637,750 research outputs found
Hydrogen as a Source of Flux Noise in SQUIDs
Superconducting qubits are hampered by flux noise produced by surface spins
from a variety of microscopic sources. Recent experiments indicated that
hydrogen (H) atoms may be one of those sources. Using density functional theory
calculations, we report that H atoms either embedded in, or adsorbed on, an
a-Al2O3(0001) surface have sizeable spin moments ranging from 0.81 to 0.87 uB
with energy barriers for spin reorientation as low as ~10 mK. Furthermore, H
adatoms on the surface attract gas molecules such as O2, producing new spin
sources. We propose coating the surface with graphene to eliminate H-induced
surface spins and to protect the surface from other adsorbates.Comment: 12 pages, 4 figure
Optical spectroscopy study of the collapsed tetragonal phase of CaFe(AsP) single crystals
We present an optical spectroscopy study on P-doped CaFeAs which
experiences a structural phase transition from tetragonal to collapsed
tetragonal (cT) phase near 75 K. The measurement reveals a sudden reduction of
low frequency spectral weight and emergence of a new feature near 3200 \cm (0.4
eV) in optical conductivity across the transition, indicating an abrupt
reconstruction of band structure. The appearance of new feature is related to
the interband transition arising from the sinking of hole bands near
point below Fermi level in the cT phase, as expected from the density function
theory calculations in combination with the dynamical mean field theory.
However, the reduction of Drude spectral weight is at variance with those
calculations. The measurement also indicates an absence of the abnormal
spectral weight transfer at high energy (near 0.5-0.7 eV) in the cT phase,
suggesting a suppression of electron correlation effect.Comment: 6 pages, 4 figure
Weak Gravitational Lensing as a Method to Constrain Unstable Dark Matter
The nature of the dark matter remains a mystery. The possibility of an
unstable dark matter particle decaying to invisible daughter particles has been
explored many times in the past few decades. Meanwhile, weak gravitational
lensing shear has gained a lot of attention as a probe of dark energy. Weak
lensing is a useful tool for constraining the stability of the dark matter. In
the coming decade a number of large, galaxy imaging surveys will be undertaken
and will measure the statistics of cosmological weak lensing with unprecedented
precision. Weak lensing statistics are sensitive to unstable dark matter in at
least two ways. Dark matter decays alter the matter power spectrum and change
the angular diameter distance-redshift relation. We show how measurements of
weak lensing shear correlations may provide the most restrictive,
model-independent constraints on the lifetime of unstable dark matter. Our
results rely on assumptions regarding nonlinear evolution of density
fluctuations in scenarios of unstable dark matter and one of our aims is to
stimulate interest in theoretical work on nonlinear structure growth in
unstable dark matter models.Comment: 12 pages, 5 figures. Minor changes, typos fixed, references added,
results and conclusions unchanged. Accepted for publication in Physical
Review
The dielectric properties of soil-water mixtures at microwave frequencies
Recent measurements on the dielectric constants of soil-water mixtures show the existence of two frequency regions in which the dielectric behavior of these mixtures was quite different. At the frequencies of 1.4 GHz to 5 GHz, there were strong evidences that the variations of the dielectric (epsilon) with water content (W) depended on soil type. While the real part of epsilon for sandy soils rose rapidly with the increase in W, epsilon for the high-clay content soils rose only slowly with W. As a consequence, epsilon was generally higher for the sandy soils than for the high-clay content soils at a given W. On the other hand, most of the measurements at frequencies 1 GHz indicated the increase of epsilon with W independent of soil types. At a given W, epsilon' (sandy soil) approximately equals epsilon (high-clay content soil) within the precision of the measurements. These observational features can be satisfactorily interpreted in terms of a simple dielectric relaxation model, with an appropriate choice of the mean relaxation frequency f(m) and the range of the activation energy (beta). It was found that smaller f(m) and larger beta were required for the high-clay content soils than the sandy soils in order to be consistent with the measured data
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