of

their common mode of action and effects on living organisms, these

different kinds of radiations are known collectively as ionizing

radiations.

All radioactive elements emit one or more of three types of penetrating

(ionizing) rays. _Alpha rays_ or particles are double-charged helium

nuclei, ⁴He (atomic number: 2; mass: 4). They are emitted by many heavy

radioactive elements, such as radium, uranium, and plutonium. _Beta

rays_ or particles can be either positive or negative. Negative beta

particles are high-speed electrons and are emitted by many radioactive

elements. Positive beta particles are positively charged electrons

(positrons), have only a transitory existence, and are less common.

_Gamma rays_ are electromagnetic radiations, a term that also describes

radiowaves, infrared rays, visible light, ultraviolet light, and X rays.

Gamma rays are usually emitted after the emission of alpha or beta

particles. In our studies of life processes, we are interested only in

the radioactive isotopes that emit gamma rays or beta particles.

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