-
3
-
-
33644648479
-
-
P. Garstecki, M. J. Fuerstman, H. A. Stone, and G. M. Whitesides, Lab Chip 6, 437 (2006).
-
(2006)
Lab Chip
, vol.6
, pp. 437
-
-
Garstecki, P.1
Fuerstman, M.J.2
Stone, H.A.3
Whitesides, G.M.4
-
5
-
-
0242492537
-
-
J. D. Tice, H. Song, A. D. Lyon, and R. F. Ismagilov, Langmuir 19, 9127 (2003).
-
(2003)
Langmuir
, vol.19
, pp. 9127
-
-
Tice, J.D.1
Song, H.2
Lyon, A.D.3
Ismagilov, R.F.4
-
7
-
-
7544247824
-
-
P. Garstecki, I. Gitlin, W. DiLuzio, G. M. Whitesides, E. Kumacheva, and H. A. Stone, Appl. Phys. Lett. 85, 2649 (2004).
-
(2004)
Appl. Phys. Lett.
, vol.85
, pp. 2649
-
-
Garstecki, P.1
Gitlin, I.2
Diluzio, W.3
Whitesides, G.M.4
Kumacheva, E.5
Stone, H.A.6
-
12
-
-
34548590903
-
-
We rationalize the stabilization as follows. The fastest growing unstable modes in the classical Rayleigh plateau instability distribute the liquid only on a local scale, i.e., they would force liquid from the junction area into the entrance of the adjacent constriction channel. Such a perturbation, however, would experience a restoring force because it requires forcing the liquid-liquid interface further into the corners. As a consequence, such perturbations are no longer unstable and the breakucan only occur through slower nonlocal perturbations. Note that this picture is also different from the convective stabilization of confined jets discussed by, (), operated at much higher Ca.
-
We rationalize the stabilization as follows. The fastest growing unstable modes in the classical Rayleigh plateau instability distribute the liquid only on a local scale, i.e., they would force liquid from the junction area into the entrance of the adjacent constriction channel. Such a perturbation, however, would experience a restoring force because it requires forcing the liquid-liquid interface further into the corners. As a consequence, such perturbations are no longer unstable and the breakup can only occur through slower nonlocal perturbations. Note that this picture is also different from the convective stabilization of confined jets discussed by P. Guillot, Phys. Rev. Lett. 99, 104502 (2007), operated at much higher Ca.
-
(2007)
Phys. Rev. Lett.
, vol.99
, pp. 104502
-
-
Guillot, P.1
-
13
-
-
54149095157
-
-
See EPAPS Document No. E-APPLAB-93-021842. Movie 1 shows oil droplet generated in a restriction channel with dimensions: h=10 μm, w=10 μm, l=100 μm at flow rates of Qw = Qo =0.01 μL/min. Movie 2 shows oil droplet generated in a restriction channel with dimensions: h=10 μm, w=10 μm, l=1000 μm at flow rates of Qw = Qo =0.0025 μL/min. For more information on EPAPS, see.
-
See EPAPS Document No. E-APPLAB-93-021842. Movie 1 shows oil droplet generated in a restriction channel with dimensions: h=10 μm, w=10 μm, l=100 μm at flow rates of Qw = Qo =0.01 μL/min. Movie 2 shows oil droplet generated in a restriction channel with dimensions: h=10 μm, w=10 μm, l=1000 μm at flow rates of Qw = Qo =0.0025 μL/min. For more information on EPAPS, see http://www.aip.org/pubservs/epaps.html.
-
-
-
|