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+*** START OF THE PROJECT GUTENBERG EBOOK 75392 ***
+
+
+
+
+
+Transcriber’s Note: Italics are enclosed in paired _underscores_;
+subscripts are indicated by a single underscore: H_2O. Superscripts are
+indicated by a caret symbol: 10^9. When a superscript is longer than
+one character, it is enclosed in curly braces: 10^{-11}. Additional
+notes will be found near the end of this ebook.
+
+
+
+
+ LITTLE BLUE BOOK NO. 1000
+ Edited by E. Haldeman-Julius
+
+
+ The Wonders
+ of Radium
+
+ Maynard Shipley
+
+
+ HALDEMAN-JULIUS COMPANY
+ GIRARD, KANSAS
+
+
+
+
+ Copyright, 1926,
+ Haldeman-Julius Company
+
+
+ PRINTED IN THE UNITED STATES OF AMERICA
+
+
+
+
+THE WONDERS OF RADIUM
+
+
+
+
+CONTENTS
+
+
+ Page
+ I. Introductory 5
+ All Matter Radioactive 9
+
+ II. Everyday Uses of Radium 16
+ Radium Makes Gems Blush 18
+ A Radium Clock 19
+
+ III. Radium and the Age of the Earth 21
+
+ IV. An Epoch-Making Discovery 30
+ How Radium is Converted to Lead 34
+
+ V. Radium in the Treatment of Cancer 45
+
+ VI. Efficiency of Radium in Treatment of Various Diseases 51
+
+ VII. Where We Get Radium 55
+ New Sources of Radium 58
+ The Radioactive Disintegration Series 60
+ Uranium I Series 63
+ Uranium Y Series 63
+ Thorium Series 64
+
+
+
+
+THE WONDERS OF RADIUM
+
+
+
+
+CHAPTER I
+
+INTRODUCTORY
+
+
+It has been well said that a general idea of what radioactivity
+signifies is a necessary part of the education of every intelligent
+person, since “it is the one thing of paramount importance in the
+chemical and physical science of the day.” But its importance extends
+much farther, since radioactivity is now employed in many departments
+of industry, as well as in biology and medicine.
+
+It is known that the rays from radium have the power to stimulate
+all forms of life, even to the extent of speeding up the growth of
+plants and of making dormant plants burst into bud. Some authorities,
+as we shall see later, are fully convinced that the radiations can
+be employed successfully in the prolongation of human life. It is
+well known that radiotherapy has, for some years now, been employed
+advantageously in the treatment of many forms of illness, and is, in
+some institutions, the sole medium for the cure or alleviation of
+cancer and other malignant growths.
+
+Not long ago the discovery was made that the curative agent in certain
+famous baths in Europe is the radium which the waters of their springs
+contain.
+
+If one could really buy bottled water which has been properly treated
+with radium rays or the “emanation,” beneficial results would no doubt
+be obtained. The trouble is that such waters are difficult to secure.
+
+“None of the foreign or domestic commercial bottled water sold
+to consumers on the claim of radioactive content really contains
+sufficient radioactivity to warrant its purchase,” according to the
+report of investigation completed by the water and beverage laboratory
+of the United States Department of Agriculture, Washington, D. C.
+
+“In the examination of 46 samples from 15 states and eight foreign
+countries, the bureau found the highest quantity of radioactivity of a
+temporary nature in a bottled water from Massachusetts.
+
+“The largest amount of permanent radioactivity was in a sample from a
+deep well in Ohio. It was found, however, that it would be necessary to
+consume 2,810 gallons of the Massachusetts water, or 1,957 gallons of
+the Ohio water daily to obtain an efficient dose of radioactive salts.
+
+“During the tests radioactivity of samples was determined by means of
+electroscopes.”
+
+When radium is taken in soluble form, 25 or 50 percent of it remains
+in the body for four or five days. The rate of excretion after that is
+only about one percent a day. “Wherever it is located, it carries on a
+constant bombardment in releasing its energy, giving strength to the
+tissues, cells and protoplasm of the body. And when once these begin
+to function actively, they begin to rebuild themselves.”
+
+Radium does not combine chemically with any known substance in the
+body. The therapeutic effects are indirect. When the electrons are
+ejected with great speed from the atoms of the radioactive salts, they
+pass through millions of other atoms, knocking out new electrons as
+they go, leaving the atoms with a positive charge, in which condition
+they are called “ions.” These positively charged particles at once
+enter into new combinations, new chemical unions, which produce new
+substances. But these may be injurious to the normal tissues as well
+as to the cells of the disease which it is desired to destroy. In some
+cases, the diseased cells are more susceptible to the rays than are the
+normal cells, in which instances the growth of the abnormal or diseased
+cells may be retarded, or they may even be totally destroyed. It is
+thus seen that application of the rays may result in alleviation of the
+disease, or, possibly, effect a complete cure, as the case may be.
+
+The action of radium on various (colloidal) substances is now well
+understood from the point of view of the biophysicist; but this phase
+of the subject is too highly technical for exposition in a book
+intended for popular circulation.
+
+While it is fully recognized that there are quite definite limitations
+to the efficacy of radioactivity in its application to disease, as a
+matter of fact the use of radium as a therapeutic agent would be much
+more extensive were it not for its high cost and scarcity. No one
+questions its exceptional value in the treatment of certain diseases,
+and a method will probably be discovered, in the near future, by which
+it may veritably be used to postpone the age of senility.
+
+A young man who had read somewhere that radium is a sure cure for any
+and all of the ills to which flesh is heir, entered a drug store and
+asked: “How much is radium an ounce?” The druggist smiled, and named
+a figure which made the young man blink. “Not really?” observed the
+prospective customer. “Then you may give me an ounce of cough lozenges.”
+
+Until quite recently, an ounce of radium cost almost as much as 3¾ tons
+of gold! That is to say, an ounce of radium, if this much could be
+purchased “off hand”--which it couldn’t--would cost about $2,500,000.
+The price was at one time $3,000,000 an ounce.
+
+When we speak of “radium,” we really mean--or ought to mean--_radium
+salts_. Pure radium soon abandons its metallic form by entering into
+chemical combinations. It is the purified radium salts that cost, as
+late as 1923, $2,500,000 an ounce--the price of ¾ of a ton of platinum,
+the most “precious” of all the metals excepting radium. In 1920, radium
+was 200 times more valuable than an equal weight of pure blue diamonds,
+and 180,600 times as valuable as gold. A cubic foot of the salts--had
+this amount been obtainable--would have been worth $7,000,000,000.
+
+The reason for the high cost of radium is not far to seek. First, the
+demand for the pure salts far exceeded the supply--and this is still
+the case, though relief is now in sight. Secondly, the scarcity of
+radium was due to the enormous amount of time and labor involved in its
+production.
+
+Although radium was discovered and isolated by Mme. Curie in 1898,
+22 years later--at the close of 1920--scarcely 140 grams (or about
+five ounces) of pure radium salts had been extracted and put on the
+world market. Of this amount, about 70 grams had been produced in the
+United States (during the preceding seven years). The market value of
+the standard salts was at this time about $100,000 a gram (about 1/28
+ounce). Eighteen grams were produced in this country in 1920, and the
+value of the purified salts was quoted in some journals as $2,160,000.
+At this price, about $100,000 worth of radium could be put into a glass
+tube about the diameter of a very coarse pencil lead and not more than
+an inch in length.
+
+To produce the gram of radium salts presented to Mme. Curie by the
+women of America (in May, 1921), 500 tons of carnotite ore--containing
+two percent or less of uranium oxide--were treated, consuming in the
+process 1,500 tons of coal, more than a ton of chemicals, and over 30
+tons of water.
+
+
+ALL MATTER RADIOACTIVE
+
+While certain substances have been designated as “radioactive,” it is
+not to be understood that these bodies alone emit charged particles, or
+radiant energy.
+
+“All bodies whatever are a constant source of visible or invisible
+radiations, which, whether of one kind or the other, are always
+radiations of light” (Le Bon, “The Evolution of Forces,” p. 318, 1908).
+
+Compounds of potassium, and also of rubidium, caesium and lanthanum, as
+shown by Campbell, Wood, McLennan, Kennedy, and other investigators,
+possess very high radioactive properties. While the atomic weight of
+potassium is only about 39, and of rubidium about 84, the typical
+radioactive elements have atomic weights ranging from 200 to 238. Of
+the 12 to 15 elements essential to life, potassium is the only one
+possessing distinct if minute radioactivity. “The activity of potassium
+may readily be demonstrated by means of the goldleaf electroscope. It
+is shown that Beta rays are emitted” (Burns). But potassium is 1000
+times weaker than uranium, and 1,000,000,000 times weaker than radium,
+in the emission of Beta (negative) rays. Caesium and lanthanum emit
+Alpha (positive) rays.
+
+Professor Dufour, the distinguished French scientist, has shown that
+even air that has been breathed emits radioactive particles. The
+presence of radioactive matter in the atmosphere has been shown to
+account for its electric conductivity. Thomson found (1906) that many
+specimens of water from deep wells contain a radioactive gas, and
+Elster and Gertel have found that a similar gas is contained in the
+soil.
+
+It is probably safe to assert, with Le Bon, that all matter, “down to
+the absolute zero of temperature,” radiates electrified and more or
+less luminous particles, albeit they are invisible to the human eye.
+
+It is because of its property of emitting negative electrons (Beta
+rays) that potassium is a necessary constituent of all living matter.
+It may, however, be replaced, under certain conditions, by other
+radioactive substances.
+
+Prof. Barton Scammel, of the British Radium Society, gave it as his
+opinion (in 1922) that further experience in the proper uses of
+potassium salts and radium in solution would lead to the realization of
+a new golden age. He predicted, among other “good tidings,” life for
+120 years in the bloom of youth, the “pep” of 25 years at 75, a third
+set of teeth, new hirsute coverings for erstwhile bald heads, muscles
+like Jack Dempsey’s.
+
+Dr. C. Everett Field, of the New York Radium Institute, stated
+publicly, in backing up Scammel’s hopes and theories, that he thinks
+another ten years will see human life vastly prolonged as a matter of
+course by the use of radium. He said:
+
+“We have ascertained beyond question that potassium salts are necessary
+to heart action, that they are slightly radioactive, and that radium
+can be substituted for them with a degree of success.
+
+“It was Dr. Zwaardemaker, physiologist of the University of Utrecht,
+who first discovered, a number of years ago, that radium could do in
+the blood stream what potassium salts do in the normal person. He took
+an animal’s heart, which was kept beating outside the animal, and
+removed the potassium element. It was not longer possible then to keep
+it in action. Then he substituted a radium solution and it was possible
+to restore action.”
+
+Dr. Field stated that it had been discovered that the systems of
+victims of cancer and other wasting diseases were deficient in
+potassium salts, and that as their systems were made to assimilate
+potassium a tonic effect was noticeable at once. The greatest trouble
+was to make the body assimilate the potassium.
+
+“The fact is,” said Dr. Field, one of the more conservative radium
+therapists, “that radium does not do the healing. But, for that matter,
+neither does any other form of healing. The healing exists within
+the organism. And radium, I am convinced, in some cases, is the most
+efficient medicine to give needed stimulus to the healing apparatus of
+diseased organisms.”
+
+Even now, he believes, radioactive treatment may prolong life at least
+15 years. For internal treatment, either doses of radioactive water,
+or extremely minute quantities of radium itself, are administered.
+Radioactive water is taken from springs found to contain traces of
+radium, or radium is used to make ordinary water radioactive. The
+difficulty with spring waters is that they lose their radioactive power
+when bottled and transported, and must be consumed at their source.
+
+“Because of this fact,” says a writer for _The Popular Science Monthly_
+(June, 1923), “a group of physicians interested in the use of radium as
+a curative stimulant have invented an ingenious device for imparting
+radioactive properties to ordinary water. As designed for use in the
+home, this instrument consists of a case containing an arrangement
+of glass tubes and vessels in which emanations from radium salts in
+solution are imparted to air, which is then mixed with the water.
+
+“A much simpler apparatus, available for office use, somewhat resembles
+a hypodermic syringe, containing special capsules of radium salts.
+Pushing a plunger forces air through the radium capsules and into a
+glass of water and is said to make the water radioactive. The doses of
+radium in each case are constant, because radium emanates at a constant
+rate, and only a certain amount can be dissolved in water, no matter
+how many times a day the apparatus is brought into use.
+
+“Whether radium treatment will prove able to restore youth to old age,
+grow new sets of teeth and perform other marvels that its more ardent
+supporters predict for it, only time will tell.
+
+“If radium treatment proves to facilitate the process of cell
+elimination, it will have gone a long way toward delivering the world
+from its enemies of disease.”
+
+The philosopher-scientist, Le Bon, makes bold to suggest that
+light-waves which are invisible to human eyes may be perceptible to
+nocturnal animals, which would include most of the lemurs and the
+felines, and some other beasts which seem to be capable of finding
+their way and carrying on their predatory or other activities in the
+dark. “To them,” says Le Bon, “the body of a living being, whose
+temperature is about 37° C., or about 98° F., ought to be surrounded
+by a luminous halo, which the want of sensitiveness of our eyes alone
+prevents our discovering. There do not exist in nature, in reality, any
+dark bodies, but only imperfect eyes.”
+
+Le Bon has also said that the human body is sufficiently radioactive
+to photograph itself by its own rays, if we could find a substance
+sensitive to these radiations, as the photographic plate is to the
+actinic rays. Nothing would then be easier, he declares, than to
+photograph a living body in the dark without any other source of light
+than the invisible light which it is continually emitting.
+
+Some recent (1924) experiments of the French scientist, Dr. Albert
+Nodon, seem to afford the actual proof of Le Bon’s _a priori_
+conclusions. In the presence of a number of noted scientists, Dr. Nodon
+exhibited three photographic plates on which were unmistakable light
+impressions, which, he claimed, were caused by the rays emitted by a
+radioactive mineral, an insect, and a green leaf, which had been placed
+on the emulsion side of the plates in a dark-room.
+
+A similar experiment, in which a dead insect and a dead leaf were used,
+resulted in no ray impressions on the plates. Dr. Nodon offered as his
+conclusion that radioactivity is an inevitable accompaniment of living
+processes, and stated that the strength of photographic impressions
+produced in experiments such as his are an accurate measure of vitality
+(see _Popular Science Monthly_, October, 1924).
+
+Radium is probably present in all the planets and stars. Some time ago
+the Astronomer Royal of England, Dr. F. W. Dyson, demonstrated the
+existence of radium and of radium emanation in the sun’s chromosphere
+(the ocean of incandescent hydrogen gas surrounding the photosphere, or
+actual surface of the sun).
+
+
+
+
+CHAPTER II
+
+EVERYDAY USES OF RADIUM
+
+
+During the World War large quantities of radium were employed by the
+Allies for night compasses, luminous dials on airplanes, gun-sights,
+etc. In times of peace it is used on pendants for locating electric
+lights and switches in the dark, key-holes, fire-extinguishers, poison
+bottles, emergency call-bells, and in many other ways. For example,
+some mining corporations use signs in their mines made luminous in the
+dark by phosphorescent paint made from radioactive substances. These
+luminous signs are not affected by atmospheric conditions.
+
+Yet for all these uses, including “radium watches” and clocks, not more
+than half an ounce of radium has been used since its discovery in 1898.
+A few millionth parts of a gram of radium, in the form of radioactive
+barium sulphate, a large portion of phosphorescent zinc sulphide
+(crystallized zinc), mixed with varnish and some adhesive substance,
+give enough material to illuminate 40 or 50 watches. One gram of
+radium (= 16 grains) combined with 20,000 grams of secret process
+phosphorescent zinc sulphide is sufficient to make 667,000 watches
+luminous for many years. The factories of this country are now turning
+out about four million radium watches annually.
+
+Unless a special preparation--known only to the manufacturer--is
+used, the luminosity of the material gradually disappears, owing to
+the destruction of the zinc sulphide crystals by the powerful rays
+constantly bombarding them, producing flashes at the rate of 200,000
+a second. The radium itself does not glow, nor does it deteriorate in
+power.
+
+If we examine a luminous dial through a magnifying glass, after the
+eyes have been in total darkness for a few minutes, tiny flashes of
+light may be seen. These are caused by the explosion of hundreds of
+millions of radium atoms. The more radium there is in the paint, the
+greater the number of flashes per second, and the more durable the
+luminosity. Since every flash means a blow upon a crystal of zinc
+sulphide, the crystals gradually break under the strain. In this
+process helium is released from the disintegrating radium atoms.
+
+Mr. M. A. Henry (_Scientific American_, April 2, 1921) points out that
+the problem of the chemist “is to produce a phophorescent substance
+which will stand up longest under the terrific bombardment of the
+radium rays and which, at the same time, will give off the most light.
+Such progress is being made in this direction that today [1921] only
+about one-twentieth the amount of radium used four years ago [1917] is
+needed in the making of luminous material. And the chemist insists that
+he has only scratched the surface of possibilities in this direction
+and that even better results can be attained. At present the life of
+the zinc crystals is from 15 to 20 years, although the radium lasts for
+centuries.
+
+“This life will be much longer if the instrument to which it is applied
+is kept away from the light most of the time. The crystals, already
+stressed by the radium rays, have an additional strain imposed by the
+light and this hastens the process of disintegration. Strong sunlight,
+especially at the seashore where the presence of much ozone in the air
+intensifies the ultra-violet rays, has a very destructive effect on
+luminous material. For this reason the manufacturers of this delicate
+substance usually guarantee it for about half its normal life, or ten
+years.”
+
+A radium-lighted fish-bait is now on the market, and fishermen say that
+this bait is very successful in attracting fish which haunt deep water.
+
+
+RADIUM MAKES GEMS BLUSH
+
+D. Berthelot, F. Bordes, C. Doelter, and others observed that the rays
+from radium induced important changes in the colors of minerals.
+
+Dr. T. Squance, of Sunderland, England, succeeded in transforming a
+sapphire of faint pink hue into a gorgeous ruby color, and a faint
+green sapphire into an oriental emerald hue. It was already known that
+a diamond exposed to the rays of radium glows with a beautiful green
+light.
+
+In experiments carried out at the United States Bureau of Mines (1921),
+in Reno, Nevada, a colorless Colorado topaz was tinted yellow by
+exposure to penetrating radiation. If a method can be devised to make
+the color permanent, the discovery will greatly increase the value of
+the gem-stone material found in the west.
+
+If we submit yellow phosphorous to the action of radioactive
+substances, it becomes changed into the red “alotropic” variety.
+Certain of the rays decompose ammonia, and water under their influence
+is subjected to electrolysis, yielding oxygen and hydrogen.
+
+
+A RADIUM CLOCK
+
+A very interesting instrument was devised by Sir William Strutt (now
+Lord Rayleigh) which has been called a “radium clock.” It consists of
+a glass vessel containing a tube of radium salts in the center, from
+which two gold leaves are hung. The inner surface of the containing
+vessel is coated with tinfoil, and this foil is grounded. The radium
+salts cause the leaves to become electrically charged. They then
+diverge, and, coming in contact with the grounded tinfoil coating, they
+are discharged, only to fall back again and repeat the process. This
+clock will operate as long as the supply of radioactive material will
+act, which in the case of pure radium would be nearly 2000 years.
+
+G. Lentner has recently succeeded in utilizing atmospheric potential by
+the aid of radioactive substances, which, in some way not yet clearly
+understood, exert an influence upon the transformer. The method is
+as follows: A post about 12 m. in height, forming a sort of antenna,
+is erected; the post ends in a collector consisting of an aluminum
+sphere provided with points covered with radioactive substances.
+This collector communicates by a conducting wire with a special
+transformer. Under these conditions the earth and atmospheric currents
+attract each other through reciprocal induction.
+
+Dr. S. A. Sochocky, the well known radium expert, has made radium
+oil paints, and made paintings with them. “Pictures painted with
+radium look like any other pictures in the daytime, but at night they
+illuminate themselves and create an interesting and weirdly artistic
+effect. This paint would be particularly adaptable for pictures of
+moonlight or winter scenes, and I have no doubt that some day a fine
+artist will make a name for himself and greatly interest us by painting
+pictures which will be unique, and particularly beautiful at night in a
+dark or semi-darkened room.”
+
+Dr. Sochocky also predicts that “the time will doubtless come when
+you will have in your own home (or someone you know will have) a room
+lighted entirely by radium. It would be possible today to illuminate
+a room, so that at night, without the aid of electricity or other
+artificial illumination, you could read fine newspaper print without
+difficulty. The light in such a room, thrown off by radium paint on
+walls and ceiling, would in color and tone be like soft moonlight,
+blue with a tint of yellow. Today, a room ten by nine feet could be
+illuminated in this way at a cost of $400, and the illumination would
+last ten years.
+
+“However, such illumination will soon be much cheaper, because of new
+discoveries as to the best materials to combine with radium to produce
+light.”
+
+
+
+
+CHAPTER III
+
+RADIUM AND THE AGE OF THE EARTH
+
+
+One of the important consequences of the discovery of radioactivity was
+to afford the scientist a means for solving the problem of the earth’s
+age. By “age of the earth” we mean here the time which has elapsed
+since the earth’s surface became fitted for the habitation of living
+beings. By means of radioactivity we can form an approximate estimate
+of the time which has passed since the formation of any given series of
+geological strata. Radium is our geological time clock.
+
+It is now known that all the common rocks and soils of which the
+earth’s crust is built up contain measurable amounts of radium.
+According to the computation made by Prof. John Joly, the total
+quantity of radioactive matter may be as much as one 500 billionth part
+of the whole volume of the globe, or something over half a cubic mile.
+
+All of the 36 known radio-elements are disintegration products of the
+primary radio-elements uranium and thorium--_i.e._, they are produced
+from one or the other of these in their long sequence of changes. And
+the rate at which the radioactive products change--their average life
+period,--from the first transmutation to the final product, radium
+lead, an isotrope of common lead, is accurately known. (Helium atoms
+are “the debris shed at the various stages of the transformation.”)
+
+It is now well established that a gram of uranium as found along with
+its products in rocks and minerals is changing at a rate represented by
+the production of 1.88 x 10^{-11} grams of helium and 1.22 x 10^{-10}
+grams of lead (isotrope) _per annum_. We do not know for a certainty,
+of course, that this rate of production has been maintained throughout
+geological time. In the opinion of Lord Rayleigh, we may safely assume
+that the rate of transformation has not changed, so that “it would seem
+that in the disintegration of a gram of uranium we have a process the
+rate of which can be relied upon to have been the same in the past as
+we now observe it to be” (_Nature_, October 27, 1921).
+
+Acting on Rutherford’s suggestion, the Hon. R. J. Strutt (later
+Lord Rayleigh) made a determination of the amount of radium in the
+superficial parts of the earth--which are alone accessible; and he
+also determined the ratio of the lead (isotope) to the uranium, which
+was found to be 1.3 (specifically, in the broggerite found in the
+Pre-Cambrian rocks at Moss, Norway). Now, if we assume--as the evidence
+seems to warrant--that the lead of this atomic weight (206.06) was
+all produced by uranium at the rate given above, we get an age of 925
+million years for these rocks. Some minerals from other Archaean rocks
+in Norway give a rather larger figure.
+
+“In other cases,” says Lord Rayleigh, “there is some complication,
+owing to the fact that thorium is associated with uranium in the
+mineral and that it, too, produces helium and an isotrope of lead of
+atomic weight probably 208 exactly, about one unit higher than common
+lead.”
+
+Sir Ernest Rutherford estimated the time required for the accumulation
+of the radium content of a uranium mineral in the Glastonbury granitic
+gneiss of the early Cambrian as no less than 500,000,000 years. Later
+investigations give some of the Pre-Cambrian rocks an antiquity of
+1,640 millions of years! The zoologist may now have all the time he
+wants for the slowly evolving organisms revealed by the sedimentary
+strata.
+
+Prof. John W. Gruner, of the geology department of the University
+of Minnesota, discovered (in 1925) microscopic forms of plant life
+(algae) embedded in iron formations of the Vermillion Range near Lake
+Armstrong, Minnesota. Most of Minnesota’s iron deposits are due to the
+algae, Dr. Gruner thinks. The growth has the property of extracting
+iron from sea water and making of it a solid shell with which to
+surround itself. Accumulations of these iron shells through millions of
+years have been embedded in rock formations forming the iron ore.
+
+Slices of rock a thousandth of an inch thick were examined under
+microscopes in the search for the algae. Algae began to flourish
+immediately after the earth, in cooling (according to one cosmological
+theory), got below the boiling point. Their form is much like seaweed,
+and they thrive at a temperature of 95° C. Dr. Gruner estimates the
+age of these algae-bearing deposits at 200,000,000 years, ten million
+years earlier than previous evidence showed.
+
+If we employ the radioactivity test as a measure of geological
+time, the age of these fossil algae would have to be placed much
+higher--older by hundreds of millions of years. And the same must be
+said of the amphibian footprints recently (1925) discovered in the
+sandstone slabs of the Grand Canyon, by the caretaker on Hermit’s
+Trail, a thousand feet below the rim of the canyon. On the older
+geological time scale, these deposits date back some 50,000,000 years
+(lower Carboniferous period--the so-called “Mississippian” system). On
+the radium time schedule, these figures would need to be multiplied
+considerably (according to Boltwood and Holmes, by a multiple of six or
+more). It should be said, however, that on the time deposits of Walcott
+and Schuchert, based on the rate of deposition of sediments, the
+lower Carboniferous (Mississippian) deposits are not older than some
+18,000,000 years.
+
+But amphibian footprints are known from the far older Devonian period,
+whose strata are, on the radium basis, some 370 million years old.
+
+Prof. Charles Schuchert, of Yale, regards the estimates of geological
+time based upon the rate of disintegration of radioactive minerals as,
+on the whole, far more reliable than estimates based upon the rate of
+deposition of sediments. No scientist pretends to be able to state
+exactly the age of strata by the amount of radium lead contained in
+them.
+
+“In a third class of cases,” Lord Rayleigh points out, “the uranium
+mineral, pitchblende, occurs in a metalliferous vein, and the lead
+isotope produced in the mineral is diluted with common lead which
+entered into its original composition, ... but the complications
+cannot, I think, be considered to modify the broad result.
+
+“A determination of the amount of helium in minerals gives an
+alternative method of estimating geological age; but helium, unlike
+lead, is liable to leak away, hence the estimate gives a minimum only.
+I have found in this way ages which, speaking generally, are about
+one-third of the values which estimates of lead have given, and are,
+therefore, generally confirmatory, having regard to leakage of helium.”
+
+Dr. Homer P. Little, of the National Research Council, Washington,
+D. C., tells us (_Scientific American Monthly_, August, 1921, p. 173)
+that “from both calculation and experiment it is found that one gram
+of uranium will produce helium at the rate of one cubic centimeter in
+9,600,000 years. The ratio between the amount of radium in a mineral
+and the amount of helium present therefore allows us to calculate the
+age of the mineral. The amount of uranium originally present compared
+to that left does not enter into the problem unless extreme lengths of
+time are under consideration, because of the fact that it is calculated
+to take 5,000 million years for one-half a given volume of uranium to
+disintegrate.
+
+“It is perfectly true that much of the helium generated may escape. The
+assumption is, however, that in some minerals comparatively little
+escapes: zircon, particularly, seems to be an effective retainer.
+This mineral shows very effectively the increasing ratio of helium
+to uranium as consecutively older rocks are examined. Recent or
+Pleistocene specimens from Vesuvius show an apparent age of 1 million
+years; Miocene specimens from the Auvergne, France, of 6.3 million. The
+Devonian of Norway furnishes specimens 54 million years in age, and the
+Upper Cambrian of Colorado specimens of 141 million years; the Archaean
+of Ceylon, of the diamond-bearing rocks of South Africa, and of certain
+rocks of Ontario furnish specimens aged 286, 321 and 715 million years,
+respectively.”
+
+The following table gives the mean of the results of Professors
+Boltwood and Holmes’ careful studies, based upon the accumulation of
+lead as a final product of the uranium series:
+
+ MILLIONS OF
+ YEARS
+ Carboniferous 340
+ Devonian 370
+ Pre-Carboniferous 410
+ Silurian or Ordovician 430
+ Pre-Cambrian:
+ Sweden 1,025
+ United States of America 1,310–1,435
+ Ceylon 1,640
+
+These results, a total of 1,400,000,000 years, greatly transcend Lord
+Rayleigh’s (Strutt’s) earlier calculations regarding the antiquity they
+assign to Paleozoic and Pre-Cambrian times.
+
+In 1918, Prof. Joseph Barrell reviewed the various methods employed
+and the results obtained in the attempt to determine from geological,
+chemical and physical evidences the time that has elapsed since the
+beginning of the Cambrian Period (when abundant fossil invertebrates
+are first met with), and reached the following time estimates for
+the principal divisions of the geologic record (exclusive of the
+Pre-Cambrian rocks):
+
+ Cenozoic time,   55,000,000 to  65,000,000 years long
+ Mesozoic time,  135,000,000 to 180,000,000 years long
+ Paleozoic time, 360,000,000 to 540,000,000 years long
+
+The time thus established covers a period of from 550,000,000 to
+700,000,000 years, or from ten to 15 times longer than has usually been
+accepted by geologists. Pre-Cambrian time was found to have a similar
+order of magnitude; but here the evidence rests largely upon the
+radioactivity of the crystalline rocks formed during this vast period.
+
+It is now universally accepted that the time required for the formation
+of the Pre-Cambrian rocks was fully as long as, if not longer than,
+that for the succeeding geological divisions. The Archaean deposits
+have a vertical thickness, in the regions north of the Great Lakes,
+estimated at about 65,000 feet, or 12 miles. Their base, as a matter
+of fact, has never been reached. It is interesting to note that the
+granites of Norway, Canada, Texas and East Africa have an indicated age
+of 1,120,000,000 years, measured in terms of radium products. Prof.
+Henry Norris Russell, of Princeton University, concludes, from his
+careful investigations in radioactivity, that the age of the earth is
+“a moderate multiple of 1000 million years.”
+
+Professor Joly has computed that if there are two parts of radioactive
+material for every million million parts of other matter throughout the
+whole volume of the earth, and this is considerably less than he has
+found on the average in the earth’s crust, then this earth, instead of
+cooling off, is actually now heating up, so that in a hundred million
+years the temperature of the core will have risen through 1,800 degrees
+centigrade.
+
+Dr. Millikan observes (_Science_, July 9, 1921) that this is a
+temperature “which will melt almost all of our ordinary substances....
+It means that a planet that seems to be dead, as this our earth seems
+to be, may, a few eons hence, be a luminous body, and that it may go
+through periods of expansion when it radiates enormously, and then of
+contraction when it becomes like our present earth, a body which is
+a heat insulator and holds in its interior the energy given off by
+radioactive processes, until another period of luminosity ensues.”
+
+Lord Rayleigh’s series of researches for the purpose of determining
+the quantity of radium present in a number of representative rocks,
+both igneous and sedimentary, seems to prove that the average amount of
+radium in the earth’s crust is about 20 times larger than the amount
+calculated by Rutherford to be necessary to retain its temperature
+unaltered. Joly’s investigations revealed values in general agreement
+with these, but in many cases he obtained a value several times greater
+than the amount found by Lord Rayleigh. Further investigations showed
+that thorium is as widely distributed as radium in the earth’s crust,
+which is true also of uranium.
+
+“Incredible as it may appear,” remarks Rutherford, “the radioactive
+bodies must have been steadily radiating energy since the time of their
+formation in the earth’s crust. While the activity of uranium itself
+must decrease with the lapse of time, the variation is so slow that an
+interval measured by millions of years would be required to show any
+detectible change.”
+
+In his 1921 address to the British Association for the Advancement of
+Science, Lord Rayleigh said: “It appears certain that the radioactive
+materials present in the earth are generating at least as much heat as
+is now leaking out from the earth into space. If they are generating
+more than this (and there is evidence to suggest that they are), the
+temperature must, according to all received views, be rising.”
+
+
+
+
+CHAPTER IV
+
+AN EPOCH-MAKING DISCOVERY
+
+
+When radium was discovered by Mme. Curie in 1898, the effect upon
+the scientific world was startling, not to say “catastrophic”--as
+one author wrote at the time--since its activities ran counter to
+every known principle of physical science. “Some of the most solid
+foundations of science were destroyed, some of its noblest edifices
+wrecked, and scientists had to nerve themselves to face and investigate
+a new form of energy.”
+
+So soon as radium compounds (salts) became available, however, the
+amount of energy given out in radioactive processes--the emission of
+powerful radiations which can be transformed into light and heat--was
+measured; and it was found that radium, weight for weight, gives out
+as much heat as any known fuel every three days, and in the course of
+fifteen years releases a quantity of energy nearly 2,000 times as much
+as is obtained from the best fuel, with no signs of exhaustion (Soddy).
+In the combustion of coal, the heat evolved is sufficient to raise a
+weight of water some 80 to 100 times the weight of the fuel from the
+freezing-point to the boiling-point. The spontaneous heat from radium
+is sufficient to heat a quantity of water equal to the weight of radium
+from the freezing-point to the boiling-point every three-quarters of an
+hour. In other words, a pound of radium contains and evolves in its
+changes the same amount of energy as 100 tons or more of coal evolve in
+their combustion.
+
+In ordinary chemical changes it is the _molecules_ (groups of
+atoms) which are altered or rearranged; in radioactive change
+the atoms themselves suffer disintegration and rearrangements.
+The energy of radioactivity, then, is--according to the accepted
+view--intra-atomic--stored-up energy within the atom itself. It was
+calculated by Prof. Curie that the energy of one gram of radium would
+suffice to lift a weight of 500 tons to a height of one mile. If it
+were possible to obtain one cubic centimeter (a thimbleful) of the
+“emanation” from radium in the form of a gas, we should find that it
+possessed the power, altogether, of emitting more than seven million
+calories of heat! A thimbleful of this invisible gas would be more
+than sufficient to raise 15,000 pounds of water 1°. But in every mass
+of radium, small or large, not more than 13 trillionths of it is
+undergoing change per second.
+
+“The processes occurring in the radio-elements,” says Rutherford again,
+“are of a character quite distinct from any previously observed in
+chemistry. Although it has been shown that the radioactivity is due
+to the spontaneous and continuous production of new types of active
+matter, the laws which control this production are different from the
+laws of ordinary chemical reactions. It has not been found possible in
+any way to alter either the rate at which the matter is produced or its
+rate of change when produced. Temperature, which is such an important
+factor in altering the rate of chemical reactions, is, in these cases,
+entirely without influence. In addition, no ordinary chemical change is
+known which is accompanied by the expulsion of charged atoms with great
+velocity.... Besides their high atomic weights, [they] do not possess
+in common any special chemical characteristics which differentiate them
+from the other elements.”
+
+It was early observed by Curie and Laborde that the temperature of a
+radium salt is always a degree or two above that of the atmosphere,
+and they estimated that a gram of pure radium would emit about 100
+gram-calories per hour. Giesel later showed that radium was always at a
+temperature 5° higher than the surrounding air, regardless of what the
+temperature of the air might be. This continues unchanged whether the
+temperature of the surroundings be 250° below zero Centigrade, or in
+the intense heat of an electric furnace.
+
+“Perhaps,” remarks a writer in _The Scientific American_ (February,
+1922), “there will come a time when we shall use the energy in the
+atoms to drive our machines, cook our food and heat our rooms. Besides,
+already today we are actually using--even if only a very tiny part--the
+atomic energy. Thus, for instance, the rays emanating from radium
+are used for therapeutic purposes and the electrons emanating from a
+glowing filament can be directed so easily that they can be used in a
+large number of apparatus for wireless telegraphy and telephony. Most
+probably plants also make use of this energy in their growth because
+it has been demonstrated that the rays of the sun liberate electrons
+from the green leaves, and lastly it may also be mentioned that we
+humans use a little of this intra-atomic energy when seeing with
+our eyes, which we are enabled to do by the photoelectric action of
+light.”[A]
+
+During the course of the process of disintegration, atoms of uranium
+and thorium and their products give rise to no fewer than 36 different
+substances (A. S. Russell), and of these at least a dozen are “new
+elements.”
+
+All of the 36 radioactive elements are disintegration products of one
+or the other of the two parent elements, uranium and thorium. They are
+arranged by the chemist in three series: namely, Uranium 1, Uranium 2
+(the Actinium Series), and Thorium. In the first series there are known
+to be 15 transmutations of matter; in the second, 11; and in the third,
+10. The periods of “half change”--the period required for one-half of a
+given quantity of a radioactive element to decompose--of the different
+radioactive elements vary all the way from thousands of millions of
+years for the longest lived primary elements--2.6x10^{10} years for
+thorium, 8x10^9 for uranium 1--to .002 second for actinium A. In the
+case of radium itself, 1,670 years are demanded for the disintegration
+of half of any portion, according to the exact measurements of Profs.
+B. O. Boltwood and Ellen Gleditsch. The stable end product appears to
+be in each case an _isotope_ of lead--leads having similar chemical
+properties but of different _atomic weights_ (_i.e._, different atomic
+composition).
+
+ [A] See Shipley, Maynard, “Electricity and Life,” ch. vi.,
+ Little Blue Book No. 722.
+
+Isotopes are groups of elements which cannot be distinguished (or
+separated from) one another by any known chemical methods, and which
+differ only in the atomic weights of the members of the group. In the
+radioactive groups, the various elements differ also in degree of
+stability of their atoms.
+
+Chemists cannot actually weigh the mass of an atom of an element on a
+pair of scales, or by any other method. But if we put down 16 as the
+“atomic weight” of oxygen, and ascertain the “combining weight” (ratio)
+of hydrogen to oxygen, we can determine the “atomic weight” of hydrogen
+(1.008). (See Shipley, “The A B C of the Electron Theory of Matter,”
+p. 14, Little Blue Book, No. 603.) The ratio of the masses of _any_
+two elements in a chemical compound can be very accurately determined.
+Without going into the details here, it may be said that the _relative_
+weights of the atoms of any element can be determined to 0.01% in many
+cases (by chemical analysis and synthesis); while the _actual_ weight
+of any atom has not yet been determined to better than 0.1%.
+
+
+HOW RADIUM IS CONVERTED TO LEAD
+
+Lead is produced from uranium by a successive series of losses of Alpha
+particles--or helium atoms. Omitting the less essential outcomes, or
+transition stages, we find that each atom of uranium spontaneously
+ejects three atoms of another element, helium, and thereby is
+converted into still another element, radium. By losing one atom of
+helium, radium, in turn, is converted into the so-called emanation,
+or _niton_. The latter quickly loses four more atoms of helium and
+is converted into lead, “uranium lead,” having an atomic weight of
+206.08. Ordinary (common) lead, constituting the vast bulk of the lead
+of the world, has a much higher atomic weight, namely, 207 (Prof.
+Theodore Richards). Lead from thorium has an atomic weight of 208; from
+actinium, 206. So we have, in fact, four kinds of lead.
+
+Omitting the less stable transition products, we may say, then, that
+an atom of uranium is converted into lead by the loss of eight atoms
+of helium--losing three to become radium, then one to become the
+emanation, and finally four to become lead. No known human agency can
+either retard or hasten this breaking down of the uranium atom into
+radium, or of the radium into emanation, with the final production of
+lead.
+
+This statement has been universally accepted as true. Nevertheless,
+Dr. A. Glaschler stated (_Nature_ [London], September 12, 1925) that
+he had succeeded in accelerating the change of uranium to uranium X
+(the first product of uranium 1) by submitting uranium oxide to “strong
+rushes of momentary high-tension currents.” As early as 1923, A. Nodon
+(_Comp. rend., 176_, 1705 [1923]) brought forward strong evidence of
+an increase of the activity of radioactive substances when outdoors
+and enclosed by envelopes of small absorbing power for Gamma rays as
+contrasted to the smaller radioactivity of the same substances in
+cellars and when heavily enveloped by lead. For a tentative explanation
+of this phenomenon, see _Science_, January 8, 1926 (Vol. LXIII, No.
+1619), pp. 44–45.
+
+Both uranium and thorium, as we have just stated, break down and become
+radium, then change to helium and lead.
+
+Says Rutherford: “Although thorium is nearly always present in old
+uranium minerals and uranium in thorium minerals, there does not appear
+to be any radioactive connection between these two elements. Uranium
+and thorium are to be regarded as two distinct radioactive elements.
+
+“With regard to actinium, there is still no definite information of its
+place in the scheme of transformations. Boltwood has shown that the
+amount of actinium in uranium minerals is proportional to the amount
+of uranium. This indicates that actinium, like radium, is in genetic
+connection with uranium....”
+
+The recently discovered product, _protoactinium_,--isolated by Hahn and
+Soddy,--is the hitherto missing link between uranium Y and actinium.
+“This substance emits Alpha rays and has an estimated period of 10,000
+years. The actinium series is believed to have its origin in a dual
+transformation of uranium X. The first branch product, representing
+about 4% of the total, is believed to be uranium Y, a Beta-ray product
+of period one day. This is directly transformed into protoactinium.”
+This element has not yet been obtained in a pure state.
+
+Many of the radioactive elements are isotropic with known chemical
+elements--_i.e._, alike in their chemical properties, but dissimilar
+in radioactive properties. Since they cannot be distinguished--or
+separated--from the ordinary elements with which they are isotropic, by
+any chemical methods, they must occupy the same place in the periodic
+classification of the elements. Radium and mesothorium, for example
+(as Soddy was first to show) do not have the same atomic weight, but
+they cannot be distinguished from each other by any chemical methods.
+Therefore they both have the atomic _number_ 88, though the atomic
+_weight_ of radium is 226 and of mesothorium 228. (See Shipley, “Origin
+and Development of the Atomic Theory,” p. 64, Little Blue Book, No.
+608.) Radium D and lead, and thorium and ionium, are examples of
+radioactive isotropes.
+
+The nature of the end-product was first suggested by Boltwood, who
+pointed out the invariable presence of lead in old radium minerals,
+and in amount to be expected from their uranium content and geologic
+age. “Thus,” says Prof. T. W. Richards, of Harvard University, “we
+must adopt a kind of limited transmutation of the elements,” although
+not of the immediately profitable type [gold] sought by the ancient
+alchemists.”
+
+Sir Ernest Rutherford, who succeeded Sir J. J. Thomson as Cavendish
+Professor of Physics at Cambridge University, was first to recognize
+that the rays from uranium and radium were not all alike, but consisted
+of three distinct kinds. In order to distinguish them clearly, without
+committing himself in advance as to their exact nature, he christened
+them Alpha, Beta, and Gamma rays--the first three letters of the Greek
+alphabet. We know now that the Alpha rays are positively charged helium
+atoms, with two negative electrons missing; that the Beta rays are
+negatively charged electrons (disembodied “particles” of electricity,
+exactly like cathode rays); and that the Gamma rays are a type of
+X-rays, not material particles but merely extremely short magnetic
+waves or oscillations, akin to ordinary light waves or rays.
+
+Dr. R. A. Millikan calls them “the wireless waves of the denizens of
+the sub-atomic world. They are ether waves, just like light or just
+like wireless waves, except that the vibration frequency ... amounts to
+30 billion billions per second. These are the Gamma rays.” This means
+that this number of light waves would pass a given point in space each
+second. Since these rays do not consist of charged particles they are
+not deflected by electromagnetic or electrostatic fields, as are the
+Alpha and Beta rays. It has been found that one gram of radium ejects
+136,000,000,000 particles a second!
+
+The Gamma rays of radium have such penetrating power that a half-inch
+sheet of lead will reduce their original intensity by only one-half,
+and they are not absolutely stopped by 20 inches. These invisible
+light waves, thousands of times shorter than those of visible light,
+are produced whenever a cathode ray (negative electron) hits matter.
+Of the atoms forming the substance penetrated, perhaps only one in a
+billion is struck. It has been said that the Gamma rays (and X-rays)
+are the result of the back-kick of ejected electrons. Prof. Comstock
+says that the connection between the Beta rays and the Gamma rays “is
+probably similar to that between the bullet and the sound in the case
+of a gun.” However this may be, we know that the Gamma rays are, after
+all, in essence only excessively minute light waves. While the longest
+visible light waves are 0.00008 centimeter, the longest Gamma rays are
+0.000000013 centimeter; and whereas the shortest visible light waves
+are 0.00004 centimeter, the shortest Gamma rays are but 0.0000000007
+centimeter.
+
+The Beta particles are ejected with a velocity of from 90,000 to
+160,000 miles a second.
+
+Prof. Gustave Le Bon calculated that it would require 340,000 barrels
+of powder to discharge one bullet at this inconceivable speed! These
+negatively charged electrons normally revolve around the positively
+charged nucleus. Under certain conditions, an electron will make 2200
+billion revolutions within an atom in one second.
+
+Radium is not only continually losing matter and energy as electricity,
+but it is also losing energy as heat. Professor and Mme. Curie
+discovered that any substance placed near radium becomes itself
+a _false_ radium. This applies to all substances. The acquired
+radioactivity persists for many hours, or even days, after the removal
+of the radium. In the case of zinc, these secondary radiations were
+found to be four times as intense as ordinary uranium. It vanishes
+sooner or later upon the removal from the neighborhood of the potent
+radium.
+
+The radioactive something which passes out of radium was not the
+already known group of Alpha, Beta and Gamma rays, but an _emanation_
+akin to gas. Rutherford, its original discoverer, was not sure that
+it was a gas, so he cautiously gave it the name _emanation_. When the
+radium was heated, or dissolved in water, the quantity of emanation
+was greatly increased, which seemed to show that it was a gas of
+some kind occluded (bound up) in the radium. The quantity obtained
+was insufficient to bring the emanation within the testing power of
+spectroscope or balance.
+
+Nevertheless, the emanation has been detected, and investigated by the
+electroscope, which measures the radium rays by the power to discharge
+its electrified gold leaves. “The electroscope is about a million
+times more sensitive than the most sensitive spectroscope and yet the
+spectroscope is capable of detecting easily the millionth part of a
+milligram of matter” (Duncan).
+
+Calculations made by Rutherford show that if a thimbleful of this
+active gas could be collected, the bombardment of its powerful rays
+would heat to a red heat, or even might melt down, the walls of the
+glass containing it. The emanation emits only Alpha rays (or particles)
+forming helium.
+
+The radium from which the emanation has been abstracted, after the
+lapse of an hour or so, loses 75% of its activity. During the course
+of a single month, radium will be found to have restored all its lost
+emanation. In thirty days it will have regained all its original
+activity. It was soon discovered that the emanation abstracted from the
+radium loses its radioactivity at the same rate and according to the
+same laws as the de-emanated radium regains it. The radium is therefore
+said to be “in equilibrium with its products.”
+
+Since these processes are wholly outside the sphere of known
+controllable forces, and cannot be created, altered or destroyed--“since
+the process is independent of the chemical form of the radium, whether
+bromide, chloride, sulphate, etc., we are absolutely shut up to the
+conviction that it is a function of the atom. We are in the presence of
+an actual decay of the atom. The atom of radium breaks down into atoms
+of emanation and the atoms of emanation in their turn break down into
+something else. The activity of emanation decays and falls to half value
+in about 3.7 days.”
+
+Although the amount of emanation produced from a gram of radium
+does not amount to more than a needle-point of the gas (= 1.3 cubic
+millimeter), this is sufficient to raise the temperature of 75 grams
+of water 1° per hour, which is enough heat to melt _more than its own
+weight of ice_ in an hour, and to raise it to the boiling-point in the
+next hour, which is equivalent to 60,000 horse-power days! In other
+words, the heat evolved by the radium emanation is more than 3,500,000
+times greater than that produced in any known chemical reaction: such
+as, for example, the union of oxygen and hydrogen to form water.
+
+It was soon discovered that if the spectrum of this mysterious gas--or
+radium emanation--be examined again after an interval of about four
+weeks, it has changed into a familiar spectrum easily recognized as
+that of the gaseous element known as helium. Here the chemist comes
+face to face with the astounding fact that the element radium is
+decomposed and produces another element, helium--a discovery made by
+Ramsay and Soddy in the summer of 1903.
+
+In the successive radioactive changes, one Alpha particle (sometimes
+called “ray”) is ejected from each atom disintegrated by the change--in
+some cases, at least, accompanied by Beta particles (negative
+electrons). The Alpha particle, as already stated, is really an atom of
+helium carrying two atomic charges of positive electricity--twice that
+of an atom of hydrogen. Strictly speaking, the Alpha particle is only
+the _nucleus_ of a helium atom, since it has lost two of its negatively
+charged electrons, which are combined in the ordinary helium atom. The
+exact velocity of the expelled Alpha particle “varies in the different
+radioactive elements” (Joly)--say from 10,000 to 18,000 miles each
+second--a velocity sufficient to carry the particle around the earth in
+less than two seconds, if unchecked.
+
+But these relatively heavy particles (of atomic size) are actually soon
+checked, even by seven centimeters (about a third of a foot) of air.
+The Beta particle (1,845 the mass of a hydrogen atom) “shoots a hundred
+times as far [as the Alpha particle] and the Gamma rays are a hundred
+times more penetrating still” (Millikan). But the Alpha particle is
+sometimes ejected with a velocity nearly 40,000 times that of a rifle
+bullet,--the velocity of the latter being about half a mile a second.
+Even the super-guns which bombarded Paris could not eject a projectile
+with a speed of more than about a mile a second. Rutherford observes
+that if it were possible to give an equal velocity to an iron cannon
+ball, the heat generated on a target would be many thousand times more
+than sufficient to melt the cannon ball and dissipate it into vapor.
+
+The flashes of light seen when the Alpha rays bombard a screen of zinc
+sulphide, as in Crookes’ spinthariscope, are due to cleavages produced
+in the zinc sulphide crystals by the impact of the Alpha rays (positive
+ions). Each impact on a crystal produces a splash of light big enough
+to be seen by a microscope.
+
+In the phosphorescence caused by the approach of an emanation of radium
+to zinc sulphate, the atoms throw off the Alpha (helium) particles to
+the number of five billion each second, with velocities of 10,000 miles
+or more a second. If the helium projectile should chance to “crash”
+into an atom of nitrogen or of oxygen, an atom of hydrogen can be
+knocked out of it, as was discovered by Sir Ernest Rutherford, perhaps
+the most distinguished of Mme. Curie’s pupils. (Strictly speaking, the
+disintegration particles are isotropes of helium, of atomic weight
+3, the atomic weight of helium being 4.) Despite its large size as
+compared with an electron (or Beta particle), the Alpha particle passes
+through a glass wall without leaving a hole behind, and without in any
+way interfering with the molecules of the glass. It shoots through
+hundreds of thousands of atoms without ever going near enough to them
+to be deflected from its course.
+
+
+
+
+CHAPTER V
+
+RADIUM IN THE TREATMENT OF CANCER
+
+
+The action of radium on human tissues was unknown until 1896, when
+Prof. Henri Becquerel of Paris, having incautiously carried a lump of
+pitchblende in his pocket, discovered on his skin, within two weeks, a
+severe inflammation, or ulcer, which was known as the famous “Becquerel
+burn.” As physicians of the nineteenth century were accustomed to
+burn out cancers with caustics, the idea occurred to them that the
+application of radium might prove to be an improvement on the older
+method.
+
+It has proved to be so, affording in many cases not only relief,
+but in some instances, even a cure, not only for cancer, but for
+many other ailments--as we shall see presently. Since that time
+active investigation into the action of radium on diseased tissues
+has been carried on, resulting in the establishment in Paris of
+the “_Laboratoire biologique du Radium_,” and also of the Radium
+Institute of Vienna, followed by the establishment of somewhat similar
+institutions in various other countries, notably in England and the
+United States.
+
+One of the most famous institutions for radiotherapy is the recently
+established Radium Institute of Paris, under the management of Mme.
+Curie and Professor Debierne. This is composed of two distinct
+compartments. In one the scientific properties of radium are studied,
+while the other is devoted to its therapeutic applications. Dr. Regaud,
+who is in charge of the latter department (a branch of the widely known
+Pasteur Institute), endeavors to cure cancer and tumors by application
+of radium and X-rays.
+
+New York City boasts a magnificently equipped Radium Institute, under
+the directorship of Dr. C. Everett Field. And an even more famous
+institution is that founded by the Mayo brothers, in Rochester,
+Minnesota, where these eminent surgeons had accumulated an entire
+gram of radium as early, at least, as 1920--the largest amount owned
+by private individuals. This great institution--now known as the Mayo
+Foundation--is no longer privately owned, but it is still under the
+direction of the Mayos.
+
+Radiotherapy (or, in France, _curietherapy_, in honor of the discoverer
+of radium) or the treatment of various diseases by radioactive
+substances, has not been applied so extensively as has treatment by
+X-rays (Roentgen rays), produced in vacuum tubes. On the other hand,
+the X-rays are not so effective (as usually applied) in the treatment
+of certain morbid conditions as are the more penetrating Gamma rays
+from radioactive substances; though the latter are essentially
+identical with X-rays--swift Beta particles, or negative electrons--of
+very short wave-length. To produce X-rays as penetrating as the Gamma
+rays, about two million volts would have to be “cut” on the discharge
+tube.
+
+The Alpha rays are not often used in medical practice, and have little
+penetrating power. They are stopped by 3½ cm. of air, or by a thin
+sheet of paper. They are employed only in the way of radium “emanation”
+(a gas) dissolved in saline solution, or by the use of needles upon
+which active deposit from radium emanation has been collected. “In
+either case the emanation water or the active deposit needles must be
+introduced into the system--whether intravenously or into the solid
+tissues,--otherwise the Alpha rays would have no power to act. In
+either case, too, they act along with the Beta and Gamma rays produced
+by the active deposit” (Lozarus-Barlow).
+
+Beta radiation is used only for superficial conditions and always in
+conjunction with Gamma radiation. “Instead of a radium salt, one of
+its products, viz., radium emanation, is often employed chemically.
+No essential difference is introduced by the use of this emanation
+excepting that its intensity undergoes a progressive diminution with
+time, since it falls to half value in 3.85 days. Early rodent cancer,
+certain conditions of the eyelids, some cutaneous non-malignant tumors
+and birth-marks, are treated successfully in this way.”
+
+Physicians of the Memorial Hospital, New York City, announced in
+October, 1925, that by filtering out 90% of the caustic Beta rays
+emanating from radium and the high voltage X-ray tube, and using
+principally the healing and stimulating Gamma rays, radiation treatment
+of cancer of the tongue, lips, nose, ears or other part of the head has
+been greatly improved.
+
+In the first six months after the new method was begun, more than 100
+cases had been treated with what were considered very satisfactory
+results. Owing to the elimination of the caustic rays, much stronger
+applications of the beneficial rays can be used, and painful effects
+are largely obviated.
+
+If experience and special research lead eventually to successful
+treatment of cancer, it will be a great boon to the human race. The
+United States leads the world in deaths from this dread disease, with
+its average of 90 per 100,000 of the population. The mean average of
+cancer deaths in Europe is 76, in Asia 54, in Africa 33, in Oceania
+73. Several races, including the American Indians, are stated to
+be entirely free from cancer, and others are partially immune. The
+Japanese, for example, are subject to all forms except cancer of the
+breast. Eighty-five percent of Americans afflicted with this malady are
+persons over 40 years of age.
+
+Science Service states that a careful analysis of cancer statistics
+gathered by the United States Census Bureau over a period of about 20
+years in ten Eastern states reveals definitely that cancer mortality
+is from 25 to 30% higher than it was about 20 years ago. This is the
+claim of Dr. J. W. Schereschewsky, of the United States Public Health
+Service, who made the statistical analysis and reported it to the
+American Medical Association. “There has been a pronounced increase in
+the observed death rate from cancer in persons 40 years old and over in
+the ten states comprising the original death registration area,” Dr.
+Schereschewsky said. “Part of this increase is due to greater precision
+and accuracy in the filling out of death returns, but the remainder is
+an actual increase in the mortality of the disease.”
+
+The only way to stop the ravages of cancer, says the Paris Academy of
+Medicine, is to diagnose it early--in time for operation. For this
+to be practicable, physicians must be specially instructed. Family
+doctors are often ignorant of all but a few forms of cancer and do
+not recognize it in its first manifestations. Women of 40 to 50 are
+apt to consider little irregularities of bleeding to be associated
+with the menopause and therefore harmless. Often this is right, but
+unfortunately the bleeding from an early cancer may not differ in the
+slightest degree from such harmless irregularities and by the time
+other symptoms have developed, the cancer has perhaps grown through
+the wall of the uterus and has spread to regions where no treatment
+can hope to reach it. The only safe rule to go by is to seek expert
+investigation for any unusual or irregular bleeding or discharge,
+however slight, especially if these occur at or near the “change of
+life.”
+
+One phase of this subject of special interest is that of the use of
+radium in the treatment of cancer, especially of the neck or lower
+end of the uterus. There is already sufficient evidence to warrant
+the statement that some cancers of this region have been permanently
+cured by radium alone. And as a relief measure in the late and hopeless
+stages of the disease, radium prolongs life, relieves pain and adds
+much to the comfort of the victim.
+
+It has been amply demonstrated that radium treatment increases the
+permanency of the results obtained by surgery, and often converts
+inoperable into operable cases.
+
+
+
+
+CHAPTER VI
+
+EFFICIENCY OF RADIUM IN TREATMENT OF VARIOUS DISEASES
+
+
+In 1923, Dr. R. E. Loucks, president of the American Radium Society,
+announced that toxic goiter had been cured by radium. Exophthalmic
+goiter has been, in most cases, successfully treated by irradiation.
+Just how the cure is effected is still unknown; for the thyroid body
+from animals exposed for many hours to the Gamma irradiations of
+radium bromide shows no perceptible histological changes. Yet far
+less radiation produces marked changes in the tadpoles derived from
+normal ova fertilized by spermatazoa which have been radiated in the
+frog, though no testicular changes can be detected with certainty
+(Encyclopaedia Britannica, Vol. 32, p. 224, 12th Ed.).
+
+Among other diseases which have been more or less successfully
+treated by radium may be mentioned lupus vulgarus, epithelial tumors,
+syphilitic ulcers, chronic itching of the skin, papillomata (an
+epithelial tumor formed by hypertrophy of the papillae of the skin
+or mucuous membrane, as a corn or a wart), angiomata (tumor composed
+chiefly of dilated blood or lymph vessels), pigmentary naevi (blemish
+of the skin due to pigment, as a birth-mark), and pruritus (itching).
+Radium has been particularly effective in treating serious affections
+of the eyes, as was first fully demonstrated by Dr. Walter S. Franklin
+and Frederick C. Cordes, of San Francisco.
+
+The most brilliant successes of radium have been in those cases “where
+some serious complicating ailment, such as heart disease, tuberculosis,
+Bright’s disease, or an extreme anemia, contra-indicates anesthesia
+or any procedure which will tax the patient’s vital resources; radium
+steps in and does its work quietly, imperceptibly and, indeed, without
+the slightest risk to life.”
+
+Dr. Howard A. Kelly, of Johns Hopkins University, has been very
+successful in curing swollen masses of glands on the sides of the neck,
+cancer of the thyroid and of the cervix, and sarcoma of the chest.
+Dr. E. S. Molyneaux of London, has cured obdurate cases of tubercular
+glands in the neck, a disease rather frequent among children. Thanks
+to the patient researches of Dr. John A. Marshall, associate professor
+of biochemistry and dental pathology at the University of California,
+it is now known that a radioactive liquid may be used for sterilizing
+infected tissue. Experiments employing the radioactive liquid in the
+treatment of root canals have been conducted at the George Williams
+Hooper Foundation for Medical Research and at the College of Dentistry
+of the University of California.
+
+Within the time that the new antiseptic has been in use at these
+colleges, 85% of all the cases treated have been successful; and,
+with one exception, no soreness or pain has followed its use. This
+radioactive preparation is a solution of radium salts, “Radium D plus
+E,” which results from the decomposition of radium emanation, which,
+readily soluble in water, possesses definite radioactive properties. In
+making the solution the tiny capillary tubes containing the decomposed
+radium are crushed under water in a mortar and the liquid is then ready
+for use in the treatment of an ulcerated root of a tooth.
+
+Dr. Marshall had been working with radium for months before
+admitting the success of his investigations, which were conducted
+in a long series of experiments on the lower animals. “Microscopic
+examinations of abscessed tissue,” he said, “which have been treated
+with radioactive solutions, indicate that the bacteria producing the
+affection were killed. And in no cases observed has the treatment
+produced radium burns; the amounts used have been too small and the
+effects of too transitory a nature. That sterilization of tissue can be
+produced, however, seems apparent.
+
+“The discovery is purely of academic interest because of the fact
+that radium is too expensive, and it is possible to obtain it only in
+limited quantities; so that the chief value of the discovery will rest
+in the fact that it will stimulate further work for the identification
+of more accessible material.”
+
+In external treatment by radium itself, emanations from a certain
+quantity of radium are allowed to focus on parts of the body over the
+diseased organs. Thus the curative functions of the diseased portion
+are stimulated to activity. The atrophying of diseased tonsils has
+been the most successful use of this form of treatment.
+
+In the destruction of disease germs the radium emanation has been
+found more useful than the direct rays. The emanations kill or check
+the growth of anthrax, typhoid, and diphtheric germs. The direct
+rays are efficient in the relief of severe cases of enurites and
+facial neuralgia, cancer, tumors, affections of the skin and abnormal
+growths. Dr. Guyenot has proved that radium effects a complete cure for
+rheumatism, which he accounts for in these words: “Uric acid circulates
+in the blood in the form of urate of soda, of which there are two
+isomeric forms differing from each other by their respective solubility
+in the blood plasms. The soluble salt is converted into an insoluble
+form.” Radium breaks up this compound. The “rheumatism” disappears.
+
+
+
+
+CHAPTER VII
+
+WHERE WE GET RADIUM
+
+
+The extraction process consists in eliminating the various substances
+in the ore until only the radium salts are left. But, in the case of
+carnotite, more than 900 different operations, requiring six months of
+labor, are required between the digging of the ore and the production
+of a gram of pure radium salt. A solution containing barium and radium
+salts in the ratio of ten parts of radium to a billion is treated with
+sulphate to precipitate an insoluble “raw sulphate of barium.”
+
+Radium ores are generally found in connection with granitic
+masses--_i.e._, in places where granite forms at least part of the
+rock of the country. The carnotite ore usually consists of a thin
+layer of sandstone which crops out on the side of a canyon wall and is
+recognized by the characteristic sulphur-yellow color. The narrow seams
+are usually in the form of pockets, so that the value of a claim is
+dubious until it has been thoroughly explored and worked.
+
+Most of the original radium minerals, such as uraninite, samarskite,
+and brannerite, are black and have a shiny fracture and a high specific
+gravity. These minerals are, however, rarely found in commercially
+valuable quantities.
+
+Pitchblende, the richest source of radium, has the same composition
+as uraninite and the same general appearance, except that it shows
+no crystal form. It occurs in veins. There are extensive deposits of
+pitchblende or uraninite at Joachimstahl, Bohemia (Czecho-Slovakia),
+containing from 30 to 70 per cent uranium oxide, from which the radium
+is extracted. But here the uranium ore occurs in small pockets in
+widely separated localities, so that it is merely a by-product of other
+mining operations. However, after separation of the uranium from the
+ore, the residues are three to five times as radioactive, weight for
+weight, as the uranium. The amount of radium in old unaltered mineral
+is always proportional to its content of uranium in the ratio of 3.3
+parts of radium by weight to ten million parts of uranium.
+
+New radium ore fields were discovered in Czecho-Slovakia in 1922. The
+production of radium in that country increased from .7746 gram in 1911,
+to 1.7118 grams in 1915, and 2.2310 grams in 1920. In 1922, steps were
+taken to modernize the plants in the Jachcymov district (Bohemia),
+where the known supply will last 20 years at the present rate of
+production--a little more than two grams a year.
+
+The famous Joachimstahl pitchblende deposits were a monopoly of the
+Austrian Government before the World War, but they are now being
+worked by the Imperial and Foreign Corporation of London, under an
+agreement with the Czecho-Slovak Government. In 1922 a loan of two
+grams of radium (valued at more than $300,000) was made to Oxford
+University, for a period of fifteen years. This material is being used
+for experimental purposes by Prof. Frederick Soddy, of Oxford, and his
+associates. It has been stated that one of the chief objectives is
+the discovery of a method for the release and control of intra-atomic
+energy.
+
+Pitchblende has been found in only a few places--in Bohemia
+(Czecho-Slovakia), southern Saxony, Cornwall, and Gilpin County,
+Colorado. So far, this ore has not been the source of any radium
+produced in this country.
+
+When the original radium minerals (uraninite, samarskite, brannerite,
+etc.) break down through weathering, other radium minerals are formed
+from them, such as autunite, trobernite, carnotite, and tyuyamunite.
+The two latter ores are the most widespread and abundant. Autunite, a
+phosphate of calcium and uranium, is as active as uranium. Carnotite
+and tyuyamunite cannot be distinguished visually from each other.
+Both are a bright canary-yellow in color, and are powdery, finely
+crystalline, or, rarely, clay-like in texture. Both these minerals are
+found in the same section of Utah and of Colorado, usually associated
+with fossil wood and other vegetation, in friable, porous, fine-grained
+sandstone.
+
+The only other deposits that yield tyuyamunite in marked quantity are
+those of Tyua-Muyun, in the Andiyan district, Ferghana Government,
+central Asiatic Russia (Russian Turkestan), where it occurs with rich
+copper ores in a pipe in limestone.
+
+The radium salts--hydrous sulphate, chloride, or bromide--are all white
+or nearly white substances, no more remarkable in appearance than
+common salt. Neither radium nor the radium minerals are in themselves
+luminescent. Tubes containing radium salts glow because they include
+impurities which the invisible radiations from the radium cause to give
+light. The pure radium metal has been isolated only two or three times,
+and few persons have seen it.
+
+
+NEW SOURCES OF RADIUM
+
+In 1921, a rich deposit of pitchblende was discovered in the province
+of Ontario, Canada. Since 1921 there has been a rather considerable
+exportation of radioactive minerals from Madagascar; and in 1922
+deposits of uranium oxide (U_3O_8) were discovered in Switzerland.
+During the same year an unknown Belgian traveler sold to a curio dealer
+a strange stone picked up in the Congo. The dealer sold it to the
+British Museum. Upon examination the stone was found to be radioactive.
+Belgian geologists were immediately informed, and a Belgian mission
+was sent to the Katanga district, where the stone was found. Two veins
+of chalcolite (torbernite) containing substances rich in radium were
+soon located by the geologists, one near the Portuguese frontier.
+Chalcolite, the crystallized phosphate of copper and uranium, is twice
+as active as uranium.
+
+The newly discovered mineral has been given the name “curite,”
+in honor of Mme. Curie, the discoverer of radium. These deposits
+are now known to be the richest in the world. And, what is hardly
+less important, the radium may be isolated by simple dissolution in
+nitric acid, even in the cold. It is also readily dissolved in warm
+hydrochloric acid. Only 15 tons of the ore need to be treated to
+produce a gram of radium.
+
+Curite is found in three forms, as translucent reddish brown
+needle-like crystals; as compact saccharoid crystalline aggregates,
+orange in color; and as orange-colored earthy masses surrounding the
+preceding variety. The chemical composition is expressed by the formula
+2(PbO)5(UO_3)4(H_2O).
+
+In 1924 a pitchblende deposit, very rich in radium, was discovered in
+Ferghana, in Russian Turkestan. Soviet Russia is now mining the ore and
+extracting the radium, which is kept at the Radium Institute of the
+Academy of Science.
+
+Curiously enough, more than $500,000 worth of radium has been added to
+the world’s store of this valuable element by “boiling down” British
+cannons used in the World War. No fewer than five grams--less than a
+tablespoonful--have been secured by British scientists by this process.
+The radium is stored in a lead safe weighing almost two tons--a
+container which was invented by a Dr. Kuss, and the composition of
+which is known only to himself. One of the greatest difficulties of
+scientists has been to find some material which would prevent the
+constant bombardment of the radium rays.
+
+One important result of these recent discoveries--especially that of
+the Congo deposits--is that the price of radium dropped $30,000 a gram,
+and sells now at the rate of $70,000 a gram instead of some $100,000.
+The Standard Chemical Company of Denver, Colorado, has been obliged to
+close down its three-story laboratory, which until the close of the
+year 1922 had, for several years previously, been producing a million
+dollars’ worth of radium annually. The Paradox Valley carnotite ore
+cannot be worked in competition with the rich deposits of the Belgian
+Congo. It has been stated that five pounds annually could be produced
+from these Congo deposits. The Colorado company had been selling at the
+rate of $58,500,000 a pound. The Congo company can profitably sell the
+precious element at $29,250,000 less a pound.
+
+So, unless war breaks out again to prevent shipments from abroad, the
+United States of America will produce no more radium for a long while
+to come.
+
+
+THE RADIOACTIVE DISINTEGRATION SERIES
+
+In order to show the decomposition products of the two parent
+radioactive elements--Uranium and Thorium--and their chief
+characteristics, together with their relations to one another, and the
+time required for the product (element) to be half transformed, it is
+customary to arrange them in a _disintegration series_. There are
+three series, Uranium I, Uranium Y, and Thorium.
+
+In the first table given below is shown how the series known as
+Uranium I is transformed into the end-product, uranium lead. This is
+followed by the Uranium Y (or Actinium) series, and by the Thorium
+series; the end-product of all three being a characteristic type of
+lead. In the tables T is the “time-period” of a product, or the time
+required for the product to be _half transformed_. In the column
+“Rays” is shown what type of ray, or rays, is, or are, emitted during
+the disintegration process--A=Alpha rays (or particles), B=Beta
+rays (negative electrons), and G=Gamma rays (or X-rays of very high
+“frequency”).
+
+“In the great majority of cases,” says Sir Ernest Rutherford, “each
+of the radioactive elements breaks up in a definite way, giving rise
+to one Alpha or Beta particle and to one atom of the new product.
+Undoubted evidence, however, has been obtained that in a few cases the
+atoms break up in two or more distinct ways, giving rise to two or more
+products characterized by different radioactive properties. A branching
+of the uranium series was early demanded in order to account for the
+origin of Actinium.”
+
+In the first column is given the “atomic weight” of each radioactive
+element, the weight decreasing with (almost) every “disintegration
+period.” The figures followed by an interrogation point are
+Rutherford’s, and indicate that slightly different figures are given by
+other authorities.
+
+
+URANIUM I SERIES
+
+ T (average Rays (given out in
+ Element Atomic time-period--half each
+ Weight transformed) decomposition)
+ ---------------------------------------------------------------------
+ Uranium I 238 4.5 × 10^9 yrs. Alpha
+ Uranium X1 234 23.8 days Beta, Gamma
+ Uranium X2 234 1.15 min. Beta, Gamma
+ Uranium II 234 About 2 × 10^6 yrs. Alpha
+ Ionium 230 About 9 × 10^4 yrs. Alpha
+ Radium 226 (+) 1700 yrs. Alpha
+ Niton (Emanation) 222 3.85 days Alpha
+ Radium A 218 3.05 min. (?) Alpha
+ Radium B 214 26.8 min. (?) Beta, Gamma
+ Radium C 214 19.5 min. (?) Alpha, Beta, Gamma
+ Radium C′ 214 10^{-6} sec. (?) Alpha
+ Radium D 210 (+) 16 yrs. Beta, Gamma
+ Radium E 210 (+) 4.85 days Beta, Gamma
+ Radium F (Polonium) 210 (+) 136.5 days Alpha
+ Radium G (End-product 206 ............... ...............
+ uranium-lead)
+ ---------------------------------------------------------------------
+
+
+URANIUM Y (ACTINIUM) SERIES
+
+ T (average Rays (given out in
+ Element Atomic time-period--half each
+ Weight transformed) decomposition)
+ ---------------------------------------------------------------------
+ Uranium Y (branching 234 (+) 24.6 hrs. Beta
+ from Uranium II) (2.2 days?)
+ Protoactinium 230 About 10^4 yrs. (?) Alpha
+ Actinium 226 20 yrs. Beta
+ Radio-actinium 226 19 days Alpha
+ Actinium X 222 (+) 11.2 days Alpha
+ Actinium (Emanation) 218 3.92 sec. Alpha
+ Actinium A 214 .002 sec. Alpha
+ Actinium B 210 36 min. (?) Beta, Gamma
+ Actinium C 210 2.16 min. (?) Alpha
+ Actinium D 206 4.76 min. Beta, Gamma
+ Actinium E (End-product 206 ............... ...............
+ actinium-lead)
+ ---------------------------------------------------------------------
+
+
+THORIUM SERIES
+
+ T (average Rays (given out in
+ Element Atomic time-period--half each
+ Weight transformed) decomposition)
+ ---------------------------------------------------------------------
+ Thorium 232.1 2.2 × 10^{10} yrs. Alpha
+ Mesothorium I 228 6.7 yrs. Beta, Gamma
+ Mesothorium II 228 6.2 hrs. (?) Beta, Gamma
+ Radio-thorium 228 1.90 yrs. (?) Alpha
+ Thorium X 224 3.64 days Alpha
+ Thorium (Emanation) 220 54 sec. (?) Alpha
+ Thorium A 216 .14 sec. (?) Alpha
+ Thorium B 216 10.6 hrs. (?) Beta, Gamma
+ Thorium C 212 60 min. (?) Alpha
+ Thorium D 208 3.2 min. (?) Beta, Gamma
+ Thorium E (End-product 208 ............... ...............
+ thorium-lead)
+ ---------------------------------------------------------------------
+
+
+
+
+Transcriber’s Notes
+
+
+Punctuation, hyphenation, and spelling were made consistent when a
+predominant preference was found in the original book; otherwise they
+were not changed.
+
+Simple typographical errors were corrected; unbalanced quotation
+marks were remedied when the change was obvious, and otherwise left
+unbalanced.
+
+This book uses terminology that was current at the time of publication,
+and reflects the state of science as it was understood by the author at
+that time.
+
+
+
+*** END OF THE PROJECT GUTENBERG EBOOK 75392 ***