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Physical Chemical, and Radiological Properties of Slurry Particulate Fallout Collected During Operation Redwing Research and Development Technical Report Usnrdl-TR-170 NS 088-001 5 May 1957

Dated
May 5, 1957
Document type
Report
Length
24 pages
Open the original scanArchive record OSTI ID 16079172 · public domain

Archive description

The properties of individual fallout particles produced by nuclear det onations at zero height over shallow sea water are analytically descri bed for the first time. The particles produced during operation redwi ng were slurry masses composed of water, dissolved and crystalline sea salts, and seawater-insoluble solids from the weapon, barge, and ocea n floor. Special techniques were used to measure the chloride, water, and insoluble-solids content of individual slurry particles. Autorad iography showed that the activity is primarily associated with the sol ids. A table of experimental data presents particle size versus time of arrival after detonation as well as measurements of particle densit y and relative specific activity. Estimates of mass and relative acti vity of fallout per unit area for certain locations about the shot poi nt are shown.

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Machine-read from the scan, so expect some errors. Lines that couldn’t be read are left out.

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I Fkproductiofi of this document in any .form by other than activiti+s of the Department of Defense is not authorized unless specifically approved by the Secretary of the Navy or the Chief of Naval Operations aa appropriate.

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PHYSICAL, CHEMICAL, AND RADIOLOGICAL PROPERTIES OF SLURRY PARTICULATE FALLOUT COLLECTED DURING Research and Development Technical Radiological Capabilities Branch Chemical Technology Division Commanding Officer and Director Captain Floyd B. Schultz, USN San Francisco 24, California

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The properties of individual fallout particles produced by nuclear detonations at zero height over shallow seta water are analytically described for the first time. The particles prom duced during Operation REDWING were slurry masses composed of water, dissolved and crystalline sea salts, and seawater-insoluble solids from the weapon, barge9 and ocean floor. Special techniques were used to measure the chloride o water, and insoluble -solids content of individual slurry par 0 titles. Autoradiography showed that the activity is primarily associated with the solids. A table of experimental data presents particle size versus time of arrival after detonation as well as measurements of particle density and relative specific activity. Estimates of mass and relative activity of fallout per unit area for certain locations about the shot point are shown.

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Nuclear devices fired over sea water at previous weapons tests yielded fallout which was different from that associated with land surface detonations. The analytical methods previously used on dry fallout were grossly inadequate for this Certain tests at Operation REDWING yielded slurry-like fallout. Therefore, new analytical methods were required to assess the material ,properly. The fallout from two seawater-surface nuclear events at Operation REDWING has been analyzed using new quantitative techniques for the measurement of chloride and slurry droplet water content. Particle size, density and radiological properties of the slurry fallout havebeenassessed satisfactorily for the first time.

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The experimental study reported was initiated to develop methods for the analysis of samples obtained from Project 2.6.3, Operation REDWING. The study was done under Bureau of Ships Project Number NS 088-001, Technical Objective SR-2, and is described as Program 2, Problem 1, in this laboratory’s “Preliminary Presentation of USNRDL Technical Program for FY 1957, It February 1956.

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and CDR T. E. Shea of the Bureau of Ships, Washington, Brooklyn, for their assistance in certain field phases of O’Connor of this laboratory’s Analytical and Standards Branch is noteworthy, The assistance by Mr, D, Puppione and Mr. V. DaGragnano , also of this laboratory, in data analysis is appreciated, The editorial advice given by Mr. J. Todd has been invaluable in the preparation of this report,

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Some of the nuclear devices fired in Operation REDWING during the Spring of 1956 at the Eniwetok Proving Ground were detonated on or near the surface of the lagoon water. Up to this time, only limited data had been gathered on the physical-chemical-radiological properties of individual fallout particles from such bursts. Therefore, two events, Flathead and Navajo, were selected as subjects for an extensive fallout study. The nuclear devices fired were situated on steel barges anchored in relatively deep lagoon water. The principal sources of material expected to comprise the fallout were the barge complex, the surrounding seawater and perhaps some lagoon bottom solids. It was hypothesized that sea salts would constitute the major portion of any fallout. With this in mind, a special reagent film’, quantitative for submicroscopic amounts of chloride, was developed. Since sea salts are hygroscopic, it was felt that the fallout particles would pick up atmospheric water and arrive at the sampling stations as slurry-like droplets. Therefore, the reagent film was calibrated to measure this water content.2 The influence of the barge complex on particle composition was unassessed prior to the Operation. Sampling stations were located at varying distances from the shot points e These stations were aboard anchored barges, type YFNB, and manned ships, type YAG and LST. An array of specialized .sampling devices was located at each station. Particles collected in the incremental type of collector, 3r4 were used for these fallout studies. Since this device sequentially exposed trays containing chloride reagent film, particles could be classified by time .of arrival. One of the ship sampling stations was connected by an elevator device to a radiation-shielded laboratory, permitting almost immediate examination of fallout samples D METHODS OF ANALYSIS The analytical methods developed were so devised that the physical, chemical, and radiological properties of the individual particles could

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be evaluated. Physical observation could detail the state of the material as it landed at the station, Chemical treatment would allow the separation and measurement of soluble salts and seawater-insoluble ones which were to be defined as “insoluble solids. ‘1 Radiological evaluation would assess the particle radioactivity. These experimental values then would define the physical state of the particles, particle size, density, particle specific activity9 total activity, and’mass of fallout per unit area. wsment of Phvsical Properti.es Visual observations made in the shielded laboratory confirmed the slurry droplet nature of the fallout. Crystalline materials were observed to be suspended. in the liquid portion of the droplets,, The characteristic cubic. shape of sodium chloride was detected. After the dissolution of soluble halides, an insoluble+olids component remained on the film. It was apparent that the slurry droplets contained three major constituents: water, soluble sea salts, and insoluble solids from the environmental Measurement nf Halide Content The reagent film for particle h.alide analysis utilized a commercial gelatin film in which colloidal red silver dichromate was precipitated by a special method. 1 Soluble halides deposited on the film were later dissolved by saturated hot water vapor and diffused into the gel structure where they were precipitated as silver salts. A microscope measurcment of the reaction area yielded, by calibration, the weight of halides reported as sodium chloride. by this method is from 10m6 to 10 easurable range of sodium chloride When a droplet strikes the reagent film it spreads to a certain constant degree related to the volume of water in the droplet,$ Insoluble solids within each fallout slurry droplet outlined this maximum spread on the collecting film. A calibration curve% was constructed giving the volume of wat.er in a slurry droplet as a function of the area covered by the ins oluble ==solids trace, This area has been termed the ~8s1urry artifact. I1 The smallest water volume measurable by this technique is

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Fig. 1 Reaction of Slurry Fallout Particle on Reagent Film. The white circular area is halide reaction representing 2.9 x 10m7 g NaCl. The central elliptical area is slurry artifact of insoluble solids representing 7.2 x low7 cc. Particle density is 1.19 g/cc. The annular rings in the chloride reaction area are thought to be

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Measurement of Insoluble-Solids Content No known chemical method can measure the weight or volume of insoluble solids in a deposited slurry fallout particle. Therefore, a method for comparing the volume of the fallout particle with standard volumes was developed. Five standard volumes ranging from 10B7 to 10-9 cc were used for the visual comparison in the microscope. They were formed by aspirating and collecting on reagent film small slurry droplets from measured aluminum oxide suspensions. The water content of each droplet was measured by its slurry artifact. By arithmetic proportion the approximate volume of aluminum oxide was known. Five appropriately sized aluminum oxide artifacts were mounted on a microscope slide as a comparison standard. Each fallout slurry artifact was then visually compared with the standards, and estimates made of the volume of insoluble solids. The physical-chemical composition of the fallout insoluble solids component is being investigated at this laboratory, Measurement of Radiolopical Properties After solution and diffusion of the soluble halides into the reagent film, autoradiographs were made by adaptations of the LaRiviere-Ichiki method. 6 These studies showed the activity to be primarily centered in the insoluble-solids portion of the fallout particle (Fig. 2). These solids were subjected to salt water leaching by the liquid phase of the droplet for at least part of their falling period. Ionic activity available for solution dissolved in this solvent. Upon striking the film the dissolved activity diffused with the water into the gelatin and there -was rigidly held. It was felt that if the active solids portion of fallout could be stripped from the film and both parts counted, a rough estimate of easily soluble ionic activity could be made. One Flathead film sample containing myriads of fallout impressions was selected for stripping and counting. The insoluble solids on the reagent film were thoroughly leached in hot water vapor at 7OoC for several hours allowing further diffusion of ionic activity into the film. While the gelatin of the reagent film was still tacky from the vapor treatments a thick layer of transparent acrylic spray was applied and allowed to dry, The assemblage was then soaked in distilled water for an hour to permit diffusing moisture to loosen the solids from the gel. The acrylic film was then stripped from the gelatin, removing most of the insoluble solids with it. This stripping process was repeated until no microscopically visible insoluble solids remained on the reagent film. The commercial gelatin of ‘the film is so tightly bound to its substrate

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that none is removed with the stripped solids. Confirmation of this was obtained by dissolving the acrylic film strippings in organic solvents and examining the solutions for insoluble gelatin pieces; none were observed. Both the stripped reagent film and the removed solids were counted in a crystal well counter. Sixteen percent of the activity remained on the reagent film. This represents. short-exposure, water-soluble activity together with certain colloidal size solids below the visible range of the microscope, Each of the many other fallout particles with its chloride reaction area was cut from the reagent film. The photon activity was then assessed in the crystal well counter containing a Z-in. NaI(T1) crystal with a sample well 3/4 in. in diameter and 1 -l/2 .in. deep. The counting efficiency for fission products is in the region of 40 percent. Decay and coincidence loss curves were constructed for the instrument using early time fallout, enabling activities of individual particles to be reliably corrected to The condensed and averaged data of Flathead and Navajo are presented in Table 1. The data are grouped in increments of time of arrival at the various ship stations. Some of the particles measured for one variable were not measured for others. Thus a maximum and minimum number of particles measured is sometimes reported for a given time It was found in general that the insoluble solids comprise less than 4 percent of the weight and less than 2 percent of the volume of slurry droplets o Therefore, in the size and density considerations this component was neglected. It was assumed that the water present in the slurry’particles was saturated with sodium chloride. The fact that dissolved sodium chloride occupies about 19 percent less volume in a saturated water solution than does an equal weight of dry crystalline sodium chloride was considered in the calculations. The activity is primarily associated with the insoluble solids. Since no precise measure of mass or volume of this component is available, activity as a function of sodium chloride mass is reported. Estimates were made of the specific activity of the insoluble solids. One method involved the direct stripping, weighing, and measuring of activity of solids from a reagent film. Another method involved the

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Fig. 2 Autoradiograph of Slurry Fallout Particle Trace and Its Chloride Reaction Area Showing the Radioactivity to be Concentrated in the Centrally Located Insoluble Solids Portion. The black central smear is the autoradiograph masking the solids. Patterns on the reagent film are caused by severe tropical sun reaction on the photosensitive film. Cirborne sea salt particles.

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Arrival Average Average Ship Particles NaCl Mass (a) The diameterof the sphericalslurrydropletat the time of arrival (c) Calculatedvalue based on total tray count,nmber of particlesper tray3 and averageNaCl mass per particle

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calculation of an average activity per slurry particle, and an estimate of the average volume and weight of insoluble solids per particle by the standard spot comparison method. The two independent methods gave an average value for Flathead of 1 x 1013 c/m/g at H t 12 in the well counter. The latter method only was used for Navajo, resulting in a value of 1 x 1012 c/m/g of insoluble Table 2 presents experimental data on the total activity per unit area for the two events for various stations. These data are in terms of a count (at H t 12) in the crystal well counter. The total mass of sodium chloride per unit area is a calculated value obtained by dividing the total activity per unit area for a given station (Table 2) by the average activity per NaCl mass (Table 1). Sodium chloride represents the major solid mass of fallout. Since the water content depends on the humidity conditions through which the particle passed, the weight of water is not considered a part of fallout mass. However, if one wishes to compute the approximate weight of water, one multiplies the mass of NaCl by 1.2. which is the average weight ratio of water to NaCl. A plot of the dependent variables, activity per unit area versus NaCl mass per unit area, presents Table 2 data as a necessarily smooth curve (Fig. 3). With this plot one can roughly deduce relative activity by a measure of sodium chloride per square foot or the converse. The very high initial values of sodium chloride mass per square foot have not been plotted on the The particle densities (Table 1) cluster about a mean value which is nearly the same for both events. The mean density for the 1- to 3-hr period is close to the overall mean value. By whatever means the ratio of water to solids reaches equilibrium, this mechanism is fairly rapid. Equilibrium has been reached by the time the particle lands. InNavajo there appears to be a sharp decrease in density after Ht13. This time corresponds to the after-sunset hours when changes in ambient atimospheric conditions might be expected. The particle size (Table 1, ltNavajolt) generally decreases with time, although it is noteworthy that there is little droplet size variation in 15 hr. For any given time period, one need not discuss particle size distribution since the standard deviation of the mean diameter is so small..

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Total Activity and Mass of Fallout Total Total Mass Total Total Mass (a) Photon count in crystal well counter at H+12.

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Early arriving particles appear to have a much higher ratio of so,dium chloride to activity than do later arrivals (,Table 1, last column. ) Such a variation might be indicative of early large droplet fallout from the cloud stem region where the concentration of activity may be less. The sampling is small, however, so caution must be exercised in the interpretation of these data. The calculations of .total mean values of specific activity (Table 1) do not include these initial values, nor does the calculation of this value for Navajo include the approximate values defined by footnote (c) of the table. …

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