Spectral Analyses of High-Frequency Pn, Sn Phases from Very Shallow Focus Earthquakes.

1983 ◽  
Author(s):  
D. A. Walker
1980 ◽  
Author(s):  
Daniel A. Walker ◽  
George H. Sutton ◽  
C. S. McCreery

Science ◽  
1978 ◽  
Vol 199 (4335) ◽  
pp. 1333-1335 ◽  
Author(s):  
D. A. WALKER ◽  
C. S. MCCREERY ◽  
G. H. SUTTON ◽  
F. K. DUENNEBIER

2016 ◽  
Vol 115 (3) ◽  
pp. 1372-1380 ◽  
Author(s):  
Mai K. ElMallah ◽  
David A. Stanley ◽  
Kun-Ze Lee ◽  
Sara M. F. Turner ◽  
Kristi A. Streeter ◽  
...  

Power spectral analyses of electrical signals from respiratory nerves reveal prominent oscillations above the primary rate of breathing. Acute exposure to intermittent hypoxia can induce a form of neuroplasticity known as long-term facilitation (LTF), in which inspiratory burst amplitude is persistently elevated. Most evidence indicates that the mechanisms of LTF are postsynaptic and also that high-frequency oscillations within the power spectrum show coherence across different respiratory nerves. Since the most logical interpretation of this coherence is that a shared presynaptic mechanism is responsible, we hypothesized that high-frequency spectral content would be unchanged during LTF. Recordings of inspiratory hypoglossal (XII) activity were made from anesthetized, vagotomized, and ventilated 129/SVE mice. When arterial O2 saturation (SaO2) was maintained >96%, the XII power spectrum and burst amplitude were unchanged for 90 min. Three, 1-min hypoxic episodes (SaO2 = 50 ± 10%), however, caused a persistent (>60 min) and robust (>400% baseline) increase in burst amplitude. Spectral analyses revealed a rightward shift of the signal content during LTF, with sustained increases in content above ∼125 Hz following intermittent hypoxia and reductions in power at lower frequencies. Changes in the spectral content during LTF were qualitatively similar to what occurred during the acute hypoxic response. We conclude that high-frequency content increases during XII LTF in this experimental preparation; this may indicate that intermittent hypoxia-induced plasticity in the premotor network contributes to expression of XII LTF.


2020 ◽  
Author(s):  
antoine Grisart ◽  
Bo Vinther ◽  
vasileos Gkinis ◽  
Trevor Popp ◽  
Barbara Stenni ◽  
...  

<p>The iconic curve of D in water showing the 8 glacial/interglacial cycles from the EPICA Dome C ice<br>core is now a reference in paleoclimate. It shows past temperature variability back to 800 ka over the<br>3200 m deep ice core with a 55 cm resolution. However, the millennial and centennial scale<br>variability gets more challenging to observe in the deepest part of the core. Indeed, the time<br>resolution worsens when going deeper in the ice because of the ice thinning: it is larger than 200<br>years at 2500 m depth. Furthermore, isotopic diffusion affects the signal at the bottom of the ice<br>core. Pol et al., (2010) have thus shown that the sub-millennial MIS (Marine Isotopic Stage) 19 signal<br>(3157-3181 m deep) is erased because of diffusion and high resolution doesn’t add any further<br>information at this depth. In this study we want to better characterize the increase of the isotopic<br>diffusion with depth by providing new high resolution water isotopes at several intervals over the<br>EPICA ice core (EDC).<br>We present here published high resolution (11 cm) d18O measurements over the EDC ice core as<br>well as new records of high resolution (11 cm) D over MIS 7;13 and 14). We use spectral analyses to<br>determine at which depth the isotopic diffusion erases the sub-millennial variability. We also show<br>that cold periods exhibit a larger variability of water isotopes than interglacial periods.<br>The information obtained here is crucial for the new project Beyond EPICA oldest ice core, which has<br>the goal of analyzing a 1.5 Ma old ice core. In the deepest part, 1 m of ice core could represent<br>10 000 years of climate archive.</p>


1978 ◽  
Vol 5 (9) ◽  
pp. 745-747 ◽  
Author(s):  
George H. Sutton ◽  
Charles S. McCreery ◽  
Frederick K. Duennebier ◽  
Daniel A. Walker

1989 ◽  
Vol 66 (2) ◽  
pp. 886-893 ◽  
Author(s):  
C. L. Webber

Spectral analyses were performed on phrenic neurogram recordings from 18 cats to identify high-frequency oscillations (HFOs) inherent in the signals at different phases of inspiratory activity. Gating the analysis for the entire inspiratory phase resulted in dual spectral HFOs (27 and 83 Hz), both of which persisted when the analysis was repeated on the later phase of phrenic inspiratory activity alone (29 and 82 Hz). A third pass at the same data, gating for just the early phase of phrenic discharge, however, resulted in single spectral HFOs at the higher frequency only (86 Hz). Because both early and late recruited phrenic motoneurons carry both higher and lower spectral frequencies, these results demonstrate that the lower frequency HFO is distinctly delayed in onset compared with the higher frequency HFO, the latter of which is believed to have a brain stem origin. This delayed onset may be important in identifying the source of the lower frequency HFO, which appears to be specific to various respiratory efferent systems.


2015 ◽  
Vol 527 ◽  
pp. 894-907 ◽  
Author(s):  
Clément Duvert ◽  
Hervé Jourde ◽  
Matthias Raiber ◽  
Malcolm E. Cox

1988 ◽  
Vol 102 ◽  
pp. 239
Author(s):  
M.S.Z. Chaghtai

Using R.D. Cowan’s computations (1979) and parametric calculations of Meinders et al (1982), old analyses are thoroughly revised and extended at Aligarh, of Zr III by Khan et al (1981), of Nb IV by Shujauddin et Chaghtai (1985), of Mo V by Tauheed at al (1985). Cabeza et al (1986) confirmed the last one largely.Extensive studies have been reported of the 1–e spectra, Zr IV (Rahimullah et al 1980; Acquista and Reader 1980), Nb V (Shujauddin et al 1982; Kagan et al 1981) and Mo VI (Edlén et al 1985). Some interacting 4p54d2levels of these spectra have been reported from our laboratory, also.Detailed spectral analyses of transitions between excited states have furnished complete energy values for J ≠ 1 levels of these spectra during 1970s and 80s. Shujauddin et al (1982) have worked out Nb VI and Tauheed et al (1984) Mo VII from our lab, while Khan et al (1981) share the work on Zr V with Reader and Acquista (1979).


Author(s):  
W. E. Lee ◽  
A. H. Heuer

IntroductionTraditional steatite ceramics, made by firing (vitrifying) hydrous magnesium silicate, have long been used as insulators for high frequency applications due to their excellent mechanical and electrical properties. Early x-ray and optical analysis of steatites showed that they were composed largely of protoenstatite (MgSiO3) in a glassy matrix. Recent studies of enstatite-containing glass ceramics have revived interest in the polymorphism of enstatite. Three polymorphs exist, two with orthorhombic and one with monoclinic symmetry (ortho, proto and clino enstatite, respectively). Steatite ceramics are of particular interest a they contain the normally unstable high-temperature polymorph, protoenstatite.Experimental3mm diameter discs cut from steatite rods (∼10” long and 0.5” dia.) were ground, polished, dimpled, and ion-thinned to electron transparency using 6KV Argon ions at a beam current of 1 x 10-3 A and a 12° angle of incidence. The discs were coated with carbon prior to TEM examination to minimize charging effects.


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