Differential ionization studies at forward anglesSpringer Science and Business Media LLC - Tập 89 - Trang 129-131 - 1994
á. Kövér, G. Laricchia, M. Charlton
The energy distribution of the scattered positron and electron projectiles
following ionization of Ar have been measured around 0‡ and 100 eV impact
energy. At 30‡ an estimate of the absolute double differential cross-section of
both outgoing particles (electron and positron) was determined at 100 eV impact
energy.
A laser ion source for on-line mass separationSpringer Science and Business Media LLC - Tập 74 - Trang 193-204 - 1992
P. Van Duppen, P. Dendooven, M. Huyse, L. Vermeeren, Z. N. Qamhieh, R. E. Silverans, E. Vandeweert
A laser ion source based on resonance photo ionization in a gas cell is
proposed. The gas cell, filled with helium, consists of a target chamber in
which the recoil products are stopped and neutralized, and an ionization chamber
where the atoms of interest are selectively ionized by the laser light. The
extraction of the ions from the ionization chamber through the exit hole and
skimmer is similar... hiện toàn bộ
Transverse field dependence of muonium relaxation: Spin exchange and chemical reactionSpringer Science and Business Media LLC - Tập 87 - Trang 965-970 - 1994
Masayoshi Senba, James J. Pan, Donald J. Arseneau, Susan Baer, Mee Shelley, Rodney Snooks, Donald G. Fleming
It has been shown experimentally that the muonium relaxation due to spin
exchange is 1.5 times faster in intermediate transverse fields (say, atB=50 G,
where the so-called two-frequency muonium signal is observed) than in low fields
(say, atB=5 G), in agreement with an earlier theoretical prediction. It has also
been confirmed experimentally that this distinct field dependence is totally
absent in... hiện toàn bộ
Coherent excitation of multilevel systems by laser radiationSpringer Science and Business Media LLC - Tập 37 - Trang 49-70 - 1987
A. A. Makarov
Different problems of coherent quasi-resonant excitation of multilevel systems
in monochromatic radiation fields are discussed. Analytically solvable examples
are presented, and, on this basis, some principal effects of cohrent multilevel
dynamics are treated.
Zero and longitudinal field μSR in UAsSpringer Science and Business Media LLC - Tập 64 - Trang 449-451 - 1991
A. Kratzer, G. M. Kalvius, L. Asch, F. J. Litterst, F. N. Gygax, B. Hitti, A. Schenck, C. A. Scott, K. Mattenberger, O. Vogt
Recent Results on Ne and Mg from the MISTRAL Mass Measurement Program at ISOLDESpringer Science and Business Media LLC - - 2001
D. Lunney, C. Monsanglant, G. Audi, G. Bollen, C. Borcea, H. Doubre, C. Gaulard, S. Henry, M. deSaintSimon, C. Thibault, C. Toader, N. Vieira
The MISTRAL experiment (Mass measurements at ISOLDE with a Transmission and
Radiofrequency spectrometer on-Line), conceived for very short-lived nuclides,
has reached the end of its commissioning phase. Installed in 1997, results have
been obtained consistent with all aspects of the projected spectrometer
performance: nuclides with half-lives as short as 30 ms have been measured and
accuracies of ... hiện toàn bộ
Temperature dependence of the hyperfine quadrupolar interaction in K2ZrF6Springer Science and Business Media LLC - Tập 13 - Trang 307-313 - 1983
J. A. Martínez, A. M. Rodríguez, M. C. Caracoche, R. C. Mercader, A. R. López Garcia, P. C. Rivas
The thermal dependence of the hyperfine quadrupolar interaction of181Ta at Zr
sites in K2ZrF6 has been studied by TDPAC between RT and 511 °C. Four phases of
ever increasing symmetry have been found in the range RT-437 °C. The possible
existence of a healing mechanism with an activation energy of 0.187±0.040 eV is
discussed for the lattice recovery in the range 270 °C–335 °C. The results at
temper... hiện toàn bộ
Determination of Iron Oxidation State in Omphacites Applied to Geothermometry of Sudetic EclogitesSpringer Science and Business Media LLC - Tập 112 - Trang 223-226 - 1998
J. Galazka-Friedman, E.R. Bauminger, N. Bakun-Czubarow
A common mineral geothermometer for eclogites is based on Fe2+-Mg exchange
reaction between garnets and clinopyroxenes. For the accurate determination of
Fe2+ in omphacites, ten omphacite samples were isolated from eight Sudetic
eclogites and studied by electron microprobe and Mössbauer spectroscopy.
Garnet-clinopyroxene equilibration temperatures for two Sudetic eclogites were
calculated.