Everdenser

Everdenser is a coined term used to describe a process, object, or model in which density increases monotonically under certain conditions. The construction combines ever- (continuously, increasingly) with denser (more dense). It does not have a fixed definition in major dictionaries or in standard scientific vocabularies, and you will mainly find it in speculative writing, preliminary models, or informal discussions about variable-density systems.

In physics and engineering, everdenser may describe media in which density, denoted rho, increases with depth or pressure. For example, a material undergoing progressive compaction or a gradient in density in a sedimentary sequence can be described as everdenser with depth. In geophysics and planetary science, density typically rises toward a planet's interior, producing inherently everdenser profiles, though the established terms would speak of density stratification rather than a coined phrase.

In mathematical modeling, an everdenser system can be formalized by a density function rho(x) that is strictly increasing on a domain, or by rho(t) that grows with time in a dynamic process. Such a property can influence buoyancy, wave speeds, and transport phenomena, depending on how density couples to momentum and mass conservation.

Limitations and usage: because it is not standard, the meaning of everdenser depends on context. It is best treated as a descriptive phrase rather than a formal technical term, used to emphasize monotone densification in a model or narrative.

See also: density, density function, monotone function, variable-density flow, stratification.