A STUDY ON BEHAVIOR OF VU PIPE WITH OVERBURDEN PRESSURE UNDER APPLICATION OF INTERNAL LOADING METHOD

Author(s):  
Koki OYAMA ◽  
Masahiro HYODO ◽  
Masaya NISHIGUCHI ◽  
Hidehiko OGATA ◽  
Masayuki ISHII
Author(s):  
Koki OYAMA ◽  
Masahiro HYODO ◽  
Hidehiko OGATA ◽  
Masayuki ISHII ◽  
Kazuhiro UENO

2018 ◽  
Vol 42 (3) ◽  
pp. 170-174 ◽  
Author(s):  
Feng Li ◽  
Wenxi Zhu ◽  
Jinrong Liang ◽  
Hua Song ◽  
Keliang Wang ◽  
...  

A series of carbon nanotube (CNT)-supported amorphous Co–B alloy catalysts were prepared by selectively depositing Co–B particles inside and/or outside of CNTs. The effects of the nanotubular structure on the physiochemical properties of the amorphous Co–B alloys were studied. It was found that the internal loading enhanced the thermal stability of the amorphous Co–B alloys and inhibited the loss of Co compared with the external loading. The internal loading also increased the proportion of elemental Co in the Co–B alloys, while the loading method did not change the valence states of either Co or B. The internally loaded Co–B particles exhibited higher hydrogenation activity for m-chloronitrobenzene ( m-CNB) than the externally loaded analogue. The kinetics of m-CNB hydrogenation were also studied.


1997 ◽  
Vol 48 (7) ◽  
pp. 726-735 ◽  
Author(s):  
Fuh‐Hwa F Liu ◽  
C‐J Hsiao

2017 ◽  
Vol 137 (6) ◽  
pp. 826-833
Author(s):  
Takaho Sekiguchi ◽  
Hiromu Odanaka ◽  
Yoshinobu Okano ◽  
Satoshi Ogino

1997 ◽  
Vol 24 ◽  
pp. 181-185 ◽  
Author(s):  
Katsuhisa Kawashima ◽  
Tomomi Yamada

The densification of water-saturated firn, which had formed just above the firn-ice transition in the wet-snow zone of temperate glaciers, was investigated by compression tests under pressures ranging from 0.036 to 0.173 MPa, with special reference to the relationship between densification rate, time and pressure. At each test, the logarithm of the densification rate was proportional to the logarithm of the time, and its proportionality constant increased exponentially with increasing pressure. The time necessary for ice formation in the firn aquifer was calculated using the empirical formula obtained from the tests. Consequently, the necessary time decreased exponentially as the pressure increased, which shows that the transformation from firn in ice can be completed within the period when the firn aquifer exists, if the overburden pressure acting on the water-saturated firn is above 0.12–0.14 MPa. This critical value of pressure was in good agreement with the overburden pressure obtained from depth–density curves of temperate glaciers. It was concluded that the depth of firn–ice transition was self-balanced by the overburden pressure to result in the concentration between 20 and 30 m.


Author(s):  
Chengcheng Liu ◽  
Koichi Suematsu ◽  
Akihito Uchiyama ◽  
Ken Watanabe ◽  
Yanbao Guo ◽  
...  

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