CHAPTER V

THE STRUCTURE OF THE ATOM

Properties of Radium

A study of the properties of radium will aid in throwing light upon

the question as to the building up of the atom. First to be considered

are the usual properties which distinguish an elementary body.

Metallic radium has been prepared by a method similar to that used in

the preparation of barium. It is a pure white metal, melting at 700 deg.,

and far more volatile than barium. It rapidly alters on exposure to

the air, probably forming a nitride. It energetically decomposes water

and the product dissolves in the water. Its atomic weight is 226.

Radium forms a series of salts analogous in appearance and chemical

action to those of barium. In the course of time they become colored,

especially if mixed barium salts. The radiations from radium produce

marked chemical effects in a number of substances. Carbon dioxide is

changed into carbon, oxygen, and carbon monoxide, and the latter is

changed into carbon and oxygen. Ammonia is dissociated into nitrogen

and hydrogen; hydrochloric acid into chlorine and hydrogen. Oxygen is

condensed into ozone. In general, the action upon gases appears to be

similar to that of the silent electric discharge. Water is decomposed

into hydrogen and oxygen. If moist radium chloride or a salt of radium

containing water of crystallization is sealed in a glass tube, the

gradual accumulation of hydrogen and oxygen will burst the tube.

The radiations rapidly decompose organic matter with the evolution of

gases. Thus grease from stopcocks of apparatus used with radium or

paraffin will give off carbon dioxide. Under an intense alpha

radiation paraffin or vaseline become hard and infusible. White

phosphorus is changed into red.

The action upon living tissue is most noteworthy, as its possible use

as a remedial agent is dependent upon this. A small amount of a radium

salt enclosed in a glass tube will cause a serious burn on flesh

exposed to it. It therefore has to be handled with care and undue

exposure to the radiations must be avoided. Cancer sacs shrivel up and

practically disappear under its action. Whether the destruction of

whatever causes the cancer is complete is at least open to serious

doubt.

The coagulating effect upon globulin is interesting. When two

solutions of globulin from ox serum are taken and acetic acid added to

one while ammonia is added to the other, the opalescence in drops of

the former is rapidly diminished on exposure to radium, showing a more

complete solution, whereas the latter solution rapidly turns to a

jelly and becomes opaque, indicating a greatly decreased solubility.

Energy Evolved by Radium

The greater part of the tremendous energy evolved by radium is due to

the emission of the alpha particles, and in comparison the beta and

gamma rays together supply only a small fraction. This energy may be

measured as heat. It was first observed that a radium compound

maintained a temperature several degrees higher than that of the air

around it. The rate of heat production was later measured by means of

an ice calorimeter and also by noting the strength of the current

required to raise a comparison tube of barium salt to the same

temperature. Both methods showed that the heat produced was at the

rate of about 135 gram calories per hour. As the emission is

continuous, one gram of radium would therefore emit about 1,180,000

gram calories in the course of a year. At the end of 2000 years it

would still emit 590,000 gram calories per year. Such a production of

energy so far surpasses all experience that it becomes almost

inconceivable. It is futile to speak of it in terms of the heat

evolved by the combustion of hydrogen, which is the greatest that can

be produced by chemical means.

This effect is unaltered at low temperatures, as has been tested by

immersing a tube containing radium in liquid air. It should be stated

that these measurements were made after the radium had reached an

equilibrium with its products; that is, after waiting at least a month

after its preparation. The evolution of heat from radium and the

radio-active substances is, in a sense, a secondary effect, as it

measures the radiant energy transformed into heat energy by the

active matter itself and whatever surrounds it. Let us repeat,

therefore, that the total amount of energy pent up in a single atom of

radium almost passes our powers of conception.

Necessity for a Disintegration Theory

The facts gathered so far justify and necessitate a theory which shall

satisfactorily explain them, and since these phenomena are not caused

by nor subject to the influence of external agencies, they must refer

to changes taking place within the atom--in other words, a theory of

disintegration. In the main, these facts may be summed up as the

emission of certain radiations from known elemental matter: the

material alpha particles with positive charge, the beta particles or

negative electrons, and the gamma rays analogous to _X_ rays. The

emission of these rays results in the production of great heat. Then

there is the law of transformations by which whole series of new

elements are generated from the original element and maintain a

constant equilibrium of growth and decay in the series. Lastly, we

have the production of helium from the alpha particles.

Disintegration Theory

In explanation of these phenomena, Rutherford offered the hypothesis

that the atoms of certain elements were unstable and subject to

disintegration. The only elements definitely known to come under this

description are the two having atoms of the greatest known mass,

thorium (232) and uranium (238).

The atoms of uranium, for instance, are supposed to be not permanent

but unstable systems. According to the hypothesis, about 1 atom in

every 10^{18} becomes unstable each second and breaks up with a

violent explosion for so small a mass of matter. One, or possibly two

alpha particles are expelled with great velocity. This alpha particle

corresponds to an atom of helium with an atomic weight of 4, and its

loss reduces the original atomic weight to 234 with the formation of a

new element, having changed properties corresponding to the new atomic

weight. This new element is uranium X_{1}.

These new atoms are far more unstable than those of uranium, and the

decomposition proceeds at a new rate of 1 in 10^{7} per second. So at

a definite, measurable rate this stepwise disintegration proceeds. The

explosions are not in all cases equally violent in going from element

to element, nor are the results the same. Sometimes alpha particles

alone are expelled, sometimes beta, or two of them together, as alpha

and beta.

The new product may remain with the unchanged part of the original

matter. Thus there would be an accumulation of it until its own decay

balances its production, resulting eventually in a state of

equilibrium.

Constitution of the Atom

In order to explain the electrical and optical properties of matter,

the hypothesis was made that the atom consisted of positively and

negatively electrified particles. Later it was shown that negative

electrons exist in all kinds of matter. Various attempts were made to

work out a model of such an atom in which these particles were held in

equilibrium by electrical forces. The atom of Lord Kelvin consisted of

a uniform sphere of positive electrification throughout which a number

of negative electrons were distributed, and J. J. Thomson has

determined the properties of this type as to the number of particles,

their arrangement and stability.

Rutherford's Atom

According to Rutherford, the atom of uranium may be looked upon as

consisting of a central charge of positive electricity surrounded by a

number of concentric rings of negative electrons in rapid motion. The

positively charged centre is made up of a complicated system in

movement, consisting in part of charged helium and hydrogen atoms, and

practically the whole charge and mass of the atom is concentrated at

the centre. The central system of the atom is from some unknown cause

unstable, and one of the helium atoms escapes from the central mass as

an alpha particle.

There are, confessedly, difficulties connected with this conception of

the atom which need not, however, be discussed here. Much remains to

be learned as to the mechanics of the atom, and the hypothesis

outlined above will probably have to be materially altered as

knowledge grows. Perhaps it may have to be entirely abandoned in favor

of some more satisfactory solution. Until such time it at least

suffices as a mental picture around which the known facts group

themselves. In this picture energy and matter lose their old-time

distinctness of definition. Discrete subdivisions of energy are

recognized which may be called charged particles without losing their

significance. Some of these subdivisions charged in a certain way or

with neutralized charge exhibit the properties of so-called matter.

Scattering of Alpha Particles

This conception of the atom would doubtless fail of much support were

it not for certain experimental facts which lend great weight to it.

Certain suppositions can be based on this theory mathematically

reasoned out and tested by experiment. Predictions thus based on

mathematical reasoning and afterward confirmed by experiment give a

very convincing impression that truth lies at the bottom.

The first of these experimental proofs comes under the head of what is

known as the scattering of the alpha particles, a phenomenon which,

when first observed, proved hard to explain. If an alpha particle in

its escape from the parent atom should come within the influence of

the supposed outer electrical field of some other atom, it should be

deflected from its course and, the intensity of the two charges being

known, the angle of deflection could be calculated. For instance, if

it came to what might be called a head-on collision with the positive

central nucleus of another atom, it would recoil if it were itself of

lesser mass, or would propel the other forward if that were the

lighter.

The experiment is carried out by placing a thin metal foil over a

radio-active body, as radium _C_, which expels alpha particles with a

high velocity, and counting the number of alpha particles which are

scattered through an angle greater than 90 deg. and so recoil toward their

source. This has been done by a number of investigators and it has

been found that the angle of scattering and the number of recoil

particles depend upon the atomic weight of the metal used as foil. For

example, if gold is used, the number of recoil atoms is one in

something less than 8,000.

Taking the atomic weight of gold into consideration, Rutherford

calculated mathematically that this was about the number which should

be driven backward. But he went further and calculated also the number

which should be returned by aluminum, which has an atomic weight of

only about one-seventh that of gold. Two investigators determined

experimentally the number for aluminum and their results agreed with

Rutherford's calculations.

The metals from aluminum to gold have been examined in this way. The

number of recoil particles increases with the atomic weight of the

metal. Comparing experiment with theory, the central charge in an atom

corresponds to about one-half the atomic weight multiplied by the

charge on an electron, or, as it is expressed, 1/2 Ae.

There is only one lighter atom than helium, namely, hydrogen, which

has a mass only one-fourth as great. When alpha particles are

discharged into hydrogen, a few of the latter atoms are found to be

propelled to a distance four times as great as that reached by the

alpha particles.

Stopping Power of Substances

Parallel with the experiments mentioned, there is what is called

the stopping power of substances. This means the depth or thickness

of a substance necessary to put a stop to the course of the alpha

particles. This gives the range of the alpha particles in such

substances and is connected in a simple way with the atomic weight,

that is, it is again fixed by the mass of the opposing atom. This

stopping power of an atom for an alpha particle is approximately

proportional to the square root of its atomic weight.

Considering gases, for instance, if the range in hydrogen be 1,

then the range in oxygen, the atomic weight of which is 16, is only

(1/16)^{1/2} or 1/4. Generally in the case of metals the weight of

matter per unit area required to stop the alpha particle is found to

vary according to the square root of the atomic weight of the metal

taken.

A Brief Account of Radio-activity · 第 5 / 6 章