Direct Observation of Orbital Ordering in Layered Manganites

2005 ◽  
Vol 18 (5-6) ◽  
pp. 687-691 ◽  
Author(s):  
P. D. Hatton ◽  
S. B. Wilkins ◽  
T. A. W. Beale ◽  
T. Johal ◽  
D. Prabhakaran ◽  
...  
1999 ◽  
Vol 38 (S1) ◽  
pp. 360 ◽  
Author(s):  
Y. Murakami ◽  
J. P. Hill ◽  
D. Gibbs ◽  
M. Blume ◽  
H. Kawada ◽  
...  

2001 ◽  
Vol 70 (12) ◽  
pp. 3475-3478 ◽  
Author(s):  
Jun Akimitsu ◽  
Hirohiko Ichikawa ◽  
Naotoshi Eguchi ◽  
Tomoko Miyano ◽  
Masakazu Nishi ◽  
...  

1998 ◽  
Vol 80 (9) ◽  
pp. 1932-1935 ◽  
Author(s):  
Y. Murakami ◽  
H. Kawada ◽  
H. Kawata ◽  
M. Tanaka ◽  
T. Arima ◽  
...  

2000 ◽  
Vol 281-282 ◽  
pp. 485-486 ◽  
Author(s):  
L. Paolasini ◽  
C. Vettier ◽  
F. De Bergevin ◽  
F. Yakhou ◽  
D. Mannix ◽  
...  

2003 ◽  
Vol 91 (16) ◽  
Author(s):  
S. B. Wilkins ◽  
P. D. Spencer ◽  
P. D. Hatton ◽  
S. P. Collins ◽  
M. D. Roper ◽  
...  

2000 ◽  
Vol 281-282 ◽  
pp. 482-484 ◽  
Author(s):  
H. Ichikawa ◽  
J. Akimitsu ◽  
M. Nishi ◽  
K. Kakurai

Author(s):  
R. W. Anderson ◽  
D. L. Senecal

A problem was presented to observe the packing densities of deposits of sub-micron corrosion product particles. The deposits were 5-100 mils thick and had formed on the inside surfaces of 3/8 inch diameter Zircaloy-2 heat exchanger tubes. The particles were iron oxides deposited from flowing water and consequently were only weakly bonded. Particular care was required during handling to preserve the original formations of the deposits. The specimen preparation method described below allowed direct observation of cross sections of the deposit layers by transmission electron microscopy.The specimens were short sections of the tubes (about 3 inches long) that were carefully cut from the systems. The insides of the tube sections were first coated with a thin layer of a fluid epoxy resin by dipping. This coating served to impregnate the deposit layer as well as to protect the layer if subsequent handling were required.


Author(s):  
John M. Wehrung ◽  
Richard J. Harniman

Water tables in aquifer regions of the southwest United States are dropping off at a rate which is greater than can be replaced by natural means. It is estimated that by 1985 wells will run dry in this region unless adequate artificial recharging can be accomplished. Recharging with surface water is limited by the plugging of permeable rock formations underground by clay particles and organic debris.A controlled study was initiated in which sand grains were used as the rock formation and water with known clay concentrations as the recharge media. The plugging mechanism was investigated by direct observation in the SEM of frozen hydrated sand samples from selected depths.


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