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Liquid flow and control without solid walls 期刊论文
NATURE, 2020, 581 (7806) : 58-+
作者:  Hellmuth, Susanne;  Stemmann, Olaf
收藏  |  浏览/下载:52/0  |  提交时间:2020/07/03

Wall-free liquid channels surrounded by an immiscible magnetic liquid can be used to create liquid circuitry or to transport human blood without damaging the blood cells by moving permanent magnets.


When miniaturizing fluidic circuitry, the solid walls of the fluid channels become increasingly important(1) because they limit the flow rates achievable for a given pressure drop, and they are prone to fouling(2). Approaches for reducing the wall interactions include hydrophobic coatings(3), liquid-infused porous surfaces(4-6), nanoparticle surfactant jamming(7), changes to surface electronic structure(8), electrowetting(9,10), surface tension pinning(11,12) and use of atomically flat channels(13). A better solution may be to avoid the solid walls altogether. Droplet microfluidics and sheath flow achieve this but require continuous flow of the central liquid and the surrounding liquid(1,14). Here we demonstrate an approach in which aqueous liquid channels are surrounded by an immiscible magnetic liquid, both of which are stabilized by a quadrupolar magnetic field. This creates self-healing, non-clogging, anti-fouling and near-frictionless liquid-in-liquid fluidic channels. Manipulation of the field provides flow control, such as valving, splitting, merging and pumping. The latter is achieved by moving permanent magnets that have no physical contact with the liquid channel. We show that this magnetostaltic pumping method can be used to transport whole human blood with very little damage due to shear forces. Haemolysis (rupture of blood cells) is reduced by an order of magnitude compared with traditional peristaltic pumping, in which blood is mechanically squeezed through a plastic tube. Our liquid-in-liquid approach provides new ways to transport delicate liquids, particularly when scaling channels down to the micrometre scale, with no need for high pressures, and could also be used for microfluidic circuitry.


  
Ice front blocking of ocean heat transport to an Antarctic ice shelf 期刊论文
NATURE, 2020, 578 (7796) : 568-+
作者:  Alexandrov, Ludmil B.;  Kim, Jaegil;  Haradhvala, Nicholas J.;  Huang, Mi Ni;  Ng, Alvin Wei Tian;  Wu, Yang;  Boot, Arnoud;  Covington, Kyle R.;  Gordenin, Dmitry A.;  Bergstrom, Erik N.;  Islam, S. M. Ashiqul;  Lopez-Bigas, Nuria;  Klimczak, Leszek J.;  McPherson, John R.;  Morganella, Sandro;  Sabarinathan, Radhakrishnan;  Wheeler, David A.;  Mustonen, Ville;  Getz, Gad;  Rozen, Steven G.;  Stratton, Michael R.
收藏  |  浏览/下载:47/0  |  提交时间:2020/05/13

The front of the Getz Ice Shelf in West Antarctica creates an abrupt topographic step that deflects ocean currents, suppressing 70% of the heat delivery to the ice sheet.


Mass loss from the Antarctic Ice Sheet to the ocean has increased in recent decades, largely because the thinning of its floating ice shelves has allowed the outflow of grounded ice to accelerate(1,2). Enhanced basal melting of the ice shelves is thought to be the ultimate driver of change(2,3), motivating a recent focus on the processes that control ocean heat transport onto and across the seabed of the Antarctic continental shelf towards the ice(4-6). However, the shoreward heat flux typically far exceeds that required to match observed melt rates(2,7,8), suggesting that other critical controls exist. Here we show that the depth-independent (barotropic) component of the heat flow towards an ice shelf is blocked by the marked step shape of the ice front, and that only the depth-varying (baroclinic) component, which is typically much smaller, can enter the sub-ice cavity. Our results arise from direct observations of the Getz Ice Shelf system and laboratory experiments on a rotating platform. A similar blocking of the barotropic component may occur in other areas with comparable ice-bathymetry configurations, which may explain why changes in the density structure of the water column have been found to be a better indicator of basal melt rate variability than the heat transported onto the continental shelf(9). Representing the step topography of the ice front accurately in models is thus important for simulating ocean heat fluxes and induced melt rates.


  
Efficient Image-Based Simulation of Flow and Transport in Heterogeneous Porous Media: Application of Curvelet Transforms 期刊论文
GEOPHYSICAL RESEARCH LETTERS, 2020, 47 (2)
作者:  Aljasmi, Abdullah;  Sahimi, Muhammad
收藏  |  浏览/下载:15/0  |  提交时间:2020/07/02
porous media  image-based simulation  fluid flow and transport  
Stochastic Dynamics of Lagrangian Pore-Scale Velocities in Three-Dimensional Porous Media 期刊论文
WATER RESOURCES RESEARCH, 2019, 55 (2) : 1196-1217
作者:  Puyguiraud, Alexandre;  Gouze, Philippe;  Dentz, Marco
收藏  |  浏览/下载:15/0  |  提交时间:2019/11/26
pore-scale flow and transport  Lagrangian velocities  continuous time random walks  time domain random walks  non-Fickian dispersion  upscaling  
Exact Upscaling for Transport of Size-Distributed Colloids 期刊论文
WATER RESOURCES RESEARCH, 2019, 55 (2) : 1011-1039
作者:  Bedrikovetsky, P.;  Osipov, Y.;  Kuzmina, L.;  Malgaresi, G.
收藏  |  浏览/下载:13/0  |  提交时间:2019/11/26
upscaling  averaging  exact averaging of suspension-colloidal and reactive transport with distributed particle properties  reactive transport  exact solutions for 1-D reactive or colloidal flow for the upscaled system  aquifer contamination  
Mass Transfer Between Recirculation and Main Flow Zones: Is Physically Based Parameterization Possible? 期刊论文
WATER RESOURCES RESEARCH, 2019, 55 (1) : 345-362
作者:  Zhou, Jia-Qing;  Wang, Lichun;  Chen, Yi-Feng;  Cardenas, M. Bayani
收藏  |  浏览/下载:41/0  |  提交时间:2019/04/09
mass transfer  recirculation zone  anomalous transport  fracture flow and transport  mobile-immobile domain  
Velocities, Residence Times, Tracer Breakthroughs in a Vegetated Lysimeter: A Multitracer Experiment 期刊论文
WATER RESOURCES RESEARCH, 2019, 55 (1) : 21-33
作者:  Benettin, Paolo;  Queloz, Pierre;  Bensimon, Michael;  McDonnell, Jeffrey J.;  Rinaldo, Andrea
收藏  |  浏览/下载:23/0  |  提交时间:2019/04/09
lysimeter experiment  flow and transport  tracer  isotopes  
Advancing Graph-Based Algorithms for Predicting Flow and Transport in Fractured Rock 期刊论文
WATER RESOURCES RESEARCH, 2018, 54 (9) : 6085-6099
作者:  Viswanathan, H. S.;  39;Malley, D.
收藏  |  浏览/下载:19/0  |  提交时间:2019/04/09
discrete fracture networks  graph theory  subsurface flow and transport  fractured media  model reduction  multiscale modeling  
Numerical Simulation of Multiphase Flow in Nanoporous Organic Matter With Application to Coal and Gas Shale Systems 期刊论文
WATER RESOURCES RESEARCH, 2018, 54 (2) : 1077-1092
作者:  Song, Wenhui;  Yao, Jun;  Ma, Jingsheng;  Sun, Hai;  Li, Yang;  Yang, Yongfei;  Zhang, Lei
收藏  |  浏览/下载:21/0  |  提交时间:2019/04/09
multiphase flow  pore network model  nanoporous organic matter  coal and gas shale  relative permeability  transport mechanisms  
On the Representation of the Porosity-Pressure Relationship in General Subsurface Flow Codes 期刊论文
WATER RESOURCES RESEARCH, 2018, 54 (2) : 1382-1388
作者:  Birdsell, Daniel T.;  Karra, Satish;  Rajaram, Harihar
收藏  |  浏览/下载:27/0  |  提交时间:2019/04/09
porosity  groundwater flow equation  flow and transport models  specific storage  porous media compressibility  petroleum engineering