scholarly journals Spectral Deferred Corrections with Fast-wave Slow-wave Splitting

2016 ◽  
Vol 38 (4) ◽  
pp. A2535-A2557 ◽  
Author(s):  
Daniel Ruprecht ◽  
Robert Speck
Keyword(s):  
Slow Wave ◽  
Fast Wave ◽  
Wave Splitting ◽  
Spectral Deferred Corrections

La S-adénosyl-L-homocystéine : 1. Inductrice de sommeil

1980 ◽  
Vol 58 (2) ◽  
pp. 160-166 ◽  
Author(s):  
Pierre Fonlupt ◽  
Maurice Roche ◽  
Lucien Cronenberger ◽  
Henri Pacheco
Keyword(s):  
Slow Wave ◽  
Fast Wave ◽  
Serotonin Metabolism ◽  
Sleep Patterns

S-Adenosylhomocysteine, 0.1–20 mg/kg, influences the sleep patterns of rat, cat and rabbit by increasing the slow-wave and fast-wave sleep for 6 h. The SAH effects are increased by p-chlorophenylalanine and iproniazid and unchanged by reserpine. SAH effects are correlated with modification of norepinephrine and serotonin metabolism.

A novel hybrid slow-wave/fast-wave traveling-wave amplifier

1997 ◽  
Vol 25 (5) ◽  
pp. 1150-1154 ◽  
Author(s):  
W. Lawson ◽  
A. Fernandez ◽  
T. Hutchings ◽  
G.P. Saraph
Keyword(s):  
Slow Wave ◽  
Traveling Wave ◽  
Fast Wave ◽  
Traveling Wave Amplifier

scholarly journals Edge plasma parameters affecting fast wave and slow wave intensities in scrape off layer

2020 ◽  
Author(s):  
L. Ai ◽  
L. N. Liu ◽  
C. M. Qin ◽  
X. J. Zhang ◽  
Y. P. Zhao
Keyword(s):  
Slow Wave ◽  
Edge Plasma ◽  
Fast Wave ◽  
Plasma Parameters

Plastic Waves of Combined Stresses Due to Longitudinal Impact of a Pretorqued Tube—Part 1: Experimental Results

1970 ◽  
Vol 37 (4) ◽  
pp. 1107-1112 ◽  
Author(s):  
J. Lipkin ◽  
R. J. Clifton
Keyword(s):  
Slow Wave ◽  
Longitudinal Strain ◽  
Fast Wave ◽  
Longitudinal Impact ◽  
Strain Response ◽  
Torsional Strain ◽  
Time Profiles ◽  
Combined Stresses ◽  
Fast Waves ◽  
Longitudinal Strains

Experiments are reported in which annealed aluminum tubes are subjected to a static plastic torque followed by a longitudinal compressive impact. Measurements are made of both longitudinal and shear strain-time profiles at stations along the specimen. Qualitatively, the strain response at the gages corresponds to the arrival of a fast wave for which torsional strain decreases while longitudinal strain increases followed by a slow wave for which both torsional and longitudinal strains increase. Between the slow and fast waves and following the slow wave, a strain rate of the order of 10 sec−1 is maintained.

IMEX peer methods for fast-wave–slow-wave problems

2017 ◽  
Vol 118 ◽  
pp. 221-237 ◽  
Author(s):  
Behnam Soleimani ◽  
Oswald Knoth ◽  
Rüdiger Weiner
Keyword(s):  
Slow Wave ◽  
Fast Wave ◽  
Wave Problems

Upper‐Crustal Anisotropy of the Conjugate Strike‐Slip Fault Zone in Central Tibet Analyzed Using Local Earthquakes and Shear‐Wave Splitting

2019 ◽  
Vol 109 (5) ◽  
pp. 1968-1984 ◽  
Author(s):  
Chenglong Wu ◽  
Xiaobo Tian ◽  
Tao Xu ◽  
Xiaofeng Liang ◽  
Yun Chen ◽  
...  
Keyword(s):  
Shear Wave ◽  
Fault Zone ◽  
Shear Wave Splitting ◽  
Strike Slip ◽  
Fast Wave ◽  
Lithospheric Deformation ◽  
Crustal Anisotropy ◽  
Local Earthquakes ◽  
Wave Splitting ◽  
Central Tibet

Abstract Remarkable V‐shaped conjugate strike‐slip faults extend along the Bangong–Nujiang suture in central Tibet. Motions of these faults are considered to accommodate ongoing east–west extension and north–south contraction. Fabrics within the fault zone that are anisotropic to seismic waves can provide clues as to the unusual scale and style of lithospheric deformation. With the goal of determining the upper‐crustal anisotropy pattern in central Tibet, we measured shear‐wave splitting parameters (fast wave polarization direction and delay time) using waveforms generated by 194 local earthquakes recorded by 49 stations of the SANDWICH network. Stations located in eastern and western zones of the study area show anisotropy directions that agree well with the maximum horizontal compressive stress direction. The fast polarization directions at stations near active strike‐slip faults generally run parallel to the strikes of these faults. Pervasive inactive thrust faults caused by Cretaceous–Tertiary shortening in central Tibet also clearly correlate with the anisotropy detected at nearby stations. These results demonstrate that both local structures and stress contribute to upper‐crustal anisotropy in the region. Combining the new results with previous SKS‐wave splitting results and other seismic evidence, we propose that deformation in the upper crust is mechanically decoupled from that in the upper mantle, due to eastward middle‐lower crustal flow. This crustal flow causes basal shearing required for the formation of conjugate strike‐slip faults in central Tibet.

scholarly journals Fast-wave current drive above the slow-wave density limit

1990 ◽  
Vol 64 (11) ◽  
pp. 1258-1261 ◽  
Author(s):  
D. P. Sheehan ◽  
R. McWilliams ◽  
N. S. Wolf ◽  
D. Edrich
Keyword(s):  
Slow Wave ◽  
Current Drive ◽  
Fast Wave ◽  
Density Limit

scholarly journals Fast wave current drive above the slow wave density limit

1989 ◽  
Author(s):  
R. McWilliams ◽  
D. P. Sheehan ◽  
N. S. Wolf ◽  
D. Edrich
Keyword(s):  
Slow Wave ◽  
Current Drive ◽  
Fast Wave ◽  
Density Limit
Sign in / Sign up

Export Citation Format

Share Document