The phrase "a stable layer of" is correct and usable in written English.
It can be used when describing a consistent or unchanging stratum of material, substance, or concept in various contexts, such as science, engineering, or metaphorical discussions.
Example: "The geologist explained that a stable layer of sedimentary rock underlies the entire region, providing valuable insights into the area's geological history."
Alternatives: "a consistent layer of" or "an unchanging layer of".
This change corresponds well with the GB solidus line (i.e., the formation of a stable layer of a liquid-like GB phase called GB prewetting) observed previously.
This indicates that an irreversible electrochemical transformation has been achieved during the first cycle and a stable layer of hydr(oxide) formed on the surface of the copper electrode.
The voltammogram on a glassy carbon (GC) electrode in a melt containing 0.025 mol dm−3 [M] SbCl3 showed a couple of redox peak corresponding to the Sb/Sb III) redox reaction, and a stable layer of pure Sb was deposited under the constant potential control.
Shang et al. [23] explained the rise in hydrogen desorption temperature as a result of the formation of a stable layer of cerium hydride on particle surfaces, stating that the creation of this surface layer would be problematic for the diffusion of hydrogen from inside the particles outward.
If this procedure is used correctly, a stable layer of graft will result.
Only trace amounts of Al were detected in the supernatant of 1, which suggested a stable layer of Al(OH 3 consistent with the excellent radiolabelling results above.
During most of the sampling period (80% of the time), a stable layer was observed at 08 00 h, with the occasional presence of near-surface thermal inversions; by noon, when solar heating breaks the stable layer, a well-developed mixing layer reached up to 2000 m above ground level (AGL), with a shallow superadiabatic layer near the surface.
Although potential temperature profiles were similar above 500 m at 15:00 and 18 00 h, the colder temperatures at 18 00 h, indicated the formation of a stable layer close to the surface).
While cross-polar flights account for only a tiny percent of total global emissions from aviation, the standard cruising altitude for commercial planes in the Arctic is the stratosphere, an extremely stable layer of the atmosphere.
During the observation period between December 23 24 (upper panel of Fig. 3), a stable layer with a large vertical potential temperature gradient formed at a height of about 2 km.
Introducing a flexible and stable layer of PVP on surface of Sn NPs can effectively prevent the aggregation of Sn NPs and counteract the pulverization of Sn NPs due to the large volume changes generated during the lithiation-delithiation processes.
