scholarly journals The future of high-pressure mineral physics

Eos ◽  
2005 ◽  
Vol 86 (40) ◽  
pp. 365 ◽  
Author(s):  
Robert C. Liebermann
Science ◽  
1993 ◽  
Vol 262 (5132) ◽  
pp. 370-372 ◽  
Author(s):  
E. Ito

Minerals ◽  
2020 ◽  
Vol 10 (4) ◽  
pp. 344
Author(s):  
William A. Bassett

The late Taro Takahashi earned a particularly well-deserved reputation for his research at Lamont Geological Observatory on carbon dioxide and its transfer between the atmosphere and the oceans. However, his accomplishments in Mineral Physics, the field embracing the high-pressure–high-temperature properties of materials, has received less attention in spite of his major contributions to this emerging field focused on the interiors of Earth and other planets. In 1963, I was thrilled when he was offered a faculty position in the Geology Department at the University of Rochester, where I had recently joined the faculty. Taro and I worked together for the next 10 years with our talented students exploring the blossoming field just becoming known as Mineral Physics, the name introduced by Orson Anderson and Ed Schreiber, who were also engaged in measuring physical properties at high pressures and temperatures. While their specialty was ultrasonic velocities in minerals subjected to high pressures and temperatures, ours was the determination of crystal structures, compressibilities, and densities of such minerals as iron, its alloys, and silicate minerals, especially those synthesized at high-pressure, such as silicates with the spinel structure. These were materials expected to be found in the Earth’s interior and could therefore provide background for the interpretation of geophysical observations.


Minerals ◽  
2019 ◽  
Vol 9 (12) ◽  
pp. 761
Author(s):  
Robert Cooper Liebermann

In 1976, I took up a faculty position in the Department of Geosciences of Stony Brook University. Over the next half century, in collaboration with graduate students from the U.S., China and Russia and postdoctoral colleagues from Australia, France and Japan, we pursued studies of the elastic properties of minerals (and their structural analogues) at high pressures and temperatures. In the 1980s, together with Donald Weidner, we established the Stony Brook High Pressure Laboratory and the Mineral Physics Institute. In 1991, in collaboration with Alexandra Navrotsky at Princeton University and Charles Prewitt at the Geophysical Laboratory, we founded the NSF Science and Technology Center for High Pressure Research.


1991 ◽  
Vol 18 (6) ◽  
pp. 1147-1150 ◽  
Author(s):  
R. Boehler ◽  
A. Chopelas

2011 ◽  
Vol 67 (a1) ◽  
pp. C526-C527
Author(s):  
N. Hirao ◽  
Y. Ohishi ◽  
T. Matsuoka ◽  
T. Mitsui ◽  
E. Ohtani

2021 ◽  
Vol 245 ◽  
pp. 01043
Author(s):  
Xuchen Zhu ◽  
Yannan Du ◽  
Bin Ren ◽  
Xiaoying Tang ◽  
Zhigang Yang ◽  
...  

Because of its structural characteristics, the serpentine high-pressure heater has thinner tubesheet compared with the traditional U-tube high-pressure heater, which solves the bottleneck of tubesheet manufacturing and becomes an important auxiliary machine for millions of secondary reheating units in the future. In this paper, the typical working conditions are selected, and the bending design methods of domestic and foreign serpentine tubes are adopted respectively. The results show that compared with Chinese standards, the bending can be thinned. Subsequent tests and finite element simulations verify the reliability of foreign methods and explore the optimization design methods of domestic serpentine tubes.


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