Formation and breakup of compound pendant drops at the tip of a capillary and its effect on upstream velocity fluctuations

Zhizhao Che, Teck Neng Wong, Nam Trung Nguyen, J. C. Chai

Research output: Contribution to journalArticlepeer-review

6 Citations (Scopus)

Abstract

In this paper, the formation and breakup process of compound pendant drops (CPDs, pendant drops with smaller drops or bubbles in them) at the tip of a glass capillary and its effect on upstream velocity fluctuation are experimentally investigated. The formation process of an air/water compound drop from a CPD consists of four main stages. First, an air plug in the capillary flows into the small liquid pendant drop to initialize a small CPD. Next, a liquid slug flows into the CPD, and the liquid in the CPD accumulates. Subsequently, an air plug flows into the CPD, and it coalesces with the existing air bubble in the CPD. The accumulation and coalescence stages repeat, until the CPD reaches a critical weight, then the CPD finally breaks up to produce a compound drop. For the air/SDS-solution system, the bubbles in the CPDs do not coalesce, and the contact line of the CPDs initially climbs along the capillary and then moves downwards with the growth of the CPDs. The upstream velocity fluctuates during the periodical formation and breakup of the CPD due to Laplace pressure variation at the tip of the glass capillary. By adding surfactant into water, the fluctuation of the upstream velocity decreases. The size distribution of the compound drops produced by the breakup of CPDs is quantified, and the results show that the current system is able to produce monodisperse compound drops.

Original languageEnglish
Pages (from-to)1022-1029
Number of pages8
JournalInternational Journal of Heat and Mass Transfer
Volume55
Issue number4
Early online date2 Nov 2011
DOIs
Publication statusPublished - 31 Jan 2012
Externally publishedYes

Fingerprint

Dive into the research topics of 'Formation and breakup of compound pendant drops at the tip of a capillary and its effect on upstream velocity fluctuations'. Together they form a unique fingerprint.

Cite this