Isotherms for the uranium-hydrogen system at temperatures of 700–1065°C and pressures to 137.89 MPa
✍ Scribed by John F. Lakner
- Book ID
- 103891087
- Publisher
- Elsevier Science
- Year
- 1986
- Weight
- 266 KB
- Volume
- 139-140
- Category
- Article
- ISSN
- 0378-4363
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✦ Synopsis
Pressure vs composition (P-C) isotherms for the UH system for temperatures of 700-1065°C and pressures to 137.89 MPa are shown. The sample was contained in a concentric vessel and located within a secondary vessel. Plateau pressure at 1065°C is 700 atm. The single-phase region on the hydrogen-rich side starts at a H/U ratio of 2.35. Physical property measurements showed a thermal conductivity, k, value of 0.003 cal/cm s K, R c = 50. Experimentally determined plateau pressures are compared with values obtained by other workers. The UH system retains broad, two-phase plateaus at temperatures to 1065°C. The critical temperature must be above 1065°C.
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