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. 2015 Mar 24;9(2):024107. doi: 10.1063/1.4916228

FIG. 3.

FIG. 3.

Four regimes observed for the formation of alternating droplets as a function of the capillary number Ca. (a) Experimental results observed by Zheng et al.13 in case of λ = 1.0 and the carrier fluid and the aqueous streams were both viscous (μ = 16 mPa·s). (b) Present computational results.