Institution
Tokyo Institute of Technology
Education•Tokyo, Tôkyô, Japan•
About: Tokyo Institute of Technology is a education organization based out in Tokyo, Tôkyô, Japan. It is known for research contribution in the topics: Thin film & Catalysis. The organization has 46775 authors who have published 101656 publications receiving 2357893 citations. The organization is also known as: Tokyo Tech & Tokodai.
Topics: Thin film, Catalysis, Polymerization, Laser, Phase (matter)
Papers published on a yearly basis
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TL;DR: In this article, a new numerical method is proposed for multidimensional hyperbolic equations, which uses a cubic spatial profile within grids, and is described in an explicit finite-difference form by assuming that both the physical quantity and its spatial derivative obey the master equation.
307 citations
TL;DR: The gas-solid reaction between methane and cerium oxide (CeO2) directly produced a synthesis gas with H2/CO ratio of 2.1±0.1.
307 citations
TL;DR: The authors proposed an implicit display theory of irony in order to provide a plausible explanation of how irony is distinguished from nonirony, which is consistent with the empirical findings from psycholinguistics.
306 citations
TL;DR: Melting phase relations and element partitioning data show that these liquids could host many incompatible elements at the base of the mantle, such that seismically anomalous zones near the boundary between the core and the mantle may result from isolated pockets of melt.
Abstract: Interrogating physical processes that occur within the lowermost mantle is a key to understanding Earth's evolution and present-day inner composition. Among such processes, partial melting has been proposed to explain mantle regions with ultralow seismic velocities near the core-mantle boundary, but experimental validation at the appropriate temperature and pressure regimes remains challenging. Using laser-heated diamond anvil cells, we constructed the solidus curve of a natural fertile peridotite between 36 and 140 gigapascals. Melting at core-mantle boundary pressures occurs at 4180 ± 150 kelvin, which is a value that matches estimated mantle geotherms. Molten regions may therefore exist at the base of the present-day mantle. Melting phase relations and element partitioning data also show that these liquids could host many incompatible elements at the base of the mantle.
306 citations
TL;DR: In this article, the significance of possible influential factors with the use of the experimental design method was examined with the help of laboratory experiments, including surface roughness of steel, 50 percent diameter of sand, sand type, test type (simple shear and shear box), and uniformity coefficient of sand.
306 citations
Authors
Showing all 46967 results
| Name | H-index | Papers | Citations |
|---|---|---|---|
| Matthew Meyerson | 194 | 553 | 243726 |
| Yury Gogotsi | 171 | 956 | 144520 |
| Masayuki Yamamoto | 171 | 1576 | 123028 |
| H. Eugene Stanley | 154 | 1190 | 122321 |
| Takashi Taniguchi | 152 | 2141 | 110658 |
| Shu-Hong Yu | 144 | 799 | 70853 |
| Kazunori Kataoka | 138 | 908 | 70412 |
| Osamu Jinnouchi | 135 | 885 | 86104 |
| Hector F. DeLuca | 133 | 1303 | 69395 |
| Shlomo Havlin | 131 | 1013 | 83347 |
| Hiroyuki Iwasaki | 131 | 1009 | 82739 |
| Kazunari Domen | 130 | 908 | 77964 |
| Hideo Hosono | 128 | 1549 | 100279 |
| Hideyuki Okano | 128 | 1169 | 67148 |
| Andreas Strasser | 128 | 509 | 66903 |