716,645 research outputs found
Theory of tunneling spectroscopy for chiral topological superconductors
We study the charge conductance of an interface between a normal metal and a
superconducting quantum anomalous Hall system, based on the recursive Green's
function. The angle resolved conductance gamma(ky, eV) with the momentum ky
parallel to the interface and the bias voltage V shows a rich structure
depending on the Chern number N of the system. We find that when the bias
voltage is tuned to the energy dispersion of the edge mode, eV = Eedge(ky), the
angle resolved conductance gamma(ky,Eedge(ky)) shows a pronounced even-odd
effect; the conductance vanishes for N = 0 or 2 while it takes a universal
value 2e^2/h for N = 1. In particular, in N = 2 phase, we find that the
conductance gamma(ky,Eedge(ky)) becomes zero due to interference of two
degenerate Majorana edge modes, although the corresponding surface spectral
weight remains non-zero.Comment: 10 pages, 10 figure
The Marmara Sea Gateway since ~16Â ky BP: non-catastrophic causes of paleoceanographic events in the Black Sea at 8.4 and 7.15Â ky BP
The Late Quaternary history of connection of the Black Sea to the Eastern
Mediterranean has been intensely debated. Ryan, Pitman and coworkers
advocate two pulses of outflow from the Black Sea to the world ocean at
~16–14.7 ky BP and ~11–10 ky BP. From ~14.7–11 ky BP and from ~10–8.4
ky BP, they suggest that the level of the Black Sea fell to ~ -100 m. At 8.4 ky
BP, they further claim that a catastrophic flood occurred in a geological
instant, refilling the Black Sea with saline waters from the Mediterranean. In
contrast, we continue to gather evidence from seismic profiles and dated cores
in the Marmara Sea which demonstrate conclusively that the proposed flood
did not occur. Instead, the Black Sea has been at or above the Bosphorus sill
depth and flowing into the world ocean unabated since ~10.5 ky BP. This
conclusion is based on continuous Holocene water-column stratification
(leading to sapropel deposition in the Marmara Sea and the Aegean Sea),
proxy indicators of sea-surface salinity, and migration of endemic species
across the Bosphorus in both directions whenever appropriate hydrographic
conditions existed in the strait. The two pulses of outflow documented by
Ryan, Pitman and coworkers find support in our data, and we have modified our earlier interpretations so that these pulses now coincide with the
development of mid-shelf deltas: \Delta 2 (16–14.7 ky BP) and \Delta 1 (10.5–9 ky BP)
at the southern end of the Bosphorus Strait. However, continued Black Sea
outflow after 9 ky BP prevented the northward advection of Mediterranean
water and the entry of open-marine species into the Black Sea for more than
1000 years. Sufficient Mediterranean water to change the Sr-isotopic
composition of slope and shelf water masses was not available until ~8.4 ky
BP (along with the first arrival of many varieties of marine fauna and flora),
whereas euryhaline molluscs did not successfully populate the Black Sea
shelves until ~7.15 ky BP. Instead of relying on catastrophic events, we
recognize a slow, progressive reconnection of the Black Sea to the world
ocean, accompanied by significant time lags
Coming out as sacrament
Glaser, Chris. Coming out as sacrament. Louisville, Ky: Westminster/John Knox Press, 1998. Grenz, Stanley J. Welcoming but not affirming: an evangelical response to homosexuality. Louisville, Ky: Westminster/John Knox Press, 1998
Microstructured KY(WO4)2:Gd3+, Lu3+, Yb3+ channel waveguide laser
Epitaxially grown, 2.4-μm-thin layers of KY(WO4)2:Gd3+, Lu3+, Yb3+, which exhibit a high refractive index contrast with respect to the undoped KY(WO4)2 substrate, have been microstructured by Ar beam milling, providing 1.4-μm-deep ridge channel waveguides of 2 to 7 μm width, and overgrown by an undoped KY(WO4)2 layer. Channel waveguide laser operation was achieved with a launched pump power threshold of only 5 mW, a slope efficiency of 62% versus launched pump power, and 76 mW output power
Sensitivity of the Oceanic Turbulent Boundary Layer to Cyclic Insolation Change with Response Periods of 23 to 2.5 Ky: an Equatorial Atlantic Record for the Last 200 Ka
Time series of sea-surface temperature in cores sited beneath the region of maximum divergence centered on 10 degrees W are characterized by two sets of periodic signals. The dominant signal is centered on a period of 23 Ky and is coherent with and lags, approx. 2.5 Ky, the precessional component of orbitally controlled insolation. The subdominant periods occur between 4.0 and 2.5 Ky. Both sets of signals record variation in the seasonal intensity of oceanic divergence modulated by variation in tropical easterly intensity. The longer periods are a response to precessional forcing. The forcing responsible for the shorter periods is unknown
Dynamical coupled-channel model of kaon-hyperon interactions
The pi N --> KY and KY --> KY reactions are studied using a dynamical
coupled-channel model of meson-baryon interactions at energies where the baryon
resonances are strongly excited. The channels included are: pi N, K \Lambda,
and K\Sigma. The resonances considered are: N^* [S_{11}(1650), P_{11}(1710),
P_{13}(1720),D_{13}(1700)]; \Delta^* [S_{31}(1900), P_{31}(1910),
P_{33}(1920)]; \Lambda ^* [S_{01}(1670), P_{01}(1810)] \Sigma^* [P_{11}(1660),
D_{13}(1670)]; and K^*(892). The basic non-resonant \pi N --> KY and KY --> KY
transition potentials are derived from effective Lagrangians using a unitary
transformation method. The dynamical coupled-channel equations are simplified
by parametrizing the pi N -->pi N amplitudes in terms of empirical pi N
partial-wave amplitudes and a phenomenological off-shell function. Two models
have been constructed. Model A is built by fixing all coupling constants and
resonance parameters using SU(3) symmetry, the Particle Data Group values, and
results from a constituent quark model. Model B is obtained by allowing most of
the parameters to vary around the values of model A in fitting the data. Good
fits to the available data for pi^- p to K^0 \Lambda, K^0 \Sigma^0 have been
achieved. The investigated kinematics region in the center-of-mass frame goes
from threshold to 2.5 GeV. The constructed models can be imbedded into
associated dynamical coupled-channel studies of kaon photo- and
electro-production reactions.Comment: 35 pages, 11 Figure
Optical spectroscopy of rare-earth ions doped KY(WO4)2 thin films
KY(WO4)2 thin films doped with Dy3+, Tb3+, Yb3+, were grown onto KY(WO4)2 substrates using liquid-phase epitaxy. Spectroscopic investigations of the grown layers were performed. Obtained results were compared with spectra given for bulk crystals. Upconversion experiments after direct Yb3+ excitation in Dy3+-Yb3+ and Tb3+-Yb3+ codoped layers will be also presented
Dynamical coupled-channel approach to hadronic and electromagnetic production of kaon-hyperon on the proton
A dynamical coupled-channel formalism for processes and
is presented which provides a comprehensive investigation of
recent data on the reaction. The non-resonant
interactions within the subspace are derived from effective
Lagrangians, using a unitary transformation method. The calculations of
photoproduction amplitudes are simplified by casting the coupled-channel
equations into a form such that the empirical amplitudes
are input and only the parameters associated with the channel are
determined by performing -fits to all of the available data for and . Good
agreement between our models and those data are obtained. In the fits to channels, most of the parameters are constrained within of
the values given by the Particle Data Group and/or quark model predictions,
while for parameters, ranges compatible with broken
symmetry are imposed. The main reaction mechanisms in photoproduction are singled out and issues related to newly suggested
resonances , , and are studied. Results illustrating
the importance of using a coupled-channel treatment are reported. Meson cloud
effects on the transitions are also discussed.Comment: Accepted Physical Review
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