US3486027A - Track registration bulk tracing method - Google Patents

Track registration bulk tracing method Download PDF

Info

Publication number
US3486027A
US3486027A US580873A US3486027DA US3486027A US 3486027 A US3486027 A US 3486027A US 580873 A US580873 A US 580873A US 3486027D A US3486027D A US 3486027DA US 3486027 A US3486027 A US 3486027A
Authority
US
United States
Prior art keywords
boron
matter
particles
tracks
uranium
Prior art date
Legal status (The legal status is an assumption and is not a legal conclusion. Google has not performed a legal analysis and makes no representation as to the accuracy of the status listed.)
Expired - Lifetime
Application number
US580873A
Inventor
Henry W Alter
Current Assignee (The listed assignees may be inaccurate. Google has not performed a legal analysis and makes no representation or warranty as to the accuracy of the list.)
General Electric Co
Original Assignee
General Electric Co
Priority date (The priority date is an assumption and is not a legal conclusion. Google has not performed a legal analysis and makes no representation as to the accuracy of the date listed.)
Filing date
Publication date
Application filed by General Electric Co filed Critical General Electric Co
Application granted granted Critical
Publication of US3486027A publication Critical patent/US3486027A/en
Anticipated expiration legal-status Critical
Expired - Lifetime legal-status Critical Current

Links

Classifications

    • GPHYSICS
    • G21NUCLEAR PHYSICS; NUCLEAR ENGINEERING
    • G21HOBTAINING ENERGY FROM RADIOACTIVE SOURCES; APPLICATIONS OF RADIATION FROM RADIOACTIVE SOURCES, NOT OTHERWISE PROVIDED FOR; UTILISING COSMIC RADIATION
    • G21H5/00Applications of radiation from radioactive sources or arrangements therefor, not otherwise provided for 
    • G21H5/02Applications of radiation from radioactive sources or arrangements therefor, not otherwise provided for  as tracers

Definitions

  • This invention relates to methods for analyzing for the presence of small amounts of materials added for tracing purposes.
  • the solid-state nuclear track detectors make it possible to detect matter which produces charged particles when irradiated with neutrons, with a sensitivity about one million times greater than the best previously-available chemical or physical techniques.
  • the chemist requires at least about grams of a sample of matter to determine its presence, and even the best techniques with an emission spectrometer require 10* or 10 grams of sample.
  • As few as thirty million atoms (about 10- grams) of plutonium 239 (P11 can be detected by the formation of radiation-damage tracks in solid-state nuclear track detection to determine the distribution of matter producing charged particles when irradiated with neutrons dispersed in a fiuid at a dilution many times greater than that previously possible with any prior analysis techniques.
  • the detection method of this invention can be performed at low cost because such small amounts of material are required. Moreover, there is no radiation hazard in the system under analysis because it is not necessary to have radioactive elements in the system analyzed.
  • the method of this invention detects the distribution of added matter dispersed in a fluid by collecting a sample of the fluid with the dispersed matter in it.
  • the dispersed matter is concentrated and placed adjacent to a solid material which is susceptible to the formation of radiation-damage tracks by charged particles.
  • the concentrated matter is irradiated with neutrons to generate charged particles which penetrate the material and leave radiation-damage tracks that indicate the presence of the added matter.
  • the matter is in the form of finely-divided particles, preferably in the range of about 0.1 to about 10 microns.
  • a micron is 10 meters or 10,000 angstrom units.
  • Some of the elements which are useful in the method of this invention are boron, uranium, plutonium, and lithium. Certain isotopes of these elements undergo nuclear reaction when bombarded with neutrons and emit fragments which leave radiation damage in solid materials such as cellulose nitrate, Lexan (a trademark for a polycarbonate resin such as bisphenolacetone carbonate), mica, Mylar (a trademark for a film of polyethylene terephthalate), and Lucite (a trademark for methacrylate ester polymers).
  • an alpha particle leaves a radiation-damage track in cellulose nitrate but not in Lexan. Heavier fragments, such as those from uranium fission, leave tracks in both cellulose nitrate and Lexan. Since solid-state nuclear track detectors are insensitive to beta and gamma rays and neutrons, a nuclear reactor may conveniently be used as a neutron source.
  • An alternate technique for improving the sensitivity of the method when there is a natural background of the fissionable matter used in the detection system is to combine two elements in single particles composed of a compound such as uranium boride or a glass containing uranium and boron. These particles are then dispersed in the fluid to be traced or analyzed. The particles are subsequently collected, concentrated, and placed adjacent a solid-state nuclear track detector such as a cellulose nitrate film. Thereafter, the particles are irradiated with neutrons. The coincidence of heavier fission-fragment tracks from the uranium and alpha tracks from the boron uniquely distinguishes the dispersed particles from the material which occurs naturally in the fluid. Moreover, since the boron and uranium are combined stoichiometrically or in a fixed ratio in all particles, the alpha and heavy fission-fragment tracks appear in a definite ratio regardless of particle size.
  • a compound such as uranium boride or a glass
  • the fissionable matter dispersed in the fluid may also occur naturally, such as uranium particles dispersed in a stream of water or air. In this case, the particles are collected, concentrated, and analyzed to determine the location of a uranium ore body.
  • the detection method of this invention is useful for studying flow rates, flow distribution, concentration dis tribution, dilution-mixing data, leakage and recharge rates,
  • meteorology ore prospecting (10 grams of natural uranium can be detected), alloy analysis, biology, control of uranium-plutonium contamination, smog control and analysis, and wear tracing such as in bearings and other moving parts.
  • Example I.--Sewage efi luent tracing A typical sewage plant for a large city discharges 10 liters per day of effluent in the ocean. It is desired to determine the presence of the efiluent at a dilution factor of 10 which is at least one hundred times better than the existing methods which measure either Water salinity or bacteria content. It is then necessary to trace x10 or 10 liters of water. A 0.5 micron diameter particle of natural boron weighs about 1.5 X10" grams. Such a particle yields about 7 tracks at a relatively low neutron exposure of 10 neutrons per square centimeter. Approximately 10 particles of boron per liter are needed for the quantitative determination of dilution (with approximately 30% error).
  • the plume or distribution of the sewage efiluent is determined by collecting l-liter samples at various locations offshore at the point of effiuent outfall.
  • Ocean water contains a substantial amount of dissolved boron which acts as a background and tends to mask the presence of the particulate boron added to the sewage efiluent distribution.
  • the boron in each liter sample is concentrated by either evaporation or filtration. In the case of evaporation, the dissolved boron and the added particulate boron are present together.
  • the tracks produced by the particulate boron appear in clusters as compared to the relatively scattered single tracks produced by the dissolved boron. Thus, it is possible to distinguish the added from the naturally-occurring boron.
  • the filter passes the dissolved boron but retains the particulate boron.
  • the concentrated boron particles are placed adjacent a film of cellulose nitrate, or other suitable solid-state nuclear track detector, and irradiated with neutrons for a total exposure of about 10 neutrons per square centimeter.
  • the boron atoms which capture neutrons produce charged particles (alpha particles and Li ions) which form tracks in the film. These tracks, which are about 8 microns long and to 100 angstrom units wide, are too small to be seen except with an electron microscope.
  • the cellulose nitrate film with the radiation-damage tracks is immersed in a solution of 6 N sodium hydroxide at to 60 C. for 1 to minutes.
  • the sodium hydroxide selectively attacks that portion of the cellulose nitrate film which has been damaged by the alpha particles and Li ions and enlarges the tracks to a width of between about 0.5 to about 20 microns, which can be observed with a conventional optical microscope.
  • the tracks are counted, or the image through the microscope photographed, to provide a permanent record, if desired.
  • the number of track clusters indicates the amount of tracers boron particles present, and thus indicate the amount of sewage efiluent in the sample.
  • the tracer boron naturally present in the seawater tends to interfere with the tracer measurement just described. Accordingly, the tracer boron is combined with another element or elements to make it relatively insoluble. This material is finely divided to the right particle size so that it remains suspended in the water during the time requirer for the tracing of the flow of the sewage effluent. Ordinarily, a life of about 1 week for the particles is sufficient.
  • boron silicate glass is grouped to particle size between about 0.1 and about 2.0 microns. The particles are carefully graded so that they have uniform size and, therefore, remain uniformly suspended in the sewage efiluent and surrounding seawater.
  • the boron silicate glass particles gradually settle or dissolve in the seawater so they do not remain indefinitely present and produce interferring background for subsequent measurements.
  • Other examples of boron compounds which can be used for tracing are B Si, B Si, B C, BP, and BN.
  • Lithium can also ve used as a tracer.
  • suitable lithium compounds for tracing are Li SiO and Li SiO and various types of lithium glasses. In this case, neutron irradiation produces alpha particles and tritons from the lithium-6 isotope.
  • the particles are of a chemical and physical nature such that they do not react with their environment and disperse uniformly in the fluid being traced, do not cohere with each other or with other solids that might be present in the system, and do not undergo selective adsorption in the system under analysis.
  • the particles are relatively insoluble in the fluid when there is a background problem, such as boron naturally in sea water.
  • the particulate tracer material can be made to match the bulk fluid density of the medium in which it is dispersed. Since the sub-micron particles do not settle rapidly in the fluid, this method now makes the tracing of large quantities of fluids possible with small amounts of material and without the concurrent hazards of radioactive tracing. It also avoids the disadvantages attendant with the use of dyes, which must be used in enormous amounts to achieve tracing not nearly as accurate as the present technique provides, and which may react chemically with the environment.
  • Example II Tracing with mixed elements Particulate tracing such as that described in Example I above is made even more specific and less subject to interference from possible natural background by the use of mixtures or chemical compounds, such as uranium borosilicate glasses or uranium boride particles, which are relatively insoluble, and which contain known proportions of elements that each undergo reaction with neutrons to produce separate distinctive charged particles.
  • the uranium boride is reduced to a selected particle size and dispersed in the sewage efiluent as described in Example 1. Samples of the eflluent and ocean water in which it is discharged are collected.
  • the particulate uranium boride particles are concentrated by filtration or evaporation, placed adjacent a cellulose nitrate film, and irradiated with neutrons as previously described. At those locations where the uranium boride particles are located, there is a coincidence of fission-fragment and alpha tracks.
  • the fission of the uranium on capturing a neutron produces fission-fragment tracks about 20 microns long in the cellulose nitrate.
  • the boron produces alpha tracks only about 5 microns long in the cellulose nitrate. The boron which occurs naturally in the sample, i.e., not associated with uranium, creates only alpha tracks in the cellulose nitrate film.
  • the tracer boron is easily distinguished from the naturally-occurring boron.
  • the definite ratio of uranium-to-boron in the tracer produces a definite ratio of alpha tracks-to-fission-fragment tracks so the measurement is independent of the particle size of the uranium boride. This facilitates tracing a plurality of comingling streams by the use of tracers which have elements combined in different proportions, and in difierent compounds.
  • Example III Air Tracing One thousandcubic feet of air is readily filtered and analyzed for its particulate boron content, which can be in any of the forms described above in Example 1. Substantially all of the air over a given surface of the earth is under a height of 20 kilometers. Then particles of boron per 1000 cubic feet of air is easily detected as described above for Example I. The following Table 1 shows the amount of boron needed to place particles of boron per 1000 cubic feet in the atmosphere over different areas to a height of 20 kilometers.
  • Table 1 shows 1 gram of boron particles dispersed as a particulate tracer source (0.5 micron in diameter) in 1000 cubic feet of air, the marked 1000 cubic feet of air can be detected to a dilution factor of 7 x 10
  • the tracing technique of this invention permits tracing and following the movement of large air masses for either gross or micrometeorological studies.
  • the sensitivity is further enhanced by collecting more air sample or increasing the neutron radiation time over that given in Example 1.
  • This invention in effect, replaces radioactive tracers in many of their applications and extends the use of tracer techniques in areas where radioactive hazards make radioactive tracers inapplicable.
  • Example IV -Uranium prospecting
  • Uranium compounds found in ore bodies are usually relatively insoluble. Erosion of each ore body by water and air gives rise to water-borne and air-borne particulates characteristic of the ore containing uranium. The particulates are carried away from the ore body by air currents or Water streams.
  • the ore body is located by collecting air or water samples at a plurality of locations spaced from each other and the ore body, concentrating the particulates from the ore body by filtration, placing the concentrated particulates in contact with Lexan or equivalent material, and irradiating them with neutrons to form radiation tracks in the material due to the fission fragments occurring when the uranium atoms capture neutrons.
  • the Lexan film is then etched as described in Example I and observed to determine the particulate density of a given sample. Where there is a gradient of uranium concentration, there is an indication that the samples have been carried from an ore body bearing uranium, and the ore body is located by following the gradient in the direction in which the uranium concentration increases.
  • Example V.Wear studies Another example of practical use of the method of this invention is in wear tracing.
  • hearings or other parts which were to be tested for wearing were made to incorporate radioactive particles which were abraded off in the lubricating fluid (usually oil) during the testing operation. Thereafter, the radioactivity of the lubricating fluid was measured to determine the amount of wear of the part.
  • Wear tracing with the method of this invention is much more sensitive, and does not require the use of radioactive materials during the running of the part under test. For example, boron-l0 is included in the material of which wear is to be tested, but in amounts which have no effect on the properties of the material. Typically, the
  • material is made into a bearing, piston, or the like, which is lubricated by oil.
  • the lubricating fluid is filtered, or the boron particles which may have been abraded off into the fluid are otherwise suitably concentrated, and then analyzed for track etching as described above in the foregoing examples.
  • this invention provides an inexpensive, highly-sensitive method for tracing without radioactive hazards.
  • the technique can be used to study flow rates, flow distribution, concentration distribution, dilution-mixing problems (e.g., sewage plants), leakage and recharge rates (ground water studies), meteorology (hurricanes and other storms), ore prospecting, alloy analysis, control of uranium and plutonium concentration, smog control wear tracing, and numerous other systems.
  • a method of detecting the distribution of particulate fissionable matter dispersed in a fluid comprising collecting a sample of the fluid with the dispersed matter in it, concentrating the matter in the sample, placing the concentrated matter adjacent a solid material which is susceptible to the formation of radiation-damage tracks by charged particles emitted when the matter reacts with neutrons, and irradiating the concentrated matter with neutrons to generate charged particles which penetrate the solid material and leave radiation-damage tracks that directly form a permanent record indicating the presence of the fissionable particulate matter.
  • the method of detecting the distribution of particulate matter dispersed in a fluid comprising collecting a sample of the fluid with the dispersed matter in it, concentrating the matter, placing the concentrated matter on a solid material, the solid material being susceptible to the formation of radiation-damage tracks by fragments emitted from either of the fissionable elements in the matter, the tracks formed by fragments from each of the fissionable elements being distinguishable, and irradiating the concentrated matter with neutrons 'to generate fragments which pass through some of the solid material and leave radiation-damage tracks that directly form a permanent record indicating the presence of the matter and the ratio of the elements combined.
  • the solid material is selected from the group consisting of cellulose nitrate, cellulose acetate, cellulose acetate butyrate, polycarbonate resin, mica, polyethylene terephthalate, and methacrylate ester polymers.
  • the method according to claim 1 which includes the step of selectively etching the radiation-damage portion of the solid material to enlarge the size of the tracks and make them visible under an optical microscope.

Landscapes

  • Physics & Mathematics (AREA)
  • Engineering & Computer Science (AREA)
  • General Engineering & Computer Science (AREA)
  • High Energy & Nuclear Physics (AREA)
  • Measurement Of Radiation (AREA)
  • Analysing Materials By The Use Of Radiation (AREA)

Description

United States Patent Int. Cl. G21h 5/00 US. Cl. 250106 15 Claims ABSTRACT OF THE DISCLOSURE A bulk tracing technique using-track-registration materials is disclosed. This technique has exceptional sensitivity and a unique ability to discriminate over background. Basically, this method detects the distribution of added particulate fissionable matter dispersed in a fluid by collecting a sample of the fluid with the dispersed matter therein. The dispersed matter is concentrated and placed adjacent to a solid material which is susceptible to the formation of radiation-damage tracks by charged particles. The concentrated matter is irradiated with neutrons to generate charged particles which penetrate the material and leave radiation-damage tracks that indicate the presence of the added matter.
This invention relates to methods for analyzing for the presence of small amounts of materials added for tracing purposes.
It has recently been discovered that energetic charged particles, such as alpha particles and fission fragments from the heavier atoms, leave tracks of radiation damage in various types of materials. Such tracks can be seen with an electron microscope, but can also be made visible in an optical microscope if the material in which the tracks are made is selectively attacked by chemical reagents in the radiation-damage tracks. Such materials are called solid-state nuclear track detectors, and are described in an article entitled Track Registration in Various Solid-State Nuclear Track Detectors by Fleischer, et al, published in Physical Review, volume 133, Number A, Mar. 2, 1964. Solid-state nuclear track detectors will not yield tracks when irradiated with beta or gamma rays or neutrons.
When certain isotopes of given elements are bombarded with neutrons, the atoms of these elements capture neutrons and produce charged particles with various energies. For example, boron-10, on capturing a neutron, emits an alpha particle and a lithium-7 ion. These relatively lightweight charged partices leave a damage track in cellulose nitrate about 8 microns long. Uranium, on the other hand, fissions into much larger and more energetic fragments which leave tracks about 20 microns long in a variety of solid-state nuclear track detectors.
The solid-state nuclear track detectors make it possible to detect matter which produces charged particles when irradiated with neutrons, with a sensitivity about one million times greater than the best previously-available chemical or physical techniques. For example, the chemist requires at least about grams of a sample of matter to determine its presence, and even the best techniques with an emission spectrometer require 10* or 10 grams of sample. As few as thirty million atoms (about 10- grams) of plutonium 239 (P11 can be detected by the formation of radiation-damage tracks in solid-state nuclear track detection to determine the distribution of matter producing charged particles when irradiated with neutrons dispersed in a fiuid at a dilution many times greater than that previously possible with any prior analysis techniques.
3,486,027 Patented Dec. 23, 1969 In addition to high sensitivity, the detection method of this invention can be performed at low cost because such small amounts of material are required. Moreover, there is no radiation hazard in the system under analysis because it is not necessary to have radioactive elements in the system analyzed.
Briefly, the method of this invention detects the distribution of added matter dispersed in a fluid by collecting a sample of the fluid with the dispersed matter in it. The dispersed matter is concentrated and placed adjacent to a solid material which is susceptible to the formation of radiation-damage tracks by charged particles. The concentrated matter is irradiated with neutrons to generate charged particles which penetrate the material and leave radiation-damage tracks that indicate the presence of the added matter.
In the presently-preferred method, the matter is in the form of finely-divided particles, preferably in the range of about 0.1 to about 10 microns. A micron is 10 meters or 10,000 angstrom units. Some of the elements which are useful in the method of this invention are boron, uranium, plutonium, and lithium. Certain isotopes of these elements undergo nuclear reaction when bombarded with neutrons and emit fragments which leave radiation damage in solid materials such as cellulose nitrate, Lexan (a trademark for a polycarbonate resin such as bisphenolacetone carbonate), mica, Mylar (a trademark for a film of polyethylene terephthalate), and Lucite (a trademark for methacrylate ester polymers). These materials have different characteristics for recording damage tracks. For example, an alpha particle leaves a radiation-damage track in cellulose nitrate but not in Lexan. Heavier fragments, such as those from uranium fission, leave tracks in both cellulose nitrate and Lexan. Since solid-state nuclear track detectors are insensitive to beta and gamma rays and neutrons, a nuclear reactor may conveniently be used as a neutron source.
Many of the fluids which are to be analyzed for the added matter may contain a naturally-occurring background of the matter used in the analysis. In such cases, the sensitivity of the analysis is increased in accordance with this invention by dispersing the added matter in partculate form which is of limited solubility so that it can subsequently be filtered from a sample of the fluid and thus separated from the dissolved background matter.
An alternate technique for improving the sensitivity of the method when there is a natural background of the fissionable matter used in the detection system is to combine two elements in single particles composed of a compound such as uranium boride or a glass containing uranium and boron. These particles are then dispersed in the fluid to be traced or analyzed. The particles are subsequently collected, concentrated, and placed adjacent a solid-state nuclear track detector such as a cellulose nitrate film. Thereafter, the particles are irradiated with neutrons. The coincidence of heavier fission-fragment tracks from the uranium and alpha tracks from the boron uniquely distinguishes the dispersed particles from the material which occurs naturally in the fluid. Moreover, since the boron and uranium are combined stoichiometrically or in a fixed ratio in all particles, the alpha and heavy fission-fragment tracks appear in a definite ratio regardless of particle size.
The fissionable matter dispersed in the fluid may also occur naturally, such as uranium particles dispersed in a stream of water or air. In this case, the particles are collected, concentrated, and analyzed to determine the location of a uranium ore body.
The detection method of this invention is useful for studying flow rates, flow distribution, concentration dis tribution, dilution-mixing data, leakage and recharge rates,
meteorology, ore prospecting (10 grams of natural uranium can be detected), alloy analysis, biology, control of uranium-plutonium contamination, smog control and analysis, and wear tracing such as in bearings and other moving parts.
These and other aspects of the invention will be more fully understood from the following detailed description and specific examples.
Example I.--Sewage efi luent tracing A typical sewage plant for a large city discharges 10 liters per day of effluent in the ocean. It is desired to determine the presence of the efiluent at a dilution factor of 10 which is at least one hundred times better than the existing methods which measure either Water salinity or bacteria content. It is then necessary to trace x10 or 10 liters of water. A 0.5 micron diameter particle of natural boron weighs about 1.5 X10" grams. Such a particle yields about 7 tracks at a relatively low neutron exposure of 10 neutrons per square centimeter. Approximately 10 particles of boron per liter are needed for the quantitative determination of dilution (with approximately 30% error). This then requires 10 particles per day of natural boron (added as a source of fissionable matter to the eflluent from the sewage plant). The weight of boron is, therefore, l0 l.5 10- or 150 grams. Thus, only 150 grams of boron per day added uniformly to the efiluent are sufficient to trace the eflluent in the ocean to a dilution factor of 10 Boron is a good element to use for such tracing work because it is relatively inexpensive, and has a large capture cross section for neutrons to produce alpha particles.
The plume or distribution of the sewage efiluent is determined by collecting l-liter samples at various locations offshore at the point of effiuent outfall. Ocean water contains a substantial amount of dissolved boron which acts as a background and tends to mask the presence of the particulate boron added to the sewage efiluent distribution. The boron in each liter sample is concentrated by either evaporation or filtration. In the case of evaporation, the dissolved boron and the added particulate boron are present together. The tracks produced by the particulate boron appear in clusters as compared to the relatively scattered single tracks produced by the dissolved boron. Thus, it is possible to distinguish the added from the naturally-occurring boron. This distinction is not necessary in using filtration to concentrate the boron particles added to the sewage effluent. In this case, the filter passes the dissolved boron but retains the particulate boron. In either case, the concentrated boron particles are placed adjacent a film of cellulose nitrate, or other suitable solid-state nuclear track detector, and irradiated with neutrons for a total exposure of about 10 neutrons per square centimeter. The boron atoms which capture neutrons produce charged particles (alpha particles and Li ions) which form tracks in the film. These tracks, which are about 8 microns long and to 100 angstrom units wide, are too small to be seen except with an electron microscope. Since examination with an electron microscope is time consuming and expensive, the cellulose nitrate film with the radiation-damage tracks is immersed in a solution of 6 N sodium hydroxide at to 60 C. for 1 to minutes. The sodium hydroxide selectively attacks that portion of the cellulose nitrate film which has been damaged by the alpha particles and Li ions and enlarges the tracks to a width of between about 0.5 to about 20 microns, which can be observed with a conventional optical microscope. The tracks are counted, or the image through the microscope photographed, to provide a permanent record, if desired. The number of track clusters indicates the amount of tracers boron particles present, and thus indicate the amount of sewage efiluent in the sample.
As mentioned previously, the soluble boron naturally present in the seawater tends to interfere with the tracer measurement just described. Accordingly, the tracer boron is combined with another element or elements to make it relatively insoluble. This material is finely divided to the right particle size so that it remains suspended in the water during the time requirer for the tracing of the flow of the sewage effluent. Ordinarily, a life of about 1 week for the particles is sufficient. Conveniently, boron silicate glass is grouped to particle size between about 0.1 and about 2.0 microns. The particles are carefully graded so that they have uniform size and, therefore, remain uniformly suspended in the sewage efiluent and surrounding seawater. The boron silicate glass particles gradually settle or dissolve in the seawater so they do not remain indefinitely present and produce interferring background for subsequent measurements. Other examples of boron compounds which can be used for tracing are B Si, B Si, B C, BP, and BN. Lithium can also ve used as a tracer. Examples of suitable lithium compounds for tracing are Li SiO and Li SiO and various types of lithium glasses. In this case, neutron irradiation produces alpha particles and tritons from the lithium-6 isotope.
For optimum results, the particles are of a chemical and physical nature such that they do not react with their environment and disperse uniformly in the fluid being traced, do not cohere with each other or with other solids that might be present in the system, and do not undergo selective adsorption in the system under analysis. Preferably, the particles are relatively insoluble in the fluid when there is a background problem, such as boron naturally in sea water.
From the foregoing description it will be seen that the particulate tracer material can be made to match the bulk fluid density of the medium in which it is dispersed. Since the sub-micron particles do not settle rapidly in the fluid, this method now makes the tracing of large quantities of fluids possible with small amounts of material and without the concurrent hazards of radioactive tracing. It also avoids the disadvantages attendant with the use of dyes, which must be used in enormous amounts to achieve tracing not nearly as accurate as the present technique provides, and which may react chemically with the environment.
Example II.Tracing with mixed elements Particulate tracing such as that described in Example I above is made even more specific and less subject to interference from possible natural background by the use of mixtures or chemical compounds, such as uranium borosilicate glasses or uranium boride particles, which are relatively insoluble, and which contain known proportions of elements that each undergo reaction with neutrons to produce separate distinctive charged particles. The uranium boride is reduced to a selected particle size and dispersed in the sewage efiluent as described in Example 1. Samples of the eflluent and ocean water in which it is discharged are collected. The particulate uranium boride particles are concentrated by filtration or evaporation, placed adjacent a cellulose nitrate film, and irradiated with neutrons as previously described. At those locations where the uranium boride particles are located, there is a coincidence of fission-fragment and alpha tracks. The fission of the uranium on capturing a neutron produces fission-fragment tracks about 20 microns long in the cellulose nitrate. The boron produces alpha tracks only about 5 microns long in the cellulose nitrate. The boron which occurs naturally in the sample, i.e., not associated with uranium, creates only alpha tracks in the cellulose nitrate film. Thus, the tracer boron is easily distinguished from the naturally-occurring boron. Moreover, the definite ratio of uranium-to-boron in the tracer produces a definite ratio of alpha tracks-to-fission-fragment tracks so the measurement is independent of the particle size of the uranium boride. This facilitates tracing a plurality of comingling streams by the use of tracers which have elements combined in different proportions, and in difierent compounds.
Example III.Air Tracing One thousandcubic feet of air is readily filtered and analyzed for its particulate boron content, which can be in any of the forms described above in Example 1. Substantially all of the air over a given surface of the earth is under a height of 20 kilometers. Then particles of boron per 1000 cubic feet of air is easily detected as described above for Example I. The following Table 1 shows the amount of boron needed to place particles of boron per 1000 cubic feet in the atmosphere over different areas to a height of 20 kilometers.
It is clear from Table 1 that relatively small quantities of source material can label very large air masses. In any application to local or general meteorology where it is desired to trace the direction and dilution of a given moving air mass, more mass with a given source up to a point of dilution to the total volume shown in the above Table. For example, Table 1 shows 1 gram of boron particles dispersed as a particulate tracer source (0.5 micron in diameter) in 1000 cubic feet of air, the marked 1000 cubic feet of air can be detected to a dilution factor of 7 x 10 The tracing technique of this invention permits tracing and following the movement of large air masses for either gross or micrometeorological studies. The sensitivity is further enhanced by collecting more air sample or increasing the neutron radiation time over that given in Example 1.
Similar calculations show the value of the method of this invention in oceanography for the study of currents and mixing phenomena, the study of surface and ground water for conservation and control, the displacement of large oil deposits with gas or water in secondary recovery operations, the tracing of pipelines, and any studies of large-scale mixing in industry such as steel, cement, or numerous other chemical processes.
This invention, in effect, replaces radioactive tracers in many of their applications and extends the use of tracer techniques in areas where radioactive hazards make radioactive tracers inapplicable.
Example IV.-Uranium prospecting The sensitivity of the analytical method of this invention is well demonstrated in uranium prospecting. Uranium compounds found in ore bodies are usually relatively insoluble. Erosion of each ore body by water and air gives rise to water-borne and air-borne particulates characteristic of the ore containing uranium. The particulates are carried away from the ore body by air currents or Water streams. The ore body is located by collecting air or water samples at a plurality of locations spaced from each other and the ore body, concentrating the particulates from the ore body by filtration, placing the concentrated particulates in contact with Lexan or equivalent material, and irradiating them with neutrons to form radiation tracks in the material due to the fission fragments occurring when the uranium atoms capture neutrons. The Lexan film is then etched as described in Example I and observed to determine the particulate density of a given sample. Where there is a gradient of uranium concentration, there is an indication that the samples have been carried from an ore body bearing uranium, and the ore body is located by following the gradient in the direction in which the uranium concentration increases.
Example V.Wear studies Another example of practical use of the method of this invention is in wear tracing. In the past, hearings or other parts which were to be tested for wearing were made to incorporate radioactive particles which were abraded off in the lubricating fluid (usually oil) during the testing operation. Thereafter, the radioactivity of the lubricating fluid was measured to determine the amount of wear of the part. Wear tracing with the method of this invention is much more sensitive, and does not require the use of radioactive materials during the running of the part under test. For example, boron-l0 is included in the material of which wear is to be tested, but in amounts which have no effect on the properties of the material. Typically, the
, material is made into a bearing, piston, or the like, which is lubricated by oil. After appropriate time of test, the lubricating fluid is filtered, or the boron particles which may have been abraded off into the fluid are otherwise suitably concentrated, and then analyzed for track etching as described above in the foregoing examples.
From the foregoing description, it is apparent that this invention provides an inexpensive, highly-sensitive method for tracing without radioactive hazards. The technique can be used to study flow rates, flow distribution, concentration distribution, dilution-mixing problems (e.g., sewage plants), leakage and recharge rates (ground water studies), meteorology (hurricanes and other storms), ore prospecting, alloy analysis, control of uranium and plutonium concentration, smog control wear tracing, and numerous other systems.
I claim:
1. A method of detecting the distribution of particulate fissionable matter dispersed in a fluid, the method comprising collecting a sample of the fluid with the dispersed matter in it, concentrating the matter in the sample, placing the concentrated matter adjacent a solid material which is susceptible to the formation of radiation-damage tracks by charged particles emitted when the matter reacts with neutrons, and irradiating the concentrated matter with neutrons to generate charged particles which penetrate the solid material and leave radiation-damage tracks that directly form a permanent record indicating the presence of the fissionable particulate matter.
2. The method according to claim 1 in which the matter is particulate and in the size range of about 0.1 micron to about microns.
3. The method according to claim 1 which includes the step of forming the matter into finely-divided particles, and dispersing them in the fluid.
4. The method according to claim 1 in which the matter is relatively insoluble in the fluid.
5. The method according to claim 4 in which the matter has a solubility of less than about 0.1 part per 100 parts of the fluid.
6. The method according to claim 1 in which the matter is boron.
7. The method according to claim 1 in which the matter is uranium.
8. The method of detecting the distribution of particulate matter dispersed in a fluid, the matter being a combination of one element which produces charged particles in one range of energy and mass and another element which produces charged particles in a substantially higher range of energy and mass, the method comprising collecting a sample of the fluid with the dispersed matter in it, concentrating the matter, placing the concentrated matter on a solid material, the solid material being susceptible to the formation of radiation-damage tracks by fragments emitted from either of the fissionable elements in the matter, the tracks formed by fragments from each of the fissionable elements being distinguishable, and irradiating the concentrated matter with neutrons 'to generate fragments which pass through some of the solid material and leave radiation-damage tracks that directly form a permanent record indicating the presence of the matter and the ratio of the elements combined.
9. The method according to claim 8 in which the solid material is selected from the group consisting of cellulose nitrate, cellulose acetate, and cellulose acetate butyrate.
10. The method according to claim 1 in which the solid material is selected from the group consisting of cellulose nitrate, cellulose acetate, cellulose acetate butyrate, polycarbonate resin, mica, polyethylene terephthalate, and methacrylate ester polymers.
11. The method according to claim 1 which includes the step of selectively etching the radiation-damage portion of the solid material to enlarge the size of the tracks and make them visible under an optical microscope.
12. The method according to claim 1 which includes 7 the step of filtering the sample of fluid to concentrate the dispersed matter in the sample.
13. The method according to claim 1 in which the fluid is liquid, and including the step of evaporating the liquid to concentrate the matter in it.
14. The method according to claim 1 in which the matter is selected from the group consisting of B Si, B Si, B C, BP, BN, boron glass, Li SiO Li SiO lithium glass, uranium glass, uranium boride, plutonium glass, and plutonium compounds.
15. The method of detecting the presence of a uranium ore body from which particles of uranium are dispersed by natural forces in a naturally-occurring ambient fluid References Cited UNITED STATES PATENTS 2,874,303 2/1959 Lane 250-83 3,149,233 9/1964 Wilson et al.
3,227,881 10/1962 Gordon.
3,242,338 3/1966 Danforth et al.
3,002,091 9/1961 Armstrong 250106 X 3,254,210 5/1966 Schmitt 25043.5
3,335,278 8/1967 Price et al. 25083.1
ARCHIE R. BORCHELT, Primary Examiner S. ELBAUM, Assistant Examiner US. Cl. X.R. 25 043.5
UNITED STATES PATENT OFFICE CERTIFICATE OF CORRECTION Patent No. 3 486, 027 Dated December 23, 1969 Inventor(s) Henry W, Alter It is certified that error appears in the above-identified patent and that said Letters Patent are hereby corrected as shown below:
Column 1, line 68, line omitted after the word "track", should be (new paragraph) This invention uses solid-state nuclear -dete ctor 5.
Column 4,
track--. Column 3, line 73, "tracers" should be --tracer--. line 6, "requirer" should be --required--; line 9, "grouped" should be --ground--. Column 5, line 8, "Ihen" should be --'l en--; line 27, line omitted after the word "more", should be --than 10 particles per 1000 cubic feet will be found in such a--. Column 6, line 72, delete the comma after "distinguishable".
SIGNED AN'U Q FTiLED 6 Anew Edward M. Fletcher, Ir. WILLIAM E- SGH L Oomissionor of Patents FORM po'losu (@697 uscoMM-oc 60376-969 i ILS GOVERNNENT PRINYH'G OFFICE: \D" 0-36-3!
US580873A 1966-09-21 1966-09-21 Track registration bulk tracing method Expired - Lifetime US3486027A (en)

Applications Claiming Priority (1)

Application Number Priority Date Filing Date Title
US58087366A 1966-09-21 1966-09-21

Publications (1)

Publication Number Publication Date
US3486027A true US3486027A (en) 1969-12-23

Family

ID=24322929

Family Applications (1)

Application Number Title Priority Date Filing Date
US580873A Expired - Lifetime US3486027A (en) 1966-09-21 1966-09-21 Track registration bulk tracing method

Country Status (1)

Country Link
US (1) US3486027A (en)

Citations (7)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
US2874303A (en) * 1953-11-17 1959-02-17 William B Lane Method and apparatus for controlling refractory lined furnace temperatures
US3002091A (en) * 1958-11-03 1961-09-26 Frederick E Armstrong Method of tracing the flow of liquids by use of post radioactivation of tracer substances
US3149233A (en) * 1960-06-30 1964-09-15 Standard Oil Co Multiple tracer tagging technique
US3227881A (en) * 1962-10-15 1966-01-04 Shell Oil Co Corrosion monitoring by activation analysis
US3242338A (en) * 1958-11-03 1966-03-22 Gen Motors Corp Method for wear testing
US3254210A (en) * 1961-08-16 1966-05-31 Gen Dynamics Corp Method for determining organically bound halide in a liquid
US3335278A (en) * 1963-09-11 1967-08-08 Gen Electric High level radiation dosimeter having a sheet which is permeable to damage track producing particles

Patent Citations (7)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
US2874303A (en) * 1953-11-17 1959-02-17 William B Lane Method and apparatus for controlling refractory lined furnace temperatures
US3002091A (en) * 1958-11-03 1961-09-26 Frederick E Armstrong Method of tracing the flow of liquids by use of post radioactivation of tracer substances
US3242338A (en) * 1958-11-03 1966-03-22 Gen Motors Corp Method for wear testing
US3149233A (en) * 1960-06-30 1964-09-15 Standard Oil Co Multiple tracer tagging technique
US3254210A (en) * 1961-08-16 1966-05-31 Gen Dynamics Corp Method for determining organically bound halide in a liquid
US3227881A (en) * 1962-10-15 1966-01-04 Shell Oil Co Corrosion monitoring by activation analysis
US3335278A (en) * 1963-09-11 1967-08-08 Gen Electric High level radiation dosimeter having a sheet which is permeable to damage track producing particles

Similar Documents

Publication Publication Date Title
McDowell Liquid scintillation alpha spectrometry
Fleischer et al. Uranium and boron content of water by particle track etching
Moore et al. Age determinations of fossil corals using 230Th/234Th and 230Th/227Th
Salbu et al. Sources contributing to radionuclides in the environment: with focus on radioactive particles
Todd et al. A new method for the rapid measurement of 224Ra in natural waters
Cazala et al. Improvement in the determination of 238U, 228-234Th, 226-228Ra, 210Pb, and 7Be by γ spectrometry on evaporated fresh water samples
Bhat et al. Radiometric and trace element studies of ferromanganese nodules
US3486027A (en) Track registration bulk tracing method
Goswani et al. Estimation of uranium and boron contents in plants and soils by nuclear particle etch technique
Assinder et al. Neptunium in intertidal coastal and estuarine sediments in the Irish Sea
Dudey et al. APPLICATION OF ACTIVATION ANALYSIS AND Ge (Li) Ge (Li) DETECTION TECHNIQUES FOR THE DETERMINATION OF STABLE ELEMENTS IN MARINE AEROSOLS¹
Lo et al. Location, identification, and size distribution of depleted uranium grains in reservoir sediments
McHenry et al. The use of radioactive tracers in sedimentation research
Degueldre Identification and Speciation of Actinides in the Environment
Bhandari et al. A rapid beta gamma coincidence technique for determination of natural radionuclides in marine deposits
Lavrenchik Global Fallout Products of Nuclear Explosions
Ali Determination of radon gas concentrations 222 Rn in water samples of Rivers and ground wells in Basrah Governorate, Iraq.
Liehu Geological analysis by track etch method
Johnson LOS ALAMOS LAND AREAS ENVIRONMENTAL RADIATION SURVEY 1972.
Barker Determination of Radioactive Materials in Water
Baudisch et al. Geochemistry of the Saratoga Basin, the radioactivity of Saratoga Spring waters and rocks
de Moraes et al. Radon detection in soils by solid state nuclear track detectors
Lee Operational Characteristics of a Fission Gas Detector
Su Determination of trace quantity of alpha emitter by isotope dilution method using solid state nuclear track detector
Bondareva et al. New data on the level of contamination with tritium aerosol fallout in the nearest influence zone of the mining–chemical combine of the Rosatom State Corporation