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General Kenneth Nichols and the Manhattan Project
Nichols
The Oak Ridger has published the latest in a series of articles about General Kenneth D. Nichols, the Manhattan Project, and the 1954 Atomic Energy Act. The series has been produced by Nichols’ grandniece Barbara Rogers Scollin and Oak Ridge (Tenn.) city historian David Ray Smith. Gen. Nichols (1907–2000) was the district engineer for the Manhattan Engineer District during the Manhattan Project.
As Smith and Scollin explain, Nichols “had supervision of the research and development connected with, and the design, construction, and operation of, all plants required to produce plutonium-239 and uranium-235, including the construction of the towns of Oak Ridge, Tennessee, and Richland, Washington. The responsibility of his position was massive as he oversaw a workforce of both military and civilian personnel of approximately 125,000; his Oak Ridge office became the center of the wartime atomic energy’s activities.”
W. Brian Clarke, Stanley J. Bos, Brian M. Oliver
Fusion Science and Technology | Volume 43 | Number 2 | March 2003 | Pages 250-255
Technical Note | doi.org/10.13182/FST03-A264
Articles are hosted by Taylor and Francis Online.
Measurements of He, 3He/4He, Ne and 13 other components (H2, HD, D2, CH4, H2O, HDO, D2O, N2, CO, C2H6, O2, Ar, and CO2) in four samples of gas from SRI International (SRI) are reported. Three samples were collected from SRI Case-type stainless steel cells containing ~10 g of Pd/C catalyst initially loaded with ~3 atm D2 at ~200°C, and the fourth sample (not identified) was stated to be a control. Case and the SRI researchers have claimed to observe 4He in concentrations of ~100 parts per million (ppm) and up to 11 ppm, respectively, produced in these cells via the fusion reaction D + D = 4He + 23.8 MeV. Others found no evidence for 4He addition that cannot be readily explained by leaks from the atmosphere into the SRI cells. One sample appears to be identical in composition to air, and the other three have been seriously affected by leak(s) into and from the SRI cells. The rare gas "forensic" evidence includes 3He/4He ratios and He and Ne concentrations that are almost identical to air values. The samples also show high N2 (a primary indicator of air), low O2, and high CO and CO2 due to reaction of incoming atmospheric O2 with C in the catalyst. In two samples, the original D2 (or H2) has almost completely disappeared by outflow through the leak(s). These results have obvious implications concerning the validity of the excess 4He concentrations claimed by Case and the SRI researchers.