"structural discontinuity" is a correct and usable phrase in written English, particularly in academic or technical contexts.
It refers to a break, gap, or interruption in the structure or organization of something, usually a system or process. Example: The collapse of the company was caused by a structural discontinuity in their supply chain, leading to a significant decrease in production and revenue.
The morphology index, M, weighs three basic features of MULTICELL morphology: local EXTRACELLULAR arrangement, E, structural discontinuity, D, and a structure's overall shape, S. For each CELL, the algorithm computes a numerical score based on its neighborhood arrangement.
The principle involved in this type of modification is called structural discontinuity.
With resilient channels you can mount the new panels on the wall yet still maintain a narrow gap for structural discontinuity.
Furthermore, the current nanoparticle-based electrodes suffer from additional disadvantages, such as structural discontinuity, non-uniform dispersion and serious agglomeration during operation.
Structural discontinuity can be added to wall surfaces by constructing a new wall, using conventional framing techniques, parallel to the existing wall and facing the source of the noise.
Our results show that a structural discontinuity in the catchment (i.e. abrupt slope decrease at the junction between piedmonts and the alluvial plain from 2 to 10% to < 0.1%) could be compensated by functional continuity during floods.
A complete study of collapse caldera formation should ideally involve multiple aspects such as regional tectonics, system geometry, magma and host rock properties, fluid-structure interaction, pre-existing structural discontinuities, and deformation history.
The model is based on the pre-requisites for LPS: an aquifer lithology that enables build-up of high bicarbonate and Ca2 + to sustain CaCO3 oversaturation after spring emergence, combined with intense groundwater percolation especially along structural discontinuities (e.g., fault zones, joints, schistosity), and a proper hydrogeological structure of the discharging area.
Real solids invariably contain structural discontinuities and localized regions of disorder.
For example, isograd patterns that are cut by faults clearly indicate that metamorphism predated fault displacement, whereas isograd sequences that overprint structural discontinuities imply the reverse.
However, moments are important at low frequencies when sources are in the proximity of structural discontinuities.
