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Bombing-Test

For estimating filtration rate (therefore, operating pressure and size of the filter), washing characteristics, and other important features, small-scale tests such as the leaf or pressure bomb tests described earlier are usually essential. In the conduct and interpretation of such tests, and for advice on labor requirements, maintenance schedule, and selection of accessory equipment the assistance of a dependable equipment vendor is advisable. [Pg.1723]

At the Installation, Sakharov worked with many colleagues, in particular Yakov Zcldnvich and David Frank-Kamenetskii. Sakharov made key contributions to the Soviets first full-fledged H-bomb, tested in 1955. He also made many contributions to basic physics, perhaps the most important being his thesis that the universe is composed of matter (rather than all matter having been annihilated against antimatter) is likely to be related to charge-parity (CP) noninvariance. [Pg.1026]

July 16. First atomic bomb test at Aamogordo, New Mexico, under the code name Manhattan Project. ... [Pg.1247]

Heat Test. Loss 1st 48 hrs 0,07% loss 2nd 48 hrs 0.00% explosion in 100 hrs none Hygroscopicity. % wt gain at 30°, 90% RH trace Vacuum Stability Test, cc/40 hrs at 90° none 100° none 120° 0.11 Sand Bomb Test (200g). 16.3 g sand Sensitivity to Initiation. Minimum detonating charge, g LA 0.20 Tetryl 0.25 Solubility. g/lOOcc solvent in water at 100° 0.10 NB at 150°, <15. Sol in acet ac, nitric acid, caustic potash v sol in dimethyl form-amide insol in ethyl ale, benz, butyl acetate, CC14 ethyl ether (Ref 6)... [Pg.439]

Oxidation. Based on the Norma-Hoff max oxidation bomb test, the phosphorus shall show the following oxidation characteristics Induction period — the minimum induction period shall be 20 hours. Oxidation rate — the maximum... [Pg.729]

Nuclear bomb produced " 002 and (as HTO) have been used to describe and model this rapid thermocline ventilation (Ostlund et ah, 1974 Sarmiento et ah, 1982 Fine et al., 1983). For example, changes in the distributions of tritium (Rooth and Ostlund, 1972) in the western Atlantic between 1972 (GEOSECS) and 1981 (TTO) are shown in Fig. 10-10 (Ostlund and Fine, 1979 Baes and Mulholland, 1985). In the 10 years following the atmospheric bomb tests of the early 1960s, a massive penetration of F1 (tritium) into the thermocline has occurred at all depths. Comparison of the GEOSECS and TTO data, which have a 9 year time difference, clearly shows the rapid ventilation of the North Atlantic and the value of such transient" tracers. A similar transient effect can be seen in the penetrative distribution of manmade chlorofluorocarbons, which have been released over a longer period (40 years) (Gammon et al., 1982). [Pg.241]

The gross flux of carbon from atmosphere to ocean is thus ca. 80 Pg C/yr. There are several complications with the above calculation. The isotopic ratios must be steady-state values, which are unavailable due to the changes resulting from atmospheric atom bomb testing. The few available pre-bomb measurements from the late 1950s (Broecker et ah, 1960) together with determinations in corals (Druffel and Linick, 1978) are invaluable tools for determin-... [Pg.300]

Let s calculate the mass that was converted into energy in the first atomic bomb test. Measurements on the ground indicated that the explosive force of the bomb was equivalent to 37,200,000 pounds (16,874,000 kg) of TNT. That is so much TNT that scientists now measure atomic bomb explosions in kilotons (kt) of TNT. A kiloton is equal to 1,000 tons or 2,000,000 pounds (907,185 kg). Using the new units, the yield of the first bomb would be ... [Pg.40]

Reference materials for radioisotopes have mainly been used for purposes relating to nuclear and radiation safety. Historically, the development of such materials first arose from the need to assess the risk to human populations caused by worldwide contamination of food and the environment as a consequence of atomic bomb testing - particularly from bombs exploded in the atmosphere. Even now, although atmospheric testing ceased many years ago, the residues from these tests still remain the main source of radionuclides such as Cs and °Sr in the global environment (though locally, other sources may be more important in some countries). [Pg.143]

There are also a number of less continuous but still natural net heat sources e.g. the heat released from volcanoes, earth quakes, and meteorites. There are also some anthropogenic sources form nuclear bomb tests, conventional bombs and explosives. [Pg.77]

At the same time, the public s faith in science and technology was eroding. Radioactive fallout from atomic bomb tests was poisoning cows milk, and the thalidomide antinausea medicine prescribed to pregnant women in Europe had caused severe birth defects in 8000 children. Above all, the enormous growth of the chemical industry and pollution after World War II put public pressure on Congress to clean up the nation s air and water. [Pg.166]

Tim Beardsley. Testing s Toll. Scientific American. 273 (Aug. 1995) 28. Source for bomb tests. [Pg.234]

A mass of evidence seems to confirm that the mixing rate of radiocarbon in the atmosphere is rapid, and that with respect to its radiocarbon content the atmosphere can be considered as a homogeneous entirety. The contamination of samples with matter from an extraneous source can nevertheless invalidate this assumption. Two types of contamination can be differentiated physicochemical contamination and mechanical intrusion. There are two forms of physicochemical contamination. One is due to the dilution of the concentration of radiocarbon in the atmosphere by very old carbon, practically depleted of radiocarbon, released by the combustion of fossil fuel, such as coal and oil. The other is by the contamination with radiocarbon produced by nuclear bomb tests during the 1950s and later in the twentieth century. The uncertainties introduced by these forms of contamination complicate the interpretation of data obtained by the radiocarbon dating method and restrict its accuracy and the effective time range of dating. [Pg.310]

Radioactive substances Atmospheric faiiout from bomb testing ioss from sunken submarines emissions in cooiing waters of nuciear power piants Bioaccumuiation into seafood poses heaith risk to humans. [Pg.770]

The scope and scale of pollution from radionuclides has been greatly reduced due to (1) the cessation of aboveground nuclear bomb testing, (2) an international ban on the dumping of nuclear wastes at sea, and (3) better control of discharges from power and fuel reprocessing plants. [Pg.807]

When using the positive pressure method it is sometimes either impractical or in fact impossible to measure the leakage rate directly while it could certainly be sensed in an envelope which encloses the test specimen. The measurement can be made by connecting that envelope to the leak detector or by accumulation (increasing the concentration) of the test gas inside the envelope. The bombing test is a special version of the accumulation test (see Section 5.7.4). In the so-called sniffer technique, another variation of the of the positive pressure technique, the (test) gas... [Pg.113]

When dealing with small, hermetically sealed parts where the enclosure is leaky, krypton 85, a gaseous, radioactive isotope, can first be forced into the device by applying pressure from the outside. Once an exactly measured holding period has elapsed the pressure will be relieved, the component flushed and the activity of the gas charge will be measured. In the same way it is also possible to use helium as the test gas (see Section 5.7.4, bombing test). [Pg.115]

The bombing test is use to check the tightness of components which are already hermetically sealed and which exhibit a gas-filled, internal cavity. The components to be examined (e.g. transistors, 1C housings, dry-reed relays, reed contact sw/itches, quartz oscillators, laser diodes and the like) are placed in a pressure vessel which is filled with helium. Operating with the test gas at relatively high pressure (5 to 10 bar) and leaving the system standing over several hours the test gas (helium) will collect inside the... [Pg.123]

Accdg to Ref 14, p 9-49, the tests may be performed with Test Set Mkl72Modl (our Fig 6) Test Set 180Mod0 (shown in Fig 9-25 of Ref 14) and Test Set Mkl48Mod0, which is a Sand Bomb Test, briefly discussed under "Output Tests for Electric Detonators ... [Pg.1087]


See other pages where Bombing-Test is mentioned: [Pg.247]    [Pg.20]    [Pg.38]    [Pg.853]    [Pg.133]    [Pg.440]    [Pg.950]    [Pg.81]    [Pg.258]    [Pg.306]    [Pg.144]    [Pg.178]    [Pg.192]    [Pg.82]    [Pg.22]    [Pg.27]    [Pg.330]    [Pg.53]    [Pg.333]    [Pg.140]    [Pg.282]    [Pg.807]    [Pg.921]    [Pg.123]    [Pg.452]    [Pg.285]    [Pg.213]    [Pg.1085]    [Pg.143]   
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Atom bomb tests

Atomic bomb testing

Atomic bomb tests

Bomb drop test

Bomb tests

Bomb, chemical testing

Hydrogen bomb tests

Hydrogen cyanide bomb testing

Nuclear bomb testing

Nuclear bomb testing carbon

Nuclear bomb tests, atmospheric

Rotary bomb oxidation test

Sand test bomb

Soviet Union atomic bomb tested

Soviet Union hydrogen bomb tested

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