Isotope shift between U234 and U238 in secondary uranium minerals of some hydrothermal deposits

1965 ◽  
Vol 19 (1) ◽  
pp. 964-966
Author(s):  
P. I. Chalov ◽  
Ya. A. Musin ◽  
T. V. Tuzova ◽  
K. I. Merkulova
Keyword(s):  
Isotope Shift ◽  
Hydrothermal Deposits ◽  
Uranium Minerals

DIAMAGNETIC ANISOTROPY, ISOTOPE SHIFT AND COOLING-SPEED EFFECTS IN SUPERCONDUCTING (TMTSF)2C104CRYSTALS

1983 ◽  
Vol 44 (C3) ◽  
pp. C3-1041-C3-1045 ◽  
Author(s):  
H. Schwenk ◽  
K. Andres ◽  
F. Wudl ◽  
E. Aharon-Shalom
Keyword(s):  
Isotope Shift ◽  
Diamagnetic Anisotropy ◽  
Cooling Speed

Mercury-204 Determination by Emission Spectroscopy

1965 ◽  
Vol 19 (3) ◽  
pp. 87-89 ◽  
Author(s):  
F. M. Smith
Keyword(s):  
Coefficient Of Variation ◽  
Isotope Shift ◽  
Emission Spectroscopy ◽  
Electrodeless Discharge ◽  
Discharge Lamp ◽  
Isotope Concentration ◽  
Single Determination ◽  
Time Required

The determination of mercury-204 was made by using the isotope shift of the 3984 A mercury line excited by electrodeless discharge. Densitometric traces were made from film recordings of the 3984 A line and the areas under the component peaks were determined. Ratios of each of these areas to the sum of the areas from all the line components are plotted against the isotope concentration to produce a working curve. The coefficient of variation for this method is approximately 11 percent The time required for a single determination (after fabrication of the discharge lamp) is about two hours.

Jdependences of the isotope shift and hyperfine structure in Gd i 4f75d6s29D, 4f75d6s6p9D, and9Fterms

1990 ◽  
Vol 42 (3) ◽  
pp. 1416-1423 ◽  
Author(s):  
W. G. Jin ◽  
H. Sakata ◽  
M. Wakasugi ◽  
T. Horiguchi ◽  
Y. Yoshizawa
Keyword(s):  
Hyperfine Structure ◽  
Isotope Shift

J and term dependences in the isotope shift of Eu I

1986 ◽  
Vol 1 (1) ◽  
pp. 55-64 ◽  
Author(s):  
H. Br�ggemeyer ◽  
H. Esrom ◽  
V. Pfeufer ◽  
A. Steudel ◽  
J. Bauche
Keyword(s):  
Isotope Shift
Sign in / Sign up

Export Citation Format

Share Document