Analysis and design of multipole, super-conducting rotating electric machines for ship propulsion.

Massachusetts Institute of Technology. Dept. of Mechanical Engineering. Thesis. 1974. M.S.MICROFICHE COPY ALSO AVAILABLE IN BARKER ENGINEERING LIBRARY.Includes bibliographical references.M.S

Analysis of loss mechanisms in superconducting windings for rotating electric generators

Thesis (Ph.D.)--Massachusetts Institute of Technology, Dept. of Mechanical Engineering, 1981.MICROFICHE COPY AVAILABLE IN ARCHIVES AND ENGINEERING.Vita.Includes bibliographical references.by Joseph Vito Minervini.Ph.D

RADIOGENIC ISOTOPE INVESTIGATION OF SOURCES, TRANSPORT, AND DEPOSITION OF RARE EARTH ELEMENTS IN THE OWENS LAKE DRAINAGE BASIN, EASTERN CALIFORNIA

Owens Lake is situated in a mostly-closed basin fed by water and sediments derived primarily from the eastern Sierra Nevada range. Radiogenic isotope variations in USGS Owens Lake core OL-92 were used in conjunction with major and trace element concentrations in streams draining the eastern Sierras to investigate sediment provenance, the chemical weathering and transport of rare earth elements (REE) in the Owens Lake drainage basin, and possible climate-related shifts in weathering patterns of the eastern Sierras during the last ~30 ka. Filtered (<0.45 μm) stream water samples not influenced by hydrothermal fluids or agriculture fall below world average-normalized values for major cations. Concentrations of Nd in the stream water samples are less than 1 nmol L-1, too dilute for isotopic analysis. Strontium and neodymium isotopic analyses were conducted on the carbonate and silicate fractions of sediment samples representing deposition in Owens Lake from ~30 ka to ~10 ka. The fraction of carbonate in Owens Lake sediments increases from ~7 to 67 % during this period, reflecting the desiccation of the lake. Strontium, samarium, and neodymium are strongly partitioned into Owens Lake chemical sediments. Over the past ~30 ka, epsilon Nd values of clastic sediments in Owens Lake remain relatively constant, near -6.5. Chemical sediments remain approximately one epsilon unit higher than the clastic sediments until ~12 ka ago, at which time they shift to less radiogenic values, matching those of the clastic sediment. Differential mineral weathering of more common mineral phases over REE-enriched accessory phases is the most likely cause of the isotopic shift in Owens Lake chemical sediments at ~12 ka ago. Preferential weathering of hornblende could displace the Nd isotopic composition of Owens Lake chemical sediments away from that of the clastic fraction. Depletion of hornblende could allow the Nd isotopic composition of the two sediment fractions to return to similar values. This study represents the first Nd isotope study of a lacustrine system and suggests Nd isotopes could be a useful paleoclimate proxy. Additional work in older Owens Lake sediments and in other lake systems is clearly warranted