63 research outputs found
The dynamics of surges in the 3 February 2015 avalanches in Vallee de la Sionne
Five avalanches were artificially released at the VallĂŠe de la Sionne test site in the west of Switzerland on 3 February 2015 and recorded by the GEOphysical flow dynamics using pulsed Doppler radAR Mark 3 radar system. The radar beam penetrates the dilute powder cloud and measures reflections from the underlying denser avalanche features allowing the tracking of the flow at 111 Hz with 0.75 m downslope resolution. The data show that the avalanches contain many internal surges. The large or âmajorâ surges originate from the secondary release of slabs. These slabs can each contain more mass than the initial release, and thus can greatly affect the flow dynamics, by unevenly distributing the mass. The small or âminorâ surges appear to be a roll wave-like instability, and these can greatly influence the front dynamics as they can repeatedly overtake the leading edge. We analyzed the friction acting on the fronts of minor surges using a Voellmy-like, simple one-dimensional model with frictional resistance and velocity-squared drag. This model fits the data of the overall velocity, but it cannot capture the dynamics and especially the slowing of the minor surges, which requires dramatically varying effective friction. Our findings suggest that current avalanche models based on Voellmy-like friction laws do not accurately describe the physics of the intermittent frontal region of large mixed avalanches. We suggest that these data can only be explained by changes in the snow surface, such as the entrainment of the upper snow layers and the smoothing by earlier flow fronts
Comparing Flow Thresholds and Dynamics for Oscillating and Inclined Granular Layers
The onset and dynamics of flow in shallow horizontally oscillating granular layers are studied as a function of the depth of the layer and imposed acceleration. Measurements of the flow velocity made from the top and side are presented in the frame of reference of the container. As is also found for avalanches of inclined layers, the thresholds for starting and stopping of flow are slightly different. The variation with depth of the starting acceleration Îstart for the oscillating layer is similar to the corresponding variation of the tangent of the starting angle tan(Îstart) for avalanches in the same container at low frequencies, but deviates as the frequency is increased. However, the threshold behavior depends significantly on the measurement protocol. Just above Îstart, the motion decays with time as the material reorganizes over a minute or so, causing the apparent threshold to increase. Furthermore, the rms velocity as a function of acceleration rises more sharply above the starting threshold if the first minute or so of excitation is discarded. Once excited, the rheology of the material is found to vary in time during the cycle in surprising ways. If the maximum inertial force (proportional to the container acceleration amplitude) is slightly higher than that required to produce flow, the flow velocity grows as soon as the inertial force exceeds zero in each cycle, but jamming occurs long before the inertial force returns to zero. At higher Î, the motion is fluidlike over the entire cycle. However, the fraction of the cycle during which the layer is mobile is typically far higher than what one would predict from static considerations or the behavior of the inclined layer. Finally, we consider the flow profiles as a function of both the transverse distance across the cell at the free surface and also as a function of the vertical coordinate in the boundary layer near the sidewall. These profiles have time-dependent shapes and are therefore significantly different from profiles previously measured for avalanche flows
The Dynamics of CO 2 âDriven Granular Flows in Gullies on Mars
Martian gullies are landforms consisting of an erosional alcove, a channel, and a depositional apron. A significant proportion of Martian gullies at the midâlatitudes is active today. The seasonal sublimation of CO2 ice has been suggested as a driver behind presentâday gully activity. However, due to a lack of in situ observations, the actual processes causing the observed changes remain unresolved. Here, we present results from flume experiments in environmental chambers in which we created CO2âdriven granular flows under Martian atmospheric conditions. Our experiments show that under Martian atmospheric pressure, large amounts of granular material can be fluidized by the sublimation of small quantities of CO2 ice in the granular mixture (only 0.5% of the volume fraction of the flow) under slope angles as low as 10°. Dimensionless scaling of the CO2âdriven granular flows shows that they are dynamically similar to terrestrial twoâphase granular flows, that is, debris flows and pyroclastic flows. The similarity in flow dynamics explains the similarity in deposit morphology with levees and lobes, supporting the hypothesis that CO2âdriven granular flows on Mars are not merely modifying older landforms, but they are actively forming them. This has farâreaching implications for the processes thought to have formed these gullies over time. For other planetary bodies in our solar system, our experimental results suggest that the existence of gully like landforms is not necessarily evidence for flowing liquids but that they could also be formed or modified by sublimationâdriven flow processes
Approximate Decoherence of Histories and 't Hooft's Deterministic Quantum Theory
This paper explores the possibility that an exactly decoherent set of
histories may be constructed from an approximately decoherent set by small
distortions of the operators characterizing the histories. In particular, for
the case of histories of positions and momenta, this is achieved by doubling
the set of operators and then finding, amongst this enlarged set, new position
and momentum operators which commute, so decohere exactly, and which are
``close'' to the original operators. The enlarged, exactly decoherent, theory
has the same classical dynamics as the original one, and coincides with the
so-called deterministic quantum theories of the type recently studied by 't
Hooft. These results suggest that the comparison of standard and deterministic
quantum theories may provide an alternative method of characterizing emergent
classicality. A side-product is the surprising result that histories of momenta
in the quantum Brownian motion model (for the free particle in the
high-temperature limit) are exactly decoherent.Comment: 41 pages, plain Te
Somewhere in the Universe: Where is the Information Stored When Histories Decohere?
We investigate the idea that decoherence is connected with the storage of
information about the decohering system somewhere in the universe. The known
connection between decoherence of histories and the existence of records is
extended from the case of pure initial states to mixed states. Records may
still exist but are necessarily imperfect. We formulate an
information-theoretic conjecture about decoherence due to an environment: the
number of bits required to describe a set of decoherent histories is
approximately equal to the number of bits of information thrown away to the
environment in the coarse-graining process. This idea is verified in a simple
model consisting of a particle coupled to an environment that can store only
one bit of information. We explore the decoherence and information storage in
the quantum Brownian motion model. It is shown that the variables that the
environment naturally measures and stores information about are the Fourier
components of the function (describing the particle trajectory). The
records storing the information about the Fourier modes are the positions and
momenta of the environmental oscillators at the final time. Decoherence is
possible even if there is only one oscillator in the environment. The
information count of the histories and records in the environment add up
according to our conjecture. These results give quantitative content to the
idea that decoherence is related to ``information lost''.Comment: 48 pages, plain Tex. Second revisio
GPsâ role security and therapeutic commitment in managing alcohol problems: a randomised controlled trial of a tailored improvement programme
Improving preventive health care in Aboriginal and Torres Strait Islander primary care settings
Mental health clinician attitudes to the provision of preventive care for chronic disease risk behaviours and association with care provision
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