947 research outputs found

    Measurement of Effective Temperatures in an Aging Colloidal Glass

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    We study the thermal fluctuations of an optically confined probe particle, suspended in an aging colloidal suspension, as the suspension transforms from a viscous liquid into an elastic glass. The micron-sized bead forms a harmonic oscillator. By monitoring the equal-time fluctuations of the tracer, at two different laser powers, we determine the temperature of the oscillator, ToT_{\text{o}}. In the ergodic liquid the temperatures of the oscillator and its environment are equal while, in contrast, in a nonequilibrium glassy phase we find that ToT_{\text{o}} substantially exceeds the bath temperature.Comment: 4 pages (minor changes, accepted Phys. Rev. Lett.

    2. Wochenbericht SO242/1 DISCOL REVISITED

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    3. Wochenbericht SO242/1 DISCOL REVISITED

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    12. - 19. August 201

    Monitoring temporal variability of bubble release at seeps: The hydroacoustic swath system GasQuant

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    A lander-based hydroacoustic swath system, GasQuant, was deployed in an intensely bubbling seep area at the shelf west of the Crimea Peninsula, Black Sea. With its horizontally oriented swath (21 beams, 63° swath angle, 180 kHz) GasQuant operates in a sonar-like mode and monitors bubbles remotely, exploiting their strong backscattering when crossing the swath. All active seep spots were monitored simultaneously within the covered area (2075 m2). Even applying simple processing and visualization techniques (moving average for filtering, FFT for spectrum analyses; swath and trace plots) identified 17 seeps of different activity patterns that have been grouped as follows: (1) sporadically active with one to a few long bursts (up to 18 min) or randomly occurring short bursts (350 bursts or >20% active). Studying the bubble release variability of single seeps and of the entire area allows speculation about the external and internal processes that modulate the bubble release. In the study area none of the 17 seeps was found to be permanently active. Only one was active for 75% and another one for 45% of the time monitored. The rest only released bubbles during less than 20% of the time with an overall average of only 12%. This would have strong implications for flux extrapolations if these were based on very accurate but few short-term measurements. Both strong overestimates and underestimates are possible. High-resolution monitoring over at least one tidal cycle as with the GasQuant system might help to get an idea of the temporal variability. Thus flux extrapolations can be corrected to better reflect the real seep activity

    1. Wochenbericht POS526

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    POSEIDON POS526 24.07.2018 - 12.08.2018 Dogger Bank und Tisler Ree

    Technogenic soils in Zielona GĂłra

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    1. Weekly Report AL548 / MineMoni II

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    3rd November to 17th November 2020, Kiel - Kie
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