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Τι (ποιος) είναι external instability - ορισμός

FLUID BREAKUP OF A FALLING STREAM

Plateau-Raleigh instability; Rayleigh instability; Plateau-Rayleigh instability

$Intermediate stage of a jet breaking into drops. Radii of curvature in the axial direction are shown. Equation for the radius of the stream is <math>R(z) = R_0 + A_k \cos(kz)</math>, where <math>R_0</math> is the radius of the unperturbed stream, <math>A_k</math> is the amplitude of the perturbation, <math>\scriptstyle z</math> is distance along the axis of the stream, and <math>k</math> is the wave number$

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.

https://en.wikipedia.org/wiki/Genome_instability

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.

https://en.wikipedia.org/wiki/Chromosome_instability

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.

https://en.wikipedia.org/wiki/Plateau–Rayleigh_instability

Βικιπαίδεια

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.

https://en.wikipedia.org/wiki/Plateau–Rayleigh instability