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Observation of Brownian motion in liquids at short times: instantaneous velocity and memory loss.
Kheifets S, Simha A, Melin K, Li T, Raizen MG. Kheifets S, et al. Science. 2014 Mar 28;343(6178):1493-6. doi: 10.1126/science.1248091. Science. 2014. PMID: 24675957
Measurement of the instantaneous velocity of Brownian motion of suspended particles in liquid probes the microscopic foundations of statistical mechanics in soft condensed matter. However, instantaneous velocity has eluded experimental observation for more than a century s …
Measurement of the instantaneous velocity of Brownian motion of suspended particles in liquid probes the microscopic foundations of statisti …
Direct visual observation of thermal capillary waves.
Aarts DG, Schmidt M, Lekkerkerker HN. Aarts DG, et al. Science. 2004 May 7;304(5672):847-50. doi: 10.1126/science.1097116. Science. 2004. PMID: 15131300 Free article.
We studied the free fluid-fluid interface in a phase-separated colloid-polymer dispersion with laser scanning confocal microscopy and directly observed thermally induced capillary waves at the interface in real space. Experimental results for static an …
We studied the free fluid-fluid interface in a phase-separated colloid-polymer dispersion with laser scanning confocal microsc …
Melting Temperature and Partial Melt Chemistry of H2O-Saturated Mantle Peridotite to 11 Gigapascals.
Kawamoto T, Holloway JR. Kawamoto T, et al. Science. 1997 Apr 11;276(5310):240-3. doi: 10.1126/science.276.5310.240. Science. 1997. PMID: 9092469
Given reasonable H2O abundances in Earth's mantle, an H2O-rich fluid could exist only in a region defined by the wet solidus and thermal stability limits of hydrous minerals, at depths between 90 and 330 kilometers. The experimental partial melts monotonously …
Given reasonable H2O abundances in Earth's mantle, an H2O-rich fluid could exist only in a region defined by the wet solidus and t …