16,387 research outputs found
Zero Temperature Phases of the Electron Gas
The stability of different phases of the three-dimensional non-relativistic
electron gas is analyzed using stochastic methods. With decreasing density, we
observe a {\it continuous} transition from the paramagnetic to the
ferromagnetic fluid, with an intermediate stability range () for the {\it partially} spin-polarized liquid. The freezing
transition into a ferromagnetic Wigner crystal occurs at . We
discuss the relative stability of different magnetic structures in the solid
phase, as well as the possibility of disordered phases.Comment: 4 pages, REVTEX, 3 ps figure
Shear localization as a mesoscopic stress-relaxation mechanism in fused silica glass at high strain rates
Molecular dynamics (MD) simulations of fused silica glass deforming in pressure-shear, while revealing useful insights into processes unfolding at the atomic level, fail spectacularly in that they grossly overestimate the magnitude of the stresses relative to those observed, e. g., in plate-impact experiments. We interpret this gap as evidence of relaxation mechanisms that operate at mesoscopic lengthscales and which, therefore, are not taken into account in atomic-level calculations. We specifically hypothesize that the dominant mesoscopic relaxation mechanism is shear banding. We evaluate this hypothesis by first generating MD data over the relevant range of temperature and strain rate and then carrying out continuum shear-banding calculations in a plate-impact configuration using a critical-state plasticity model fitted to the MD data. The main outcome of the analysis is a knock-down factor due to shear banding that effectively brings the predicted level of stress into alignment with experimental observation, thus resolving the predictive gap of MD calculations
River-bed armoring as a granular segregation phenomenon
Gravel-river beds typically have an "armored" layer of coarse grains on the
surface, which acts to protect finer particles underneath from erosion. River
bed-load transport is a kind of dense granular flow, and such flows are known
to vertically segregate grains. The contribution of granular physics to
river-bed armoring, however, has not been investigated. Here we examine these
connections in a laboratory river with bimodal sediment size, by tracking the
motion of particles from the surface to deep inside the bed, and find that
armor develops by two distinct mechanisms. Bed-load transport in the
near-surface layer drives rapid segregation, with a vertical advection rate
proportional to the granular shear rate. Creeping grains beneath the bed-load
layer give rise to slow but persistent segregation, which is diffusion
dominated and insensitive to shear rate. We verify these findings with a
continuum phenomenological model and discrete element method simulations. Our
results suggest that river beds armor by granular segregation from below ---
rather than fluid-driven sorting from above --- while also providing new
insights on the mechanics of segregation that are relevant to a wide range of
granular flows
Latitudinal variation of the solar photospheric intensity
We have examined images from the Precision Solar Photometric Telescope (PSPT)
at the Mauna Loa Solar Observatory (MLSO) in search of latitudinal variation in
the solar photospheric intensity. Along with the expected brightening of the
solar activity belts, we have found a weak enhancement of the mean continuum
intensity at polar latitudes (continuum intensity enhancement
corresponding to a brightness temperature enhancement of ).
This appears to be thermal in origin and not due to a polar accumulation of
weak magnetic elements, with both the continuum and CaIIK intensity
distributions shifted towards higher values with little change in shape from
their mid-latitude distributions. Since the enhancement is of low spatial
frequency and of very small amplitude it is difficult to separate from
systematic instrumental and processing errors. We provide a thorough discussion
of these and conclude that the measurement captures real solar latitudinal
intensity variations.Comment: 24 pages, 8 figs, accepted in Ap
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