289 research outputs found

    Drag Force Scaling for Penetration Into Granular Media

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    Impact dynamics is measured for spherical and cylindrical projectiles of many different densities dropped onto a variety non-cohesive granular media. The results are analyzed in terms of the material-dependent scaling of the inertial and frictional drag contributions to the total stopping force. The inertial drag force scales similar to that in fluids, except that it depends on the internal friction coefficient. The frictional drag force scales as the square-root of the density of granular medium and projectile, and hence cannot be explained by the combination of granular hydrostatic pressure and Coulomb friction law. The combined results provide an explanation for the previously observed penetration depth scaling

    Avalanche statistics and time-resolved grain dynamics for a driven heap

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    We probe the dynamics of intermittent avalanches caused by steady addition of grains to a quasi-two dimensional heap. To characterize the time-dependent average avalanche flow speed v(t), we image the top free surface. To characterize the grain fluctuation speed dv(t), we use Speckle-Visibility Spectroscopy. During an avalanche, we find that the fluctuation speed is approximately one-tenth the average flow speed, and that these speeds are largest near the beginning of an event. We also find that the distribution of event durations is peaked, and that event sizes are correlated with the time interval since the end of the previous event. At high rates of grain addition, where successive avalanches merge into smooth continuous flow, the relationship between average and fluctuation speeds changes to dv Sqrt[v]

    Sinusoidal fetal heart rate pattern

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    We describe 2 cases of term anemic fetuses with different sinusoidal pattern morphology, and possible mechanisms.nbspCasesmdashThe first patient noted sudden cessation of fetal movement on the day of presentation. She had a sinusoidal FHR pattern. The newborn had a hemoglobin of 3.7 g/dl, and umbilical artery pH was 7.10 and BE -7 mEq/l. The second patient noted decreased fetal movement for several days. She had a FHR pattern with absent FHR variability, and intermittent sinusoidal elements, with late decelerations. The newbornrsquos hemoglobin was 1.5 g/dl, umbilical artery pH was 7.07 and BE -10.2 mEq/l. Both cases had positive Kleihauer-Betke tests

    Classification of KPZQ and BDP models by multiaffine analysis

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    We argue differences between the Kardar-Parisi-Zhang with Quenched disorder (KPZQ) and the Ballistic Deposition with Power-law noise (BDP) models, using the multiaffine analysis method. The KPZQ and the BDP models show mono-affinity and multiaffinity, respectively. This difference results from the different distribution types of neighbor-height differences in growth paths. Exponential and power-law distributions are observed in the KPZQ and the BDP, respectively. In addition, we point out the difference of profiles directly, i.e., although the surface profiles of both models and the growth path of the BDP model are rough, the growth path of the KPZQ model is smooth.Comment: 11 pages, 6 figure

    Asymptotic function for multi-growth surfaces using power-law noise

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    Numerical simulations are used to investigate the multiaffine exponent αq\alpha_q and multi-growth exponent βq\beta_q of ballistic deposition growth for noise obeying a power-law distribution. The simulated values of βq\beta_q are compared with the asymptotic function βq=1q\beta_q = \frac{1}{q} that is approximated from the power-law behavior of the distribution of height differences over time. They are in good agreement for large qq. The simulated αq\alpha_q is found in the range 1q≤αq≤2q+1\frac{1}{q} \leq \alpha_q \leq \frac{2}{q+1}. This implies that large rare events tend to break the KPZ universality scaling-law at higher order qq.Comment: 5 pages, 4 figures, to be published in Phys. Rev.

    Projectile interactions in granular impact cratering

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    We present evidence for the interactions between a ball and the container boundaries, as well as between two balls, that are mediated by the granular medium during impact cratering. The presence of the bottom boundary affects the final penetration depth only for low drop heights with shallow filling, in which case, surprisingly, the penetration becomes deeper. By contrast the presence of the side wall causes less penetration and also an effective repulsion. Repulsion is also found for two balls dropped side-by-side
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