tea-ring instability - meaning and definition. What is tea-ring instability
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What (who) is tea-ring instability - definition

FLUID BREAKUP OF A FALLING STREAM
Plateau-Raleigh instability; Rayleigh instability; Plateau-Rayleigh instability
  • PEG]] in water
  • Rain water flux from a canopy. Among the forces that govern drop formation: Plateau–Rayleigh instability, [[Surface tension]], [[Cohesion (chemistry)]], [[Van der Waals force]].
  • Intermediate stage of a jet breaking into drops. Radii of curvature in the axial direction are shown. Equation for the radius of the stream is <math>R(z) = R_0 + A_k \cos(kz)</math>, where <math>R_0</math> is the radius of the unperturbed stream, <math>A_k</math> is the amplitude of the perturbation, <math>\scriptstyle z</math> is distance along the axis of the stream, and <math>k</math> is the wave number
  • Water dropping from a tap

Genome instability         
HIGH FREQUENCY OF MUTATIONS WITHIN THE GENOME OF A CELLULAR LINEAGE
Genomic instability; Genetic instability
Genome instability (also genetic instability or genomic instability) refers to a high frequency of mutations within the genome of a cellular lineage. These mutations can include changes in nucleic acid sequences, chromosomal rearrangements or aneuploidy.
Chromosome instability         
TYPE OF GENOMIC INSTABILITY
Chromosomal instability; User:Gz202/sandbox; Wikipedia talk:Articles for creation/Chromosome Instability; Chromosome Instability
Chromosomal instability (CIN) is a type of genomic instability in which chromosomes are unstable, such that either whole chromosomes or parts of chromosomes are duplicated or deleted. More specifically, CIN refers to the increase in rate of addition or loss of entire chromosomes or sections of them.
Plateau–Rayleigh instability         
The Plateau–Rayleigh instability, often just called the Rayleigh instability, explains why and how a falling stream of fluid breaks up into smaller packets with the same volume but less surface area. It is related to the Rayleigh–Taylor instability and is part of a greater branch of fluid dynamics concerned with fluid thread breakup.

Wikipedia

Plateau–Rayleigh instability

The Plateau–Rayleigh instability, often just called the Rayleigh instability, explains why and how a falling stream of fluid breaks up into smaller packets with the same volume but less surface area. It is related to the Rayleigh–Taylor instability and is part of a greater branch of fluid dynamics concerned with fluid thread breakup. This fluid instability is exploited in the design of a particular type of ink jet technology whereby a jet of liquid is perturbed into a steady stream of droplets.

The driving force of the Plateau–Rayleigh instability is that liquids, by virtue of their surface tensions, tend to minimize their surface area. A considerable amount of work has been done recently on the final pinching profile by attacking it with self-similar solutions.