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Transport Velocities (transport + velocity)

Distribution by Scientific Domains
Earth and Environmental Science40%

Selected Abstracts

Dynamics of bidirectional transport of Arc mRNA in neuronal dendrites

THE JOURNAL OF COMPARATIVE NEUROLOGY, Issue 3 2007
Joseph L. Dynes
Abstract The mRNA for Arc (activity-regulated cytoskeletal protein) is delivered into dendrites and localizes selectively at active synapses. Here we use a green fluorescent protein-based labeling system and confocal microscopy to define the transport kinetics of exogenously expressed mRNA from chimaeric Arc constructs (Arc/MS2 mRNA) in the dendrites of living rat neurons in culture. Arc/MS2 mRNA assembles into particles that move independently, bidirectionally, and intermittently in a fashion indicative of transport. Transport velocities range from below 6 to 65 ,m/minute, which is consistent with actin-based and microtubule-based transport, respectively. In general, orthograde translocations are longer than retrograde translocations. Rapidly translocating Arc/MS2 mRNA particles sometimes reverse direction and decrease velocity just before stopping, suggesting that local signals regulate Arc mRNA targeting movements. These observations identify several phases of Arc mRNA movement that serve as potential points for regulating Arc mRNA localization. J. Comp. Neurol. 500:433,447, 2007. © 2006 Wiley-Liss, Inc. [source]

The use of short-lived radionuclides to quantify transitional bed material transport in a regulated river

EARTH SURFACE PROCESSES AND LANDFORMS, Issue 4 2007
Nira L. Salant
Abstract We investigate the use of the short-lived fallout radionuclide beryllium-7 (7Be; t1/2 = 53·4 days) as a tracer of medium and coarse sand (0·25,2 mm), which transitions between transport in suspension and as bed load, and evaluate the effects of impoundment on seasonal and spatial variations in bed sedimentation. We measure 7Be activities in approximately monthly samples from point bar and streambed sediments in one unregulated and one regulated stream. In the regulated stream our sampling spanned an array of flow and management conditions during the annual transition from flood control in the winter and early spring to run-of-the-river operation from late spring to autumn. Sediment stored behind the dam during the winter quickly became depleted in 7Be activity. This resulted in a pulse of ,dead' sediment released when the dam gates were opened in the spring which could be tracked as it moved downstream. Measured average sediment transport velocities (30,80 metres per day (m d,1)) exceed those typically reported for bulk bed load transport and are remarkably constant across varied flow regimes, possibly due to corresponding changes in bed sand fraction. Results also show that the length scale of the downstream impact of dam management on sediment transport is short (c. 1 km); beyond this distance the sediment trapped by the dam is replaced by new sediment from tributaries and other downstream sources. Copyright © 2006 John Wiley & Sons, Ltd. [source]

Evaluation of electroosmotic drag coefficient of water in hydrated sodium perfluorosulfonate electrolyte polymer

JOURNAL OF COMPUTATIONAL CHEMISTRY, Issue 9 2009
Liuming Yan
Abstract The electroosmotic drag coefficient of water molecules in hydrated sodium perfluorosulfonate electrolyte polymer is evaluated on the basis of the velocity distribution functions of the sodium cations and water molecules with an electric field applied using molecular dynamics simulations. The simulation results indicate that both velocity distribution functions of water molecules and of sodium cations agree well with the classic Maxwellian velocity distribution functions when there is no electric field applied. If an electric field is applied, the distribution functions of velocity component in directions perpendicular to the applied electric field still agree with the Maxwellian velocity distribution functions but with different temperature parameters. In the direction of the applied electric field, the electric drag causes the velocity distribution function to deviate from the Maxwellian velocity distribution function; however, to obey the peak shifted Maxwellian distribution function. The peak shifting velocities coincide with the average transport velocities induced by the electric field, and could be applied to the evaluation of the electroosmotic drag coefficient of water. By evaluation of the transport velocities of water molecules in the first coordination shells of sodium cations, sulfonate anion groups, and in the bulk, it is clearly shown that the water molecules in the first coordination shell of sodium cations are the major contribution to the electroosmotic drag and momentum transfer from water molecules within the first coordination shell to the other water molecules also contributes to the electroosmotic drag. © 2008 Wiley Periodicals, Inc. J Comput Chem 2009 [source]

Characteristics of Underground Water Flow at Different Water Levels in Tianshengan Karst Area, Yunnan, China

ACTA GEOLOGICA SINICA (ENGLISH EDITION), Issue 1 2010
Janja KOGOV
Abstract: Three tracing tests from the same injection point executed at low, medium, and high water levels in the karst aquifer near Tianshengan village, Lunan Stone Forest, Yunnan Province, China, have revealed the basic properties of underground water flow. They showed the general directions of water flows; tracer concentrations were observed at six successive points allowing for the calculation of apparent dominant flow velocities at these sections towards the Dalongtan karst spring. For the high water level, the discharge between single sections was between two and 10 times greater than that at low water level. For the medium water level, the flow velocity at different sections was between 1.4 and 3.7 times faster than that at low water level; and for high water level, it was between 1.3 and 2.7 times faster than that at medium water level. The fastest water flow appeared at the first section (23 cm/s at medium water level); and the slowest (0.6 cm/s at low water level) appeared where water flow must cross the Tianshengan fault (north-south direction), and later, a layer of 20-30 m thickness of quartz sandstone and shale clay-stones. It was also possible to calculate the recovery of the tracer for point 4, Dakenyan, where discharge was measured. At the medium water level, 50% of the injected tracer was detected a half-day after its first appearance and at low water level after more than 3 days. The previously published research illustrates the transport velocities of possible contaminants and their solubilities in water at different hydrological conditions. [source]